cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.898500
title: Water level and storage changes of Bamco lake during 2000‒2017

description: Following information is included:1) Date of the data acquisition time in the form of yyyy-mm-dd.2) Lake water levels are orthometric heights with respect to EGM96, WGS84, in the unit of meter.3) Uncertainty of the lake water level in the unit of meter, if it is altimetry water level. The uncertainty of optical water levels was not calculated and set to 0.4) Lake water storage changes with respect to the baseline (lake water storage of the water level baseline H0, which is a value we do not exactly know; see https://doi.pangaea.de/10.1594/PANGAEA.898409) in the unit of km^3.5) The source of the data, 0 - Landsat, 1 - Envisat, 2 - ICESat, 3 - CryoSat, 4 - Jason-1/2/3.
DOI: 10.1594/pangaea.693597
title: Mesozooplankton average length during Akademik Kovalevsky cruise AK62, Part II

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 125 µm. 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 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.898479
title: Radiosonde measurements from station Bondville (2018-09)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.898864
title: Radiosonde measurements from station Boulder, SURFRAD (2018-12)

description: Start location: Denver, CO; Distance from radiation site: 40 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.898480
title: Other measurements at 10 m from station Bondville (2018-09)
DOI: 10.1594/pangaea.900142
title: Meteorological synoptical observations from station Sonnblick (2019-02)
DOI: 10.1594/pangaea.898472
title: Other measurements at 10 m from station Bondville (2018-07)
DOI: 10.1594/pangaea.719562
title: Ultra-violet measurements from station Bondville (2002-10)

description: Version 2, 2009-06-15. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-09.
DOI: 10.1594/pangaea.807320
title: (Table 1) Concentration of pollutants in hair of East Greenland polar bears (Ursus maritimus)

description: Hair sampled from 96 East Greenland polar bears (Ursus maritimus) over the periods 1892-1927 and 1988-2009 was analyzed for cortisol as a proxy to investigate temporal patterns of environmental stress. Cortisol concentration was independent of sex and age, and was found at significantly higher (p&lt;0.001) concentrations in historical hair samples (1892-1927; n = 8) relative to recent ones (1988-2009; n = 88). In addition, there was a linear time trend in cortisol concentration of the recent samples (p&lt; 0.01), with an annual decrease of 2.7%. The recent hair samples were also analyzed for major bioaccumulative, persistent organic pollutants (POPs). There were no obvious POP related time trends or correlations between hair cortisol and hair POP concentrations. Thus, polar bear hair appears to be a relatively poor indicator of the animal's general POP load in adipose tissue. However, further investigations are warranted to explore the reasons for the temporal decrease found in the bears' hair cortisol levels.
description: All concentrations per g hair, dry weight. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
description: Supplement to: Bechshøft, Thea Ø; Rigét, Frank F; Sonne, Christian; Letcher, Robert J; Muir, Derek C G; Novak, M A; Henchey, E; Meyer, J S; Eulaers, I; Jaspers, Veerle LB; Eens, Marcel; Covaci, Adrian; Dietz, Rune (2012): Measuring environmental stress in East Greenland polar bears, 1892-1927 and 1988-2009: What does hair cortisol tell us? Environment International, 45, 15-21
DOI: 10.1594/pangaea.898439
title: Radiosonde measurements from station Bondville (2017-11)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.898526
title: Water level and storage changes of Ngangze Co lake during 2000‒2017

description: Following information is included:1) Date of the data acquisition time in the form of yyyy-mm-dd.2) Lake water levels are orthometric heights with respect to EGM96, T/P, in the unit of meter.3) Uncertainty of the lake water level in the unit of meter, if it is altimetry water level. The uncertainty of optical water levels was not calculated and set to 0.4) Lake water storage changes with respect to the baseline (lake water storage of the water level baseline H0, which is a value we do not exactly know; see https://doi.pangaea.de/10.1594/PANGAEA.898409) in the unit of km^3.5) The source of the data, 0 - Landsat, 1 - Envisat, 2 - ICESat, 3 - CryoSat, 4 - Jason-1/2/3.
DOI: 10.1594/pangaea.898527
title: Water level and storage changes of Ngoring lake during 2000‒2017

