# Indus Fan Miocene Plant Biomarker and Microfossil Data #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #----------------------------------------------------------------------- # Template Version 3.0 # Encoding: UTF-8 # NOTE: Please cite Publication, and Online_Resource and date accessed when using these data. # If there is no publication information, please cite Investigators, Title, and Online_Resource and date accessed. # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/28792 # Description: NOAA Landing Page # Online_Resource: https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/feakins2020/feakins2020.txt # Description: NOAA location of the template # # Original_Source_URL: # Description: # # Description/Documentation lines begin with # # Data lines have no # # # Archive: Paleoceanography # # Dataset DOI: # # Parameter_Keywords: biomarkers, geochemistry, carbon isotopes, nitrogen isotopes #--------------------------------------- # Contribution_Date # Date: 2020-03-26 #--------------------------------------- # File_Last_Modified_Date # Date: 2024-06-26 #--------------------------------------- # Title # Study_Name: Indus Fan Miocene Plant Biomarker and Microfossil Data #--------------------------------------- # Investigators # Investigators: Feakins, S.J.; Liddy, H.M.; Tauxe, L.; Galy, V.; Feng, X.; Tierney, J.E.; Miao, Y.; Warny, S. #--------------------------------------- # Description_Notes_and_Keywords # Description: Biomarker and isotope data from sediments collected in the Indus Fan core U1457 for 10-5 million years BP. LAST UPDATE 6/26/2024: Added IODP sample identification values to the data table. # Provided Keywords: International Ocean Discovery Program; Expedition 355; Site U1457; biomarkers #--------------------------------------- # Publication # Authors: Sarah J. Feakins, Hannah M. Liddy, Lisa Tauxe, Valier Galy, Xiaojuan Feng, Jessica E. Tierney, Yunfa Miao, Sophie Warny # Published_Date_or_Year: 2020-06-01 # Published_Title: Miocene C4 Grassland Expansion as Recorded by the Indus Fan # Journal_Name: Paleoceanography and Paleoclimatology # Volume: 35 # Edition: e2020PA003856 # Issue: 6 # Pages: # Report Number: # DOI: 10.1029/2020PA003856 # Online_Resource: https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020PA003856 # Full_Citation: # Abstract: In the late Miocene, grasslands spread across the forested floodplains of the Himalayan foreland, but the causes of the ecological transition are still debated. Recent seafloor drilling by the International Ocean Discovery Program (IODP) provides an opportunity to study the transition across a larger region as archived in the Indus submarine fan. We present a multiproxy study of past vegetation change based on analyses of the carbon isotopic composition (d13C) of bulk organic carbon, plant wax n-alkanes and n-alkanoic acids, and quantification of lignin phenols, charcoal, and pollen. We analyze the hydrogen isotopic composition (dD) of plant wax to reconstruct precipitation dD. We use the Branched and Isoprenoid Tetraether (BIT) index to diagnose shifts between terrestrial versus marine lipid inputs between turbidite and hemipelagic sediments. We reconstruct ocean temperatures using the TEX86 index only where marine lipids dominate. We find evidence for the late Miocene grassland expansion in both facies, confirming this was a regional ecosystem transformation. Turbidites contain dominantly terrestrial matter from the Indus catchment (D-depleted plant wax), delivered via fluvial transport as shown by the presence of lignin. In contrast, hemipelagic sediments lack lignin and bear D-enriched plant wax consistent with wind-blown inputs from the Indian peninsula; these show a 7.4-7.2 Ma expansion of C4 grasslands on the Indian subcontinent. Within each facies, we find no clear change in dD values across the late Miocene C4 expansion, implying consistent distillation of rainfall by monsoon