cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.145159
title: Underway physical oceanography and carbon dioxide measurements during PYXIS cruise PX101E

description: Detailed metadata description of each cruise doi:10.1594/PANGAEA.769638
DOI: 10.1594/pangaea.67696
title: Color data of sediment core GeoB7212-2
DOI: 10.1594/pangaea.315972
title: Physical properties of sediment core MD02-2539

description: All physical properties shipboard data of IMAGES IX cruise should be considered validated, but due to various problems with the calibration of the instrument it is also to be considered as preliminary.
DOI: 10.1594/pangaea.230020
title: Water content, carbon and carbonate analysis of sediment core Y80_134SGC
DOI: 10.1594/pangaea.132042
title: Geochemistry on sediment core SO106-252KG
DOI: 10.1594/pangaea.77600
title: Benthic fluxes at sediment profile station NH88-8_03_BC
DOI: 10.1594/pangaea.121660
title: Grain size composition of sediment core PS-1299-1
DOI: 10.1594/pangaea.125406
title: Chemical composition of sediment core PS-1341-1
DOI: 10.1594/pangaea.142621
title: Pollen profile 2 Radauer Born from a swamp at Torfhaus, Harz, Germany

description: Pollen zones after Firbas III-VI.
DOI: 10.1594/pangaea.93128
title: Physical oceanography at station POS212/2-CTD-801_014
DOI: 10.1594/pangaea.125151
title: Oxygen in pore water of sediment core TT013_82
DOI: 10.1594/pangaea.125493
title: Chemical composition of sediment core PSEE-7
DOI: 10.1594/pangaea.77400
title: Biogeochemical properties of sediment profile NH88-8_10
DOI: 10.1594/pangaea.76434
title: sediment samples deployment, Stn P4, Sept. 97 to May 98
DOI: 10.1594/pangaea.139164
title: Physical properties of sediment core GIK23475-1
DOI: 10.1594/pangaea.87878
title: Smear slide analysis of sediment core PM9441-4
DOI: 10.1594/pangaea.253619
title: Physical properties of sediment core MD99-2290

description: Due to problems with the core logger, all physical properties data of IMAGES V cruise should be considered unvalidated.
DOI: 10.1594/pangaea.52013
title: Density and porosity of sediment core MSSTS-1
DOI: 10.1594/pangaea.125932
title: Grain size composition of sediment core Kord-299
DOI: 10.1594/pangaea.76312
title: Nutrients in pore water in sediment core W8803B-T-92
DOI: 10.1594/pangaea.131725
title: Color reflectance of sediment core MD03-2614G
DOI: 10.1594/pangaea.77078
title: Carbon and carbonate content of core GEOFAR KF12 sediment samples
DOI: 10.1594/pangaea.55775
title: Grain size distribution of surface sediments from Lake Pjassino
DOI: 10.1594/pangaea.83761
title: Hydrochemistry measured on water bottle samples during Professor Multanovskiy cruise PM88
DOI: 10.1594/pangaea.138711
title: Heavy metal contents in different size fractions of bottom sediments from the South China Sea, core Ast-8761
DOI: 10.1594/pangaea.393384
title: Water temperature from profiling float 278897

description: Temperatures and pressures were calculated from the counts that were sent ashore from the float. Trajectory file in NetCDF format: http://hs.pangaea.de/Projects/WOCE/PFLOAT/2788_D.zip
DOI: 10.1594/pangaea.191104
title: (Table 1) Detrital modes for sand grains in sediment core CRP-2/2A

