cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.77526
title: Sediment-water exchanges at LMER_MB_16_BOTTLE
DOI: 10.1594/pangaea.77539
title: Sediment-water exchanges at LMER_NB_1_BOTTLE
DOI: 10.1594/pangaea.76435
title: Pressure (GTD) from mooring P4
DOI: 10.1594/pangaea.77311
title: Physical oceanography from CTD POS181_308
DOI: 10.1594/pangaea.77399
title: Biogeochemical properties of sediment profile NH88-8_06
DOI: 10.1594/pangaea.77629
title: Benthic fluxes at lander station W9106A_108_LANDER
DOI: 10.1594/pangaea.77312
title: Physical oceanography from CTD POS181_309
DOI: 10.1594/pangaea.77403
title: Biogeochemical properties of sediment profile NH88-8_18
DOI: 10.1594/pangaea.77404
title: Biogeochemical properties of sediment profile NH88-8_19
DOI: 10.1594/pangaea.327610
title: Bacteria abundance and dividing cells in sediment core GT03-31RL
DOI: 10.1594/pangaea.81039
title: Nutrients, chlorophyll a and nitrogen uptake rates of site P12 (1993-03-09)
DOI: 10.1594/pangaea.183751
title: (Appendix 1) Carbonate content in relation to sediment type described for sediment core CRP-3

description: Determinations of total carbonate contents in the CRP-3 core yield additional information and knowledge, in the context of integrated investigations, thus enabling or enhancing the interpretation and characterization of depositional environment, sedimentation, and diagenesis. In the case of drilling profiles, they help to discern vertical gradation of facies sequences with repeating patterns or with changes in time. A total of 98 bulk samples originating from the Palaeogene strata (Early Oligocene and ?Late Eocene) in the CRP-3 borehole were studied, the depth interval being 0-823.11 metres below sea floor (mbsf). Ages for the Cenozoic strata (Fig. 1) are taken from the Cape Roberts Science Team (2000a, 2000b), Bücker et al. (this volume), and Sagnotti et al. (2000, this vol.) and are shown in the columns A and B of figure 1. No investigations were performed on the underlying ?Devonian strata from 823.11-939.42 mbsf (final depth). Twenty-eight of a total of 34 lithostratigraphic Cenozoic units of the borehole were sampled (Appendix 1). Fourty-seven samples (8.97-349.78 mbsf) are from the Early Oligocene section, whereas 51 samples (357.80-788.94 mbsf) originate from the Early Oligocene or ?Late Eocene strata. The sampling intervals are on average about 5-9 m for the Early Oligocene section and about 6-11 in in the Early Oligocene/?Late Eocene strata. All the samples were taken from sections of the profile of not more than 1-2 cm thickness. The samples were split; the portions of the samples were used for investigations with regard to clay minerals (Ehrmann, this volume), heavy minerals (Ehrmann, this volume), and mineralogy as revealed by XRD analyses (Neumann & Ehrmann, this volume).
description: Supplement to: Dietrich, Hans G; Klosa, D; Wittich, C (2001): Carbonate content in CRP-3 drillcore, Victoria Land Basin, Antarctica. Terra Antartica, 8(3), 299-302
DOI: 10.1594/pangaea.75567
title: Smear slide analysis of sediment core LO09/1-1
DOI: 10.1594/pangaea.135033
title: Grain size composition of Barents Sea bottom sediments from the core ASV11-1006-2
DOI: 10.1594/pangaea.415942
title: Continuous meteorological surface measurement during THOMAS G THOMPSON cruise TT1996_3
DOI: 10.1594/pangaea.74110
title: Clay mineral distribution of ODP Hole 104-643A
DOI: 10.1594/pangaea.122761
title: Chemical composition of Norwegian Sea bottom sediments from the core AMK18-2074
DOI: 10.1594/pangaea.135042
title: Grain size composition of Barents Sea bottom sediments from the core ASV11-858-2
DOI: 10.1594/pangaea.74100
title: Clay mineral distribution of ODP Hole 104-642B
DOI: 10.1594/pangaea.74378
title: Documentation of sediment core SED-02

