# Central Equatorial Pacific Dust Flux, Productivity and d15N Data for 0-27ka #----------------------------------------------------------------------- # World Data Center for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # NOTE: Please cite original publication, online resource and date accessed when using this data. # If there is no publication information, please cite Investigator, title, online resource and date accessed. # # Description/Documentation lines begin with # # Data lines have no # # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/ # Online_Resource: http://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/by_contributor/costa2015/costa2015-d15n.txt # # Archive: Paleoceanography # # Parameter_Keywords: geochemistry, lithology, nitrogen isotopes #--------------------------------------- # Contribution_Date # Date: 2015-11-10 #--------------------------------------- # Title # Study_Name: Central Equatorial Pacific Dust Flux, Productivity and d15N Data for 0-27ka #--------------------------------------- # Investigators # Investigators: Costa, K.M.; McManus, J.F.; Anderson, R.F.; Ren, H.; Sigman, D.M.; Winckler, G.; Fleisher, M.Q.; Marcantonio, F.; Ravelo, A.C. #--------------------------------------- # Description and Notes # Description: Site Information: # MC # BB # Lat(N) Long(W) Depth(m) # 14 13 -0.22 156 3049 # 21 20 1.27 157.3 2850 # 26 25 2.46 159.4 3545 # 29 28 2.97 159.2 3152 # 33 32 5.2 160.4 2933 # 39 36 6.83 161 2859 # Provided Keywords: Holocene, Last Glacial Period, dust, productivity, Th isotopes, opal, barium #--------------------------------------- # Publication # Authors: Costa, K.M.; McManus, J.F.; Anderson, R.F.; Ren, H.; Sigman, D.M.; Winckler, G.; Fleisher, M.Q.; Marcantonio, F. and Ravelo, A.C. # Published_Date_or_Year: 2015 # Published_Title: No iron fertilization in the Equatorial Pacific during the Last Ice Age # Journal_Name: Nature # Volume: 529 # Issue: # Pages: 519-522 # Report Number: # DOI: # Abstract: The “major” nutrients for phytoplankton growth (nitrogen, phosphorus, and silicon) are supplied to the surface waters of the Equatorial Pacific (EP) by wind-driven upwelling along the equator. Their consumption by phytoplankton is thought to be limited in part by the low concentrations of the critical micro-nutrient iron. Greater atmospheric dust deposition may have fertilized the EP with iron during the Last Glacial Period (LGP, 17-27,000 years ago). Here we present meridional transects of dust (232Th), phytoplankton productivity (opal, 231Pa/230Th, excess Ba), and the degree of nitrate consumption (foraminifera-bound d15N) from the Central EP for Holocene and LGP time slices. Despite two- to three-fold greater dust deposition in the Central EP, productivity was the same or lower during the LGP compared to the Holocene, and the degree of nitrate consumption was unchanged. These biogeochemical findings suggest that the relatively greater ice age dust fluxes were inadequate to drive significant iron fertilization in the Central EP, which may be because the absolute rate of dust deposition in the LGP, despite being greater than the Holocene rate, was still very low. The lower productivity coupled with unchanged nitrate consumption suggests lower subsurface major nutrient concentrations in the Central EP during the LGP. As these nutrients are today dominantly sourced from the Subantarctic Zone of the Southern Ocean, the Central EP data are consistent with more complete nutrient consumption in the Subantarctic, apparently because of iron fertilization in that region, where absolute dust fluxes were much higher. Thus, ice age iron fertilization ultimately worked to lower, not raise, Equatorial Pacific productivity. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: National Science Foundation # Grant: AGS-15-02889, OCE-10-60947 #--------------------------------------- # Site Information # Site_Name: Line Islands # Location: Central Equatorial Pacific # Country: # Northernmost_Latitude: 6.83 # Southernmost_Latitude: -0.22 # Easternmost_Longitude: -156 # Westernmost_Longitude: -161 # Elevation: -2850 #--------------------------------------- # Data_Collection # Collection_Name: Line Island d15N Costa15 # First_Year: 27000 # Last_Year: 2000 # Time_Unit: cal yr BP # Core_Length: # Notes: #--------------------------------------- # Chronology: # # Core Depth (cm) Radiocarbon Age (yrs) ± Calendar Age (yrs) ± # 14MC 0 3460 35 3340 110 # 14MC 8 5770 30 6200 90 # 13BB 34 14580 40 17260 180 # 13BB 53 20760 70 24440 250 # # 21MC 0 2330 25 1950 80 # 21MC 8 3500 35 3390 110 # 20BB 40 14685 40 17400 200 # 20BB 55 19100 70 22540 160 # # 26MC 0 3900 35 3880 130 # 26MC 8 4740 35 4980 130 # 25BB 25 15950 60 18800 140 # 25BB 35 22400 100 26200 230 # # 29MC 0 4200 15 4300 80 # 29MC 8 4770 20 5020 110 # 28BB 54 16600 60 19550 220 # 28BB 76 25400 160 29030 360 # # 33MC 0 4930 35 5270 150 # 33MC 8 5260 20 5610 40 # 32BB 25 15350 75 18170 220 # 32BB 35 19300 75 22750 240 # # 39MC 0 4730 45 4960 130 # 39MC 8 5800 20 6230 80 # 36BB 15 11650 25 13150 140 # 36BB 25 16700 90 19670 190 # #--------------------------------------- # Variables # Data variables follow that are preceded by "##" in columns one and two. # Variables list, one per line, shortname-tab-longname components (9 components: what, material, error, units, seasonality, archive, detail, method, C or N for Character or Numeric data) ## SampleID Sample ID,,,NA,,,,,C ## Time_Slice Time Slice name,,,NA,,,,,C ## lat_N latitude,,,degrees N,,Paleoceanography,, ,N ## d15Ng.rub-avg delta 15N,Globigerinoides ruber,,per mil,,Paleoceanography,average, ,N ## d15Ng.rub-avg_err2s delta 15N,Globigerinoides ruber,2sigma error,per mil,,Paleoceanography,average, ,N ## d15Ng.sac-avg delta 15N,Globigerinoides sacculifer,,per mil,,Paleoceanography,average, ,N ## d15Ng.sac-avg_err2s delta 15N,Globigerinoides sacculifer,2sigma error,per mil,,Paleoceanography,average, ,N ## d15Ng.tum-avg delta 15N,Globorotalia tumida,,per mil,,Paleoceanography,average, ,N ## d15Ng.tum-avg_err2s delta 15N,Globorotalia tumida,2sigma error,per mil,,Paleoceanography,average, ,N #------------------------ # Data # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Value: NaN SampleID Time_Slice lat_N d15Ng.rub-avg d15Ng.rub-avg_err2s d15Ng.sac-avg d15Ng.sac-avg_err2s d15Ng.tum-avg d15Ng.tum-avg_err2s 14MC: 0-8 Holocene -0.22 5.01 NaN 6.13 0.51 8.35 0.75 21MC: 0-8 Holocene 1.27 6.00 NaN 7.20 0.74 8.45 0.06 26MC: 0-8 Holocene 2.46 NaN NaN 6.99 NaN 9.17 0.50 29MC: 0-8 Holocene 2.97 6.59 NaN 6.85 0.51 8.80 0.32 33MC: 0-8 Holocene 5.20 8.68 NaN 9.57 0.31 10.83 0.23 39MC: 0-8 Holocene 6.83 11.03 NaN 11.50 0.27 13.33 0.01 13BB: 39, 45 LGP -0.22 4.90 0.07 6.21 0.70 8.29 0.35 20BB: 50, 51 LGP 1.27 5.41 0.16 6.89 0.29 8.67 0.15 25BB: 25, 30 LGP 2.46 6.76 0.34 6.91 0.80 8.41 0.80 28BB: 54, 65 LGP 2.97 6.49 1.26 7.31 0.58 9.01 1.16 32BB: 30, 31 LGP 5.20 8.26 0.64 9.02 0.59 10.66 0.55 36BB: 25, 29 LGP 6.83 9.99 0.52 11.39 1.12 13.65 0.40