cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.777619
title: 7) Revised age model of sediment core CH69-K09 for the Last Interglacial (period 135-110 ka)
DOI: 10.1594/pangaea.779618
title: Planktonic foraminifer occurrences and zonations from IODP Hole 313-M0029A

description: Sediment depth is given in mbsf. LO = last occurrence, FO = first occurrence.
DOI: 10.1594/pangaea.351434
title: Pore water samples and chemistry of Hole 302-M0002A
DOI: 10.1594/pangaea.779542
title: Planktonic foraminifer occurrences and zonations from IODP Hole 313-M0027A

description: Sediment depth is given in mbsf. Preservation: VG = very good, G = good, M = medium. X = present. FO = first occurrence, LO = last occurrence.
DOI: 10.1594/pangaea.868033
title: Alkalinity and delta13C values for fluid samples from IODP Hole 357-M0068B
DOI: 10.1594/pangaea.867841
title: Concentrations of anions in fluid samples from IODP Hole 357-M0075A

description: Sample precisions were ±3.9% for Cl, ±2.2% for Br, and ±4.3% for SO4, whereas both NO3 and F were at the limit of detection.
DOI: 10.1594/pangaea.868038
title: Alkalinity and delta13C values for fluid samples from IODP Hole 357-M0071C
DOI: 10.1594/pangaea.351433
title: Pore water samples and chemistry of Hole 302-M0001A
DOI: 10.1594/pangaea.868375
title: X-ray diffraction results from IODP Hole 357-M0069A

description: Percentages were released by the software, sometimes with excess. Total sum &lt;100% likely reflects the presence of amorphous or poorly crystallized material.
DOI: 10.1594/pangaea.867530
title: Magnetic susceptibility and demagnetized inclinations measured on discrete samples from IODP Hole 357-M0075B
DOI: 10.1594/pangaea.868781
title: Moisture and density (MAD) measured on IODP Hole 357-M0068B
DOI: 10.1594/pangaea.868741
title: Color data (CRF) of IODP Hole 357-M0068B
DOI: 10.1594/pangaea.868700
title: Natural gamma radiation from IODP Hole 357-M0071C
DOI: 10.1594/pangaea.868701
title: Natural gamma radiation from IODP Hole 357-M0072A
DOI: 10.1594/pangaea.867834
title: Concentrations of anions in fluid samples from IODP Hole 357-M0072A

description: Sample precisions were ±3.9% for Cl, ±2.2% for Br, and ±4.3% for SO4, whereas both NO3 and F were at the limit of detection.
DOI: 10.1594/pangaea.869854
title: Concentrations of major elements in fluid samples from IODP Hole 357-M0073A
DOI: 10.1594/pangaea.868860
title: Physical properties (MSCL fast track) of IODP Hole 357-M0071B
DOI: 10.1594/pangaea.868867
title: Physical properties (MSCL fast track) of IODP Hole 357-M0076A
DOI: 10.1594/pangaea.869890
title: Concentrations of trace elements in fluid samples from IODP Hole 357-M0072X
DOI: 10.1594/pangaea.870630
title: Visual core description and core images from IODP Hole 357-M0071C
DOI: 10.1594/pangaea.869887
title: Concentrations of trace elements in fluid samples from IODP Hole 357-M0075X
DOI: 10.1594/pangaea.870634
title: Visual core description and core images from IODP Hole 357-M0075A
DOI: 10.1594/pangaea.870617
title: Thin sections from IODP Hole 357-M0075A
DOI: 10.1594/pangaea.868454
title: Sensor signal time log from IODP Hole 357-M0072A
DOI: 10.1594/pangaea.869888
title: Concentrations of trace elements in fluid samples from IODP Hole 357-M0076B
DOI: 10.1594/pangaea.761245
title: Correlation of seismic sequence boundaries to core surfaces, IODP Hole 313-M0027A

