# Paleo-pCO2 Database Global C3 Plant pCO2 Data over the Past 30 Thousand Years #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # Template Version 4.0 # Encoding: UTF-8 # NOTE: Please cite original publication, NOAA Landing Page URL, dataset and publication DOIs (where available), and date accessed when using downloaded data. # If there is no publication information, please cite investigator, study title, NOAA Landing Page URL, and date accessed. # # Description/Documentation lines begin with '#' followed by a space # Data lines have no '#' # # NOAA_Landing_Page: https://www.ncdc.noaa.gov/access/paleo-search/study/36134 # Landing_Page_Description: NOAA Landing Page of this file's parent study, which includes all study metadata. # # Study_Level_JSON_Metadata: https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/json/noaa-forcing-36134.json # Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata. # # Data_Type: Climate Forcing # # Dataset_DOI: 10.1130/2015151 # # Science_Keywords: Last Glacial Maximum #--------------------------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/climate_forcing/trace_gases/Paleo-pCO2/land_plant_d13c_1_schubert_2015.txt # Data_Download_Description: NOAA Template File; Global C3 Plant pCO2 Data # # Original_Source_URL:10.1130/2015151 # Original_Source_Description: GSA Data Repository DOI #--------------------------------------- # Contribution_Date # Date: 2022-03-07 #--------------------------------------- # File_Last_Modified_Date # Date: 2022-10-19 #--------------------------------------- # Title # Study_Name: Paleo-pCO2 Database Global C3 Plant pCO2 Data over the Past 30 Thousand Years #--------------------------------------- # Investigators # Investigators: Schubert, Brian; Jahren, Hope #--------------------------------------- # Description_Notes_and_Keywords # Description: File updated in October 2022 - new paleo pCO2 format #--------------------------------------- # Publication # Authors: Schubert, B. A., and Jahren, A. H. # Published_Date_or_Year: 2015 # Published_Title: Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2 # Journal_Name: Geology # Volume: 43 # Edition: # Issue: 5 # Pages: 435-438 # Report_Number: # DOI: 10.1130/G36467.1 # Online_Resource: # Full_Citation: # Abstract: Changes in the carbon isotope composition of terrestrial plant tissue (d13C) are widely cited for evidence of shifts in climate, vegetation, or atmospheric chemistry across a wide range of time scales. A global compilation of d13C data from fossil leaves and bulk terrestrial organic matter (TOM) spanning the past 30 k.y., however, shows wide variability and no discernable trend. Here we analyze these data in terms of a relative change in net carbon isotope fractionation between the d13C value of plant tissue and that of atmospheric CO2 [D13C = (d13CCO2 – d13C)/(1 + d13C/1000)] and identify a global 2.1‰ shift in leaf and TOM D13C that is synchronous with a global rise in pCO2 documented from ice core data. We apply a relationship describing the effect of pCO2 on D13C to the global record of D13C change documented here to reconstruct pCO2 levels across the past 30 k.y. Our reconstructed pCO2 levels are in excellent agreement with the ice core data and underscore the potential of the global terrestrial d13C record to serve as an accurate pCO2 proxy #--------------------------------------- # Funding_Agency # Funding_Agency_Name: US Department of Energy # Grant: DE-FG02-13ER16412, DE-FG02-09ER16002 #--------------------------------------- # Site_Information # Site_Name: Global # Location: Global # Northernmost_Latitude: 90 # Southernmost_Latitude: -90 # Easternmost_Longitude: 180 # Westernmost_Longitude: -180 # Elevation_m: #--------------------------------------- # Data_Collection # Collection_Name: C3plants_pC02_schubert2015 # First_Year: 30000 # Last_Year: -65 # Time_Unit: calendar year before present # Core_Length_m: # Parameter_Keywords: carbon dioxide # Notes: Method 1: Can be used when d13COM at a reference time (time 0) is known. #--------------------------------------- # Chronology_Information # Chronology: #--------------------------------------- # Variables # PaST_Thesaurus_Download_Resource: https://www.ncei.noaa.gov/access/paleo-search/skos/past-thesaurus.rdf # PaST_Thesaurus_Download_Description: Paleoenvironmental Standard Terms (PaST) Thesaurus terms, definitions, and relationships in SKOS format. # # Data variables follow that are preceded by "##" in columns one and two. # Variables list, one per line, shortname-tab-var components: what, material, error, units, seasonality, data type, detail, method, C or N for Character or Numeric data) # #------------------------ # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: NA proxy first_author_last_name publication_year doi age_ka Age_uncertainty_pos_ka Age_uncertainty_neg_ka CO2_ppm CO2_uncertainty_pos_ppm CO2_uncertainty_neg_ppm Name of person entering data Contact email address reference of the data product Publication Year DOI Additional publications that are part of the dataset Explanation for each additional publications link to the dataset Sample ID Rock formation name Modern Latitude (decimal degree, south negative) Modern Longitude (decimal degree, west negative) Paleo Latitude (decimal degree, south negative) Paleo Longitude (decimal degree, west negative) stratigraphic level (m) Age (Ma) Age_max (Ma) Age_min (Ma) Reference(s) for age d13COM, t (‰) d13COM, t uncertainty ±2s (‰ PDB) n d13COM, t (number of analyses) Reference(s) for d13COM, t d13Catm, t=0 (‰ PDB) d13Catm, t=0 uncertainty ±1s (‰ PDB) n d13Catm, t=0 (number of replicate analyses) reference for d13Catm, t=0 d13COM, t=0 (‰ PDB) d13COM, t=0 uncertainty ±2s (‰ PDB) n d13COM, t=0 (number of replicate analyses) reference for d13COM, t=0 d13Catm, t (‰ PDB) d13Catm, t uncertainty ±2s (‰ PDB) n d13Catm, t (number of replicate analyses) reference for d13Catm, t pCO2, t=0 (ppmv) pCO2, t=0 uncertainty ± 1s (ppmv) reference for pCO2, t=0 Type of OM substrates Bulk organic matter or n-alkanes etc. Chain length if n-alkanes reference on OM substrates Mean Annual Precipitation mm/yr Mean Annual Precipitation_uncertainty_pos mm/yr Mean Annual Precipitation_uncertainty_neg mm/yr Method for MAP estimates reference on MAP A (unitless) A uncertainty ± 1s B (unitless) B uncertainty ± 1s C (unitless) C uncertainty ± 1s Atmospheric CO2 ppmV Atmospheric CO2_max ppmV Atmospheric CO2_min ppmV Atmopsheric CO2_97.5 percentile ppmV Atmopsheric CO2_2.5 percentile ppmV Reference for CO2 determination notes land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3 NA NA 299 65 50 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0025 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.53 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Andersson et al. (2012; Fig. 3; fen deposits) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 299 NA NA 429 199 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4 NA NA 315 70 53 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0036 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.25 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.53 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Andersson et al. (2012; Fig. 3; fen deposits) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 315 NA NA 455 209 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5 NA NA 315 70 53 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0045 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.25 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.53 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Andersson et al. (2012; Fig. 3; fen deposits) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 315 NA NA 455 209 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.2 NA NA 323 73 54 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0052 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.38 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.53 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Andersson et al. (2012; Fig. 3; fen deposits) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 323 NA NA 469 215 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6 NA NA 288 62 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.8 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.53 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Andersson et al. (2012; Fig. 3; fen deposits) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 288 NA NA 412 192 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.7 NA NA 266 55 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0067 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.4 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.53 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Andersson et al. (2012; Fig. 3; fen deposits) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 266 NA NA 376 176 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.5 NA NA 265 54 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0075 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.4 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.53 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Andersson et al. (2012; Fig. 3; fen deposits) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 265 NA NA 373 175 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.25 NA NA 239 46 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00825 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.88 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.53 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Andersson et al. (2012; Fig. 3; fen deposits) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 239 NA NA 331 157 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.6 NA NA 249 50 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0086 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.13 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.53 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.42 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Andersson et al. (2012; Fig. 3; fen deposits) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 249 NA NA 349 165 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9 NA NA 300 66 50 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.13 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.53 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.45 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Andersson et al. (2012; Fig. 3; fen deposits) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 300 NA NA 432 200 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.4 NA NA 241 47 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0094 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.53 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.48 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Andersson et al. (2012; Fig. 3; fen deposits) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 241 NA NA 335 159 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.7 NA NA 191 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0097 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.75 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.53 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -6.5 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Andersson et al. (2012; Fig. 3; fen deposits) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 191 NA NA 263 121 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.926 NA NA 279 39 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.010926 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.95 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.62 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 279 NA NA 357 213 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.114 NA NA 256 34 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011114 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.52 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.64 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 256 NA NA 324 194 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.193 NA NA 272 37 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011193 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.83 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.65 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 272 NA NA 346 208 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.25 NA NA 279 39 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01125 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.97 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.65 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 279 NA NA 357 213 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.291 NA NA 280 39 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011291 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 280 NA NA 358 214 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.325 NA NA 267 36 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011325 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.76 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 267 NA NA 339 203 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.361 NA NA 232 30 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011361 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 232 NA NA 292 174 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.71 NA NA 246 32 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01171 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.36 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 246 NA NA 310 186 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.761 NA NA 246 32 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011761 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.36 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 246 NA NA 310 186 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.914 NA NA 261 35 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011914 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.69 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.72 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 261 NA NA 331 199 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.075 NA NA 245 32 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012075 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.38 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.73 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 245 NA NA 309 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.273 NA NA 247 32 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012273 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.43 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.75 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 247 NA NA 311 187 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.457 NA NA 298 43 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012457 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.43 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.76 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 298 NA NA 384 228 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.513 NA NA 287 41 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012513 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.24 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.77 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 287 NA NA 369 219 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.677 NA NA 249 33 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012677 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.51 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.78 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 249 NA NA 315 189 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.696 NA NA 259 35 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012696 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.71 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.78 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 259 NA NA 329 197 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.734 NA NA 246 32 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012734 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.45 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.79 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 246 NA NA 310 186 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.753 NA NA 238 31 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012753 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.26 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.79 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 238 NA NA 300 180 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.773 NA NA 262 35 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012773 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.78 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.79 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 262 NA NA 332 200 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.813 NA NA 263 36 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012813 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.81 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.79 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 263 NA NA 335 201 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.875 NA NA 236 30 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012875 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.24 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.79 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 236 NA NA 296 178 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.896 NA NA 275 38 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012896 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.05 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.8 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 275 NA NA 351 209 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.957 NA NA 227 29 28 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012957 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.02 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.8 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 227 NA NA 285 171 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.081 NA NA 222 29 28 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013081 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.91 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.81 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 222 NA NA 280 166 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.336 NA NA 251 33 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013336 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.6 NA NA Beerling (1996; Fig. 1b) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.56 NA NA Beerling (1996; Fig. 1b) -6.82 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling (1996; Fig. 1b) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 251 NA NA 317 191 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0 NA NA 265 36 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.8 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.86 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 265 NA NA 337 201 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.1 NA NA 255 34 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.1 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 255 NA NA 323 193 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.2 NA NA 309 46 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0002 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.1 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 309 NA NA 401 235 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.25 NA NA 232 30 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00025 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.6 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 232 NA NA 292 174 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.3 NA NA 250 33 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0003 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 250 NA NA 316 190 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.35 NA NA 245 32 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00035 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.9 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 245 NA NA 309 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.4 NA NA 262 35 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0004 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.25 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 262 NA NA 332 200 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.45 NA NA 264 36 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00045 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.3 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 264 NA NA 336 200 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.5 NA NA 288 41 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.75 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 288 NA NA 370 220 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.55 NA NA 256 34 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00055 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.15 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 256 NA NA 324 194 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.6 NA NA 317 47 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0006 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.25 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 317 NA NA 411 241 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.65 