description: Dynamic provenance variations are deduced from sand-grain detrital modes in samples obtained from the CRP-2/2A drillcore. Below an important unconformity at 307 metres below sea floor (mbsf), sand grains in most of the sequence were dominantly derived from Beacon sandstone and Ferra dolerite sources, although alternating with subordinate thicknesses of strata derived from a predominantly granitoid source (Granite Harbour Intrusive Complex; GHIC). Above the 307 mbsf unconformities, the reverse situation occurs, with most sediments dominantly sourced in the GHIC. Contributions from other sources (e.g. Jurassic Kirkpatrick basalt lavas and Proterozoic metamorphic basement) are also persistent but minor. An input of fresh volcanic detritus commenced at 307 mbsf and is ubiquitous in all the younger sediments. At least three (probably four) episodes of volcanism are identified, each lasting 1-2 M.yr in duration. The initial influx at 307 mbsf corresponds to the initiation of the McMurdo Volcanic Group (MVG) at c. 25 Ma and is much younger than estimates made previously by other workers for the oldest MVG volcanic activity in the McMurdo Sound region (Eocene?). Simultaneous major changes in the proportion of clast lithologies in CRP-2/2A suggest that the 307 mbsf unconformity is the most important petrological break within the cored sequence. It is speculated that the petrological contrasts across the unconformity are genetically associated with important climatic changes and/or rapid uplift episode(s) in the Transantarctic Mountains.
description: Supplement to: Smellie, John L (2000): Erosional history of the Transantarctic Mountains deduced from sand grain detrital modes in CRP-2/2A, Victoria Land Basin, Antarctica. Terra Antartica, 7(4), 545-552
DOI: 10.1594/pangaea.60017
title: Grain size analysis on sediment core OK92_2182
DOI: 10.1594/pangaea.80057
title: Physical properties of sediment core MD01-2400

description: Due to various technical problems with the MST, all MST data should be handled with care
DOI: 10.1594/pangaea.68886
title: Tab 6b, Grain size distribution of sediment core SO82_4-2
DOI: 10.1594/pangaea.184649
title: Physical oceanography and nutrients at station DYNAPROC_071
DOI: 10.1594/pangaea.401357
title: Water temperature and current velocity from surface drifter SVP_15673
DOI: 10.1594/pangaea.137231
title: Grain size composition of bottom sediments from East Asian marginal seas, core Ast-1983
DOI: 10.1594/pangaea.138100
title: Physical oceanography at station ANTARES-IV_TOWYO_158
DOI: 10.1594/pangaea.145262
title: Underway physical oceanography and carbon dioxide measurements during Ryofu Maru cruise RF0301

description: Detailed metadata description of each cruise doi:10.1594/PANGAEA.769638
DOI: 10.1594/pangaea.145279
title: Underway physical oceanography and carbon dioxide measurements during Ryofu Maru cruise RF0704

description: Detailed metadata description of each cruise doi:10.1594/PANGAEA.769638
DOI: 10.1594/pangaea.145285
title: Underway physical oceanography and carbon dioxide measurements during Prince of Seas cruise POS_225_94

description: Detailed metadata description of each cruise doi:10.1594/PANGAEA.769638
DOI: 10.1594/pangaea.79123
title: Sediment-water exchanges at LMER_SB_32_BC
DOI: 10.1594/pangaea.121845
title: Grain size composition of sediment core PSEE-25-2
DOI: 10.1594/pangaea.315991
title: Physical properties of sediment core MD02-2562