description: Following information is included:1) Date of the data acquisition time in the form of yyyy-mm-dd.2) Lake water levels are orthometric heights with respect to EGM96, T/P, in the unit of meter.3) Uncertainty of the lake water level in the unit of meter, if it is altimetry water level. The uncertainty of optical water levels was not calculated and set to 0.4) Lake water storage changes with respect to the baseline (lake water storage of the water level baseline H0, which is a value we do not exactly know; see https://doi.pangaea.de/10.1594/PANGAEA.898409) in the unit of km^3.5) The source of the data, 0 - Landsat, 1 - Envisat, 2 - ICESat, 3 - CryoSat, 4 - Jason-1/2/3.
DOI: 10.1594/pangaea.931273
title: GDGT concentration of sediment core MD-2
DOI: 10.1594/pangaea.935021
title: Age determination of Mosaik T1 (MOS_T1) peat core from Canada

description: 14C and 210Pb age determination of a high-resolution peat core from the Past Global Changes - Carbon in Peat on EArth through Time (PAGES_C-PEAT) Project.
DOI: 10.1594/pangaea.898466
title: Radiosonde measurements from station Bondville (2018-06)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.935092
title: Age determination of Beretta (MRB13_3) peat core from Canada

description: 14C and 210Pb age determination of a high-resolution peat core from the Past Global Changes - Carbon in Peat on EArth through Time (PAGES_C-PEAT) Project.
DOI: 10.1594/pangaea.774378
title: MSCL measurements from IODP Hole 316-C0008B

description: Update on 2018-01-19: Parameter 'Susceptibility, volume' has been converted from [10**-5 SI] to [10**-6 SI]. All values were previously given in the wrong unit.
DOI: 10.1594/pangaea.894754
title: Remote sensing quantifies widespread abundance of permafrost region disturbances across the Arctic and Subarctic, RTS dataset

description: The RTS datasets contain the perimeters of detected active retrogressive thaw slumps.Vector format: ESRI ShapefileProjection: Geographic WGS84 (EPSG:4326)Vector type: PolygonThe datasets are documented in detail in the linked document (Nitze_etal_2018: Data Documentation v1.0).
DOI: 10.1594/pangaea.898516
title: Water level and storage changes of Kusai lake during 2000‒2017

description: Following information is included:1) Date of the data acquisition time in the form of yyyy-mm-dd.2) Lake water levels are orthometric heights with respect to EGM96, T/P, in the unit of meter.3) Uncertainty of the lake water level in the unit of meter, if it is altimetry water level. The uncertainty of optical water levels was not calculated and set to 0.4) Lake water storage changes with respect to the baseline (lake water storage of the water level baseline H0, which is a value we do not exactly know; see https://doi.pangaea.de/10.1594/PANGAEA.898409) in the unit of km^3.5) The source of the data, 0 - Landsat, 1 - Envisat, 2 - ICESat, 3 - CryoSat, 4 - Jason-1/2/3.
DOI: 10.1594/pangaea.898517
title: Water level and storage changes of Kyebxang Co lake during 2000‒2017

description: Following information is included:1) Date of the data acquisition time in the form of yyyy-mm-dd.2) Lake water levels are orthometric heights with respect to EGM96, WGS84, in the unit of meter.3) Uncertainty of the lake water level in the unit of meter, if it is altimetry water level. The uncertainty of optical water levels was not calculated and set to 0.4) Lake water storage changes with respect to the baseline (lake water storage of the water level baseline H0, which is a value we do not exactly know; see https://doi.pangaea.de/10.1594/PANGAEA.898409) in the unit of km^3.5) The source of the data, 0 - Landsat, 1 - Envisat, 2 - ICESat, 3 - CryoSat, 4 - Jason-1/2/3.
DOI: 10.1594/pangaea.949525
title: Raw pollen counts from sediment core KBS 2 of lake Jezioro Skorupiaki in western Poland
DOI: 10.1594/pangaea.931269
title: GDGT concentration of sediment core MD-1
DOI: 10.1594/pangaea.949523
title: Radiocarbon dates from the combined sediment core (Wus 1, Wus 3) of lake Jezioro Ostrow in western Poland
DOI: 10.1594/pangaea.955839
title: δ18O and δ13C and Oxcal deposition model interpolated ages of stalagmite SIB-4 from Sibaki Cave, Southwestern Iran