NA NA 242 31 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00065 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.85 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 242 NA NA 304 182 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.7 NA NA 279 39 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0007 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.6 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 279 NA NA 357 213 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.8 NA NA 320 48 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0008 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.3 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 320 NA NA 416 242 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.9 NA NA 240 31 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0009 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.8 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 240 NA NA 302 182 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.95 NA NA 293 42 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00095 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.85 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 293 NA NA 377 225 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1 NA NA 249 33 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 249 NA NA 315 189 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.1 NA NA 279 39 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0011 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.6 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 279 NA NA 357 213 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.15 NA NA 274 38 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00115 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 274 NA NA 350 210 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.2 NA NA 274 38 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0012 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 274 NA NA 350 210 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.3 NA NA 299 43 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0013 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.95 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 299 NA NA 385 229 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.35 NA NA 290 41 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00135 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.8 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 290 NA NA 372 222 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.4 NA NA 271 37 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0014 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 271 NA NA 345 207 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.5 NA NA 269 37 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0015 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.4 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 269 NA NA 343 205 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.6 NA NA 252 33 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0016 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.05 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 252 NA NA 318 192 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.65 NA NA 252 33 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00165 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.05 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 252 NA NA 318 192 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.7 NA NA 274 38 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0017 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 274 NA NA 350 208 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.8 NA NA 238 31 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0018 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.75 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 238 NA NA 300 180 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.9 NA NA 306 45 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0019 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.05 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 306 NA NA 396 234 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.95 NA NA 264 36 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00195 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.3 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 264 NA NA 336 200 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.05 NA NA 264 36 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00205 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.3 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 264 NA NA 336 200 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.1 NA NA 259 35 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0021 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.2 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 259 NA NA 329 197 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.2 NA NA 260 35 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0022 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.2 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 260 NA NA 330 198 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.3 NA NA 243 31 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0023 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.85 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 243 NA NA 305 183 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.45 NA NA 286 41 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00245 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.7 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 286 NA NA 368 218 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.55 NA NA 273 38 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00255 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 273 NA NA 349 209 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.6 NA NA 278 39 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0026 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.55 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 278 NA NA 356 212 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.75 NA NA 258 34 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00275 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.15 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 258 NA NA 326 196 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.8 NA NA 239 31 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0028 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.75 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 239 NA NA 301 181 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.9 NA NA 270 37 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0029 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.4 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 270 NA NA 344 206 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3 NA NA 233 30 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.6 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 233 NA NA 293 175 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.1 NA NA 246 32 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0031 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.9 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 246 NA NA 310 186 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.2 NA NA 276 38 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0032 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 276 NA NA 352 210 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.4 NA NA 276 38 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0034 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 276 NA NA 352 210 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.65 NA NA 256 34 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00365 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.1 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 256 NA NA 324 194 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.75 NA NA 311 46 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00375 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.1 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 311 NA NA 403 237 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.9 NA NA 305 45 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0039 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 305 NA NA 395 233 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4 NA NA 251 33 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 251 NA NA 317 191 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.2 NA NA 293 42 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0042 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.8 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 293 NA NA 377 225 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.3 NA NA 254 34 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0043 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.05 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 254 NA NA 322 192 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.4 NA NA 276 38 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0044 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 276 NA NA 352 210 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.55 NA NA 375 60 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00455 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -30 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 375 NA NA 495 277 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.8 NA NA 266 36 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0048 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.3 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 266 NA NA 338 202 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5 NA NA 296 43 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.85 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 296 NA NA 382 226 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.8 NA NA 296 43 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0058 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.85 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 296 NA NA 382 226 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.3 NA NA 317 47 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0063 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.2 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 317 NA NA 411 241 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.8 NA NA 305 45 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0078 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.05 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 305 NA NA 395 233 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.3 NA NA 260 35 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0083 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.25 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 260 NA NA 330 198 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.9 NA NA 323 49 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0089 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.4 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.45 NA NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) -6.44 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Salix leaves NA Beerling and Rundgren (2000; Fig. 3a, ages rounded to the nearest 50 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 323 NA NA 421 245 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.681 NA NA 273 57 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000681 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.2 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 273 NA NA 387 181 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.791 NA NA 297 64 50 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002791 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.6 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 297 NA NA 425 197 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.575 NA NA 281 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003575 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.3 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 281 NA NA 399 187 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.538 NA NA 246 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006538 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.6 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 246 NA NA 344 162 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.392 NA NA 259 52 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.010392 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.1 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 259 NA NA 363 171 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.666 NA NA 632 224 139 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012666 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -30.3 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.78 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 632 NA NA 1080 354 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.723 NA NA 246 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013723 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.1 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 246 NA NA 344 162 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16.539 NA NA 220 42 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.016539 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.4 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.76 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 220 NA NA 304 144 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18.816 NA NA 143 29 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018816 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.8 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.59 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 143 NA NA 201 81 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 19.818 NA NA 168 32 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.019818 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.7 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 168 NA NA 232 102 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 20.246 NA NA 207 39 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.020246 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.9 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 207 NA NA 285 133 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 20.655 NA NA 207 39 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.020655 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.9 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.59 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 207 NA NA 285 133 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 20.956 NA NA 206 39 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.020956 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.9 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 206 NA NA 284 132 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 21.747 NA NA 163 32 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.021747 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.6 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.65 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 163 NA NA 227 97 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22.161 NA NA 174 33 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.022161 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.67 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 174 NA NA 240 106 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22.474 NA NA 170 33 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.022474 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.9 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.69 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 170 NA NA 236 104 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22.798 NA NA 192 37 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.022798 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.6 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 192 NA NA 266 122 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23.249 NA NA 126 26 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.023249 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.2 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.71 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 126 NA NA 178 66 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23.679 NA NA 186 35 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.023679 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.4 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.16 NA NA Brincat et al. (2000; Fig. 1; Table 2) -6.69 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Brincat et al. (2000; Fig. 1; Table 2) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 186 NA NA 256 116 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.05 NA NA 361 86 63 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.2 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 361 NA NA 533 235 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.383 NA NA 517 151 105 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000383 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.8 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 517 NA NA 819 307 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.546 NA NA 202 38 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000546 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.2 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 202 NA NA 278 130 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.602 NA NA 238 46 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000602 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.1 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 238 NA NA 330 156 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.655 NA NA 358 85 63 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000655 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.2 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 358 NA NA 528 232 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.677 NA NA 407 102 75 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000677 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.8 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 407 NA NA 611 257 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.76 NA NA 343 80 59 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00076 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 343 NA NA 503 225 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.885 NA NA 246 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000885 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.3 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 246 NA NA 344 162 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.92 NA NA 246 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00092 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.3 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 246 NA NA 344 162 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.941 NA NA 336 77 57 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000941 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.9 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 336 NA NA 490 222 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.357 NA NA 155 30 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001357 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.7 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 155 NA NA 215 91 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.874 NA NA 252 50 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001874 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.4 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 252 NA NA 352 166 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.906 NA NA 293 63 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001906 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.2 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 293 NA NA 419 195 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.919 NA NA 299 65 50 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001919 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.3 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 299 NA NA 429 199 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.972 NA NA 299 65 50 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001972 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.3 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 299 NA NA 429 199 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.022 NA NA 305 67 51 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002022 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.4 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 305 NA NA 439 203 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.335 NA NA 312 69 52 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002335 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.5 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 312 NA NA 450 208 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.352 NA NA 267 55 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002352 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.7 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 267 NA NA 377 177 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.546 NA NA 257 52 