cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.218128
title: (Table T2) Stable oxygen and carbon isotope ratios of the benthic and planktonic foraminifera, carbonate content, and percent fragmentation of planktonic foraminifers for ODP Site 177-1089 in the Southern Ocean

description: Depth is modified composite depth (mcd). Stable isotope analyses were conducted at the University of Florida (UF) Hole C, and Scripps Institution of Oceanography (SIO) Hole A and B. Carbonate contenet and fragmentation determined at the Unifersity of Florida (UF).
DOI: 10.1594/pangaea.626591
title: (Table 3) Isotope data from nine sites on a north-south transect from the Congo Fan (4°S) to the Cape Basin (30°) representing the glacial stage MIS 2

description: calc. % C4: Estimates are based on 5% C4 plants in the Congo area and a d13C value of C4 plants of -21 per mil.
DOI: 10.1594/pangaea.140004
title: Stable isotopes on Globigerinoides ruber in sediment core GeoB2819-1
DOI: 10.1594/pangaea.757371
title: (Figure 2) Plant wax n-alkane carbon isotopes for tropical western Africa for samples from the Last Glacial Maximum, Heinrich Stadial 1, the mid-Holocene and the late Holocene
DOI: 10.1594/pangaea.803644
title: (Table 4) Stable deuterium and carbon isotope ratios of selected methane samples from ODP Leg 164 sites
DOI: 10.1594/pangaea.965924
title: Planktonic d18O and Mg/Ca ratios and sea seawater temperature reconstructions of sediment core SK218-1

description: Radiocarbon ages measured on planktonic foraminifera Globigerinoides ruber alba and stable oxygen isotope and Mg/Ca ratios measured on the same species. For Mg/Ca and d18O measurements shells from the 250-350 micrometer size fraction were used. Mg/Ca measurements are based on 30-40 shells that were cleaned using an oxidative cleaning step. Seawater temperature estimates were calculated using the T = ln(Mg/Ca/0.09)/0.38 following 10.1029/2001GC000200.
DOI: 10.1594/pangaea.779363
title: (Table 3) Stable carbon and oxygen isotope composition of live and dead benthic foraminifera in surface sediments at NEW-Polynya stations

description: -2,55 m depth is mean of bottom water (bw) samples between -5 and -0.1 m. -0.05 m depth is mean of MUC bottom water sample.
DOI: 10.1594/pangaea.757219
title: (Table 2) Sea surface reconstruction for ODP Leg 167 sites

description: Sediment depth is composite depth (mcd), except Hole 167-1017B 16.52 to 28.92 where seiment depth is revised composite depth (rmcd).
DOI: 10.1594/pangaea.716660
title: (Table 1) B/Ca and d11B ratios of foraminifera from marine surface sediments

description: All environmental parameters taken from nearby GLODAP site
DOI: 10.1594/pangaea.54702
title: Stable isotopes of sediment core GeoB2019-1
DOI: 10.1594/pangaea.742740
title: (Table T1) Stable carbon and oxygen isotope ratios of Globigerinoides ruber from ODP Site 184-1146

description: Of the 1224 analyses, 307 were on C. wuellerstorfi and 917 on U. peregrina. A total of 135 samples were measured for both species. Based on the median difference between these 135 paired analyses, we convert C. wuellerstorfi to values consistent with U. peregrina by subtracting 0.74 from the 13C values (making them lighter) and adding 0.64 to the 18O values (making them heavier). All data reported are relative to U. peregrina.
DOI: 10.15468/dl.2z7ys4
title: Occurrence Download

description: A dataset containing 1956 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Rumex stenophyllus Ledeb.)",
 "BasisOfRecord is one of (Specimen, Human Observation, Observation, Living Specimen, Machine Observation, Literature Occurrence)",
 "Geometry POLYGON((-180 -90,180 -90,180 90,-180 90,-180 -90))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "Year is greater than or equal to 1945"
 ]
}