description: Samples for carbon and oxygen isotopic analysis were micromilled at 3.0 and 0.2 mm increments along the main growth axis. Approximately 3000 samples were measured using a semi-automated gas preparation and introduction system (Gasbench II) linked to a Delta V Plus isotope ratio mass spectrometer (both ThermoFisher) at the University of Innsbruck, following the methods of Spötl and Vennemann (2003). Isotope values are reported relative to the Vienna Pee Dee Belemnite (VPDB) reference. Long-term analytical precision is better than 0.1‰ (1σ) for both δ13C and δ18O.
DOI: 10.1594/pangaea.733179
title: Physical oceanography during Moana Wave cruise HOT-37 on section PRS2
DOI: 10.1594/pangaea.719526
title: Ultra-violet measurements from station Bondville (2002-01)

description: Version 2, 2009-06-15. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-09.
DOI: 10.1594/pangaea.918549
title: The Antarctic crust and upper mantle: a flexible 3D model and framework for interdisciplinary research

description: Example outputs from agrid model.ant_gia_dem_0.tiff is a simplified GIA model, using seismic data to constrain lithosphere thickness and crustal thickness.Aq0.tiff is a steady-state heat flow model with a simple segmented crust, but not including neotectonism. The values in particularly West Antarctica is therefore underestimated.
DOI: 10.1594/pangaea.750921
title: Meteorological observations during Nieuw Lekkerland cruise from Batavia to the Netherlands started at 1849-11-11
DOI: 10.1594/pangaea.691477
title: Monthly landings in 1998, Tongoy, Chile
DOI: 10.1594/pangaea.949533
title: Stratigraphic description from peat core L1.00 of the Pawki Ług mire in western Poland
DOI: 10.1594/pangaea.691017
title: Mesozooplankton average length during Akademik Kovalevsky cruise AK7/3, Part II

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 0.145 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, 200-500 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.949530
title: Raw pollen counts from peat core L1.00 of the Pawki Ług mire in western Poland
DOI: 10.1594/pangaea.955974
title: Measured isotope activity ratios, calculated ages and monte-carlo derived age error, and Oxcal deposition model U-Th ages and associated age error of the stalagmite SIB-4 from Sibaki Cave, Southwestern Iran

description: A total of 32 230Th ages were measured along the growth axis of SIB-4 stalagmite. 100-200 mg of calcite powder was drilled per sample in a laminar-flow hood following growth lamina. The samples were chemically prepared at the Department of Earth Sciences, University of Oxford. The samples were spiked with a mixed 229Th-236U spike, dissolved in HNO3 and refluxed on a hot-plate overnight for spike-sample equilibration. Chemical separation of U and Th was done following procedures adapted from Edwards et al. (1987). The separated U and Th fractions were analysed on a Nu Plasma multi-collector inductively coupled plasma mass spectrometer, following the procedure described in Carolin et al. (2019). Individual 230Th ages with their 95% confidence intervals were calculated using an in-house Monte Carlo script that incorporates chemical blank errors, analytical uncertainties and initial 230Th/232Th uncertainties. The initial 230Th/232Th (atomic ratio) is estimated to be between 0.5 to 10.8 ppm (uniform distribution), equivalent to an activity ratio of 0.1 to 2.0. This range encompasses both the bulk earth value (230Th/232Th activity = 0.82) and the median detritus value calculated in a collection of speleothem studies (230Th/232Th activity = 1.5) (Hellstrom, 2006). Notably, SIB-4 samples exhibit large 230Th/232Th, with 90% of samples showing 230Th/232Th activity greater than 1000. This is due to high U content and low detrital Th content of the stalagmite. Thus, the age corrections related to detrital contamination are small (median of just 4 years), which is much less than the overall age error of ca. 100 years (2s).
DOI: 10.1594/pangaea.773357
title: (Table T2) Clinopyroxene compositions and structural formulas of ODP Site 200-1224 Eocene ferrobasalts