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002546 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.5 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 257 NA NA 361 171 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.946 NA NA 226 43 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002946 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.8 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 226 NA NA 312 148 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.214 NA NA 248 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003214 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.3 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 248 NA NA 346 164 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.336 NA NA 248 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003336 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.3 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 248 NA NA 346 164 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.344 NA NA 253 51 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003344 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.4 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 253 NA NA 355 167 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.426 NA NA 258 52 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003426 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.5 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 258 NA NA 362 172 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.402 NA NA 231 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004402 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.9 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 231 NA NA 319 151 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.478 NA NA 240 47 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004478 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.1 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 240 NA NA 334 158 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.662 NA NA 244 48 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004662 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.2 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 244 NA NA 340 160 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.294 NA NA 332 76 57 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006294 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.8 NA NA Cathalot et al. (2013) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -24.81 NA NA Cathalot et al. (2013) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Cathalot et al. (2013) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 332 NA NA 484 218 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1 NA NA 244 48 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -30.25 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 244 NA NA 340 160 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2 NA NA 257 52 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -30.5 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 257 NA NA 361 171 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3 NA NA 270 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -30.75 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 270 NA NA 382 180 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4 NA NA 225 43 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.75 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 225 NA NA 311 147 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5 NA NA 247 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -30.25 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 247 NA NA 345 163 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6 NA NA 271 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -30.75 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 271 NA NA 383 181 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7 NA NA 313 70 52 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.007 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -31.5 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 313 NA NA 453 209 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8 NA NA 327 74 55 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.008 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -31.75 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 327 NA NA 475 217 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9 NA NA 292 63 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -31.25 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.45 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 292 NA NA 418 194 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10 NA NA 274 57 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -31 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.53 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 274 NA NA 388 182 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11 NA NA 269 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -31 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.63 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 269 NA NA 381 179 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12 NA NA 264 54 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -31 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.73 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 264 NA NA 372 176 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13 NA NA 260 53 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -31 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.8 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 260 NA NA 366 172 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14 NA NA 271 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.014 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -31.25 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 271 NA NA 383 181 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15 NA NA 235 45 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.015 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -30.5 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 235 NA NA 325 155 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16 NA NA 165 32 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.016 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.79 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 165 NA NA 229 99 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17 NA NA 118 25 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.017 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.5 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.72 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 118 NA NA 168 58 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18 NA NA 149 29 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.75 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.64 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 149 NA NA 207 85 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 19 NA NA 157 31 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.019 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 157 NA NA 219 93 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 20 NA NA 164 32 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.25 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 164 NA NA 228 98 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 21 NA NA 115 25 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.021 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.25 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 115 NA NA 165 57 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22 NA NA 99 23 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.022 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.5 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 99 NA NA 145 41 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23 NA NA 118 25 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.023 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.5 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 118 NA NA 168 58 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 24 NA NA 113 25 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.024 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.25 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -30.8 NA NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) -6.68 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Damsté et al., (2011; Fig. 3a, solid line; ages to the nearest 1,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 113 NA NA 163 55 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.363 NA NA 340 78 58 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003363 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.3 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 340 NA NA 496 224 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.033 NA NA 269 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004033 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.1 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 269 NA NA 381 179 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.677 NA NA 279 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004677 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.3 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 279 NA NA 397 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.163 NA NA 285 60 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006163 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.4 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 285 NA NA 405 189 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.554 NA NA 252 50 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009554 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.9 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.49 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 252 NA NA 352 166 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.713 NA NA 281 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009713 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.5 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.5 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 281 NA NA 399 187 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.382 NA NA 300 65 50 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.010382 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.9 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 300 NA NA 430 200 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.745 NA NA 335 77 57 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.010745 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.5 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 335 NA NA 489 221 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.786 NA NA 303 66 51 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.010786 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.61 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 303 NA NA 435 201 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.053 NA NA 216 41 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012053 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.3 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.73 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 216 NA NA 298 140 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.94 NA NA 216 41 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01394 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.4 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 216 NA NA 298 140 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.949 NA NA 274 57 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013949 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.7 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 274 NA NA 388 182 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.963 NA NA 190 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013963 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.7 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 190 NA NA 262 120 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14.145 NA NA 212 40 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.014145 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.3 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.85 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 212 NA NA 292 136 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14.474 NA NA 219 42 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.014474 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.5 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.85 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 219 NA NA 303 143 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15.826 NA NA 242 47 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.015826 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.8 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 242 NA NA 336 160 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15.882 NA NA 202 38 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.015882 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.8 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 202 NA NA 278 128 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16.358 NA NA 226 43 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.016358 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.6 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.77 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 226 NA NA 312 148 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16.707 NA NA 190 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.016707 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.6 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.74 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 190 NA NA 262 120 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16.72 NA NA 178 34 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01672 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.2 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.74 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 178 NA NA 246 110 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16.768 NA NA 191 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.016768 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.6 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.74 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 191 NA NA 263 121 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16.975 NA NA 191 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.016975 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.6 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.72 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 191 NA NA 263 121 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17.712 NA NA 162 31 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.017712 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -18.6 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 162 NA NA 224 96 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18.087 NA NA 232 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018087 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.6 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.63 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 232 NA NA 320 152 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18.139 NA NA 220 42 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018139 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.3 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.63 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 220 NA NA 304 142 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18.455 NA NA 205 39 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018455 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.9 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.61 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 205 NA NA 283 131 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18.965 NA NA 199 38 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018965 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.7 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 199 NA NA 275 127 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 19.576 NA NA 196 37 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.019576 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.6 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 196 NA NA 270 124 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 21.904 NA NA 168 32 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.021904 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -18.8 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -21.19 NA NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Galy et al (2008; Table 1; Fig. 6, using apparent age of 3,000 yrs) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 168 NA NA 232 102 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.295 NA NA 298 65 50 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000295 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23 NA NA Gouveia et al., (2002; Fig. 6) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.53 NA NA Gouveia et al., (2002; Fig. 6) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Gouveia et al., (2002; Fig. 6) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 298 NA NA 428 198 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.734 NA NA 266 55 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002734 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.4 NA NA Gouveia et al., (2002; Fig. 6) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.53 NA NA Gouveia et al., (2002; Fig. 6) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Gouveia et al., (2002; Fig. 6) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 266 NA NA 376 176 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.478 NA NA 272 57 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004478 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.5 NA NA Gouveia et al., (2002; Fig. 6) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.53 NA NA Gouveia et al., (2002; Fig. 6) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Gouveia et al., (2002; Fig. 6) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 272 NA NA 386 180 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.912 NA NA 288 62 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004912 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.8 NA NA Gouveia et al., (2002; Fig. 6) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.53 NA NA Gouveia et al., (2002; Fig. 6) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Gouveia et al., (2002; Fig. 6) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 288 NA NA 412 192 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.292 NA NA 288 62 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005292 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.8 NA NA Gouveia et al., (2002; Fig. 6) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.53 NA NA Gouveia et al., (2002; Fig. 6) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Gouveia et al., (2002; Fig. 6) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 288 NA NA 412 192 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.245 NA NA 225 43 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.010245 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.7 NA NA Gouveia et al., (2002; Fig. 6) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.53 NA NA Gouveia et al., (2002; Fig. 6) -6.55 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Gouveia et al., (2002; Fig. 6) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 225 NA NA 311 147 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13 NA NA 154 30 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.8 NA NA Gouveia et al., (2002; Fig. 6) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.53 NA NA Gouveia et al., (2002; Fig. 6) -6.8 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Gouveia et al., (2002; Fig. 6) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 154 NA NA 214 90 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0 NA NA 231 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.7 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.86 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 231 NA NA 319 151 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1 NA NA 257 52 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.8 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 257 NA NA 361 171 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2 NA NA 262 54 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.9 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 262 NA NA 370 174 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3 NA NA 274 57 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.1 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 274 NA NA 388 182 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4 NA NA 279 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.2 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 279 NA NA 397 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5 NA NA 282 60 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.25 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 282 NA NA 402 188 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6 NA NA 285 61 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.3 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 285 NA NA 407 189 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7 