description: Notes: GTS = geologic timescale. GTS 2008 = Ogg et al. (2008). Predicted age for BKSA95 (Cande and Kent, 1995) from Monteverde et al. (2008) and Miller et al. (1998). Seismic sequence boundaries from Monteverde et al. (2008), Miller et al. (1998), and Sheridan et al. (2000). Predicted depths based on seismic velocity function. Predicted depth and ages for seismic sequence boundaries MIC3a to o1 from Monteverde et al. (2008) for the pre-Pleistocene and Sheridan et al. (2000) for the Pleistocene. Two predicted depths in two way travel time (TWT) and depth (mbsf) are given, the first from Monteverde et al. (2008) and the second from Mountain et al. (2009). Actual depth and actual core are the best fit to surfaces or other contacts noted in the cores. Preliminary age is derived from "Chronology." MIC = marine isotope chron, MFS = maximum flooding surface, SB = sequence boundary GTS2008 (Ogg et al., 2008), TS = transgressive surface, FS = flooding surface, EOT = Eocene-Oligocene transition. NR = none recovered. USF = upper shoreface, SOT = shoreface-offshore transition.
DOI: 10.1594/pangaea.913970
title: Relative abundances of planktonic Foraminifers of IODP Hole 381-M0078A

description: Samples contain &gt;100 individuals counts. Species appearing in trace percentages (&lt;5%) are excluded. D = dominant, VA = very abundant, A = abundant, C = common, F = few.
DOI: 10.1594/pangaea.757424
title: Description of lithologic section units of IODP Hole 313-M0029A
DOI: 10.1594/pangaea.786018
title: (Table T1-4) Stable carbon and oxygen isotope ratios of cool-water Bryozoa Nevianipora sp. from ODP Leg 182 sites
DOI: 10.1594/pangaea.831370
title: (Table S1) Enrichment factors of all element/Al ratios compared to average shale of IODP Exp302 holes

description: DEPTH, sediment/rock [m] is given in mcd.
DOI: 10.1594/pangaea.399464
title: Natural gamma-ray spectrometry-pass1 of Hole 302_M0004B
DOI: 10.1594/pangaea.899490
title: A summary of consistently dated Atlantic sediment cores over the last 40 thousand years

description: Rapid changes in ocean circulation and climate have been observed in marine-sediment and ice cores over the last glacial period and deglaciation, highlighting the non-linear character of the climate system and underlining the possibility of rapid climate shifts in response to anthropogenic greenhouse gas forcing. To date, these rapid changes in climate and ocean circulation are still not fully explained. One obstacle hindering progress in our understanding of the interactions between past ocean circulation and climate changes is the difficulty of accurately dating marine cores. Here, we present a set of 92 marine sediment cores from the Atlantic Ocean for which we have established age-depth models that are consistent with the Greenland GICC05 ice core chronology, and computed the associated dating uncertainties, using a new deposition modeling technique. This is the first set of consistently dated marine sediment cores enabling paleoclimate scientists to evaluate leads/lags between circulation and climate changes over vast regions of the Atlantic Ocean. Moreover, this data set is of direct use in paleoclimate modeling studies.
DOI: 10.1594/pangaea.707038
title: (Table 3) Tie points of Hole 302-M0004C
DOI: 10.1594/pangaea.829755
title: (Table S1) Age determination of Atlantic Ocean sediment cores

description: Well-dated benthic foraminifer oxygen isotopic records (d18O) from different water depths and locations within the Atlantic Ocean exhibit distinct patterns and significant differences in timing over the last deglaciation. This has two implications: on the one hand, it confirms that benthic d18O cannot be used as a global correlation tool with millennial-scale precision, but on the other hand, the combination of benthic isotopic records with independent dating provides a wealth of information on past circulation changes. Comparing new South Atlantic benthic isotopic data with published benthic isotopic records, we show that (1) circulation changes first affected benthic d18O in the 1000-2200 m range, with marked decreases in benthic d18O taking place at ~17.5 cal. kyr B.P. (ka) due to the southward propagation of brine waters generated in the Nordic Seas during Heinrich Stadial 1 (HS1) cold period; (2) the arrival of d18O-depleted deglacial meltwater took place later at deeper North Atlantic sites; (3) hydrographic changes recorded in North Atlantic cores below 3000 m during HS1 do not correspond to simple alternations between northern- and southern-sourced water but likely reflect instead the incursion of brine-generated deep water of northern as well as southern origin; and (4) South Atlantic waters at ~44°S and ~3800 m depth remained isolated from better-ventilated northern-sourced water masses until after the resumption of North Atlantic Deep Water (NADW) formation at the onset of the Bølling-Allerod, which led to the propagation of NADW into the South Atlantic.
description: Core ENAM9321 age model is mainly based on correlation to GRIP ice d18O (Rasmussen et al., 1998). Core NA87-22 age model is fully described by Waelbroeck et al. (2001, 2006). Core MD95-2037 is published in the work by Gherardi et al. (2009). Core M35003-4 is described by Rühlemann et al. (1999). Core GeoB1711 is described by Vidal et al. (1999) and Waelbroeck et al. (2006). Core MD99-2334K is described by Skinner et al. (2003). Resulting errors on the calendar age have been computed in the present study as the maximum between the error on the calibrated age and the offset between the calibrated age and GISP2 age (Meese et al., 1997). Core KNR31 GPC-5 14C dates are from (Keigwin and Jones, 1994). Calendar ages have been computed using the Calib6.0 software (Stuiver and Reimer, 1993) and calibration data set marine09.14C (Reimer et al., 2009), assuming no additional surface reservoir age correction. Core MD07-3076 age model is fully described by Skinner et al. (2010).
description: Supplement to: Waelbroeck, Claire; Skinner, Luke C; Labeyrie, Laurent D; Duplessy, Jean-Claude; Michel, Elisabeth; Vázquez Riveiros, Natalia; Gherardi, Jeanne-Marie; Dewilde, Fabien (2011): The timing of deglacial circulation changes in the Atlantic. Paleoceanography, 26(3), PA3213
DOI: 10.1594/pangaea.757360
title: Correlation of seismic sequence boundaries to core surfaces, IODP Hole 313-M0028A