 The dataset includes 1956 records from 140 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0003668-250310093411724/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.711134
title: (Table 1) Rock description and nitrogen concentrations and isotopic compositions of altered oceanic crust samples from ODP Hole 185-801C

description: The basement at Site 801 is divided into 4 intervals (the alkaline basalt sills and 3 MORB sections) according to the geochemical characterization of more than 100 communal samples (Plank et al., 2000; http://www-odp.tamu.edu/publications/185_IR/185ir.htm). For each interval, one composite was made for submarine extrusives (FLO) and clastic rocks (VCL) by combing proportional communal samples. FLO and VCL are then combined into the MIX composite in a ratio of 30-70%. The SUPER composite was made for the entire MORB interval by combing the 3 MORB composites. The SED composite was made for the intercalated sediments in the upper 230 m of the basement (mostly in Sequences I, III, and IV, see descriptions by Plank et al. (2000); http://www-odp.tamu.edu/publications/185_IR/185ir.htm; Alt (2003); doi:10.1029/2002GC000400).
DOI: 10.1594/pangaea.775315
title: (Table AT1) TOC concentrations and δ¹³C of sediments from ODP Holes 170-1040C and 205-1254A decalcified with varying HCl concentrations

description: All samples used for comparisons were either frozen onboard immediately upon recovery (Leg 205) or stored refrigerated for a prolonged period (Leg 170).
DOI: 10.1594/pangaea.832230
title: Stable carbon and oxygen isotopic compsoition of Globorotalia inflata of sediment core MD01-2446
DOI: 10.1594/pangaea.871121
title: Stable oxygen isotope record of Globigerina bulloides of sediment core HER_MC_MR03_1b
DOI: 10.1594/pangaea.774007
title: (Appendix Table AT4) δ¹⁸O and δ¹³C of Cibicidoides wuellerstorfi for ODP Site 202-1241

description: Analytical reproducibility of the laboratory standard typically was about ±0.06 per mil for d18O and ±0.03 per mil for d13C (±1 sigma). Sediment depth is given in mcd. For each isotope analysis, up to five specimens of Cibicidoides wuellerstorfi were picked from the 250 to 500 µm fraction.
DOI: 10.1594/pangaea.846350
title: Foraminiferal δ¹⁸O, Mg/Ca, and paleotemperatures for 27 Myr of ODP Hole 120-747A
DOI: 10.1594/pangaea.843932
title: Chemical composition of Holocene sediment core M51/3_562 from the Eastern Mediterranean Sea
DOI: 10.1594/pangaea.706925
title: (Table 2) Chemical composition of terrigenous material from sediment core TT013_144
DOI: 10.1594/pangaea.767420
title: (Table 2) Isotopic analyses from TVG 97

description: Crust samples are Mg-calcite with 7 mol% MgCO3. Acharax samples are pure calcite.
DOI: 10.1594/pangaea.688720
title: (Appendix B2) Stable carbon and oxygen isotope ratios of bulk samples of the Paleocene-Eocene Thermal Maximum interval of ODP Hole 207-1260B in the equatorial Atlantic
DOI: 10.1594/pangaea.769673
title: (Table 3) Carbon and oxygen isotopic data of carbonates from Core SLR 37-1, HYC 25-1 and an aragonite crust from station DR 35-1