NA NA 281 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.007 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.25 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 281 NA NA 399 187 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8 NA NA 279 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.008 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.25 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 279 NA NA 397 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9 NA NA 273 57 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.2 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.45 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 273 NA NA 387 181 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10 NA NA 264 54 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.1 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.53 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 264 NA NA 372 176 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11 NA NA 236 46 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.6 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.63 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 236 NA NA 328 154 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12 NA NA 208 40 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.73 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 208 NA NA 288 134 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13 NA NA 191 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.6 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.8 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 191 NA NA 263 121 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14 NA NA 245 48 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.014 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 245 NA NA 341 161 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15 NA NA 234 45 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.015 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.75 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 234 NA NA 324 154 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16 NA NA 175 34 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.016 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.1 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.79 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 175 NA NA 243 107 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17 NA NA 187 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.017 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.4 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.72 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 187 NA NA 259 117 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18 NA NA 197 37 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.6 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.64 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 197 NA NA 271 125 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 19 NA NA 188 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.019 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.3 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 188 NA NA 260 118 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 20 NA NA 182 35 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.1 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 182 NA NA 252 114 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 21 NA NA 170 33 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.021 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.75 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 170 NA NA 236 104 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22 NA NA 176 34 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.022 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 176 NA NA 244 108 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23 NA NA 191 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.023 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.5 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 191 NA NA 263 121 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 24 NA NA 147 29 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.024 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.68 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 147 NA NA 205 85 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 25 NA NA 196 37 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.025 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.5 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.55 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 196 NA NA 270 124 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 26 NA NA 156 30 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.026 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.25 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 156 NA NA 216 92 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 27 NA NA 137 28 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.027 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.5 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 137 NA NA 193 75 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 28 NA NA 170 33 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.028 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.75 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 170 NA NA 236 104 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 29 NA NA 186 35 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.029 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.25 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 186 NA NA 256 116 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 30 NA NA 130 27 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.03 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.2 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -27.09 NA NA Hatté et al., (1998, Fig. 3A, Achenheim) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Achenheim) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 130 NA NA 184 70 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0 NA NA 247 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.55 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.86 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 247 NA NA 345 163 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1 NA NA 270 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.55 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 270 NA NA 382 180 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2 NA NA 271 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.55 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 271 NA NA 383 181 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3 NA NA 272 57 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.55 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 272 NA NA 386 180 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4 NA NA 275 58 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.6 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 275 NA NA 391 183 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5 NA NA 278 58 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.65 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 278 NA NA 394 186 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6 NA NA 280 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.7 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 280 NA NA 398 186 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7 NA NA 279 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.007 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.7 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 279 NA NA 397 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8 NA NA 275 57 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.008 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.65 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 275 NA NA 389 183 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9 NA NA 269 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.6 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.45 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 269 NA NA 381 179 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10 NA NA 263 54 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.55 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.53 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 263 NA NA 371 175 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11 NA NA 242 47 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.2 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.63 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 242 NA NA 336 160 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12 NA NA 213 40 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.6 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.73 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 213 NA NA 293 137 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13 NA NA 222 42 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.9 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.8 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 222 NA NA 306 144 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14 NA NA 222 42 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.014 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.95 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 222 NA NA 306 144 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15 NA NA 212 40 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.015 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.7 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 212 NA NA 292 136 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16 NA NA 214 41 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.016 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.7 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.79 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 214 NA NA 296 138 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17 NA NA 215 41 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.017 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.65 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.72 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 215 NA NA 297 139 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18 NA NA 232 45 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.64 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 232 NA NA 322 152 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 19 NA NA 222 42 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.019 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.7 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 222 NA NA 306 144 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 20 NA NA 205 39 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.25 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 205 NA NA 283 131 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 21 NA NA 188 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.021 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.8 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 188 NA NA 260 118 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22 NA NA 187 35 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.022 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.8 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 187 NA NA 257 117 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23 NA NA 217 41 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.023 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.7 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 217 NA NA 299 141 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 24 NA NA 196 37 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.024 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.1 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.68 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 196 NA NA 270 124 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 25 NA NA 199 38 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.025 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.05 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.55 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 199 NA NA 275 127 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 26 NA NA 195 37 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.026 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 195 NA NA 269 123 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 27 NA NA 202 38 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.027 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.2 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 202 NA NA 278 128 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 28 NA NA 206 39 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.028 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.3 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 206 NA NA 284 132 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 29 NA NA 206 39 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.029 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.3 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 206 NA NA 284 132 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 30 NA NA 214 41 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.03 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.5 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.57 NA NA Hatté et al., (1998, Fig. 3A, Nuβloch) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Hatté et al., (1998, Fig. 3A, Nuβloch) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 214 NA NA 296 138 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.008 NA NA 293 63 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000008 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.7 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.82 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 293 NA NA 419 195 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.171 NA NA 264 54 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000171 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.7 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 264 NA NA 372 176 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.431 NA NA 289 62 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001431 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.2 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 289 NA NA 413 193 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.218 NA NA 285 60 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002218 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.1 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 285 NA NA 405 189 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.223 NA NA 290 62 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002223 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.2 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 290 NA NA 414 194 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.597 NA NA 296 64 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002597 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.3 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 296 NA NA 424 198 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.227 NA NA 286 61 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003227 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.1 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 286 NA NA 408 190 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.133 NA NA 270 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004133 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.8 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 270 NA NA 382 180 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.406 NA NA 270 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004406 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.8 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 270 NA NA 382 180 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.531 NA NA 260 53 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004531 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.6 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 260 NA NA 366 172 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.551 NA NA 250 50 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004551 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.4 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 250 NA NA 350 166 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.828 NA NA 275 58 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004828 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.9 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 275 NA NA 391 183 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.38 NA NA 246 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00538 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.3 NA NA Huang et al., (1996; Table 1; acid brown) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.87 NA NA Huang et al., (1996; Table 1; acid brown) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; acid brown) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 246 NA NA 344 162 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.005 NA NA 440 114 83 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.1 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.83 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 440 NA NA 668 274 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.045 NA NA 399 99 73 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000045 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.5 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 399 NA NA 597 253 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.54 NA NA 349 82 61 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00054 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.6 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 349 NA NA 513 227 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.707 NA NA 328 75 56 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000707 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.3 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 328 NA NA 478 216 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.661 NA NA 365 87 64 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001661 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.8 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 365 NA NA 539 237 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.574 NA NA 351 82 61 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002574 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.6 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 351 NA NA 515 229 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.573 NA NA 325 73 55 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005573 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.2 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 325 NA NA 471 215 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.651 NA NA 294 63 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005651 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.7 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 294 NA NA 420 196 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.896 NA NA 293 63 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006896 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.7 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 293 NA NA 419 195 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.963 NA NA 224 43 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.007963 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.3 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 224 NA NA 310 146 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.218 NA NA 256 52 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009218 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.1 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.46 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 256 NA NA 360 170 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.559 NA NA 187 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.010559 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.5 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 187 NA NA 259 117 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.896 NA NA 180 34 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011896 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.4 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.72 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 180 NA NA 248 112 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.383 NA NA 188 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012383 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.7 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -25.33 NA NA Huang et al., (1996; Table 1; pleaty gley) -6.76 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Huang et al., (1996; Table 1; pleaty gley) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 188 NA NA 260 118 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.817 NA NA 274 57 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.007817 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.55 NA NA Kao et al., (2008; TOC dates from Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.5 NA NA Kao et al., (2008; TOC