description: Sediment cores of project SEDANO (SEdiment Drifts of the ANtarctic Offshore)
DOI: 10.1594/pangaea.122691
title: Chemical composition of bottom sediments from the core DM49-4416-2
DOI: 10.1594/pangaea.314707
title: Dissolved inorganic carbon in sediment core GT03-28GC
DOI: 10.1594/pangaea.101248
title: Smear slide analysis of Hole 38-344
DOI: 10.1594/pangaea.314955
title: Methane, bicarbonate methanogenesis production rate in sediment core GT03-58VC
DOI: 10.1594/pangaea.81962
title: Sea surface chlorophyll concentration from upwelling radiances of buoy IOS_92-15_B4742

description: Battery voltage: 15V
DOI: 10.1594/pangaea.82165
title: Photosynthetic active radiation measurements of P4 (1990-02-07T14:30)
DOI: 10.1594/pangaea.88917
title: GISP2-D Borehole Geometry

description: Inclination and azimuth was meas. 1993, 1994, 1995 using Univy of Copenhagens geophysical logging system (UCPH), described by Gundestrup et al., (1994). Continued measurements will reveal the rate at which the ice is deforming as a function of depth in the ice sheet; ice deformation measurements are needed to constrain ice dynamics models developed for the GISP2 and GRIP sites. Given the slow deformation rates at GISP2, these measurements will need to be continued through at least 1999. Depth is true vertical depth
DOI: 10.1594/pangaea.327782
title: Dissolved inorcganic carbon in sediment core HE191_789
DOI: 10.1594/pangaea.80695
title: Oceanographic and optical profile at station M56_59-73
DOI: 10.15468/dl.rgdx3j
title: Occurrence Download

description: A dataset containing 494 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Continent is South America",
 "TaxonKey is Plagiochila adianthoides (Sw.) Lindenb."
 ]
}

 The dataset includes 494 records from 44 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031613-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.314674
title: Bacteria abundance in sediment core HE191_789
DOI: 10.1594/pangaea.315086
title: Methane, bicarbonate methanogenesis production rate in sediment core HE191_821
DOI: 10.1594/pangaea.70651
title: Colour measurements on sediment core MD01-2457 from Porcupine Basin

description: shipboard dataset
DOI: 10.1594/pangaea.82184
title: Light intensity of P20 (1990-05-15T18:00)
DOI: 10.1594/pangaea.70653
title: Colour measurements on sediment core MD01-2452 from Porcupine Basin

description: shipboard dataset
DOI: 10.1594/pangaea.185039
title: Physical oceanography from downcast CTD station HE208_703/04

description: Calibration of CTD was three years ago; use data with care !
DOI: 10.1594/pangaea.133751
title: Age model of DSDP Hole 24-236
DOI: 10.1594/pangaea.130364
title: Particulate matter concentration from filtered niskin bottles at station KIWI-9/2-6
DOI: 10.1594/pangaea.139215
title: Grain density in sediment core SO106-286KL
DOI: 10.1594/pangaea.68885
title: Tab 6a, Grain size distribution of sediment core SO82_2-2
DOI: 10.1594/pangaea.68581
title: Physical properties of sediment core MD01-2394

description: Due to various technical problems with the MST gear on board, all MST data of this core should be used with caution
DOI: 10.1594/pangaea.68582
title: Physical properties of sediment core MD01-2395

description: Due to various technical problems with the MST gear on board, all MST data of this core should be used with caution
DOI: 10.1594/pangaea.393906
title: Water temperature from profiling float 61700