description: Notes: BKSA95 from Cande and Kent (1995). Seismic picks from Seisworks. Predicted depth and ages for seismic sequence boundaries m1 to m5.8 from Monteverde et al. (2008). Two predicted depths in two way travel time (TWT) and depth (mbsf) are given, the first from Monteverde et al. (2008). Actual depth and actual core are the best fit to surfaces or other contacts noted in the cores. Preliminary age and age error are derived from "Chronology". NR = not resolved. MFS = maximum flooding surface, FS = flooding surface, TS = transgressive surface, SB = sequence boundary, SOT = shoreface-offshore transition, off = offshore.
DOI: 10.1594/pangaea.870633
title: Visual core description and core images from IODP Hole 357-M0074A
DOI: 10.1594/pangaea.896608
title: Age model of sediment core BEN14-P4 from Lake Benit
DOI: 10.1594/pangaea.754281
title: Total organic carbon, sulphur and mineral content of sediments of Hole 313-M0027A
DOI: 10.1594/pangaea.868457
title: Sensor signal time log from IODP Hole 357-M0076B
DOI: 10.1594/pangaea.875684
title: (Table S9) Carbon and oxygen isotope values for pedogenic carbonate samples collected from Gilmore Hill core A organized by stratigraphic level
DOI: 10.1594/pangaea.912830
title: Trace metal and metalloid elements of sediment core DAM17-02 from the Eure River, France (pseudo-total digestion)
DOI: 10.1594/pangaea.871671
title: (Table 3) Age-depth models of IODP Hole 347-M0063D
DOI: 10.1594/pangaea.912538
title: Fluxes of CO2, CH4 and N2O and reservoir metabolism of twelve Mediterranean reservoirsin Southern Spain

description: Simultaneous fluxes of CO2, CH4 and N2O in twelve reservoirs in Southern Spain during the stratification period and the mixing period were measured using a Picarro G2508 gas analyzer connected to a floating chamber. For each reservoir in each sampling period, we took 3-5 measurements for 40 min. We calculated the daily (from 10 am to 4 pm) average (mean) and the standard error (SE) from these measurements. Flux calculations were based on Zhao et al (2015). To obtain the reservoir radiative forcings we summed the corresponding forcing due to CO2 emissions, the warming potential (GWP) of CH4 in terms of CO2 equivalents, and the warming potential of N2O in terms of CO2 equivalents. We used 34 to convert CH4 in CO2 equivalent and 298 to convert N2O in CO2 equivalent in a 100-year time horizon, including the climate-carbon feedbacks (IPCC 2013). We measured ambient temperature, barometric pressure (HANNA HI 9828), and wind speed (MASTECH MS6252A) at the beginning of each flux measurement. We recorded dissolved oxygen concentration and water temperature using a miniDOT (PME) submersible water logger during the stratification period, and calculated the lake metabolism (i.e., gross primary production, net production and respiration rate) according to Staehr et al (2010).
DOI: 10.1594/pangaea.733925
title: (Table 3) Stable isotope data from the analysis of fish bones and the calculated salinity range in IODP Exp302

