cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.bvth3y
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
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 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069717-240626123714530/datasets/export for details.
DOI: 10.1594/pangaea.221441
title: Physical properties of Hole 44-390A
DOI: 10.1594/pangaea.320149
title: Water temperature real-time profiles from cruise NAWF90 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.322204
title: Water temperature real-time profiles from cruise 6222898 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.322207
title: Water temperature real-time profiles from cruise 6267698 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.262939
title: Minor-element chemical analyses of Hole 37-335
DOI: 10.1594/pangaea.250277
title: (Table 2) Distribution of calcareous nannofossils in DSDP Site 92-597

description: Species abundance: V = very abundant (100+ specimens per field of view), A = abundant (11 to 100 specimens per field of view), C = common (1 to 10 specimens per field of view), F = few (1 specimen per 2 to 10 fields of view), R = rare (1 specimen per 50 fields of view), P = present (1 specimen 50 or more fields of view), - = absent.
DOI: 10.1594/pangaea.228054
title: Interstitial water chemistry of Hole 17-165

description: Details given in volume 17, chapter 17
DOI: 10.1594/pangaea.262603
title: Major-element chemical analyses of Hole 89-462A
DOI: 10.1594/pangaea.262098
title: Major-element chemical analyses of Hole 84-566
DOI: 10.1594/pangaea.321051
title: Water temperature XBT profiles from cruise 181093001 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.476464
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_AN_37N/80

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.904398
title: Foraminifer and IRD counts from ODP Site 162-983

description: Throughout the last glacial cycle millennial timescale variations in atmospheric CO2 occurred in parallel with perturbations in deep ocean circulation, which were themselves reflected by observable changes in surface conditions across the North Atlantic region. Here we use continuous proxy records to argue that an equivalent relationship has held throughout the last 800kyr i.e. since before the first occurrence of Heinrich events sensu stricto. Our results highlight the importance of internal climate dynamics in amplifying external (insolation) forcing on the climate system to produce the large amplitude of glacial terminations (deglaciations) during the mid to late Pleistocene. We show that terminations are characterized by an interval of intense ice rafting followed by a subsequent and abrupt shift to anomalously warm surface conditions (with respect to the more gradually evolving background state), which we interpret to reflect an abrupt recovery of deep ocean circulation in the Atlantic. According to our synthesis, this is followed by a period of enhanced (or at least anomalous) overturning lasting thousands of years until equilibrium interglacial conditions are attained and during which atmospheric CO2 is likely to decrease. Our results therefore suggest that deglacial oscillations in ocean circulation can have a lasting influence on early interglacial climate and highlight the transient nature of atmospheric CO2 overshoots associated with the onset of some previous interglacials. Accordingly we suggest that these intervals should be considered as a part of the deglacial process. This has implications for studies concerned with the evolution of atmospheric CO2 during interglacial periods including the Holocene.
description: Supplement to: Barker, Stephen; Knorr, Gregor; Conn, Stephen; Lordsmith, Sian; Newman, Dhobasheni; Thornalley, David J R (2019): Early Interglacial Legacy of Deglacial Climate Instability. Paleoceanography and Paleoclimatology, 34(8), 1455-1475
DOI: 10.1594/pangaea.258000
title: Paleomagnetic of Hole 84-566
DOI: 10.1594/pangaea.261469
title: Paleomagnetic and rock magnetic measurements of igneous and metamorphic rocks of Hole 66-493
DOI: 10.1594/pangaea.223398
title: Calcium carbonate bulk analysis of Hole 87-582
DOI: 10.1594/pangaea.228508
title: Interstitial water chemistry of Hole 9-83

description: Details given in volume 9, chapter 16
DOI: 10.1594/pangaea.721806
title: (Table DR1) Trace element concentrations in zircons from ODP Hole 153-923A
DOI: 10.1594/pangaea.228784
title: Interstitial water chemistry of Hole 18-172, raw data

description: Values are taken directly from the chemistry technicians shipboard notebook.
DOI: 10.1594/pangaea.723885
title: (Table DR2) Planktic and benthic foraminifreral isotope data for ODP Hole 207-1258B
DOI: 10.5281/zenodo.13326292
title: Data for "Influence of Wobbling Tryptophan and Mutations on PET Degradation Explored by QM/MM Free Energy Calculations" paper
DOI: 10.5281/zenodo.13326293
title: Data for "Influence of Wobbling Tryptophan and Mutations on PET Degradation Explored by QM/MM Free Energy Calculations" paper
DOI: 10.1594/pangaea.708694
title: (Table 5) Preservation factors for free and bound diols and keto-ols, steroids, triterpenoids, and some other lipid biomarkers in turbidites from ODP Hole 157-951B
DOI: 10.15468/dl.cum227
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
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 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069718-240626123714530/datasets/export for details.
DOI: 10.1594/pangaea.717811
title: Depth, age, strontium isotopic ratios and trace elemental ratios of samples from DSDP Hole 44-392A