description: Atomic formulae calculated on the basis of six oxygens. Element oxides in wt%.
DOI: 10.1594/pangaea.913044
title: Pluviographic observations of rainfall at station Kur'ya (76027)
DOI: 10.1594/pangaea.719506
title: Ultra-violet measurements from station Bondville (2001-08)

description: Version 2, 2009-06-15. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-09.
DOI: 10.1594/pangaea.719536
title: Other measurements at 10 m from station Bondville (2002-03)

description: Version 2, 2009-06-15
DOI: 10.1594/pangaea.733137
title: Radiosonde measurements from station Sede Boqer (2008-12)

description: Start location: Bet-Dagan,Israel; Distance from radiation site: 120 km
DOI: 10.1594/pangaea.949526
title: Radiocarbon dates from sediment core KBS 2 of lake Jezioro Skorupiaki in western Poland
DOI: 10.1594/pangaea.949528
title: Stratigraphic description from sediment core KBS 2 of lake Jezioro Skorupiaki in western Poland
DOI: 10.1594/pangaea.886284
title: TRIOS standard deviation of upwelling radiance gathered at three turbid estuarine sites (Gironde, La Plata, Scheldt)
DOI: 10.1594/pangaea.693638
title: Mesozooplankton average mass during Akademik Kovalevsky cruise AK95, Part II

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 125 µm. 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 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.494679
title: Physical oceanography during cruise K7477XXXXXC
DOI: 10.1594/pangaea.892925
title: Multiple proxies for sediment core P1-93AR-P23 collected from the Northwind Ridge, western Arctic Ocean
DOI: 10.1594/pangaea.892924
title: Multiple proxies for sediment core HLY0503-03JPC collected from the Northwind Ridge, western Arctic Ocean
DOI: 10.1594/pangaea.899812
title: Dinoflagellate cyst production index of sediment cores of the southwest Pacific
DOI: 10.1594/pangaea.883524
title: Valleys of Herschel Island, Yukon, Canada

description: The dataset is composed of 2 shapefiles including the main delineated drainage basins and manually digitized valleys of Herschel Island, Yukon Territory, Canada.The main valleys of Herschel Island (valleys_Herschel.shp) are mapped based on a GeoEye-1 multispectral satellite image acquired on 31.08.2011.The main drainage basins of Herschel Island (basins_Herschel.shp) were created on ArcGIS 10.3 using the watershed Tool. Flow direction and Flow accumulation were derived from a 12-m Intermediate Digital Elevation Model acquired in 2012, TanDEM-X data © DLR &lt;2015&gt;.
DOI: 10.1594/pangaea.884551
title: Individual stomach content of herring and sprat collected during a field cruise in the NE Baltic Sea, July 2015
DOI: 10.1594/pangaea.949522
title: Raw pollen counts from the combined sediment core (Wus 1, Wus 3) of lake Jezioro Ostrow in western Poland
DOI: 10.1594/pangaea.897875
title: Rare earth element (REE) concentrations from bulk sediment leachates of sediment core HLY0501-01JPC from the Chukchi sea margin
DOI: 10.1594/pangaea.808054
title: (Table 1) Total organic carbon, calcium carbonate and nitrogen at DSDP Holes 80-559 and 80-550B

description: Concentrations of organic and inorganic nitrogen have been measured on Leg 80 sediments. The inorganic nitrogen content is relatively constant, 0.02-0.03 wt.%. Because most of the inorganic nitrogen occurs as NH3 or (NH4)+ fixed on clays, clay-poor sediments have lower inorganic nitrogen contents.Organic nitrogen content depends upon both the type and the quantity of organic matter present. In Leg 80 sediments, woody kerogens contain much less organic nitrogen than do kerogens of algal origin. Furthermore, pelagic samples of low organic carbon content have less organic nitrogen than predicted, because of loss during diagenesis.DSDP shipboard analytical procedures do not distinguish between organic and inorganic nitrogen. Great caution must therefore be exercised in interpreting C/N ratios.
description: Supplement to: Waples, Douglas W (1985): Organic and inorganic nitrogen in sediments from Leg 80, Deep Sea Drilling Project. In: De Graciansky, PC; Poag, CW; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Gov. Printing Office), 80, 993-997
DOI: 10.1594/pangaea.915072
title: Ceilometer raw data measured at Neumayer Station (2019-10), links to files