description: An area of massive barite precipitations was studied at a tectonic horst in 1500 m water depth in the Derugin Basin, Sea of Okhotsk. Seafloor observations and dredge samples showed irregular, block- to column-shaped barite build-ups up to 10 m high which were scattered over the seafloor along an observation track 3.5 km long. High methane concentrations in the water column show that methane expulsion and probably carbonate precipitation is a recently active process. Small fields of chemoautotrophic clams (Calyptogena sp., Acharax sp.) at the seafloor provide additional evidence for active fluid venting. The white to yellow barites show a very porous and often layered internal fabric, and are typically covered by dark-brown Mn-rich sediment; electron microprobe spectroscopy measurements of barite sub-samples show a Ba substitution of up to 10.5 mol% of Sr. Rare idiomorphic pyrite crystals (1%) in the barite fabric imply the presence of H2S. This was confirmed by clusters of living chemoautotrophic tube worms (1 mm in diameter) found in pores and channels within the barite. Microscopic examination showed that micritic aragonite and Mg-calcite aggregates or crusts are common authigenic precipitations within the barite fabric. Equivalent micritic carbonates and barite carbonate cemented worm tubes were recovered from sediment cores taken in the vicinity of the barite build-up area. Negative ?13C values of these carbonates (&gt;?43.5‰ PDB) indicate methane as major carbon source; ?18O values between 4.04 and 5.88‰ PDB correspond to formation temperatures, which are certainly below 5°C. One core also contained shells of Calyptogena sp. at different core depths with 14C-ages ranging from 20 680 to &gt;49 080 yr. Pore water analyses revealed that fluids also contain high amounts of Ba; they also show decreasing SO42- concentrations and a parallel increase of H2S with depth. Additionally, S and O isotope data of barite sulfate (?34S: 21.0–38.6‰ CDT; ?18O: 9.0–17.6‰ SMOW) strongly point to biological sulfate reduction processes. The isotope ranges of both S and O can be exclusively explained as the result of a mixture of residual sulfate after a biological sulfate reduction and isotopic fractionation with 'normal' seawater sulfate. While massive barite deposits are commonly assumed to be of hydrothermal origin, the assemblage of cheomautotrophic clams, methane-derived carbonates, and non-thermally equilibrated barite sulfate strongly implies that these barites have formed at ambient bottom water temperatures and form the features of a Giant Cold Seep setting that has been active for at least 49 000 yr.
DOI: 10.1594/pangaea.842217
title: Stable carbon isotopes from bulk carbonates, MI, and the distribution of different GDGTs for sediment Core 08
DOI: 10.5281/zenodo.15009318
title: UNDERSTANDING THE SYSTEM OF FORMATION OF COMPENSATORY COMPETENCE AMONG FOOD PRODUCTION STUDENTS
DOI: 10.5281/zenodo.15009319
title: UNDERSTANDING THE SYSTEM OF FORMATION OF COMPENSATORY COMPETENCE AMONG FOOD PRODUCTION STUDENTS
DOI: 10.1594/pangaea.688709
title: (Appendix A) Stable carbon and oxygen isotope ratios of Recent planktic foraminifera from the Little Bahama Bank, western Atlantic

description: Sample depth is 0-2 cm
DOI: 10.1594/pangaea.223483
title: Stable isotope data of sediment core GeoB1508-4
DOI: 10.1594/pangaea.884580
title: Stable carbon isotope record during Termination II in sediment core GL1090

description: This dataset was updated on 2018-09-17: column no 1 with sediment depth was added.
DOI: 10.1594/pangaea.884582
title: Stable oxygen isotope record during Termination I in sediment core GL1090

description: This dataset was updated on 2018-09-17: column no 1 with sediment depth was added.
DOI: 10.1594/pangaea.820274
title: Planktic foraminifer stable oxygen isotope record of IODP Site 306-U1314

description: Sediment depth is given in mcd.
DOI: 10.1594/pangaea.837745
title: Stable isotope ratios of Maestrichtian foraminifera of DSDP Hole 39-357
DOI: 10.1594/pangaea.837747
title: Stable isotope ratios of Maestrichtian foraminifera of DSDP Hole 80-548
DOI: 10.1594/pangaea.771395
title: Lipids of sediment core GeoB9307-3
DOI: 10.1594/pangaea.786688
title: (Table 1) Sample information and analytical data for bulk material with standard deviation (1 Sigma)
DOI: 10.1594/pangaea.784179
title: (Table T4) Age vs. stable isotopes of benthic foraminifers for a spliced core of ODP Sites 184-1147 and 184-1148

description: Sediment depth is given in mcd. Specimens were chosen from the &gt;63 µm fraction. Isotope values adjusted after Shackleton et al. (1995, doi:10.2973/odp.proc.sr.138.117.1995). Note that the data is for a spliced section: Three advanced piston corer holes at ODP Site 184-1147 and two extended core barrel holes at ODP Site 184-1148 were cored and combined into a composite (spliced) stratigraphic section.
DOI: 10.1594/pangaea.223480
title: Stable isotope data of sediment core GeoB1408-3
DOI: 10.1594/pangaea.777751
title: (Table 1) Stable carbon and oxygen isotope ratios of benthic foraminifera of ODP Hole 184-1148A