description: All physical properties shipboard data of IMAGES IX cruise should be considered validated, but due to various problems with the calibration of the instrument it is also to be considered as preliminary.
DOI: 10.1594/pangaea.115016
title: Physical oceanography around Spitsbergen in 1993 from CTD SVALB1993_9
DOI: 10.1594/pangaea.184747
title: Physical oceanography and nutrients at station DYNAPROC_231
DOI: 10.1594/pangaea.106533
title: Stable isotope analysis on sediment core HU90-013-013
DOI: 10.1594/pangaea.401922
title: Water temperature and current velocity from surface drifter SVP_21187
DOI: 10.1594/pangaea.66318
title: Stable isotope data of sediment core GEOFAR KF16
DOI: 10.1594/pangaea.137880
title: Oxygen concentration at station ANTARES-IV_TOWYO_271
DOI: 10.1594/pangaea.184703
title: Physical oceanography and nutrients at station DYNAPROC_138
DOI: 10.1594/pangaea.121719
title: Grain size composition of sediment core PS-1369
DOI: 10.1594/pangaea.401396
title: Water temperature and current velocity from surface drifter SVP_15906
DOI: 10.1594/pangaea.125340
title: Chemical composition of sediment core PS-1265
DOI: 10.1594/pangaea.184621
title: Physical oceanography and nutrients at station DYNAPROC_011
DOI: 10.1594/pangaea.104463
title: Grain size analysis of sediment core PG1180-5
DOI: 10.1594/pangaea.184795
title: Physical oceanography and nutrients at station DYNAPROC_279
DOI: 10.1594/pangaea.125407
title: Chemical composition of sediment core PS-1342
DOI: 10.1594/pangaea.186148
title: Stable isotope analysis on planktic foraminifera in sediment core CH119-12PG
DOI: 10.1594/pangaea.186150
title: Stable isotope analysis on planktic foraminifera in sediment core CH119-18PC
DOI: 10.1594/pangaea.186151
title: Stable isotope analysis on planktic foraminifera in sediment core CH119-18PG
DOI: 10.1594/pangaea.186152
title: Stable isotope analysis on planktic foraminifera in sediment core P6508-36B
DOI: 10.1594/pangaea.93019
title: Physical oceanography at station POS202/1b-CTD-765_005
DOI: 10.1594/pangaea.125150
title: Oxygen in pore water of sediment core TT013_77
DOI: 10.1594/pangaea.230035
title: Water content, carbon and carbonate analysis of sediment core Y80_107TC
DOI: 10.1594/pangaea.77504
title: Porewater chemistry of sediment profile Aurelia_08_1984_14
DOI: 10.1594/pangaea.263958
title: (Table 1) Stable oxygen isotope ratios of Neogloboquadrina pachyderma sinistral from sediment core V28-14
DOI: 10.1594/pangaea.358379
title: (Table 3) Stable isotope ratios of Neogloboquadrina pachyderma from sediment core HU77-149
DOI: 10.1594/pangaea.121725
title: Grain size composition of sediment core PS-1380
DOI: 10.1594/pangaea.126838
title: Heavy and light minerals in 100-50 µm size fraction of bottom sediments from core PS-1352
DOI: 10.1594/pangaea.137166
title: Chemical composition of non-metalliferous sediments from the Red Sea Rift Zone, core PS-258GR
DOI: 10.1594/pangaea.314747
title: Methane concentration in sediment core GT03-28GC
DOI: 10.1594/pangaea.57448
title: Total organic carbon in surface sediments of the Ob and Yenisei estuaries and adjacent coastal areas, appendix 1

description: Two main mechanisms are controlling the accumulation of organic matter in the sediments of the Kara Sea. The large rivers Ob and Yenisei supply significant quantities of freshwater onto the shelf (Lisitsyn and Vinogradov, 1995; Bobrovitskaya et al., 1996; Johnson et al., 1997) and deliver terrigenous organie matter and aquatic algae. Additionally, marine organic matter is produced in the water column.In order to distinguish between the different sources of the organic material maceral analysis, organic-geochemical bulk Parameters and biomarkers (short- and long-chain D-alkanes, fatty acids and pigments) were used to determine the quality (marine vs. terrigenous) and quantity of the organic carbon fraction in the surface sediments taken during the 28th cruise of RV Akademik Boris Petrov (Matthiessen and Stepanets, 1998) (Fig. 1). Previous organic-geochemical investigations (i.e., total organic-carbon content (TOC), hydrogen indices (Hl), CIN-ratios) indicate the importance of terrigenous input of organic matter (Galimov et al., 1996; Stein, 1996). Studies of lipid biomarkers in surface sediments in the Ob estuary show also a predominance of terrestrial constituents and an increase in planktonogenic and bacterial lipids further offshore (Belyaeva and Eglinton, 1997).In complex systems such as the Eurasian continental margin characterized by high input of terrestriallaquatic organic matter and strong seasonal variation in sea-ice Cover and primary productivity, the Interpretation of the organic geochemical data is much more complicated and restricted in comparison to similar data Sets from low-latitude open-ocean environments (Fahl and Stein, 1998). Microscopical studies (maceral analysisl palynology), however, allow a direct visual inspection of the particulate organic matter and allow to differentiate particles of different biological sources. Thus, a combination of both methods as shown in this study, yields a more precise identification of organic-carbon sources.
description: Supplement to: Boucsein, Bettina; Fahl, Kirsten; Siebold, Martina; Stein, Ruediger (1999): Quantity and quality of organic carbon in surface sediments of the Ob and Yenisei estuaries and adjacent coastal areas: marine productivity vs. terrigenous input. In: Matthiessen, J; Stepanets, O V; Stein, R; Fütterer, D K & Galimov, E M (eds.), The Kara Sea Expedition of RV Akademik Boris Petrov 1997: First Results of a Joint Russian-German Pilot Study, Reports on Polar Research, Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, 300, 116-126
DOI: 10.1594/pangaea.79366
title: Bolboforma abundance in sediment Hole 90-593
DOI: 10.1594/pangaea.67667
title: Color data of sediment core GeoB7174-5
DOI: 10.1594/pangaea.105711
title: Geochemistry of porewater in sediment core GeoB3706-3
DOI: 10.1594/pangaea.199780
title: Resistivity formation factor in sediment porewater profile CD86_02_BC5
DOI: 10.1594/pangaea.358953
title: Stable isotopes measured on foraminifera from the 120 kyr time slice reconstruction in sediment core V28-304
DOI: 10.1594/pangaea.101269
title: Smear slide analysis of Hole 38-352
DOI: 10.1594/pangaea.125338
title: Chemical composition of sediment core PSEE-8-2
DOI: 10.1594/pangaea.132175
title: Grain size composition of Pechora Sea bottom sediments from the core ASV13_1100-GC
DOI: 10.1594/pangaea.126932
title: Heavy and light minerals in 100-50 µm size fraction of bottom sediments from core PSEE-197
DOI: 10.1594/pangaea.140267
title: Nutrients in porewater of sediment profile 10BC35-2
DOI: 10.1594/pangaea.121778
title: Grain size composition of sediment core PS-894
DOI: 10.1594/pangaea.87882
title: Smear slide analysis of sediment core PM9462-1
DOI: 10.1594/pangaea.126788
title: Heavy and light minerals in 100-50 µm size fraction of bottom sediments from core PS-1299-1
DOI: 10.1594/pangaea.223652
title: Stable isotopes of sediment core GeoB2116-4
DOI: 10.1594/pangaea.66329
title: Sound velocity of sediment core GeoB3807-3
DOI: 10.1594/pangaea.77113
title: TOC, δ¹³C and accumulation rates of core KD9502-14, Laptev Sea