dynamics. Yet, a cooling in the Arabian Sea is coincident with the C4 expansion. #--------------------------------------- # Publication # Authors: Lisa Tauxe, Sarah J. Feakins # Published_Date_or_Year: 2020-07-01 # Published_Title: A Reassessment of the Chronostratigraphy of Late Miocene C3-C4 Transitions # Journal_Name: Paleoceanography and Paleoclimatology # Volume: 35 # Edition: e2020PA003857 # Issue: 7 # Pages: # Report_Number: # DOI: 10.1029/2020PA003857 # Online_Resource: https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020PA003857 # Full_Citation: # Abstract: Combining magnetostratigraphic and carbon isotopic data for the late Miocene can provide a temporal framework for an isotopic shift first documented in soil carbonate nodules of northern Pakistan. The shift has been interpreted as a change in vegetation from trees and shrubs (using the C3 photosynthetic pathway) to grassland (using the C4 pathway). The cause of the event has been hotly debated and its timing is close to a shift in carbon isotopes in the marine realm. Further understanding depends critically on chronology. Unfortunately, temporal calibration of the various records published over decades relied on different time scales. To address the lack of a consistent chronology, we have reevaluated the constraints for the carbon isotopic shifts recorded from the Indian subcontinent. These show a diachronous transition ranging in age from about 7.8 Ma in Pakistan to as late at 6 Ma in Nepal. The record from IODP Expedition 355 Site U1457, drilled on the Indus fan shows that the transition in peninsular India began at about 7.2 Ma. Similar records from the African margin saw an earlier shift to C4 dominance starting around 10 Ma and those from Australia and South America transitioned later, during the Pliocene. The diachroneity around the globe does not invalidate pCO2 as a driver, but is consistent with it being one of several drivers of the global C4 expansion. #------------------ # Funding_Agency # Funding_Agency_Name: US National Science Foundation # Grant: OCE 14-50528, EAR 1547263 #--------------------------------------- # Site Information # Site_Name: IODP Site U1457 # Location: Ocean>Indian Ocean # Country: # Northernmost_Latitude: 17.17639 # Southernmost_Latitude: 17.17639 # Easternmost_Longitude: 67.93917 # Westernmost_Longitude: 67.93917 # Elevation: -3523 #--------------------------------------- # Data_Collection # Collection_Name: Feakins2020 # First_Year: 10370000 # Last_Year: 5630000 # Time_Unit: cal yr BP # Core_Length: # Notes: #--------------------------------------- # Chronology_Information # Chronology: # # site IODP Site # hole IODP Hole # core IODP core # type IODP type # sect IODP core section # w working half of core # top top offset (cm) within section # bottom bottom offset (cm) within sectio # depth_m in ccsf scale in meters # age_ma on the GPTS2012 timescale # alt_age_ma alternative age based on Indian Ocean calibration # label numbering scheme from Routledge et al., 2019 # type datum type CN = nannofossil, PF = foraminifera, MR = magnetostratigraph # event datum, bottom (B) or top (T) of a species, or a named magnetic timeperiod. # site hole core type sect cc top bottom depth_m age_ma alt_age_ma label type Event # U1457 C 37 R 6 cc 20 25 539.65 5.59 NaN 28 CN T Discoaster quinqueramus # U1457 C 35 R 6 cc 0 5 526.64 5.92 NaN 29 PF T Globoquadrina dehiscens # U1457 C 44 R 5 NaN 64 NaN 610.36 5.94 NaN 30 CN T Nicklithus amplificus # U1457 C 46 R 1 NaN 68 NaN 624.23 6.733 NaN 32 MR C3Ar # U1457 C 45 R 2 NaN 24 NaN 615.5 6.6 NaN 33 PF B Pulleniatina primalis # U1457 C 46 R 4 NaN 40 NaN 628.34 6.91 6.7 35 CN B Nicklithus amplificus # U1457 C 48 R 1 NaN 9 NaN 643.04 7.285 7.29 36 MR C3Br.2r # U1457 C 48 R 2 NaN 60 NaN 645.05 7.3 7.2 38 CN B Amaurolithus spp. # U1457 C 50 R 1 NaN 57 NaN 662.92 7.454 NaN 39 MR C3Br.2n # U1457 C 51 R 2 NaN 92 NaN 674.47 7.642 NaN 41 MR C4n.1r # U1457 C 67 R 6 cc 0 5 832.85 8.12 NaN 42 CN B Discoaster quinqueramus # U1457 C 68 R 6 cc 9 14 845.62 8.68 NaN 43 CN T Minylitha convallis # U1457 C 69 R 6 cc 25 30 856.5 9.21 NaN 44 CN T Discoaster bollii # U1457 C 70 R 6 cc 18 23 864.64 9.69 NaN 45 CN T Catinaster coalitus # U1457 C 70 R 6 NaN 35 NaN 864.18 9.79 NaN 46 MR C5n # U1457 C 72 R 6 cc 23 28 885.02 9.83 NaN 47 PF B Neogloboquadrina acostaensis # U1457 C 84 R 6 cc 10 15 1001.08 10.4 NaN 48 CN B Discoaster bellus # U1457 C 84 R 6 cc 10 15 1001.08 10.89 NaN 49 CN B Catinaster coalitus # #--------------------------------------- # 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) # ## site sample identification,,,,,paleoceanography;climate reconstructions,,,C,International Ocean Discovery Program Site ## hole sample identification,,,,,paleoceanography;climate reconstructions,,,C,International Ocean Discovery Program Hole ## core sample identification,,,,,paleoceanography;climate reconstructions,,,N,International Ocean Discovery Program Core ## type sample identification,,,,,paleoceanography;climate reconstructions,,,C,International Ocean Discovery Program drilling type ## sect sample identification,,,,,paleoceanography;climate reconstructions,,,N,International Ocean Discovery Program Section ## w sample identification,,,,,paleoceanography;climate reconstructions,,,C,working half of core ## top sample identification,,,,,paleoceanography;climate reconstructions,,,N,top offset (cm) within section ## bottom sample identification,,,,,paleoceanography;climate reconstructions,,,N,bottom offset (cm) within section ## code sample identification,,,,,paleoceanography;climate reconstructions,,,C,requestor code ## IODP_ID sample identification,,,,,paleoceanography;climate reconstructions,,,C,International Ocean Discovery Program sample identifier ## depth_m depth,,,meter,,paleoceanography;climate reconstructions,,,N,Depth CCSF scale (meters) below sea floor ## age_ma age,,,million years ago,,paleoceanography;climate reconstructions,,,N,on the GPTS2012 timescale ## d13Calk29 delta 13C,C29 n-alkane,,per mil VPDB,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## d13Calk31 delta 13C,C31 n-alkane,,per mil VPDB,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## d13Calk33 delta 13C,C33 n-alkane,,per mil VPDB,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## d13Calk29s delta 13C,C29 n-alkane,one standard deviation,per mil VPDB,,paleoceanography,,isotope ratio mass spectrometry,N, ## d13Calk31s delta 13C,C31 n-alkane,one standard deviation,per mil VPDB,,paleoceanography,,isotope ratio mass spectrometry,N, ## d13Calk33s delta 13C,C33 n-alkane,one standard deviation,per mil VPDB,,paleoceanography,,isotope ratio mass spectrometry,N, ## d13Calkn number of samples,,,count,,paleoceanography,,,N,number of plant wax alkane replicates ## d13Cacid28 delta 13C,C28 n-alkanoic acid,,per mil VPDB,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## d13Cacid30 delta 13C,C30 n-alkanoic acid,,per mil VPDB,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## d13Cacid32 delta 13C,C32 n-alkanoic acid,,per mil VPDB,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## d13Cacid28s delta 13C,C28 n-alkanoic acid,one standard deviation,per mil VPDB,,paleoceanography,,isotope ratio mass spectrometry,N, ## d13Cacid30s delta 13C,C30 n-alkanoic acid,one standard deviation,per mil VPDB,,paleoceanography,,isotope ratio mass spectrometry,N, ## d13Cacid32s delta 13C,C32 n-alkanoic acid,one standard deviation,per mil VPDB,,paleoceanography,,isotope ratio mass spectrometry,N, ## d13Cacidn number of samples,,,count,,paleoceanography,,,N,number of plant wax alkanoic acid replicates ## d13C_OC delta 13C,organic matter,,per mil VPDB,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## d13C_oc_s delta 13C,organic matter,one standard deviation,per mil VPDB,,paleoceanography,,isotope ratio mass spectrometry,N, ## d13C_oc_n number of