description: Changes in intermediate and deep ocean circulation likely played a significant role in global carbon cycling and meridional heat/moisture transport during the middle Miocene climate transition (~14 Ma). High-resolution middle Miocene (16-13 Ma) benthic foraminifer stable isotope records from the South China Sea reveal a reorganization of regional bottom waters, which preceded the globally recognized middle Miocene ~1 per mil d18O increase (13.8 Ma) by 100,000 years. An observed reversal of the benthic foraminifera d13C gradient between ODP Sites 1146 (2092 m) and 1148 (3294 m; 13.9–13.5 Ma) is interpreted to reflect an increase in the southward flux of low d13C deep (&gt; 2000 m) Pacific Ocean waters (Flower and Kennett, 1993, doi:10.1029/93PA02196; Shevenell and Kennett, 2004). Large-scale changes in Pacific intermediate and deep ocean circulation, coupled with enhanced global carbon cycling at the end of the Monterey Carbon Isotope excursion, likely acted as internal feedbacks to the Earth's climate system. These feedbacks reduced the sensitivity of Antarctica to lower latitude-derived heat/moisture and facilitated the transition of the Earth's climate system to a new, relatively stable glacial state.
description: Sediment depth is given in mcd. Benthic foraminifer standards: d13C = Cibicidoides wuellerstorfi, d18O = Uvigerina peregrina, size fraction &gt;150 µm.
description: Supplement to: Tian, Jun; Shevenell, Amelia E; Wang, Pinxian; Li, Qianyu; Cheng, Xinrong (2009): Reorganization of Pacific Deep Waters linked to middle Miocene Antarctic cryosphere expansion: A perspective from the South China Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 284(3-4), 375-382
DOI: 10.1594/pangaea.227254
title: Delta 13C and delta 15N of sediment core GeoB1008-3
DOI: 10.1594/pangaea.263617
title: Bulk 15N, and 13Corg ratios, and calculation of unutilized nitrate of surface samples off the southwest coast of Africa (Table 1)

description: Bulk delta15N values in surface sediment samples off the southwestern coast of Africa were measured to investigate the biogeochemical processes occurring in the water column. Nitrate concentrations and the degree of utilization of the nitrate pool are the predominant controls on sedimentary delta15N in the Benguela Current region. Denitrification does not appear to have had an important effect on the delta15N signal of these sediments and, based on delta15N and delta13C, there is little terrestrial input.
description: f = Nitrate unutilized from the ratio of [NO3] in surface water (from Conkright et al., 1994) to [NO3] in upwelled water and f estimated based on sedimentary 15N using Eqs. 1 and 2 from Altabet and Francois (1994, doi:10.1029/93GB03396)
description: Supplement to: Holmes, M Elizabeth; Müller, Peter J; Schneider, Ralph R; Segl, Monika; Wefer, Gerold (1998): Spatial variation in euphotic zone nitrate utilization based on 15N in surface sediments. Geo-Marine Letters, 18(1), 58-65
DOI: 10.1594/pangaea.54868
title: Delta 15N of sediment core GeoB1016-3
DOI: 10.1594/pangaea.422432
title: Stable isotope analysis of bulk carbonate in sediment core PG1170
DOI: 10.1594/pangaea.767419
title: (Table 1) Carbonate mineralogical and isotopic analyses of carbonate subsamples from station TV-GKG 40
DOI: 10.1594/pangaea.783544
title: (Table T1) Calcium carbonate, organic carbon and δ¹³C concentration in ODP Site 186-1150 sediments
DOI: 10.1594/pangaea.713179
title: Globigerinoides ruber (white) isotopes of sediment core GeoB2109-1
DOI: 10.1594/pangaea.693966
title: (Table 2) Stable carbon ond oxygen isotope ratios of planktonic foraminifera in Late Miocene sediments of ODP Site 184-1146 in the western Pacific

description: Depth is composite depth (mcd)
DOI: 10.1594/pangaea.775830
title: (Table S1) Stable carbon and oxygen isotope ratios of Cibicides wuellerstorfi from ODP Hole 164-994C
DOI: 10.1594/pangaea.54867
title: Delta 15N of sediment core GeoB1008-3
DOI: 10.1594/pangaea.688710
title: (Appendix A) Stable carbon and oxygen isotope ratios of Recent planktic foraminifera from the Ceara Rise in the western equatorial Atlantic

description: sample depth is 1-3 cm
DOI: 10.1594/pangaea.59765
title: (Table 2e) Alkenones, stable isotopes and sea surface temperature from sediment core KC20B
DOI: 10.1594/pangaea.871120
title: Stable oxygen isotope record of Globigerina bulloides of sediment core HER_MC_MR03_1a
DOI: 10.1594/pangaea.771883
title: (Table S2) Stable carbon and oxygen isotope ratios of planktonic foraminifera of ODP Site 207-1259