description: AGES after 14C ages of core KD9502-14 from Bauch et al. (1999) datataset: doi:10.1594/PANGAEA.85170, age is given in calibrated calendar years, CALIB 4.1.2 (Stuiver & Reimer, 1993)
DOI: 10.1594/pangaea.77507
title: Porewater chemistry of sediment profile Aurelia_08_1984_16
DOI: 10.1594/pangaea.357085
title: Paleoecological investigation of Hessische Senke at site NW2
DOI: 10.1594/pangaea.65424
title: Planktic foraminifera (%) of sediment core MD97-2151
DOI: 10.1594/pangaea.87875
title: Smear slide analysis of sediment core PM9402-3
DOI: 10.1594/pangaea.124145
title: Beam attenuation and transmissometer data from upcast at station TT007_5-MULVFS6
DOI: 10.1594/pangaea.76306
title: Nutrients in pore water in sediment core W8803B-T-57
DOI: 10.1594/pangaea.126857
title: Heavy and light minerals in 100-50 µm size fraction of bottom sediments from core PS-1394
DOI: 10.1594/pangaea.122922
title: Chemical composition of Barents Sea bottom sediments from the core ASV11-833
DOI: 10.1594/pangaea.77612
title: Benthic fluxes at lander station NH88-8_16_LANDER
DOI: 10.1594/pangaea.78947
title: Sediment characteristics at BS9522_LANDER
DOI: 10.1594/pangaea.104461
title: Grain size analysis of sediment core PG1180-3
DOI: 10.1594/pangaea.77980
title: Benthic fluxes at PACFLUX-II_W
DOI: 10.1594/pangaea.138716
title: Heavy metal contents in different size fractions of bottom sediments from the South China Sea, core Ast-8792
DOI: 10.1594/pangaea.122882
title: Chemical composition of surface sediments from the Norwegian Sea at the station AMK33-3277
DOI: 10.1594/pangaea.125891
title: Grain size composition of sediment core Kord-16
DOI: 10.1594/pangaea.54990
title: Carbonate content of sediment core CRP-1 (Table 1)