description: The salinity profiles have been checked for spurious points as well as sensor drift. The drift correction has not been applied to each profile so ther is still a use at your own risk warning on them. Some original files had data thrown away and so filled the data with null values. These profiles have been removed from the data included here. Also if a temperature or salinity was missing, the pressure level has been removed from the profiles here. Trajectory file in NetCDF format: http://hs.pangaea.de/Projects/WOCE/PFLOAT/617_D.zip
DOI: 10.1594/pangaea.125996
title: Grain size composition of sediment core Kord-630
DOI: 10.1594/pangaea.59409
title: GeoB2108-1
DOI: 10.1594/pangaea.79098
title: Sediment-water exchanges at LMER_SB_29_BC
DOI: 10.1594/pangaea.68873
title: Geochemistry of sediment core AB_2
DOI: 10.1594/pangaea.93127
title: Physical oceanography at station POS212/2-CTD-800_013
DOI: 10.1594/pangaea.66462
title: Radiolaria abundance of sediment trap OG5
DOI: 10.1594/pangaea.385597
title: Nutrients in porewater of sediment profile 13077-096

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.104458
title: Grain size analysis of sediment core PG1178-2
DOI: 10.1594/pangaea.62183
title: Analysis of planktic foraminifera of station M39/4_402CTD-55
DOI: 10.1594/pangaea.126999
title: Heavy and light minerals in 100-50 µm size fraction of bottom sediments from core PSEE-8-1
DOI: 10.1594/pangaea.142131
title: (Table T11) Spectral reflectance data, ODP Hole 178-1098C
DOI: 10.1594/pangaea.138132
title: Physical oceanography at station ANTARES-IV_TOWYO_190
DOI: 10.1594/pangaea.137714
title: Oxygen concentration at station ANTARES-IV_TOWYO_106
DOI: 10.1594/pangaea.184680
title: Physical oceanography and nutrients at station DYNAPROC_115
DOI: 10.1594/pangaea.184787
title: Physical oceanography and nutrients at station DYNAPROC_271
DOI: 10.1594/pangaea.105252
title: (Fig. 4) Clay mineralogy on sediment core CIROS-1
DOI: 10.1594/pangaea.124160
title: Beam attenuation and transmissometer data from upcast at station TT011_4-MULVFS_TEST
DOI: 10.1594/pangaea.392861
title: Water temperature from profiling float 58700

description: Trajectory file in NetCDF format: http://hs.pangaea.de/Projects/WOCE/PFLOAT/587_D.zip
DOI: 10.15468/dl.g69w97
title: Occurrence Download

description: A dataset containing 222667 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is Specimen",
 "CoordinateUncertaintyInMeters 0.0-1000000.0",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "Issue is Geodetic datum assumed WGS84",
 "OccurrenceStatus is Present",
 "TaxonKey is Polypodiopsida"
 ]
}

 The dataset includes 222667 records from 299 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031610-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.59491
title: Pollen profile 2 from Hofstätter See, Bavaria, Germany
DOI: 10.1594/pangaea.59492
title: Pollen profile from Ledrosee site P1960
DOI: 10.1594/pangaea.59501
title: Pollen profile from Pian die Festa, Monte Baldo
DOI: 10.1594/pangaea.59445
title: (Table T1) Percentages of CaCO3, TOC, TN, TS of Site 175-1087