description: Please note, that on 2017-06-09 it was discovered that the age values were given as "ka" alhough the values were "Ma". The data are now recalculated (x1000) to fit the unit.
DOI: 10.1594/pangaea.816956
title: (Table 4) Distribution of minor and rare-earth elements in DSDP Leg 70 basalts
DOI: 10.1594/pangaea.761466
title: (Table 5) Distribution of late Eocene calcareous nannofossils in ODP Hole 149-900A

description: Species abundance: V = very abundant (&gt; 10 specimens per field of view, A = abundant (1 to 10 specimens per field), C = common (1 specimen per 2 to 10 fields), F = few (1 specimen per 11 to 50 fields), R = rare (1 specimen per 51 to 200 fields), - = not present. Sediment depth is given in mbsf.
DOI: 10.1594/pangaea.263577
title: Minor-element chemical analyses of Hole 82-557
DOI: 10.1594/pangaea.786467
title: (Table A2) Geochemistry and calculated temperatures for carbonates of ocean crust

description: Sediment depth is given in mbsf. Age represents the crustal age. Carbonate powders were analysed for C and O isotopes in a Finnigan Delta XL Plus mass spectrometer, using a gas bench with A200s autosampler at the Pacific Centre for Isotopic and Geochemical Research, University of British Columbia. Helium was used to displace air in the headspace and CO2 gas was liberated using 100% phosphoric acid. The results are reported using the d notation measured in per mil relative to the VSMOW standard. After correction for fractionation, repeated analyses of NBS 18 gave an average d13C value of -5.01 ± 0.07? and d18O value of 7.23 ± 0.08 per mil, NBS 19 gave an average d13C value of 1.93 ± 0.08 per mil and d18O value of 28.74 ± 0.18 per mil. Precision was ± 0.1 per mil on 13C and ± 0.2 per mil on 18O. Strontium isotopes were measured Strontium was separated by standard cation exchange techniques (Weis et al., 2006) and measured using a Triton thermal ionization mass spectrometry at the Pacific Centre for Isotopic and Geochemical Research, University of British Columbia. The NBS 987 standard gave 87Sr/86Sr = 0.710241 ± 0.000025 (2 s.d., n= 12); the average reproducibility was ± 0.000012 (n=3).
DOI: 10.1594/pangaea.262655
title: Major-element chemical analyses of Hole 70-510
DOI: 10.1594/pangaea.792559
title: (Table 3) K, Rb, and Sr concentrations and 87Sr/86Sr values of calcites from DSDP Site 92-597 and fish teeth from DSDP Sites 15-149, 68-502, and 98-576 and from sediment cores AMPH-116 and DODO-111
DOI: 10.1594/pangaea.250377
title: (Table 4) Distribution of planktonic and selected benthic foraminifers from DSDP Hole 87-583A

description: Species abundance: A = abundant (&gt;100 specimens/sample), C = common (32-100 specimens), F = few (10-32 specimens), R = rare (1-9 specimens), X = present, - = absent.
DOI: 10.1594/pangaea.321065
title: Water temperature BT profiles from cruise 180591007 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.663682
title: Oceanography at CTD/bottle station IFREMER_0522
DOI: 10.1594/pangaea.714908
title: Sea-bed photographs (benthos) from the Faroe Islands region along profile HM90/8_662

description: Photographs provided here represent approx. 0.6 m**2 each. They represent a subsample of approx. 70 original 70 mm photographs (1 m**2 each) per station deposited at the Zoological Museum, The Danish State Natural History Museum, Univertsity of Copenhagen. Photographs, taken vertically by Hasselblad 500EL/M with two strobes Metz mecablitz 40 CT4 in water resistant housings; Kodak Ektachrome 64; Nikon super coolscan 4000ED; JPEG compression: 300 dpi, 21.4 x 20.0 cm; J. Gutt: mailto:julian.gutt@awi.de
DOI: 10.1594/pangaea.912881
title: Continuous wave and tide observations at station BEFmate_seafloor (2017-12)
DOI: 10.1594/pangaea.711527
title: (Table 2) Stable oxygen and carbon isotope ratios of benthic foraminifera of DSDP Hole 92-598 sediments
DOI: 10.1594/pangaea.262450
title: Major-element chemical analyses of Hole 32-307
DOI: 10.1594/pangaea.250305
title: Diatom abundance of Hole 86-579