description: Determinations of total carbonate content yield additional information, in the context of integrated investigations, thus enabling or enhancing the interpretation and characterisation of the depositional environment, the processes of sedimentation and the diagenesis of sediments. In the case of drillcores, they help us to discern vertical gradations of facies sequences that have repeating patterns or show changes through time. This report presents initial results of carbonate investigations on a total of 32 bulk samples from the Quaternary and Miocene strata of the CRP-1 borehole, which reached a final depth of 147.69 metres below sea floor (mbsf). Fifteen out of a total of 18 lithostratigraphic units in the core were sampled (Tab. 1). Fourteen samples (24.85-43.85 mbsf) belong to the Quaternary, whereas 18 samples (44.53-146.51 mbsf) originate from the Miocene strata. The sampling intervals varied from 1-5 m for the Quaternary, and 1-15 m for the Miocene. All the samples originated from sections of core representing not more than 1 cm thickness.
description: Supplement to: Dietrich, Hans G; Klosa, D (1998): Carbonate contents in CRP-1 samples - initial results. Terra Antartica, 5(3), 645-646
DOI: 10.1594/pangaea.57631
title: Facies log of profile Abez
DOI: 10.1594/pangaea.125361
title: Chemical composition of sediment core PS-1289
DOI: 10.1594/pangaea.55799
title: Pollen analysis of sediment core PG1111

description: On the Taymyr Peninsula and Severnaya Zemlya Archipelago, Central Siberia, a joint German/Russian multidisciplinary research project focuses on the Late Quaternary history of climate and environment. Within the scope of this project, palynological studies were carried out on a 10.8-m core from Lama Lake, situated in the south-west of the research area. The core, which did not reach the base of the lacustrine sediments, reveals the vegetation and climate history of the last 17 000 years and demonstrates that this area was not glaciated during that time. The Pleistocene/Holocene transition is, as elsewhere in the northern hemisphere, characterized by increased temperatures during the Bølling, Allerød and Preboreal with interruptions during the Older (post-Bølling) and Younger Dryas events. The Holocene climate optimum at Lama Lake probably occurred within the Boreal period, when dense larch forests developed. The Atlantic period was characterized by warm conditions that favoured the establishment of larch-spruce forests, though a climatic deterioration is also recorded. During the Subboreal, spruce fluctuated in importance, on the basis of which it is suggested that there were two cool periods with an intervening warm period. Since 3000 B.P., the climate has become considerably cooler and forests have degenerated. During the last 1000 years, unfavourable climate conditions have resulted in a forest tundra and widespread tundra communities developing in the Lama Lake region.
description: Supplement to: Hahne, Jürgen; Melles, Martin (1997): Late and postglacial vegetation and climate history of the south-western Taymyr Peninsula (Central Siberia), as revealed by pollen analysis of sediments from Lama Lake. Vegetation History and Archaeobotany, 6(1), 1-8
DOI: 10.1594/pangaea.52199
title: Stable isotopes of sediment core RC27-61
DOI: 10.1594/pangaea.139214
title: Grain density in sediment core SO106-276KL
DOI: 10.1594/pangaea.101300
title: Smear slide analysis of Hole 47-397
DOI: 10.1594/pangaea.79004
title: Oxygen consumption at BS9719
DOI: 10.1594/pangaea.148947
title: Underway physical oceanography and carbon dioxide measurements during Ronald H. Brown cruise VENTS97L1

description: Detailed metadata description of each cruise doi:10.1594/PANGAEA.769638
DOI: 10.1594/pangaea.78655
title: Oxygen consumption at Adria1-Apr95
DOI: 10.1594/pangaea.269290
title: Hydrogen sulphide of pore water from sediment core GeoB6308-4
DOI: 10.1594/pangaea.97053
title: Sedimentation rates of Hole 39-354

description: compiled and calculated from various DSDP data sources
DOI: 10.1594/pangaea.385594
title: Nutrients in porewater of sediment profile 12926-002

description: Total carbonate (Ct) concentrations were determined on-board ship during Discovery 222 (leg A) nd 226 cruises, using colourmetric methods (Johnsson et al., 1987) with a precision of 0.2% RSD (n=10) using a sample loop of 4ml. During Discovery 231, 236 and Meteor 42/2 cruises a newly developed system (based on infrared detection of (CO2) were used for determination of total carbonate (Goyet and Snover, 1993; OSullivan and Millero, 1998). The precision of this method was also 0.2% RSD (n=10) using a sample loop of 4ml. Samples were filtrated through disposable sterile cellulose acetate filters (0.45µm) and stored refrigerated in polyethylene vials (rinsed in MQ-water) until analysis on-board.
DOI: 10.1594/pangaea.78739
title: Oxygen profiling at M-228
DOI: 10.1594/pangaea.78992
title: Oxygen consumption at BS9706
DOI: 10.1594/pangaea.97039
title: Sedimentation rates of Hole 38-339