samples,,,count,,paleoceanography,,,N,number of organic carbon replicates ## OC organic carbon,sediment,,percent,,paleoceanography,averaged,elemental analyzer,N, ## OCs organic carbon,sediment,one standard deviation,percent,,paleoceanography,,elemental analyzer,N, ## d15N delta 15N,sediment,,per mil,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## d15N_s delta 15N,sediment,one standard deviation,per mil,,paleoceanography,,isotope ratio mass spectrometry,N, ## C_N organic carbon/nitrogen,sediment,,fraction,,paleoceanography,,elemental analyzer,N, ## dD_29alk delta 2H,C29 n-alkane,,per mil VSMOW,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## dD_31alk delta 2H,C31 n-alkane,,per mil VSMOW,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## dD_33alk delta 2H,C33 n-alkane,,per mil VSMOW,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## dD_29alks delta 2H,C29 n-alkane,one standard deviation,per mil VSMOW,,paleoceanography,,isotope ratio mass spectrometry,N, ## dD_31alks delta 2H,C31 n-alkane,one standard deviation,per mil VSMOW,,paleoceanography,,isotope ratio mass spectrometry,N, ## dD_33alks delta 2H,C33 n-alkane,one standard deviation,per mil VSMOW,,paleoceanography,,isotope ratio mass spectrometry,N, ## dD_28acid delta 2H,C28 n-alkanoic acid,,per mil VSMOW,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## dD_30acid delta 2H,C30 n-alkanoic acid,,per mil VSMOW,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## dD_28acids delta 2H,C28 n-alkanoic acid,one standard deviation,per mil VSMOW,,paleoceanography,,isotope ratio mass spectrometry,N, ## dD_30acids delta 2H,C30 n-alkanoic acid,one standard deviation,per mil VSMOW,,paleoceanography,,isotope ratio mass spectrometry,N, ## 87Sr_86Sr 87Sr/86Sr,sediment,,dimensionless,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## 143Nd_144Nd 143Nd/144Nd,,,dimensionless,,paleoceanography,averaged,isotope ratio mass spectrometry,N, ## eNd epsilon neodymium,,,epsilon unit,,paleoceanography,,isotope ratio mass spectrometry,N, ## BIT_H_T notes,,,,,paleoceanography,,,C,assignment of hemipelagic (H) or turbidic (T) facies based on BIT index with a 0.4 cuttoff H<0.4 and T>0.4 ## BIT branched and isoprenoid tetraether index,sediment,,dimensionless,,paleoceanography,,mass spectrometry,N, ## isoGDGTs_ngg branched glycerol dialkyl glycerol tetraether,sediment,,parts per billion,,paleoceanography,,mass spectrometry,N, ## brGDGTs_ngg isoprenoid glycerol dialkyl glycerol tetraether,sediment,,parts per billion,,paleoceanography,,mass spectrometry,N, ## TEX86 tetraether index of 86 carbon atoms,sediment,,dimensionless,,paleoceanography; climate reconstructions,,mass spectrometry,N, ## Bay_l sea water temperature,glycerol dialkyl glycerol tetraether index,two standard deviations lower bound,degree Celsius,,paleoceanography;climate reconstructions,,,N,reconstructed using TEX86 and Bayspar ## Bay_m sea water temperature,glycerol dialkyl glycerol tetraether index,,degree Celsius,,paleoceanography;climate reconstructions,,,N,reconstructed using TEX86 and Bayspar ## Bay_h sea water temperature,glycerol dialkyl glycerol tetraether index,two standard deviations upper bound,degree Celsius,,paleoceanography;climate reconstructions,,,N,reconstructed using TEX86 and Bayspar ## Bay_mmask sea water temperature,glycerol dialkyl glycerol tetraether index,,degree Celsius,,paleoceanography;climate reconstructions,,,N,masked to show only where BIT>0.4; reconstructed using TEX86 and Bayspar ## V phenol,sediment,,parts per million,,paleoceanography,,mass spectrometry,N,Total Vanillyl phenols ## C phenol,sediment,,parts per million,,paleoceanography,,mass spectrometry,N,Total Coniferyl phenols ## S phenol,sediment,,parts per million,,paleoceanography,,mass spectrometry,N,Total Syringyl phenols ## VSC phenol,sediment,,parts per million,,paleoceanography,,mass spectrometry,N,Total Vanillyl Syringyl and Cinnamyl phenol mass (milligrams) per mass