# Late Holocene North Pacific Subtropical Gyre deep-sea proteinaceous coral d13C and d15N #---------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #---------------------------------------------------- # 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 # # Data lines have no # # # NOAA_Landing_Page: https://www.ncei.noaa.gov/access/paleo-search/study/18215 # 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-coral-18215.json # Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata. # # Data_Type: Corals and Sclerosponges # # Dataset_DOI: 10.25921/hxs7-5s18 # # Science_Keywords: #-------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/coral/central_pacific/guilderson2013/guilderson2013-haw-lan-noaa.txt # Data_Download_Description: NOAA Template File; Lanikai Isotope Data # #-------------------- # Contribution_Date # Date: 2015-03-12 #-------------------- # File_Last_Modified_Date # Date: 2025-08-20 #-------------------- # Title # Study_Name: Late Holocene North Pacific Subtropical Gyre deep-sea proteinaceous coral d13C and d15N #-------------------- # Investigators # Investigators: Guilderson, T.P.(https://orcid.org/0000-0001-9371-7059); McCarthy, M.D.; Dunbar, R.B.(https://orcid.org/0000-0002-9728-5609); Englebrecht, A.; Roark, E.B.(https://orcid.org/0000-0002-1742-9642) #-------------------- # Description_Notes_and_Keywords # Description: Hawaiian gold corals (Kulamanamana haumeaae; Sinninger et al. 2013, doi:10.1371/journa.pone.0052607), both living and fossil were collected using the Hawaii Undersea Research Laboratory’s DSRV Pisces IV and V. K. haumeaae is a cosmopolitan colonial zoanthid that forms tree-like structures with heights of several meters and basal attachment diameters up to a few 10s of cm. K. haumeaae have radial growth rates of <100µm-yr-1 and can attain ‘life spans’ of centuries to millennia (Roark et al. 2006, doi:10.3354/meps327001; Roark et al. 2009, doi:10.1073/pnas.0810875106). In Hawai’ian waters they are most abundant at ~450m, near the top of the regional low oxygen zone, and are directly attached to exposed, hard substrates. Radiocarbon (14C) analyses of polyps and a finely sectioned radial skeletal disk of a live harvested branch both documents incorporation of recently exported particulate organic carbon (Roark et al., 2009), while stable isotope analysis shows that polyps are ≤ 2 trophic levels relative to exported POC/PON (Roark et al. 2009, doi:10.1073/pnas.0810875106). Resu lts presented here include samples collected from the Hawai’ian archipelago in 2004 and 2007 (Big Island, Cross Seamount, Oahu in the Main Hawai'ian Islands; MHI, and French/East French Frigate Shoals and Brooks Bank in the North West Hawai'ian Islands; NWHI). Upon recovery, the external polyps and tissue were removed using a seawater hose from all live-collected individuals. After removing the tissue layer, the skeletons (live collected and sub-fossil) were washed with seawater followed by fresh water and allowed to air dry on deck. Stumps were cut into ~0.7-cm thick cross-section disks taken close to the basal attachment. In a small number of cases additional disks were also taken higher on the branch (or stump). Sampling was done by microdrilling center (inner) and outer samples from radial transects using a 1.8 mm spherical carbide bur. Depending on the size of the cross-section disk sub-samples between the inner and outer samples were also taken. Milled samples were decarbonated using 1N HCl at 90C, rinsed three-times with milliQ water and dried overnight on a heating block. Sub-samples were transferred to tin boats and the mass determined. Carbon and nitrogen stable isotope analyses were made via continuous-flow IRMS using a Carlo-Erba elemental analyzer connected to an Optima IRMS in the UCSC Light Isotope Facility. Results are reported in conventional per mil notation relative to V-PDB (δ13C) and air (δ15N). Reproducibility of the isotope results is ± 0.12‰ and ±0.06 (1-sd) based on reproducibility of standards (acetanilide, n=20) and replicate analyses (n=29) of coral samples for δ13C and δ15N, respectively. C:N ratios determined during analysis were ±0.15 (1-sd). Radiocarbon sub-samples were first converted to CO2 via sealed-tube combustion, and the resulting purified CO2 reduced to graphite in the presence of an iron catalyst. Individual graphite-catalyst mixtures were pressed into aluminum target holders and analyzed via accelerator mass spectrometry. Results include a background subtraction based on similarly prepared 14C-free coal and wood, sample specific δ13C corrections, and are reported as Fmodern, D14C, and conventional radiocarbon years as per Stuiver and Polach (1977, doi:10.1017/S0033822200003672), with one-sigma uncertainties. We note that in the published version of these data that IntCal 09 (Reimer et al. 2009, doi:10.1017/S0033822200034202) was used as the 14C-calendar calibration curve. Since that time IntCal 13 (Reimer et al. 2013, doi:10.2458/azu_js_rc.55.16947) has been released. We strongly recommend that the users of these data use the appropriate, most recent and up-to-date IntCal calibration data product to convert radiocarbon years to calibrated ages. Being of marine origin, the data require a site specific correction for the marine reservoir effect. Until further empirical observations are available, we recommend for Hawai’ian samples, and based on a ~40 year average of reef-building hermatypic coral data, a DELTA_R of -28±4 to be used (Druffel et al. 2001, doi:10.1017/S0033822200031593). #-------------------- # Publication # Authors: Guilderson, T.P., M.D. McCarthy, R.B. Dunbar, A. Englebrecht, and E.B. Roark # Journal_Name: Biogeosciences # Published_Title: Late Holocene Variations in Pacific Surface Circulation and Biogeochemistry Inferred From Proteinaceous Deep-Sea Corals # Published_Date_or_Year: 2013 # Volume: 10 # Issue: # Pages: 6019-6028 # Report_Number: # DOI: 10.5194/bg-10-6019-2013 # Full_Citation: # Abstract: δ15N and δ13C data obtained from samples of proteinaceous deep-sea corals collected from the North Pacific Subtropical Gyre (Hawaiian Archipelago) and the central equatorial Pacific (Line Islands) document multidecadal to century-scale variability in the isotopic composition of surface-produced particulate organic matter exported to the deep sea. Comparison of the δ13C data, where Line Islands samples are 0.6‰ more positive than the Hawaiian samples, supports the contention that the North Pacific Subtropical Gyre is more efficient than the tropical upwelling system at trapping and/or recycling nutrients within the mixed layer. δ15N values from the Line Islands samples are also more positive than those from the central gyre, and within the Hawaiian samples there is a gradient with more positive δ15N values in samples from the main Hawaiian Islands versus the French Frigate Shoals in the Northwestern Hawaiian Islands. The gradient in the Hawaiian samples likely reflects the relative importance of algal acquisition of metabolic N via dissolved seawater nitrate uptake versus nitrogen fixation. The Hawaiian sample set also exhibits a strong decrease in δ15N values from the mid-Holocene to present. We hypothesize that this decrease is most likely the result of decreasing trade winds, and possibly a commensurate decrease in entrainment of more positive δ15N-NO3 subthermocline water masses. #-------------------- # Funding_Agency # Funding_Agency_Name: US National Science Foundation # Grant: OCE-0551792, OCE-0551481, OCE-1061689 #-------------------- # Funding_Agency # Funding_Agency_Name: US National Oceanic and Atmospheric Administration (NOAA) # Grant: NA05OAR4310021 and NA05OAR4310017 #-------------------- # Funding_Agency # Funding_Agency_Name: US Department of Energy # Grant: contract W-7405-Eng-48 and DE-AC52-07NA27344 #-------------------- # Funding_Agency # Funding_Agency_Name: National Geographic Society # Grant: 