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.761515
title: (Table 3) Stratigraphic distribution of calcareous nannofossil taxa in ODP Hole 149-897C

description: Species abundance: P = present, R = rare, F = few, C = common, A = abundant, V = very abundant, O = ooze, - = not present. Sediment depth is given in mbsf.
DOI: 10.1594/pangaea.664457
title: Oceanography at CTD/bottle station IFREMER_1297
DOI: 10.1594/pangaea.854333
title: (Table S2) Stable carbon and oxygen isotope data from planktic foraminifera Morozovelloides lehneri in sieve size fraction 250-300 µm at ODP Holes 207-1260A and 207-1260B
DOI: 10.1594/pangaea.815091
title: (Table 3) Lowermost occurrence of ice-rafted detritus clasts in selected DSDP Holes

description: Sediment depth is given in mbsf. Hole 28-266 was also investigated but no IRD clasts were present.
DOI: 10.1594/pangaea.403929
title: Water temperature and current velocity from surface drifter SVP_7715554
DOI: 10.1594/pangaea.792566
title: (Appendix 1) Age model of ODP Site 207-1259

description: Sediment depth is given in mcd.
DOI: 10.1594/pangaea.743813
title: (Table 1) Distribution of calcareous nannofossils in ODP Hole 103-637A

description: Species abundance: A = abundant (1-10 specimens per vield of view at 1560 X), C = common, (1 specimen per 2-10 fields), F = few (1 specimen per 11-100 fields), R = rare (1 specimen per 101-1000 fields), - = not present.
DOI: 10.1594/pangaea.691359
title: Mesozooplankton average mass during Mikhail Lomonosov cruise ML14, Part III

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 0.125 mm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-300, 300-500, 500-1000 m) and closed at the upper depth level. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved in 3-4% buffered formaldehyde and processed on return to the laboratory. All of copepods were identified to genus level, other taxanomic groups - to type, class, order and family levels.
DOI: 10.1594/pangaea.665492
title: Oceanography at CTD/bottle station IFREMER_2332
DOI: 10.1594/pangaea.745890
title: (Table 2) Grain sizes of minerals from ODP Hole 109-670A

description: Estimates of pre-serpentinization dimensions based on measurements of primary grains and pseudomorphs.
DOI: 10.1594/pangaea.746287
title: (Table 14) Distribution of Pleistocene to late Pliocene nannofossils in ODP Hole 108-668A

description: Species abundance: A = abundant (&gt;10% of the total assemblage), C = common (1.0-10%), F = few (0.1-1.0%), R = rare (&lt;0.1%), r = reworked, - = absent.
DOI: 10.1594/pangaea.727657
title: Particulate organic carbon and nitrogen concentrations measured on water bottles samples during POLARSTERN cruise ANT-XVIII/2 (EisenEx)

description: Particulate organic carbon and nitrogen samples were acid fumed to remove inorganic carbon. Carbon and nitrogen content was measured in the course of stable isotopic analysis using a coupled elemental analyzer (Euroboprep), isotope-ratio mass spectrometer (Finigan MAT 251) system. Carbon and nitrogen mass was calculated from the corresponding, integrated ion beam intensities and standardized based on analysis of materials of known C and N content. Reference: M.A. Altabet, Limnology and Oceanography, 46(2), 368-380 (2001), doi:10.4319/lo.2001.46.2.0368.
DOI: 10.1594/pangaea.804620
title: (Table 1) Recovered pressure and total gas volume of PCS deployments at ODP Leg 164 sites

description: The pressure core sampler (PCS) is a tool designed to recover a 1385 cm**3 cylindrical sediment core at in situ pressure (Pettigrew, 1992). Quantity and composition of gas in a sediment sample at depth can be determined by releasing gas from the PCS at the surface. Shipboard data collected from PCS deployments on Leg 164 are of great interest to the scientific community because they provide the only direct information concerning in situ gas quantities and composition in deep-sea sedimentary sequences (Dickens et al., 1997, doi:10.1038/385426a0). A portion of total data collected from the PCS was published in "Downhole Tools and Sampling" sections of site chapters in the Leg 164 Initial Reports volume (Paull, Matsumoto, Wallace, et al., 1996, doi:10.2973/odp.proc.ir.164.1996). Here we present the shipboard PCS data not included in the Initial Reports volume because of time constraints. Suggested improvements for future PCS data collection also are noted here. Interpretations based on PCS data are discussed elsewhere in this volume and by Dickens et al. (1997, doi:10.1038/385426a0).
description: Sediment depth is given in mbsf. Some pressures are different than those reported by Paull, Matsumoto, Wallace, et al. (1996, doi:10.2973/odp.proc.ir.164.1996). The reason is twofold: pressure changes rapidly over the first minute, and certain pressures were recorded by more than one individual. Recovered pressure was originally given in psi and was recalculated to bar by multiplying by 0.06894757.
description: Supplement to: Dickens, Gerald Roy; Borowski, Walter S; Wehner, Hermann; Paull, Charles K; ODP Leg 164 Scientific Party (2000): Data Report: Additional shipboard information for the pressure core sampler (PCS). In: Paull, CK; Matsumoto, R; Wallace, PJ; Dillon, WP (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 164, 1-5
DOI: 10.1594/pangaea.262968
title: Minor-element chemical analyses of Hole 82-560
DOI: 10.1594/pangaea.262099
title: Major-element chemical analyses of Hole 84-566A
DOI: 10.1594/pangaea.800063
title: (Table 4) Trace element concentrations and isotope ratios for DSDP Site 89-462 basalts