description: Site 1087 is located on the continental rise of southwest Africa at a water depth of 1371 m in the southern part of the Cape Basin. The site is part of the suite of Africa margin locations drilled during Leg 175 to reconstruct the onset and evolution of the elevated biological productivity associated with the Benguela Current upwelling system. Measurements of the amounts of inorganic and organic carbon that have accumulated in sediment under this major coastal upwelling regime are essential to this reconstruction, and these were routinely done for the first 12 sites occupied during Leg 175. However, determinations of calcium carbonate and organic carbon concentrations in sediments from Site 1087 had to be deferred to postcruise analysis because the JOIDES Resolution (JR) entered Cape Town 1 day after completing this site.Sediment samples were collected at intervals of three per core from Hole 1087A and the lower part of Hole 1087C to provide a survey of the histories of post-Eocene accumulation of calcium carbonate and organic carbon at this site. The samples were freeze-dried on the ship in preparation for subsequent shore-based analysis. Concentrations of calcium carbonate and organic carbon in the sediment samples were measured at the University of Michigan after the cruise. Organic matter atomic C/N ratios were employed to infer the origin of the organic matter contained within the sediments and to explore some of the factors affecting its preservation and accumulation.
description: Supplement to: Meyers, Philip A; Robinson, Rex J (2001): Data report: Carbonate and organic carbon contents of sediments from Site 1087, Southern Cape Basin. In: Wefer, G., Berger, W.H., and Richter, C. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, 175, 1-11
DOI: 10.1594/pangaea.59032
title: Color scan of sediment core MD98-2188
DOI: 10.1594/pangaea.59040
title: Color scan of sediment core MD98-2196
DOI: 10.1594/pangaea.101305
title: Smear slide analysis of Hole 48-400
DOI: 10.1594/pangaea.57946
title: Part of the Global Seawater Oxyge-18 database, Delaygue 2000
DOI: 10.1594/pangaea.58777
title: Diatom valves in sediment core KS82-30
DOI: 10.1594/pangaea.57989
title: (Table 1) Geochemistry of sediment core ANTA91-8

description: Ages are related to the lower side of core segments. They were calculated from a 230Thex profile after normalization for magnetic susceptibility using a constant flux-constant sedimentation model.
DOI: 10.1594/pangaea.58011
title: Conductivity of ice core ngt37C95.2 from the North Greenland Traverse
DOI: 10.1594/pangaea.58012
title: Conductivity of ice core ngt39C95.2 from the North Greenland Traverse
DOI: 10.1594/pangaea.58013
title: Conductivity of ice core ngt39C95.3 from the North Greenland Traverse
DOI: 10.1594/pangaea.58014
title: Conductivity of ice core ngt42C95.2 from the North Greenland Traverse
DOI: 10.1594/pangaea.58651
title: BENGAL carbon and nitrogen content in surface sediments
DOI: 10.1594/pangaea.58022
title: Permittivity of ice core ngt37C95.2 from the North Greenland Traverse
DOI: 10.1594/pangaea.78806
title: Oxygen consumption at Polar_93_71b
DOI: 10.1594/pangaea.58027
title: Permittivity of ice core ngt39C95.3 from the North Greenland Traverse
DOI: 10.1594/pangaea.58369
title: Oceanography at CTD/bottle station IFREMER_0002
DOI: 10.1594/pangaea.58028
title: Permittivity of ice core ngt42C95.2 from the North Greenland Traverse
DOI: 10.1594/pangaea.58371
title: Oceanography at CTD/bottle station IFREMER_0004
DOI: 10.1594/pangaea.58594
title: Chemistry versus depth in firn core DML07C98_31 (B31)
DOI: 10.1594/pangaea.58499
title: Chemistry versus depth in firn core DML17C98_33 (B33)
DOI: 10.1594/pangaea.57822
title: International Bathymetric Chart of the Arctic Ocean (IBCAO) in PanMap layer format

description: The PanMap Mini-GIS software is available at doi:10.1594/PANGAEA.104840.
DOI: 10.1594/pangaea.58554
title: Chemistry versus age in firn core DML03C98_09
DOI: 10.1594/pangaea.142633
title: Pollen profile from swamp at Rappershausen site 1, Grabfeld

description: Pollen zones after Firbas Ia-Xa
DOI: 10.1594/pangaea.57721
title: Elevation lines of modelled ice sheet extension during last glacial maximum