dates from Table 1) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Kao et al., (2008; TOC dates from Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 274 NA NA 388 182 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.987 NA NA 248 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012987 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.45 NA NA Kao et al., (2008; TOC dates from Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.5 NA NA Kao et al., (2008; TOC dates from Table 1) -6.8 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Kao et al., (2008; TOC dates from Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 248 NA NA 346 164 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15.778 NA NA 255 51 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.015778 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.6 NA NA Kao et al., (2008; TOC dates from Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.5 NA NA Kao et al., (2008; TOC dates from Table 1) -6.81 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Kao et al., (2008; TOC dates from Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 255 NA NA 357 169 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16.313 NA NA 272 56 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.016313 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.9 NA NA Kao et al., (2008; TOC dates from Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.5 NA NA Kao et al., (2008; TOC dates from Table 1) -6.77 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Kao et al., (2008; TOC dates from Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 272 NA NA 384 180 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18.404 NA NA 280 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018404 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.9 NA NA Kao et al., (2008; TOC dates from Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.5 NA NA Kao et al., (2008; TOC dates from Table 1) -6.61 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Kao et al., (2008; TOC dates from Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 280 NA NA 398 186 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 21.972 NA NA 255 51 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.021972 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.45 NA NA Kao et al., (2008; TOC dates from Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.5 NA NA Kao et al., (2008; TOC dates from Table 1) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Kao et al., (2008; TOC dates from Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 255 NA NA 357 169 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 24.598 NA NA 230 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.024598 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.85 NA NA Kao et al., (2008; TOC dates from Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.5 NA NA Kao et al., (2008; TOC dates from Table 1) -6.61 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Kao et al., (2008; TOC dates from Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 230 NA NA 318 150 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.5 NA NA 321 72 54 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0015 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 321 NA NA 465 213 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2 NA NA 357 84 63 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 357 NA NA 525 231 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.5 NA NA 399 99 73 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0025 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 399 NA NA 597 253 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3 NA NA 293 63 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 293 NA NA 419 195 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.5 NA NA 266 55 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0035 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 266 NA NA 376 176 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4 NA NA 221 42 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 221 NA NA 305 143 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.5 NA NA 202 38 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0045 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 202 NA NA 278 130 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5 NA NA 202 38 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 202 NA NA 278 128 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.5 NA NA 243 48 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0055 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 243 NA NA 339 161 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6 NA NA 142 29 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 142 NA NA 200 80 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.5 NA NA 221 42 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0065 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 221 NA NA 305 143 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7 NA NA 220 42 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.007 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 220 NA NA 304 142 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.5 NA NA 265 54 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0075 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 265 NA NA 373 177 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8 NA NA 240 47 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.008 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 240 NA NA 334 158 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.5 NA NA 319 71 53 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0085 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.41 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 319 NA NA 461 213 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9 NA NA 492 138 98 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.45 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 492 NA NA 768 296 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.5 NA NA 165 32 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0095 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.49 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 165 NA NA 229 99 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10 NA NA 345 80 60 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.53 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 345 NA NA 505 225 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.5 NA NA 380 92 68 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0105 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 380 NA NA 564 244 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11 NA NA 471 128 92 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.63 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 471 NA NA 727 287 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.5 NA NA 275 57 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0115 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.68 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 275 NA NA 389 183 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12 NA NA 332 76 56 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.73 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 332 NA NA 484 220 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.5 NA NA 365 87 64 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0125 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.77 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 365 NA NA 539 237 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13 NA NA 295 64 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.8 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 295 NA NA 423 197 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.5 NA NA 360 85 63 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0135 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.83 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 360 NA NA 530 234 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14 NA NA 359 85 63 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.014 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 359 NA NA 529 233 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14.5 NA NA 324 73 55 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0145 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.85 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 324 NA NA 470 214 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15 NA NA 266 55 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.015 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 266 NA NA 376 176 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15.5 NA NA 243 48 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0155 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.82 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 243 NA NA 339 161 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16 NA NA 245 48 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.016 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.79 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 245 NA NA 341 161 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16.5 NA NA 224 43 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0165 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.76 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 224 NA NA 310 146 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17 NA NA 300 65 50 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.017 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.72 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 300 NA NA 430 200 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17.5 NA NA 190 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0175 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.68 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 190 NA NA 262 120 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18 NA NA 57 20 28 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -18.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.64 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 57 NA NA 97 1 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18.5 NA NA 231 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0185 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.61 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 231 NA NA 319 151 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 19 NA NA 212 40 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.019 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 212 NA NA 292 136 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 19.5 NA NA 149 29 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0195 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 149 NA NA 207 85 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 20 NA NA 163 31 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 163 NA NA 225 97 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 20.5 NA NA 162 31 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0205 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 162 NA NA 224 96 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 21 NA NA 211 40 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.021 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 211 NA NA 291 137 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 21.5 NA NA 135 28 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0215 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.63 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 135 NA NA 191 73 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22 NA NA 94 23 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.022 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 94 NA NA 140 36 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22.5 NA NA 77 21 28 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0225 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.69 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 77 NA NA 119 21 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23 NA NA 112 25 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.023 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 112 NA NA 162 54 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23.5 NA NA 173 33 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0235 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 173 NA NA 239 105 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 24 NA NA 303 66 51 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.024 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.68 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 303 NA NA 435 201 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 24.5 NA NA 277 58 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0245 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.62 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 277 NA NA 393 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 25 NA NA 256 52 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.025 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.55 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 256 NA NA 360 170 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 25.5 NA NA 279 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0255 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 279 NA NA 397 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 26 NA NA 307 68 51 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.026 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 307 NA NA 443 205 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 26.5 NA NA 253 51 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0265 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 253 NA NA 355 167 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 27 NA NA 253 51 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.027 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.5 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 253 NA NA 355 167 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 27.5 NA NA 136 28 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0275 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 136 NA NA 192 74 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 28 NA NA 231 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.028 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 231 NA NA 319 151 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 28.5 NA NA 162 31 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0285 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 162 NA NA 224 96 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 29 NA NA 279 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.029 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.64 NA NA Li et al., (2013; Fig. 9g, 500-yr intervals) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Li et al., (2013; Fig. 9g, 500-yr intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 279 NA NA 397 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.1 NA NA 315 71 53 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.81 NA NA Lu et al., (2012; Horqin Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.02 NA NA Lu et al., (2012; Horqin Field) -6.4 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Horqin Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 315 NA NA 457 209 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.76 NA NA 297 64 50 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00076 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.5 NA NA Lu et al., (2012; Horqin Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.02 NA NA Lu et al., (2012; Horqin Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Horqin Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 297 NA NA 425 197 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.15 NA NA 250 50 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00315 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.54 NA NA Lu et al., (2012; Horqin Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.02 NA NA Lu et al., (2012; Horqin Field) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Horqin Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 250 NA NA 350 166 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.31 NA NA 433 112 82 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01031 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.49 NA NA Lu et al., (2012; Horqin Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.02 NA NA Lu et al., (2012; Horqin Field) -6.56 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Horqin Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 433 NA NA 657 269 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.8 NA NA 848 423 213 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0108 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25 NA NA Lu et al., (2012; Horqin Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.02 NA NA Lu et al., (2012; Horqin Field) -6.61 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Horqin Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 848 NA NA 1694 422 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 19.55 NA NA 276 58 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01955 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.31 NA NA Lu et al., (2012; Horqin Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.02 NA NA Lu et al., (2012; Horqin Field) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Horqin Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 276 NA NA 392 184 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.1 NA NA 238 47 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.24 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 238 NA NA 332 156 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.29 NA NA 397 98 72 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00029 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.77 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 397 NA NA 593 253 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.39 NA NA 309 68 52 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00239 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.56 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 309 NA NA 445 205 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.29 NA NA 195 37 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00729 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.07 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 195 NA NA 269 123 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.39 NA NA 133 27 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00739 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -18.87 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 133 NA NA 187 73 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.56 NA NA 300 66 50 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00756 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.34 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 300 NA NA 432 200 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.56 NA NA 295 64 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00756 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.43 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 295 NA NA 423 197 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.81 NA NA 244 48 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00781 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.35 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 244 NA NA 340 160 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.1 NA NA 324 73 55 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0081 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.84 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.39 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 324 NA NA 470 214 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.38 NA NA 335 77 57 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00838 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.01 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.41 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 335 NA NA 489 221 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.55 NA NA 318 71 53 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00855 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.76 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.42 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 318 NA NA 460 212 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.78 NA NA 274 57 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00978 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.09 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.51 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 274 NA NA 388 182 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.98 NA NA 316 71 53 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00998 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.85 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.53 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 316 NA NA 458 210 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.045 NA NA 189 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.010045 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.09 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.53 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 189 NA NA 261 119 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11 