7717-04 #-------------------- # Funding_Agency # Funding_Agency_Name: NOAA/National Undersea Research Program # Grant: #-------------------- # Site_Information # Site_Name: Lanikai # Location: Hawaiian Islands # Northernmost_Latitude: 21.39 # Southernmost_Latitude: 21.39 # Easternmost_Longitude: -157.63 # Westernmost_Longitude: -157.63 # Elevation_m: #-------------------- # Data_Collection # Collection_Name: Hawaii-Lanikai isotopes Guilderson13 # First_Year: 5150 # Last_Year: 945 # Time_Unit: radiocarbon year before present # Core_Length_m: # Parameter_Keywords: chemistry, carbon isotopes # Notes: #-------------------- # 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) # ## SampleID sample identification,,,,,corals and sclerosponges,,,N, ## d13Cgerard delta 13C,Kulamanamana haumeaae,,per mil VPDB,,corals and sclerosponges,raw,isotope ratio mass spectrometry,N, ## d15Ngerard delta 15N,Kulamanamana haumeaae,,per mil AIR,,corals and sclerosponges,raw,isotope ratio mass spectrometry,N, ## C:N carbon/nitrogen,Kulamanamana haumeaae,,dimensionless,,corals and sclerosponges,raw,elemental analysis,N, ## FracMod 14C fraction modern,Kulamanamana haumeaae,,dimensionless,,corals and sclerosponges,corrected,accelerator mass spectrometry,N,background subtraction; corrected for sample-specific delta 13C; reported as conventional radiocarbon years per Stuiver and Polach (1977) ## FracMod_err 14C fraction modern,Kulamanamana haumeaae,one standard deviation,dimensionless,,corals and sclerosponges,corrected,accelerator mass spectrometry,N,background subtraction; corrected for sample-specific delta 13C; reported as conventional radiocarbon years per Stuiver and Polach (1977) ## D14Cgerard Delta 14C,Kulamanamana haumeaae,,per mil NBS oxalic acid,,corals and sclerosponges,corrected,accelerator mass spectrometry,N,background subtraction; corrected for sample-specific delta 13C; reported as conventional radiocarbon years per Stuiver and Polach (1977) ## D14Cgerard_err Delta 14C,Kulamanamana haumeaae,one standard deviation,per mil NBS oxalic acid,,corals and sclerosponges,corrected,accelerator mass spectrometry,N,background subtraction; corrected for sample-specific delta 13C; reported as conventional radiocarbon years per Stuiver and Polach (1977) ## age14C age,,,radiocarbon year before present,,corals and sclerosponges,,,N, ## age14C_err age,,one standard deviation,radiocarbon year,,corals and sclerosponges,,,N, #-------------------- # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: SampleID d13Cgerard d15Ngerard C:N FracMod FracMod_err D14Cgerard D14Cgerard_err age14C age14C_err 139381 -16.3 10.82 2.87 0.889 0.0045 -111 4.5 945 45 139375 -15.84 11.47 2.81 0.8483 0.0029 -151.7 2.9 1320 30 139376 -16.26 11 2.86 0.8342 0.003 -165.8 3 1455 30 139377 -16.16 11.18 2.84 0.826 0.0032 -174 3.2 1535 35 139382 -16.43 10.14 2.79 0.8148 0.0028 -185.2 2.8 1645 30 139383 -16.96 9.14 2.78 0.8046 0.0028 -195.4 2.8 1745 30 139378 -15.79 11.02 2.85 0.7624 0.0026 -237.6 2.6 2180 30 139379 -16.12 10.38 2.85 0.7378 0.0022 -262.2 2.2 2445 25 139372 -15.5 11.43 2.86 0.7335 0.0022 -266.5 2.2 2490 25 139380 -16.79 9.82 2.83 0.7141 0.0022 -285.9 2.2 2705 25 139373 -16.37 11.56 2.86 0.666 0.0025 -334 2.5 3265 35 139384 -16.09 11.37 2.84 0.6612 0.002 -338.8 2 3325 25 126091 -15.72 11.11 3.05 0.6553 0.0021 -344.7 2.1 3395 30 140886 -15.68 11.23 2.84 0.645 0.0022 -355 2.2 3520 30 138229 -15.48 11.16 2.97 0.6412 0.0021 -358.8 2.1 3570 30 139385 -16.47 11.12 2.86 0.6072 0.0019 -392.8 1.9 4010 30 139374 -16.96 10.39 2.92 0.602 0.0024 -398 2.4 4075 35 126092 -16.26 11.18 2.94 0.5931 0.0018 -406.9 1.8 4195 25 139386 -16.69 11.28 2.92 0.568 0.002 -432 2 4545 30 140885 -16.78 10.73 2.84 0.5648 0.0017 -435.2 1.7 4590 25 126093 -16.8 10.58 2.2 0.5519 0.002 -448.1 2 4775 30 138230 -16.84 10.76 3.09 0.5484 0.0017 -451.6 1.7 4825 25 126094 -16.73 10.96 2.91 0.5298 0.0016 -470.2 1.6 5105 25 126095 -16.71 11.14 2.64 0.5268 0.0017 -473.2 1.7 5150 30