description: A numerical ice-sheet model was used to reconstruct the Late Weichselian glaciation of the Eurasian High Arctic, between Franz Josef Land and Severnaya Zemlya. An ice sheet was developed over the entire Eurasian High Arctic so that ice flow from the central Barents and Kara seas toward the northern Russian Arctic could be accounted for. An inverse approach to modeling was utilized, where ice-sheet results were forced to be compatible with geological information indicating ice-free conditions over the Taymyr Peninsula during the Late Weichselian. The model indicates complete glaciation of the Barents and Kara seas and predicts a “maximum-sized” ice sheet for the Late Weichselian Russian High Arctic. In this scenario, full-glacial conditions are characterized by a 1500-m-thick ice mass over the Barents Sea, from which ice flowed to the north and west within several bathymetric troughs as large ice streams. In contrast to this reconstruction, a “minimum” model of glaciation involves restricted glaciation in the Kara Sea, where the ice thickness is only 300 m in the south and which is free of ice in the north across Severnaya Zemlya. Our maximum reconstruction is compatible with geological information that indicates complete glaciation of the Barents Sea. However, geological data from Severnaya Zemlya suggest our minimum model is more relevant further east. This, in turn, implies a strong paleoclimatic gradient to colder and drier conditions eastward across the Eurasian Arctic during the Late Weichselian.
description: Data digized from graphic/data. stored in GF3-format
description: Supplement to: Siegert, Martin J; Dowdeswell, Julian A; Melles, Martin (1999): Late Weichselian glaciation of the Russian High Arctic. Quaternary Research, 52(3), 273-285
DOI: 10.1594/pangaea.57917
title: (Table 2) Part of the global seawater delta oxygen-18 database

description: Correction of PDB data to VSMOW standard. dVSMOW=dPDB+0.27
DOI: 10.1594/pangaea.57853
title: Part of the global seawater delta oxygen-18 database from reference Punning 1991
DOI: 10.1594/pangaea.57872
title: Part of the global seawater delta oxygen-18 database from reference Pierre 1986
DOI: 10.1594/pangaea.58555
title: Chemistry versus age in firn core DML15C98_14
DOI: 10.1594/pangaea.57873
title: Part of the global seawater delta oxygen-18 database from reference Pierre 1991
DOI: 10.1594/pangaea.58282
title: Facies description at sites Jouma1, Pikalevo 1, 2, 3 and Rayadan
DOI: 10.1594/pangaea.57896
title: Part of the global seawater delta oxygen-18 database from reference Ostlund 1987
DOI: 10.1594/pangaea.184708
title: Physical oceanography and nutrients at station DYNAPROC_143
DOI: 10.1594/pangaea.57894
title: Part of the global seawater delta oxygen-18 database from reference Macdonald 1995

description: Calibration to standard deep water mass =+0.3 offset added.
DOI: 10.1594/pangaea.57930
title: Part of the global seawater delta oxygen-18 database from reference Azetsu 1997
DOI: 10.1594/pangaea.56900
title: PKDB162175
DOI: 10.1594/pangaea.57945
title: Part of the global seawater delta oxygen-18 database from reference Boiseau 1999

description: Data anomalous ! (Schmidt)
DOI: 10.1594/pangaea.57952
title: Part of the global seawater delta oxygen-18 database from reference Craig 1965

description: Correction of SMOW data to GEOSECS standard by addition of 0.07. Positions and salinities partly read off a graph. Temperatures partly interpolated from nearby stations.
DOI: 10.1594/pangaea.57263
title: Age model of ice core VEF81
DOI: 10.1594/pangaea.57274
title: Crystal area of ice core LOM82

description: including data/personal communication of Samoilov, O Yu
DOI: 10.1594/pangaea.56901
title: PKDB162174
DOI: 10.1594/pangaea.57275
title: δ¹⁸O and chloride profile along ice core VAV79
DOI: 10.1594/pangaea.57295
title: Nitrate and sulphate in ice core ngt27C94.2 from the North Greenland Traverse
DOI: 10.1594/pangaea.57317
title: (Table A4) Composition of coarse fraction of sediment POS158/1_0001/1