NA NA 300 65 50 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.68 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.63 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 300 NA NA 430 200 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.7 NA NA 209 40 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0127 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.89 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.78 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 209 NA NA 289 135 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.175 NA NA 252 50 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013175 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.94 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.81 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 252 NA NA 352 166 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.65 NA NA 288 62 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01365 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.67 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.83 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 288 NA NA 412 192 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 25.68 NA NA 241 47 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02568 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.5 NA NA Lu et al., (2012; Mu Us Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.91 NA NA Lu et al., (2012; Mu Us Dune Field) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Mu Us Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 241 NA NA 335 159 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.1 NA NA 268 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.8 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 268 NA NA 380 178 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.13 NA NA 315 70 53 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00013 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.59 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 315 NA NA 455 209 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.14 NA NA 337 77 58 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00014 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.92 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 337 NA NA 491 221 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.43 NA NA 259 53 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00043 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.6 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 259 NA NA 365 171 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.49 NA NA 252 50 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00049 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.45 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 252 NA NA 352 166 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.56 NA NA 267 55 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00056 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.77 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 267 NA NA 377 177 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.63 NA NA 267 55 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00063 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.77 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 267 NA NA 377 177 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.63 NA NA 257 52 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00063 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.57 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 257 NA NA 361 171 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.63 NA NA 224 43 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00063 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.81 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 224 NA NA 310 146 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.66 NA NA 314 70 52 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00066 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.61 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 314 NA NA 454 210 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.68 NA NA 316 70 53 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00068 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.63 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 316 NA NA 456 210 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.71 NA NA 315 70 53 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00071 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.62 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 315 NA NA 455 209 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.74 NA NA 246 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00074 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.33 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 246 NA NA 344 162 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.95 NA NA 255 51 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00095 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.52 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 255 NA NA 357 169 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.98 NA NA 276 58 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00098 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.94 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 276 NA NA 392 184 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.22 NA NA 245 48 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00122 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.32 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 245 NA NA 341 161 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.3 NA NA 279 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0013 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.99 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 279 NA NA 397 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.53 NA NA 345 80 60 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00153 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.06 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 345 NA NA 505 225 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.58 NA NA 223 42 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00158 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.78 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 223 NA NA 307 145 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.62 NA NA 270 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00162 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.83 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 270 NA NA 382 180 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.03 NA NA 231 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00203 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.97 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 231 NA NA 319 151 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.34 NA NA 292 63 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00234 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.21 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 292 NA NA 418 194 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.7 NA NA 280 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0027 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.98 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 280 NA NA 398 186 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.73 NA NA 247 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00273 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.33 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 247 NA NA 345 163 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.76 NA NA 241 47 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00276 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.18 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 241 NA NA 335 159 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.32 NA NA 261 53 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00332 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.61 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 261 NA NA 367 173 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.04 NA NA 261 53 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00404 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.61 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 261 NA NA 367 173 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.06 NA NA 336 77 58 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00406 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.9 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 336 NA NA 490 220 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.46 NA NA 237 46 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00446 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.08 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 237 NA NA 329 155 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.48 NA NA 245 48 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00448 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.25 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 245 NA NA 341 161 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.97 NA NA 290 62 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00497 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.15 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 290 NA NA 414 194 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.02 NA NA 239 47 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00502 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.13 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 239 NA NA 333 157 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.15 NA NA 234 45 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00515 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 234 NA NA 324 154 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.24 NA NA 243 48 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00524 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.21 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 243 NA NA 339 161 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.64 NA NA 288 62 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00664 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.13 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 288 NA NA 412 192 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.73 NA NA 249 50 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00773 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.39 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 249 NA NA 349 165 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.96 NA NA 239 47 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00796 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.19 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 239 NA NA 333 157 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.21 NA NA 337 77 58 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00821 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.97 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 337 NA NA 491 221 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.68 NA NA 253 51 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00868 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.53 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.42 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 253 NA NA 355 167 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.72 NA NA 294 64 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00872 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.32 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.43 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 294 NA NA 422 196 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.74 NA NA 312 69 52 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00874 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.62 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.43 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 312 NA NA 450 208 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.88 NA NA 337 77 58 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00888 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.01 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.44 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 337 NA NA 491 221 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.115 NA NA 270 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009115 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.91 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.45 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 270 NA NA 382 180 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.37 NA NA 271 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00937 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.94 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.47 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 271 NA NA 383 181 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.9 NA NA 320 72 54 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0099 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.84 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.52 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 320 NA NA 464 212 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17.73 NA NA 241 47 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01773 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.5 NA NA Lu et al., (2012; Otindag Dune Field) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.85 NA NA Lu et al., (2012; Otindag Dune Field) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments/SOM NA Lu et al., (2012; Otindag Dune Field) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 241 NA NA 335 159 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.95 NA NA 257 52 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00495 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 257 NA NA 361 171 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.298 NA NA 257 52 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005298 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 257 NA NA 361 171 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.646 NA NA 234 45 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005646 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 234 NA NA 324 154 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.994 NA NA 269 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005994 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.75 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 269 NA NA 381 179 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.342 NA NA 225 43 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006342 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.8 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 225 NA NA 311 147 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.689 NA NA 269 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006689 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.75 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 269 NA NA 381 179 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.037 NA NA 256 52 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.007037 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 256 NA NA 360 170 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.385 NA NA 310 69 52 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.007385 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.5 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 310 NA NA 448 206 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.733 NA NA 280 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.007733 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 280 NA NA 398 186 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.081 NA NA 269 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.008081 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.8 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.39 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 269 NA NA 381 179 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.6 NA NA 278 58 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0086 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.42 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 278 NA NA 394 186 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.119 NA NA 305 67 51 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009119 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.5 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.45 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 305 NA NA 439 203 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.638 NA NA 288 61 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009638 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.25 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.5 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 288 NA NA 410 192 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.157 NA NA 271 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.010157 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.54 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 271 NA NA 383 181 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.676 NA NA 245 48 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.010676 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 245 NA NA 341 161 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.195 NA NA 324 73 55 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011195 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -30 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.65 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 324 NA NA 470 214 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.714 NA NA 291 62 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011714 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.5 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 291 NA NA 415 195 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.295 NA NA 318 71 53 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012295 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -30 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.75 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 318 NA NA 460 212 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.828 NA NA 283 60 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013828 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.5 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 283 NA NA 403 189 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14.78 NA NA 234 45 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01478 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 234 NA NA 324 154 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15.733 NA NA 235 45 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.015733 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.81 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 235 NA NA 325 155 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16.686 NA NA 190 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.016686 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.25 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.74 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 190 NA NA 262 120 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17.639 NA NA 108 24 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.017639 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.83 NA NA Menking et al., (2012; Fig. 3, Minnewaska) -6.67 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Menking et al., (2012; Fig. 3, Minnewaska) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 108 NA NA 156 50 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.5 NA NA 238 46 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 238 NA NA 330 156 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1 NA NA 238 46 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 238 NA NA 330 156 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.5 NA NA 261 53 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0015 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.5 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 261 NA NA 367 173 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2 NA NA 252 51 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.3 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 252 NA NA 354 166 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.5 NA NA 251 50 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0025 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.25 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 251 NA NA 351 167 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3 NA NA 249 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.2 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 249 NA NA 347 165 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.5 NA NA 240 47 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0035 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 240 NA NA 334 158 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4 NA NA 231 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.8 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 231 NA NA 319 151 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.5 NA NA 227 43 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0045 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 227 NA NA 313 149 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5 