description: DEPTH, sediment/rock [m] is given in mcd.
DOI: 10.1594/pangaea.861806
title: Core-section summary for IODP Hole 357-M0070A
DOI: 10.1594/pangaea.881710
title: Close-up images (processed) of IODP Hole 364-M0077A
DOI: 10.1594/pangaea.883722
title: Distribution of ostracod species at IODP holes 347-M0063A and 347-M0063B

description: A total of 173 sediment samples from the upper 45 mbsf were processed for ostracod analysis at IODP site M0063. Ostracods abundance was very low. All abundances are expressed as single ostracod valves.Additionally, organic Carbon data are shown.For Site M0063 due to sediment expansion, mbsf depths were converted into adjusted mbsf (ambsf), and the latter into adjusted mcd (amcd) [Obrochta et al., 2017]. Ambsf scale is used for Holes A and B; amcd scale for Holes C, D and E.
DOI: 10.1594/pangaea.769815
title: (Table S1) Palynology of IODP Hole 302-M0004A

description: The Palaeocene/Eocene thermal maximum, 55 million years ago, was a brief period of widespread, extreme climatic warming (Zachos et al., 2003; Kennett and Stott, 1991, doi:10.1038/353225a0; Tripati and Elderfield, 2005, doi:10.1126/science.1109202), that was associated with massive atmospheric greenhouse gas input (Dickens et al., 1995, doi:10.1029/95PA02087). Although aspects of the resulting environmental changes are well documented at low latitudes, no data were available to quantify simultaneous changes in the Arctic region. Here we identify the Palaeocene/Eocene thermal maximum in a marine sedimentary sequence obtained during the Arctic Coring Expedition (Backman et al., 2006, doi:10.2204/iodp.proc.302.2006). We show that sea surface temperatures near the North Pole increased from 18 °C to over 23 °C during this event. Such warm values imply the absence of ice and thus exclude the influence of ice-albedo feedbacks on this Arctic warming. At the same time, sea level rose while anoxic and euxinic conditions developed in the ocean's bottom waters and photic zone, respectively. Increasing temperature and sea level match expectations based on palaeoclimate model simulations (Shellito et al., 2003, doi:10.1016/S0031-0182(02)00718-6), but the absolute polar temperatures that we derive before, during and after the event are more than 10 °C warmer than those model-predicted. This suggests that higher-than-modern greenhouse gas concentrations must have operated in conjunction with other feedback mechanisms -perhaps polar stratospheric clouds (Sloan and Pollard, 1998, doi:10.1029/98GL02492) or hurricane-induced ocean mixing (Emanuel et al., 2004, doi:10.1175/1520-0469(2004)061&lt;0843:ECOTCI&gt;2.0.CO;2)- to amplify early Palaeogene polar temperatures.
description: Sediment depth is given in mcd.
description: Supplement to: Sluijs, Appy; Schouten, Stefan; Pagani, Mark; Woltering, Martijn; Brinkhuis, Henk; Sinninghe Damsté, Jaap S; Dickens, Gerald Roy; Huber, Matthew; Reichart, Gert-Jan; Stein, Ruediger; Matthiessen, Jens; Lourens, Lucas Joost; Pedentchouk, Nikolai; Backman, Jan; Moran, Kathryn; Expedition 302 Scientists (2006): Subtropical Arctic Ocean temperatures during the Palaeocene/Eocene thermal maximum. Nature, 441, 610-613
DOI: 10.1594/pangaea.843032
title: Description of lithologic section units of IODP Hole 347-M0059C

description: Geocode = CSF-A [m].
DOI: 10.1594/pangaea.875655
title: (Table S3) BSN L*,a* and b* color scanning data
DOI: 10.1594/pangaea.914504
title: X-Ray fluorescence (XRF) scanning of tephra layers (10kV run) of IODP Holes 381-M0079A
DOI: 10.1594/pangaea.914508
title: X-Ray fluorescence (XRF) scanning of tephra layers (30kV run) of IODP Holes 381-M0079A
DOI: 10.1594/pangaea.837830
title: Core-section summary for IODP Hole 347-M0063E
DOI: 10.1594/pangaea.883368
title: Major element compositions in the rocks of the lower peak ring from IODP Hole 364-M0077A
DOI: 10.1594/pangaea.837828
title: Core-section summary for IODP Hole 347-M0063C
DOI: 10.1594/pangaea.837829
title: Core-section summary for IODP Hole 347-M0063D
DOI: 10.1594/pangaea.867538
title: Chemical compositions of representative lithologies from IODP Hole 357-M0069A
DOI: 10.1594/pangaea.867542
title: Chemical compositions of representative lithologies from IODP Hole 357-M0075B
DOI: 10.1594/pangaea.914489
title: X-Ray fluorescence (XRF) scanning results (10kV run) of IODP Hole 381-M0079A
DOI: 10.1594/pangaea.779619
title: Dinocyst occurrences and zonations from IODP Hole 313-M0029A