description: Components of coarse fraction (125-500 µm) in grain percentages
DOI: 10.1594/pangaea.56902
title: PKDB162173
DOI: 10.1594/pangaea.57070
title: PKDB110606
DOI: 10.1594/pangaea.56782
title: PKDB161669
DOI: 10.1594/pangaea.57071
title: PKDB161510
DOI: 10.1594/pangaea.57085
title: PKDB286304
DOI: 10.1594/pangaea.57149
title: PKDB29462
DOI: 10.1594/pangaea.56783
title: PKDB161464
DOI: 10.1594/pangaea.57151
title: PKDB24637
DOI: 10.1594/pangaea.57319
title: (Table A10) Carbonate, total organic carbon and sulphur content of sediment POS158/1_0001/1
DOI: 10.1594/pangaea.56807
title: PKDB123510
DOI: 10.1594/pangaea.57076
title: Description of loess sections in China

description: The magnetic susceptibility of loess and paleosols in central China represents a proxy climate index closely related to past changes of precipitation and vegetation, and thus to summer monsoon intensity. Time series of magnetic susceptibility constructed for three loess-paleosol sequences in the southern part of the Chinese Loess Plateau document the history of summer monsoon variation during the last 130,000 yr. They correlate closely with the oxygen isotope record of stages 1 to 5 in deep-sea sediments. Soils were forming during intervals of strong summer monsoon, whereas loess units were deposited at times of reduced monsoon intensity. The Chinese loess-paleosol sequence can thus be viewed as a proxy record of Asian monsoon variability extending over the last 2.5 myr.
description: Supplement to: An, Zhisheng; Kukla, George J; Porter, Stephen C; Xiao, Jule (1991): Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of Central China during the last 130000 years. Quaternary Research, 36(1), 29-36
DOI: 10.1594/pangaea.57152
title: PKDB22743
DOI: 10.1594/pangaea.57505
title: appendix 1
DOI: 10.1594/pangaea.57114
title: PKDB286437
DOI: 10.1594/pangaea.57228
title: Age model of ice core VAV78/79
DOI: 10.1594/pangaea.57087
title: PKDB119925
DOI: 10.1594/pangaea.57256
title: Age model of ice core AMN80
DOI: 10.1594/pangaea.57261
title: Age model of ice core VAV83
DOI: 10.1594/pangaea.56814
title: PKDB27191
DOI: 10.1594/pangaea.57262
title: Age model of ice core VAV88
DOI: 10.1594/pangaea.57276
title: Temperature in snow profile VAV82a
DOI: 10.1594/pangaea.57093
title: Nitrate and sulphate in ice core ngt03C93.2 from the North Greenland Traverse
DOI: 10.1594/pangaea.56818
title: PKDB286490
DOI: 10.1594/pangaea.57281
title: Temperature in snow profile VAV84
DOI: 10.1594/pangaea.57053
title: Mineral assemblage in the sand fraction of sediment core CRP-2A investigated by smear slides (Table 4.3)

description: Empirical detrital modes of sand grains. Data are base on counts of 100 grains, using unstained smear slides, and they are qualitative.
DOI: 10.1594/pangaea.56728
title: PKDB158872
DOI: 10.1594/pangaea.57115
title: PKDB286436
DOI: 10.1594/pangaea.57116
title: PKDB286435
DOI: 10.1594/pangaea.56815
title: PKDB19627
DOI: 10.1594/pangaea.57096
title: PKDB24780
DOI: 10.1594/pangaea.57097
title: PKDB286302
DOI: 10.1594/pangaea.57117
title: PKDB286433
DOI: 10.1594/pangaea.57121
title: PKDB286302
DOI: 10.1594/pangaea.56821
title: PKDB286384
DOI: 10.1594/pangaea.57099
title: PKDB11138
DOI: 10.1594/pangaea.57108
title: PKDB3514
DOI: 10.1594/pangaea.57129
title: PKDB160675
DOI: 10.1594/pangaea.56753
title: PKDB4937
DOI: 10.1594/pangaea.57130
title: PKDB159905
DOI: 10.1594/pangaea.57147
title: PKDB67323
DOI: 10.1594/pangaea.57112
title: PKDB286440
DOI: 10.1594/pangaea.57159
title: PKDB19228
DOI: 10.1594/pangaea.56775
title: PKDB13831
DOI: 10.1594/pangaea.57161
title: PKDB14117