NA NA 223 43 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.6 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 223 NA NA 309 145 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.5 NA NA 236 46 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0055 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.9 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 236 NA NA 328 156 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6 NA NA 236 46 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.9 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 236 NA NA 328 156 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.5 NA NA 231 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0065 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.8 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 231 NA NA 319 151 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7 NA NA 231 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.007 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.8 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 231 NA NA 319 151 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.5 NA NA 243 48 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0075 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.1 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 243 NA NA 339 161 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8 NA NA 287 61 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.008 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 287 NA NA 409 191 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.5 NA NA 348 81 60 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0085 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.41 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 348 NA NA 510 228 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9 NA NA 270 56 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.75 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.45 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 270 NA NA 382 180 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.5 NA NA 478 131 94 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0095 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.5 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.49 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 478 NA NA 740 290 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10 NA NA 354 83 62 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.2 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.53 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 354 NA NA 520 230 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.5 NA NA 446 116 85 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0105 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.3 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 446 NA NA 678 276 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11 NA NA 333 76 57 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.63 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 333 NA NA 485 219 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.5 NA NA 299 65 50 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0115 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.5 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.68 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 299 NA NA 429 199 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12 NA NA 232 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.2 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.73 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 232 NA NA 320 152 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.5 NA NA 222 42 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0125 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.77 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 222 NA NA 306 144 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13 NA NA 265 54 45 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.8 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 265 NA NA 373 175 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.5 NA NA 290 62 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0135 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.5 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.83 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 290 NA NA 414 194 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14 NA NA 219 42 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.014 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 219 NA NA 303 143 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14.5 NA NA 183 35 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0145 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.85 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 183 NA NA 253 113 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15 NA NA 180 34 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.015 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.9 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 180 NA NA 248 112 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15.5 NA NA 178 34 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0155 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.8 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -22.7 NA NA Norstrom et al., (2009; Fig. 5, 500-year intervals) -6.82 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Peat NA Norstrom et al., (2009; Fig. 5, 500-year intervals) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 178 NA NA 246 110 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1 NA NA 218 42 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.4 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 218 NA NA 302 142 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1 NA NA 277 58 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.7 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 277 NA NA 393 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2 NA NA 384 94 69 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.3 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 384 NA NA 572 246 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3 NA NA 308 68 51 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.2 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 308 NA NA 444 206 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.8 NA NA 255 51 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0038 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.2 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 255 NA NA 357 169 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4 NA NA 246 49 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 246 NA NA 344 162 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5 NA NA 321 72 54 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.4 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 321 NA NA 465 213 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.3 NA NA 260 53 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0053 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.3 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 260 NA NA 366 172 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.8 NA NA 232 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0068 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.7 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 232 NA NA 320 152 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17 NA NA 309 68 52 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.017 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.6 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.72 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 309 NA NA 445 205 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18 NA NA 184 35 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -18.7 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.64 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 184 NA NA 254 114 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18 NA NA 254 51 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.5 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.64 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 254 NA NA 356 168 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 19 NA NA 243 48 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.019 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.2 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 243 NA NA 339 161 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 19 NA NA 218 42 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.019 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.6 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 218 NA NA 302 142 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 20 NA NA 204 39 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.2 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 204 NA NA 282 130 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 21 NA NA 238 46 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.021 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.1 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 238 NA NA 330 156 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23 NA NA 238 46 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.023 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.2 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 238 NA NA 330 156 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 26 NA NA 221 41 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.026 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -19.5 NA NA Rommerskirchen et al (2006; Table 3) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -20.58 NA NA Rommerskirchen et al (2006; Table 3) -6.42 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA Rommerskirchen et al (2006; Table 3) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 221 NA NA 303 145 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.115 NA NA 211 40 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000115 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.1 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 211 NA NA 291 135 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.345 NA NA 211 40 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000345 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.1 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 211 NA NA 291 137 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.575 NA NA 252 51 43 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000575 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.1 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 252 NA NA 354 166 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.805 NA NA 283 60 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.000805 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.7 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 283 NA NA 403 189 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.245 NA NA 294 64 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001245 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.9 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 294 NA NA 422 196 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.685 NA NA 283 60 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001685 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.7 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 283 NA NA 403 189 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.125 NA NA 313 70 52 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002125 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.2 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 313 NA NA 453 209 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.565 NA NA 296 64 49 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002565 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.9 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 296 NA NA 424 198 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.988 NA NA 309 68 52 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003988 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.1 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 309 NA NA 445 205 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.411 NA NA 328 75 56 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005411 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.4 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 328 NA NA 478 216 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.834 NA NA 334 76 57 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006834 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.5 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 334 NA NA 486 220 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.257 NA NA 233 45 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.008257 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.7 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 233 NA NA 323 153 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.68 NA NA 233 45 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00968 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.8 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.5 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 233 NA NA 323 153 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.915 NA NA 220 42 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011915 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.7 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.72 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 220 NA NA 304 142 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14.15 NA NA 200 38 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01415 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.3 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.85 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 200 NA NA 276 128 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16.385 NA NA 200 38 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.016385 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.2 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.77 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 200 NA NA 276 128 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18.955 NA NA 230 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.018955 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.8 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 230 NA NA 318 150 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22.63 NA NA 210 40 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02263 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.4 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.69 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 210 NA NA 290 136 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22.695 NA NA 217 41 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.022695 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.6 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 217 NA NA 299 141 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22.76 NA NA 199 38 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02276 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.1 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 199 NA NA 275 127 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22.825 NA NA 192 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.022825 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.9 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 192 NA NA 264 122 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22.89 NA NA 178 34 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02289 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.5 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 178 NA NA 246 110 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 22.955 NA NA 178 34 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.022955 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.5 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 178 NA NA 246 110 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23.02 NA NA 188 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02302 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.8 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 188 NA NA 260 118 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23.085 NA NA 188 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.023085 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.8 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 188 NA NA 260 118 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23.15 NA NA 198 38 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02315 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -25.1 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.71 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 198 NA NA 274 126 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23.501 NA NA 185 35 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.023501 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.7 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 185 NA NA 255 115 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23.851 NA NA 179 34 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.023851 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.5 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.69 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 179 NA NA 247 111 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 24.202 NA NA 170 33 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.024202 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.2 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.66 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 170 NA NA 236 104 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 24.553 NA NA 175 33 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.024553 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.3 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.62 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 175 NA NA 241 107 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 24.903 NA NA 176 34 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.024903 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.3 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 176 NA NA 244 108 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 25.254 NA NA 158 31 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.025254 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.7 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 158 NA NA 220 94 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 25.605 NA NA 163 32 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.025605 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.9 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 163 NA NA 227 97 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 25.955 NA NA 163 32 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.025955 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.9 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 163 NA NA 227 97 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 26.306 NA NA 166 32 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.026306 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 166 NA NA 230 100 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 26.657 NA NA 158 31 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.026657 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.7 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 158 NA NA 220 94 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 27.007 NA NA 155 30 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.027007 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.6 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 155 NA NA 215 91 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 27.358 NA NA 147 29 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.027358 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.3 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 147 NA NA 205 85 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 27.628 NA NA 169 33 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.027628 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.1 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 169 NA NA 235 103 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 27.899 NA NA 175 34 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.027899 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.3 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 175 NA NA 243 107 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 28.169 NA NA 161 31 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.028169 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.8 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 161 NA NA 223 95 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 28.44 NA NA 163 32 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02844 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.9 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 163 NA NA 227 97 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 28.71 NA NA 169 33 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02871 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.1 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 169 NA NA 235 103 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 28.98 NA NA 158 31 