description: Sediment depth is given in mbsf. Ph = phytoclasts, flin = foraminifer lining, AOM = amorphous organic matter.
DOI: 10.1594/pangaea.839838
title: Composite depth scale of IODP Hole 347-M0061C
DOI: 10.1594/pangaea.843042
title: Description of lithologic section units of IODP Hole 347-M0064B

description: Geocode = CSF-A [m].
DOI: 10.1594/pangaea.844963
title: Magnetic susceptibility and Natural Remanent Magnetisation from IODP Hole 347-M0061A
DOI: 10.1594/pangaea.881720
title: CT-A (atomic number) images of IODP Hole 364-M0077A
DOI: 10.1594/pangaea.899685
title: Core-section summary for IODP Hole 381-M0078B
DOI: 10.1594/pangaea.672414
title: Physical properties of Hole 302-M0003A
DOI: 10.1594/pangaea.839852
title: Composite depth scale of IODP Hole 347-M0065A
DOI: 10.1594/pangaea.840797
title: Distribution and abundance of ostracods from IODP Hole 347-M0059C

description: Abundance: C = common, F = few, R = rare, B = barren.
DOI: 10.1594/pangaea.840798
title: Distribution and abundance of ostracods from IODP Hole 347-M0059D

description: Abundance: C = common, F = few, R = rare, B = barren.
DOI: 10.1594/pangaea.840799
title: Distribution and abundance of ostracods from IODP Hole 347-M0059E

description: Abundance: C = common, F = few, R = rare, B = barren.
DOI: 10.1594/pangaea.844968
title: Magnetic susceptibility and Natural Remanent Magnetisation from IODP Hole 347-M0062D
DOI: 10.1594/pangaea.840358
title: Microbial cell counts from IODP Hole 347-M0060B
DOI: 10.1594/pangaea.844969
title: Magnetic susceptibility and Natural Remanent Magnetisation from IODP Hole 347-M0063D
DOI: 10.1594/pangaea.837818
title: Core-section summary for IODP Hole 347-M0061L
DOI: 10.1594/pangaea.868821
title: Physical properties (MSCL raw data) of IODP Hole 357-M0070B
DOI: 10.1594/pangaea.354722
title: Results of foraminifer and ostracode analyses of Hole 302-M0002A

description: Abundance: R = rare, B = barren. Preservation: G = good.
DOI: 10.1594/pangaea.838277
title: Natural gamma radiation of IODP Hole 347-M0061B
DOI: 10.1594/pangaea.338925
title: Nannofossil abundance of Hole 302-M0004C

description: Relative abundance: A = abundant, C = common, F = few, R = rare, B=barren (numerical values are abundance in counts) / cf. = conferatur, probably belongs to the identified species
DOI: 10.1594/pangaea.438390
title: Torvane shear strength in Hole 302-M0004A
DOI: 10.1594/pangaea.733255
title: (Table 1) Element enrichment in dark versus light layers of the ''Zebra'' interval of IODP Hole 302-M0002A

description: Analysis focuses on the upper part of subunit 1/6, subunit 1/5, and the lower part of subunit 1/4 (cores M0002A-47X 3W to M0002A-44X 1W) extending from 203.70 to 191.99 mcd.
DOI: 10.1594/pangaea.659167
title: Chemical composition of Eocene sediments of Hole 302-M0004A
DOI: 10.1594/pangaea.899690
title: Core-section summary for IODP Hole 381-M0080A
DOI: 10.1594/pangaea.837807
title: Core-section summary for IODP Hole 347-M0059A
DOI: 10.1594/pangaea.843039
title: Description of lithologic section units of IODP Hole 347-M0063C