description: Sediment depth is given in mbsf, age follows the Ogg et al. (2004) timescale.
DOI: 10.1594/pangaea.819251
title: (Table 10) Carbon and oxygen isotope values for foraminifera in sediment core AOS94_B17
DOI: 10.1594/pangaea.832566
title: (Table S2) Stable isotope record of Epistominella exigua of sediment core MD02-2588
DOI: 10.1594/pangaea.786370
title: (Table T1) Chloride and sulphate content, and sulphur isotope ratios of sulphate in interstitial waters from ODP Leg 181 sites

description: DEPTH, sediment is given in mbsf. Chloride and sulfate data are from the ODP Initial Reports (Carter, RM; McCave, IN; Richter, C; Carter, L et al. 1999, doi:10.2973/odp.proc.ir.181.2000).
DOI: 10.1594/pangaea.733445
title: (Figure 2) Stable isotope ratios measured on G. bulloides from sediment core MD03-2698

description: Depth is corrected.
DOI: 10.1594/pangaea.55906
title: Analysis of organic matter in surface sediments of the equatorial Atlantic
DOI: 10.1594/pangaea.63639
title: Alkenones in surface water of METEOR cruise M46/3
DOI: 10.1594/pangaea.743085
title: Stable oxygen isotope record of planktonic and benthic foraminifera of sediment core SU92-03

description: Measured on 25 planktonic or 5 benthic foraminiferal specimens of the 250 µm to 2 mm size fraction.
DOI: 10.1594/pangaea.67489
title: Stable isotope data of ODP Hole 154-928B (Table A5)
DOI: 10.1594/pangaea.690654
title: (Appendix 1) Stable carbon and oxygen isotope ratios of planktonic foraminifera in surface sediments of the South China Sea

description: Given are raw data, for adjustment values are given in Parameter comments. Adjustment is based on a living planktonic foraminiferal database from sediment traps in the South China Sea (Cheng et al., 2002)
DOI: 10.1594/pangaea.140002
title: Stable isotopes on Globigerinoides ruber in sediment core GeoB2109-1
DOI: 10.1594/pangaea.227255
title: Delta 13C and delta 15N of sediment core GeoB1016-3
DOI: 10.1594/pangaea.223485
title: Stable isotope data of sediment core GeoB1903-3
DOI: 10.1594/pangaea.832229
title: Stable carbon and oxygen isotopic composition of Cibicidoides wuellerstorfi of sediment core MD01-2446
DOI: 10.1594/pangaea.465024
title: (Fig. 4, 5b) Stable oxygen isotopes of Globigerina bulloides from sediment core MD99-2339
DOI: 10.1594/pangaea.713178
title: Globigerinoides ruber (white) isotopes of sediment core GeoB2004-2
DOI: 10.1594/pangaea.68914
title: GeoB2204-1_Isotope
DOI: 10.1594/pangaea.871347
title: Stable carbon and oxygen isotopic composition of benthic foraminifera of IODP Site 306-U1313

description: New version, upload 2017-01-27: the mcd were given incorrectly in the old version for some of the U1313D-3H samples.Second update 2019-05-03: some depths and isotope values were corrected in U1313D-2H.
DOI: 10.1594/pangaea.933523
title: Biogenic silica, lithology and elemental composition of piston sediment core Lake850-Core2-2019 from Lake 850, Sweden