description: Analytical blank is about 2 nanogram Sr and about 0.2 nanogram Rb. 87Sr/86Sr normalized to E + A SrCO3 = 0.70800. BCR-1 143Nd/144Nd = 0.51271.
DOI: 10.1594/pangaea.320146
title: Water temperature real-time profiles from cruise JHF090 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.882643
title: Radiosonde PS105_39856 during POLARSTERN cruise PS105 (ANT-XXXII/4) on 2017-04-07 10:51h

description: Height of tropopause 16374 m, precipitable water content 1.7827 cm
DOI: 10.1594/pangaea.97097
title: Sedimentation rates of Hole 50-416

description: compiled and calculated from various DSDP data sources
DOI: 10.1594/pangaea.874817
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 74 (Holes 527, 528, 528A, 529)

description: The drilling plan for Leg 74 of the Deep Sea Drilling Project was designed to address three main scientific topics: (1) the history of the deep-water circulation in the southeastern Atlantic, (2) the nature and geologic evolution of the Walvis Ridge, and (3) the biostratigraphy and magnetic stratigraphy of this region. In order to study these subjects, a suite of five sites was drilled on the Walvis Ridge that extended from its crest (near 1000 m water depth) down its northwest flank into the Angola Basin to a depth of 4400 m.
description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
DOI: 10.1594/pangaea.220247
title: Mineral composition of silt fraction from Hole 37-335
DOI: 10.1594/pangaea.804003
title: (Table 6) Geochemisty of clinopyroxene at DSDP Leg 84 Holes

description: Elements as atoms per 6 oxygens.
DOI: 10.1594/pangaea.101486
title: Smear slide analysis of Hole 12-112
DOI: 10.1594/pangaea.322117
title: Water temperature real-time profiles from cruise 4153198 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.746306
title: (Table 14) Distribution of planktonic foraminifers in ODP Hole 108-665A

description: Species abundance: A = abundant (&gt;30%), C = common, (15-30%), F = few (3-15%), R = rare (&lt;3%), X = present, but no abundance estimated, - = absent.
DOI: 10.1594/pangaea.321325
title: Water temperature and salinity real-time profiles from cruise UFYN92 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.322521
title: Water temperature real-time profiles from cruise 4185900 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.744571
title: (Table 6) Major element composition of rocks at ODP Siite 209-1275
DOI: 10.1594/pangaea.323426
title: Water temperature and salinity CTD profiles from cruise 18TL96012 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.863978
title: Radionuclides, Nd isotopes and biogenic Opal in Atlanic Ocean sediments

description: Reconstructing past modes of ocean circulation is an essential task in paleoclimatology and paleoceanography. To this end, we combine two sedimentary proxies, Nd isotopes (epsilon-Nd) and the 231Pa/230Th ratio, both of which are not directly involved in the global carbon cycle, but allow the reconstruction of water mass provenance and provide information about the past strength of overturning circulation, respectively. In this study, combined 231Pa/230Th and epsilon-Nd down-core profiles from six Atlantic Ocean sediment cores are presented. The data set is complemented by the two available combined data sets from the literature. From this we derive a comprehensive picture of spatial and temporal patterns and the dynamic changes of the Atlantic Meridional Overturning Circulation over the past ~25 ka. Our results provide evidence for a consistent pattern of glacial/stadial advances of Southern Sourced Water along with a northward circulation mode for all cores in the deeper (&gt;3000 m) Atlantic. Results from shallower core sites support an active overturning cell of shoaled Northern Sourced Water during the LGM and the subsequent deglaciation. Furthermore, we report evidence for a short-lived period of intensified AMOC in the early Holocene.
description: Supplement to: Lippold, Jörg; Gutjahr, Marcus; Blaser, Patrick; Christner, Emanuel; de Carvalho, Maria Luiza; Mulitza, Stefan; Christl, Marcus; Wombacher, Frank; Böhm, Evelyn; Antz, Benny; Cartapanis, Olivier; Vogel, Hendrik; Jaccard, Samuel L (2016): Deep water provenance and dynamics of the (de)glacial Atlantic meridional overturning circulation. Earth and Planetary Science Letters, 445, 68-78
DOI: 10.1594/pangaea.320943
title: Water temperature XBT profiles from cruise 181892011 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.322125
title: Water temperature real-time profiles from cruise 4153998 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001