description: compiled and calculated from various DSDP data sources
DOI: 10.1594/pangaea.77079
title: Carbon and carbonate content of core GEOFAR KG18 sediment samples
DOI: 10.1594/pangaea.78802
title: Oxygen consumption at Polar_93_54
DOI: 10.1594/pangaea.227294
title: Sedimentology of core GeoB2125-1
DOI: 10.1594/pangaea.126930
title: Heavy and light minerals in 100-50 µm size fraction of bottom sediments from core PSEE-195
DOI: 10.1594/pangaea.55438
title: Stable isotope ratios measured on foraminifera of DSDP Hole 30-289
DOI: 10.1594/pangaea.101488
title: Smear slide analysis of Hole 12-114
DOI: 10.1594/pangaea.77875
title: Benthic respiration at Cruise59_071
DOI: 10.1594/pangaea.77080
title: Carbon and carbonate content of core GEOFAR KS03 sediment samples
DOI: 10.1594/pangaea.105253
title: Clay mineralogy on sediment core CIROS-2
DOI: 10.1594/pangaea.122657
title: Chemical composition of bottom sediments from the core DM49-4391-1
DOI: 10.1594/pangaea.133759
title: Age model of DSDP Hole 28-266
DOI: 10.1594/pangaea.144868
title: Underway physical oceanography and carbon dioxide measurements during Cape Hatteras cruise SAB_200503

description: Detailed metadata description of each cruise doi:10.1594/PANGAEA.769638
DOI: 10.1594/pangaea.77480
title: Porewater chemistry of sediment profile Aurelia_08_1984_01
DOI: 10.1594/pangaea.78764
title: Oxygen consumption at Polar_92_42
DOI: 10.1594/pangaea.125993
title: Grain size composition of sediment core Kord-623
DOI: 10.1594/pangaea.227375
title: Sound velocity profile of sediment core SO106-276KL
DOI: 10.1594/pangaea.145269
title: Underway physical oceanography and carbon dioxide measurements during Ryofu Maru cruise RF0410

description: Detailed metadata description of each cruise doi:10.1594/PANGAEA.769638
DOI: 10.1594/pangaea.80715
title: Oceanographic and optical profile at station M56_92-113
DOI: 10.1594/pangaea.415860
title: (Table 1) Oxygen and carbon isotopic composition of Globigerina altispira in DSDP Site 30-289, Western Equatorial Pacific
DOI: 10.1594/pangaea.97134
title: Stable isotopes on coral Porites lobata core Caubyan_XIX
DOI: 10.15468/dl.pvbwds
title: Occurrence Download

description: A dataset containing 358 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Continent is South America",
 "TaxonKey is Plagiochila alternans Lindenb. & Gottsche"
 ]
}

 The dataset includes 358 records from 37 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031615-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.59889
title: (Table 2b) Stable isotope ratios of Globigerinoides sacculifer from sediment core KN11002-0043 in the equatorial Atlantic
DOI: 10.1594/pangaea.145290
title: Underway physical oceanography and carbon dioxide measurements during Prince of Seas cruise POS_067_95

description: Detailed metadata description of each cruise doi:10.1594/PANGAEA.769638
DOI: 10.1594/pangaea.145345
title: Underway physical oceanography and carbon dioxide measurements during SKAUGRAN cruise SK23W

description: Detailed metadata description of each cruise doi:10.1594/PANGAEA.769638
DOI: 10.1594/pangaea.407874
title: Stable isotopes of sediment core 75KS23

description: sieve larger than 63
DOI: 10.1594/pangaea.407876
title: Stable isotopes of sediment core 75KS31

description: sieve larger than 63
DOI: 10.1594/pangaea.407708
title: Density and stable isotopes of sediment core OD96_30:6:1
DOI: 10.1594/pangaea.407510
title: Stable isotopes of sediment core SH1972_17
DOI: 10.1594/pangaea.407515
title: Stable isotopes of sediment core KET82-16