description: Geocode = CSF-A [m].
DOI: 10.1594/pangaea.754258
title: Natural remanent magnetization polarity estimation of Hole 313-M0027A
DOI: 10.1594/pangaea.839837
title: Composite depth scale of IODP Hole 347-M0061B
DOI: 10.1594/pangaea.704651
title: Sum peak hight and area intensities of bulk X-ray diffraction data of Hole 302-M0004A

description: Depth is given in meter composite depth (mcd) !
DOI: 10.1594/pangaea.801730
title: (Table S10) Stable isotopic composition of organic carbon from IODP Hole 313-M0029A sediments

description: Sediment depth is given in mbsf. For data on carbon composition (TC, TOC and TIC) of Hole 313-M0027A sediments see Mountain et al. (2010) dataset: doi:10.1594/PANGAEA.754294.
DOI: 10.1594/pangaea.861809
title: Core-section summary for IODP Hole 357-M0071A
DOI: 10.1594/pangaea.861810
title: Core-section summary for IODP Hole 357-M0071B
DOI: 10.1594/pangaea.659166
title: Chemical composition of Eocene sediments of Hole 302-M0002A
DOI: 10.1594/pangaea.754226
title: Strontium isotope data and age model of Hole 313-M0027A
DOI: 10.1594/pangaea.753991
title: P-wave velocity of discrete samples from Hole 313-M0028A
DOI: 10.1594/pangaea.754298
title: X-ray diffraction analysis and quantification of minerals of Hole 313-M0027A
DOI: 10.1594/pangaea.753976
title: Core-section summary for Hole 313-M0029A
DOI: 10.1594/pangaea.839857
title: Composite depth scale of IODP Hole 347-M0067A
DOI: 10.1594/pangaea.475994
title: Bulk organic geochemistry of Hole 302-M0002A

description: Comment on sulfur values: The high sulfur values &gt; 5% determined with the LECO instrument are minimum values as shown by re-measurements using an ELTRA-CS 500 instrument (which is better calibrated for very high sulfur values) (H. Brumsack, ICBM Oldenburg University, pers. comm. July 2006). This results in even lower C/S ratios in the euxinic intervals, and thus does not change but support the interpretation discussed in the paper.
DOI: 10.1594/pangaea.872468
title: Whole round core description trough liner (A0, A3) of IODP Hole 357-M0075B
DOI: 10.1594/pangaea.920938
title: Organochlorine Pesticides (OCPs) in sediment core DAM17-02 from the Eure River, France

description: We measured organochlorine pesticides (OCPs) in sediment cores (collected in two independant ponds) to study the relationships between sediment deposits characteristics and organic contaminants, and the temporal trends of OCPs were reconstructed since 1940s in the Eure River watershed, major tributary of the Seine estuary (France).The analysis of particulate OCPs from the sediment cores (MAR16-02 and DAM17-02) was performed using microwave-assisted extraction, with toluene:acetone mixture for extraction. Following the microwave-assisted extraction, a gas chromatograph (7890B, Agilent, US) coupled to a mass spectrometer (MS; 7000C) was used to measure the concentrations.
DOI: 10.1594/pangaea.844965
title: Magnetic susceptibility and Natural Remanent Magnetisation from IODP Hole 347-M0061C
DOI: 10.1594/pangaea.868453
title: Sensor signal time log from IODP Hole 357-M0069A
DOI: 10.1594/pangaea.753973
title: Core summary for Hole 313-M0029A

description: Drillers log: hdl:10013/epic.36808.d001
DOI: 10.1594/pangaea.475998
title: Bulk organic geochemistry of Hole 302-M0004A

description: Comment on sulfur values: The high sulfur values &gt; 5% determined with the LECO instrument are minimum values as shown by re-measurements using an ELTRA-CS 500 instrument (which is better calibrated for very high sulfur values) (H. Brumsack, ICBM Oldenburg University, pers. comm. July 2006). This results in even lower C/S ratios in the euxinic intervals, and thus does not change but support the interpretation discussed in the paper.
DOI: 10.1594/pangaea.837821
title: Core-section summary for IODP Hole 347-M0062B
DOI: 10.1594/pangaea.837896
title: Color data of IODP Hole 347-M0059C
DOI: 10.1594/pangaea.871672
title: (Table 4) Age-depth models of IODP Holes 347-M0063C and 347-M0063E
DOI: 10.1594/pangaea.875527
title: Lithology of surface sediments in the Porcupine area
DOI: 10.1594/pangaea.868695
title: Natural gamma radiation from IODP Hole 357-M0070A