wood (grams) ## P phenol,,,parts per million,,paleoceanography,,mass spectrometry,N,Total P phenols ## P/(V+S) phenol,,,dimensionless,,paleoceanography,,mass spectrometry,N,Ratio of P phenols to Vanillyl plus Syringyl phenols ## Cutin cutin,sediment,,parts per million,,paleoceanography,,mass spectrometry,N,Cutin acids ## S_V phenol,sediment,,,,paleoceanography,,mass spectrometry,N,Total Syringyl to Vanillyl phenol ratio ## C_V phenol,sediment,,,,paleoceanography,,mass spectrometry,N,Total Coniferyl to Vanillyl phenol ratio ## Vd_Vl organic compound index,sediment,,,,paleoceanography,,mass spectrometry,N,Total acid to aldehyde group ratio for Vanillyl phenols ## Sd_Sl organic compound index,sediment,,,,paleoceanography,,mass spectrometry,N,Total acid to aldehyde group ratio for Syringyl phenols ## VSC_OC phenol,,,parts per million,,paleoceanography,,mass spectrometry,N,Total Vanillyl Syringyl and Coniferyl phenol mass in micrograms per gram OC ## Cutin_OC cutin,,,parts per million,,paleoceanography,,mass spectrometry,N,Cutin mass micrograms per g OC ## Cphenol_OC phenol,,,parts per million,,paleoceanography,,mass spectrometry,N,Coniferyl phenol mass micrograms per g OC ## char_total_g charcoal,sediment,,count per gram,,paleoceanography,,,N,abundance count per gram sediment ## char_total_OC charcoal,,,count per gram,,paleoceanography,,,N,abundance count per gram OC ## char_L_R charcoal,sediment,,dimensionless,,paleoceanography,,,N,ratio of long/round charcoal ## char_big_small charcoal,sediment,,dimensionless,,paleoceanography,,,N,ratio of big>small charcoal ## poll_amar pollen,sediment,,fraction,,paleoceanography,,,N,Amaranthaceae pollen fraction of terrestrial pollen ## poll_grass pollen,sediment,,fraction,,paleoceanography,,,N,Grass pollen fraction of terrestrial pollen ## poll_terr_mar pollen,sediment,,dimensionless,,paleoceanography,,,N,terrestrial/marine palynomorphs ## poll_NAP_AP pollen,sediment,,dimensionless,,paleoceanography,,,N,non-arboreal/arboreal pollen ## poll_insitu_reworked pollen,sediment,,dimensionless,,paleoceanography,,,N,insitu/reworked pollen ## kab16 C16 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab17 C17 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab18 C18 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab19 C19 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab20 C20 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab21 C21 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab22 C22 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab23 C23 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab24 C24 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab25 C25 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab26 C26 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab27 C27 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab28 C28 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab29 C29 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab30 C30 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab31 C31 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab32 C32 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab33 C33 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab34 C34 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## kab35 C35 n-alkane,sediment,,parts per billion,,paleoceanography,,,N, ## aab16 C16 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab17 C17 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab18 C18 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab19 C19 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab20 C20 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab21 C21 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab22 C22 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab23 C23 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab24 C24 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab25 C25 