description: Dataset includes depth and ¹⁴C based age-depth model of core from Lake 850 taken in March 2019. Biogenic silica, density, total organic carbon (TOC), total nitrogen content (%N) and calcium carbonate content (CaCO₃) were measured by weak-alkaline extraction, by constraining volume and weight of wet and dry bulk sediment sample and by elemental analyzed COSTECH, respectively. Further, stable carbon isotopes (d¹³C) were measured by Elemental Analyzer connected to a MAT-252 mass spectrometer at Weizmann Institute of Science, Rehovot.Mass accumulation rate (MAR) is calculated from sediment density, age-depth model and biogenic silica flux is MAR multiplied by biogenic silica content.Further, the data contains elemental composition (Al, Si, P, S, Ar, K, Ca, Ti, V, Cr, Mn, Fe, Ni, Cu, Zn, Ge, Se, Br, Rb, Sr, Y, Zr, Nb, Mo, Te, Ba, La, Ce, Nd, Sm, Eu, Tb, Er, Tm, Yb, Hf, Ir, Pt, Au, Pb, Rn och, Rh inc, MS) of the sediment core from 2019 originating from ITRAX CS37 XRF from GLOBE Institute, Copenhagen University.
DOI: 10.1594/pangaea.67492
title: Stable isotope data of ODP Hole 154-929B (Table A6)
DOI: 10.1594/pangaea.733460
title: (Figure 5) Stable isotope ratios on Cibicidoides sp. from sediment core MD03-2698
DOI: 10.1594/pangaea.865414
title: Palynological counts (dinoflagellate cysts) and foraminiferal geochemistry (δ¹⁸O, d18C, Mg/Ca) of the Pliocene-Pleistocene transition in IODP Hole 306-U1313C
DOI: 10.1594/pangaea.784149
title: (Table T2) Oxygen and carbon isotope ratios for benthic foraminifers of ODP Site 184-1143

description: Sediment depth is given in mbsf. Specimens were chosen from the &gt;154 µm fraction. Adjustment factors after Shackleton et al. (1995, doi:10.2973/odp.proc.sr.138.117.1995).
DOI: 10.1594/pangaea.855375
title: Stable oxygen isotope ratios of Globorotalia inflata of sediment core RC16-86
DOI: 10.1594/pangaea.832192
title: (Table S2) Stable isotope record of benthic foraminifera of ODP Hole 117-723A
DOI: 10.1594/pangaea.871177
title: Stable carbon and oxygen isotopic compsoition of Globorotalia inflata of IODP Site 306-U1313

description: New version, upload 2017-01-24: the mcd, r-mcd and respective ages were given incorrectly in the old version for the U1313A samples.
DOI: 10.1594/pangaea.54688
title: Stable isotopes of sediment core PS2741-1
DOI: 10.1594/pangaea.871124
title: Stable oxygen isotope record of Globigerina bulloides of sediment core MINMC06-2
DOI: 10.1594/pangaea.742742
title: (Table T2) Stable carbon and oxygen isotope ratios of Uvigerina peregrina from ODP Site 184-1146

description: Of the 1224 analyses, 307 were on C. wuellerstorfi and 917 on U. peregrina. A total of 135 samples were measured for both species. Based on the median difference between these 135 paired analyses, we convert C. wuellerstorfi to values consistent with U. peregrina by subtracting 0.74 from the 13C values (making them lighter) and adding 0.64 to the 18O values (making them heavier). All data reported are relative to U. peregrina.
DOI: 10.1594/pangaea.872025
title: Stable carbon (13C) and stable oxygen (18O) isotopes of G.ruber (pink) from ODP Site 175-1077

description: Stable oxygen isotopes were measured on handpicked specimens of the planktic foraminifera Globigerinoides ruber (pink) from Site 1077 using a FINNIGAN MAT 251 and an automated Kiel carbonate preparation line.
DOI: 10.1594/pangaea.942628
title: Stable isotopes in water from Lake Locknesjön, Sweden collected between 2013 and 2018

description: This dataset presents measurements of stable isotopes in water (δD and δ18O) from Lake Locknesjön, Sweden. Water samples were collected between 2013 and 2018 and were taken from different depths down to 20 m in the lake, as well as from the lake's main tributary and its outflow. Depending on the depth, the water samples were collected from the shore, by a diving team, or with a UWITEC gravity corer. Measurements of stable isotopes in water samples were conducted at the Laboratoire des Sciences du Climat et de l'Environnement (LSCE), Gif-sur-Yvette, France. The δ18O was measured with a Finnigan MAT252 isotope ratio mass spectrometer with a precision of ±0.05‰ (two standard deviations). The δD was measured with a Picarro Analyzer (Cavity Ring-Down Spectroscopy) with a precision of±0.7‰ (one standard deviation).
DOI: 10.1594/pangaea.693829
title: Stable isotopes in opal of sediment core PS1786-1
DOI: 10.1594/pangaea.713176
title: Globigerinoides ruber (white) isotopes of sediment core GeoB1523-1
DOI: 10.1594/pangaea.206937
title: Stable oxygen isotope ratio of Neogloboquadrina pachyderma of sediment core MD99-2277