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02898 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.7 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 158 NA NA 220 94 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 29.251 NA NA 147 29 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.029251 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.3 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 147 NA NA 205 85 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 29.521 NA NA 155 30 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.029521 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.6 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 155 NA NA 215 91 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 29.791 NA NA 152 30 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.029791 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.5 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -26.48 NA NA Ruiz Pessenda et al., (2009; Table 4) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. SOM NA Ruiz Pessenda et al., (2009; Table 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 152 NA NA 212 88 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.96 NA NA 254 34 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00196 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.2 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 254 NA NA 322 192 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.34 NA NA 245 32 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00234 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 245 NA NA 309 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.76 NA NA 228 29 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00276 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.6 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 228 NA NA 286 170 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.94 NA NA 280 39 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00294 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.7 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 280 NA NA 358 214 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.96 NA NA 315 47 38 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00296 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.3 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 315 NA NA 409 239 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.72 NA NA 260 35 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00572 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.3 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 260 NA NA 330 198 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.51 NA NA 273 38 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00751 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.6 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 273 NA NA 349 209 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.51 NA NA 320 48 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00751 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.4 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 320 NA NA 416 242 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.42 NA NA 261 35 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.00842 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.4 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.41 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 261 NA NA 331 199 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.01 NA NA 297 43 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.2 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.53 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 297 NA NA 383 227 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.66 NA NA 288 41 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01166 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.2 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.69 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 288 NA NA 370 220 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.85 NA NA 323 49 39 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01185 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.8 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.71 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 323 NA NA 421 245 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.93 NA NA 310 46 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01193 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.6 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.72 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 310 NA NA 402 236 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.19 NA NA 246 32 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01219 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.4 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.74 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 246 NA NA 310 186 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.3 NA NA 304 45 36 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0133 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24.6 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.82 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 304 NA NA 394 232 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14.17 NA NA 184 24 26 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01417 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.9 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.85 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 184 NA NA 232 132 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14.3 NA NA 241 31 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0143 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.4 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.85 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 241 NA NA 303 181 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14.6 NA NA 166 22 25 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0146 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.3 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.85 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 166 NA NA 210 116 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14.81 NA NA 260 35 31 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01481 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.8 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 260 NA NA 330 198 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14.91 NA NA 270 37 32 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01491 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -24 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 270 NA NA 344 206 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15.34 NA NA 172 23 25 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01534 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.5 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.83 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 172 NA NA 218 122 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15.48 NA NA 229 30 29 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01548 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.1 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.82 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 229 NA NA 289 171 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 15.62 NA NA 221 28 28 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01562 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.9 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.82 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 221 NA NA 277 165 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16.21 NA NA 244 32 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01621 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.4 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.78 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 244 NA NA 308 184 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 16.75 NA NA 175 23 25 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01675 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.5 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.74 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 175 NA NA 221 125 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17.03 NA NA 242 31 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01703 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.3 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.72 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 242 NA NA 304 182 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17.25 NA NA 199 26 27 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01725 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.2 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 199 NA NA 251 145 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17.33 NA NA 203 26 27 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01733 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.3 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.69 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 203 NA NA 255 149 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17.506 NA NA 200 26 27 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.017506 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.2 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.68 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 200 NA NA 252 146 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 17.58 NA NA 157 22 25 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01758 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -20.8 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.67 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 157 NA NA 201 107 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 18.65 NA NA 167 23 25 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01865 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.1 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 167 NA NA 213 117 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 19.32 NA NA 197 26 26 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01932 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 197 NA NA 249 145 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 19.9 NA NA 279 39 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0199 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.9 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 279 NA NA 357 213 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 20.07 NA NA 186 24 26 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02007 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.7 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.57 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 186 NA NA 234 134 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 21.74 NA NA 250 33 30 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02174 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -23.4 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.65 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 250 NA NA 316 190 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23.11 NA NA 199 26 27 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02311 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.2 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 199 NA NA 251 145 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 23.51 NA NA 210 27 27 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02351 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.5 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.7 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 210 NA NA 264 156 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 25.33 NA NA 203 26 27 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02533 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.2 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 203 NA NA 255 149 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 26.17 NA NA 203 26 27 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02617 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.2 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 203 NA NA 255 149 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 27.37 NA NA 218 28 28 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02737 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -22.6 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 218 NA NA 274 162 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 28.02 NA NA 189 25 26 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.02802 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -21.8 NA NA Van de Water et al. (1994; Table 1) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -23.57 NA NA Van de Water et al. (1994; Table 1) -6.6 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Pinus leaves NA Van de Water et al. (1994; Table 1) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 189 NA NA 239 137 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 0.5 NA NA 275 57 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 275 NA NA 389 183 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1 NA NA 249 50 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.001 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 249 NA NA 349 165 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 1.5 NA NA 250 50 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0015 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.37 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 250 NA NA 350 166 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2 NA NA 289 62 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.002 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.75 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 289 NA NA 413 193 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 2.5 NA NA 304 67 51 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0025 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 304 NA NA 438 202 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3 NA NA 320 72 54 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.003 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.25 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 320 NA NA 464 212 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 3.5 NA NA 338 78 58 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0035 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.5 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 338 NA NA 494 222 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4 NA NA 321 72 54 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.004 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.25 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 321 NA NA 465 213 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 4.5 NA NA 229 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0045 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.5 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 229 NA NA 317 149 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5 NA NA 264 54 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.005 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.25 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 264 NA NA 372 176 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 5.5 NA NA 321 72 54 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0055 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.25 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 321 NA NA 465 213 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6 NA NA 277 58 46 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.006 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.33 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 277 NA NA 393 185 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 6.5 NA NA 191 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0065 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.5 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.34 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 191 NA NA 263 121 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7 NA NA 290 62 48 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.007 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.75 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.35 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 290 NA NA 414 194 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 7.5 NA NA 303 66 51 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0075 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.36 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 303 NA NA 435 201 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8 NA NA 334 77 57 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.008 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -29.5 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.38 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 334 NA NA 488 220 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 8.5 NA NA 237 46 41 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0085 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27.75 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.41 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 237 NA NA 329 155 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9 NA NA 205 39 37 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.009 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -27 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.45 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 205 NA NA 283 131 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 9.5 NA NA 245 48 42 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0095 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.49 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 245 NA NA 341 161 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10 NA NA 280 59 47 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.01 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.75 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.53 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 280 NA NA 398 186 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 10.5 NA NA 192 36 35 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0105 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.75 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.58 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 192 NA NA 264 122 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11 NA NA 353 83 61 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.011 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -30 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.63 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 353 NA NA 519 231 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 11.5 NA NA 259 53 44 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0115 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28.5 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.68 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 259 NA NA 365 171 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12 NA NA 179 34 34 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.012 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.5 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.73 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 179 NA NA 247 111 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 12.5 NA NA 232 45 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0125 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.77 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 232 NA NA 322 152 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13 NA NA 231 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.013 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.8 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 231 NA NA 319 151 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 13.5 NA NA 230 44 40 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.0135 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -28 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.83 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 230 NA NA 318 150 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ land_plant_d13C_1 Schubert 2015 10.1130/G36467.1 14 NA NA 167 32 33 Brian Schubert schubert@louisiana.edu Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 2015 10.1130/G36467.1 NA NA NA NA NA NA NA NA NA 0.014 NA NA Andersson et al. (2012; Fig. 3; fen deposits) -26.25 NA NA You and Liu, (2012; Fig. 4) -6.4 NA NA Lüthi, D., et al., 2008, High-resolution carbon dioxide concentration record 650,000–800,000 years before present: Nature, v. 453, p. 379–382, doi: 10.1038/nature06949. -28.44 NA NA You and Liu, (2012; Fig. 4) -6.84 NA NA Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. 270 7 Kawamura, K., Nakazawa, T., Aoki, S., Sugawara, S., Fujii, Y., and Watanabe, O., 2007, Dome Fuji ice core 338KYr wet extraction CO2 data, in IGBP PAGES/World Data Center for Paleoclimatology, ed.: Boulder CO, USA, NOAA/NCDC Paleoclimatology Program. Sediments NA You and Liu, (2012; Fig. 4) NA NA NA NA NA 28.26 26 to 30 0.22 0.16 to 0.27 23.9 19.2 to 32.9 167 NA NA 231 101 Schubert, B. A., and Jahren, A. H., 2015, Global increase in plant carbon isotope fractionation following the Last Glacial Maximum caused by increase in atmospheric pCO2: Geology, v. 43, no. 5, p. 435-438. This work predates Method 1; therefore uncertainties may differ