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab26 C26 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab27 C27 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab28 C28 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab29 C29 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab30 C30 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab31 C31 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab32 C32 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab33 C33 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## aab34 C34 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N, ## k25-35 n-alkane,sediment,,parts per billion,,paleoceanography,,,N,Summed C25:35 n-alkane ## a24-34 n-alkanoic acid,sediment,,parts per billion,,paleoceanography,,,N,Summed C24-34 n-alkanoic acid ## k/a organic compound index,sediment,,dimensionless,,paleoceanography,,,N,alkane:acid ratio ## kACL average chain length,n-alkane,,dimensionless,,paleoceanography,,,N,C24-35 ## kCPI carbon preference index,n-alkane,,dimensionless,,paleoceanography,,,N,C24-35 ## aACL average chain length,n-alkanoic acid,,dimensionless,,paleoceanography,,,N,C24-34 ## aCPI carbon preference index,n-alkane,,dimensionless,,paleoceanography,,,N,C23-34 # #------------------------ # Data # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: 999999 site hole core type sect w top bottom code IODP_ID depth_m age_ma d13Calk29 d13Calk31 d13Calk33 d13Calk29s d13Calk31s d13Calk33s d13Calkn d13Cacid28 d13Cacid30 d13Cacid32 d13Cacid28s d13Cacid30s d13Cacid32s d13Cacidn d13C_OC d13C_oc_s d13C_oc_n OC OCs d15N d15Ns C_N dDalk29 dDalk31 dDalk33 dDalk29s dDalk31s dDalk33s dDacid28 dDacid30 dDacid28s dDacid30s 87Sr_86Sr 143Nd_144Nd eNd BIT_H_T BIT isoGDGTs_ngg brGDGTs_ngg TEX86 Bay_l Bay_m Bay_h Bay_mmask V C S VSC P P/(V+S) Cutin S/V C/V Vd/Vl Sd/Sl VSC_OC Cutin_OC Cphenol_OC char_total_g char_total_OC char_L_R char_big_small poll_amar poll_grass poll_terr_mar poll_NAP_AP poll_insitu_reworked kab16 kab17 kab18 kab19 kab20 kab21 kab22 kab23 kab24 kab25 kab26 kab27 kab28 kab29 kab30 kab31 kab32 kab33 kab34 kab35 aab16 aab17 aab18 aab19 aab20 aab21 aab22 aab23 aab24 aab25 aab26 aab27 aab28 aab29 aab30 aab31 aab32 aab33 aab34 k25-35 a24-34 k/a kACL kCPI aACL aCPI U1457 C 34 R 2 W 140 150 SC 355-U1457C-34R-2-IW(140-150)-SC 510.1 999999 -26.7 -26.6 -25.7 0.5 0.4 0.3 3 999999 -21.7 -23.1 999999 0.2 0.4 2 -19.2 0.0 3 0.76 0.02 7.7 0.2 8.1 999999 999999 999999 999999 999999 999999 999999 999999 999999 999999 0.717 0.512 -7.78 H 0.062 5775 212 0.670 20 23 27 23 999999 999999 999999 999999 999999 999999 999999 999999 999999 999999 999999 999999 999999 999999 6895 902689 0.3 0.2 0.05 0.65 75 85 100 12 3 8 6 7 15 14 37 32 86 59 215 70 295 73 319 35 183 10 46 1004 30 840 0 96 72 1210 234 2435 463 2742 647 2090 445 801 161 358 83 360 1389 10585 0.13 29 4.11 27.0 4.3 U1457 C 35 R 6 W 140 150 SC 355-U1457C-35R-6-IW(140-150)-SC 525.7 999999 -27.0 -26.8 -25.6 0.3 1.1 0.8 3 -22.5 -21.8 -22.8 0.0 0.0 0.0 3 -17.3 0.1 3 0.52 0.00 6.7 0.4 7.3 999999 999999 999999 999999 999999 999999 999999 999999 999999 999999 0.720 0.512 -8.97 H 0.051 1777 54 0.701 21 25 28 25 0.83 0.03 0.33 1.19 0.97 0.84 0.10 0.39 0.03 0.35 0.44 228 19 5 999999 999999 999999 999999 999999 999999 999999 999999 999999 2 1 7 3 4 5 9 11 10 26 14 43 17 63 19 70 12 46 4 23 273 5 256 4 16 4 67 0 206 46 217 35 94 24 43 0 37 0 0 338 701 0.48 30 3.58 26.3 5.7 U1457 C 37 R 1 W 140 150 SC 355-U1457C-37R-1-IW(140-150)-SC 537.7 999999 -26.0 -27.2 -26.5 0.0 0.1 0.0 3 -21.2 -20.3 -22.1 0.5 0.2 0.0 2 -20.0 0.1 2 0.31 0.01 5.1 0.3 6.4 999999 999999 999999 999999 999999 999999 -184 999999 1 999999 0.721 0.512 -10.98 T 0.411 401 147 0.614 17 21 24 999999 6.54 0.16 2.95 9.65 2.19 0.23 0.05 0.45 0.02 0.45 0.38 3151 16 52 3925 1281950 0.8 0.7 999999 999999 999999 999999 999999 1 1 4 3 4 7 8 17 13 46 18 75 25 120 20 126 13 71 5 21 131 3 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