description: The ceilometer is mounted on the roof of the station building, the height offset was set to 25m. This offset only affects the detected cloud levels, not the full backscatter profile.
DOI: 10.1594/pangaea.885347
title: Basic measurements of radiation at station Billings (2013-04)
DOI: 10.1594/pangaea.886282
title: TRIOS standard deviation of downwelling sky radiance gathered at three turbid estuarine sites (Gironde, La Plata, Scheldt)
DOI: 10.1594/pangaea.755465
title: (Table 5) Contents of radioactive elements and main components of chemical composition in bottom sediments from Station DM8-572
DOI: 10.1594/pangaea.917826
title: Stable isotope ratios of benthic foraminifera of sediment core MD07-3082
DOI: 10.1594/pangaea.755434
title: (Table 1b) Composition of alkanes in bottom sediments from the Baltic Sea
DOI: 10.1594/pangaea.933214
title: Tethered balloon-borne meteorological measurements during the Arctic field campaign PAMARCMiP (Balloon_20180329_1752_2216)

description: New version with revised wind speed calibration for the standard meteorology sonde.
DOI: 10.1594/pangaea.845428
title: Ceilometer raw data measured at Neumayer Station (2014-11), links to files
DOI: 10.1594/pangaea.915083
title: Radiosonde raw data from Neumayer Station (2019-03), links to files
DOI: 10.1594/pangaea.897879
title: Clay mineralogical of sediment core HLY0501-01JPC from the Chukchi sea margin
DOI: 10.1594/pangaea.897878
title: Bulk mineralogical of sediment core HLY0501-01JPC from the Chukchi sea margin
DOI: 10.1594/pangaea.886285
title: TRIOS upwelling radiance gathered at three turbid estuarine sites (Gironde, La Plata, Scheldt)
DOI: 10.1594/pangaea.886283
title: TRIOS downwelling sky radiance gathered at three turbid estuarine sites (Gironde, La Plata, Scheldt)
DOI: 10.1594/pangaea.933200
title: Tethered balloon-borne meteorological measurements during the Arctic field campaign PAMARCMiP (Balloon_20180321_1737_1937)

description: New version with revised wind speed calibration for the standard meteorology sonde.
DOI: 10.1594/pangaea.898947
title: Temperature percentiles thresholds in Naples, Italy, for the base period 1961-1990
DOI: 10.1594/pangaea.933204
title: Tethered balloon-borne meteorological measurements during the Arctic field campaign PAMARCMiP (Balloon_20180324_1346_1453)

description: New version with revised wind speed calibration for the standard meteorology sonde.
DOI: 10.1594/pangaea.755394
title: (Table 1a) Sea surface temperatures and paleotemperatures off the Northwestern Africa in the area of the Canary upwelling
DOI: 10.1594/pangaea.949531
title: Radiocarbon dates from peat core L1.00 of the Pawki Ług mire in western Poland
DOI: 10.1594/pangaea.782579
title: X-ray microfocus computer tomography (MiXCT) from EDML ice core, from 150 to 150.57179 m, reconstruction, links to data

description: See raw data at doi:10.1594/PANGAEA.782578
DOI: 10.1594/pangaea.917829
title: Stable isotope ratios of benthic foraminifera of sediment core MD07-3119
DOI: 10.1594/pangaea.898944
title: Temperature percentiles thresholds in Barcelona, Spain, for the base period 1961-1990
DOI: 10.1594/pangaea.755438
title: (Table 2) Uranium concentrations and isotopic ratios in surface waters of the Atlantic Ocean in April 1977

description: Uranium concentrations and isotope ratios were measured in thirteen surface-water samples collected across the entire Atlantic Ocean. The mean isotope ratio was 1.15+/-0.01, and the mean concentration 3.1+/-0.2 µg/l.
description: Supplement to: Kuptsov, Vladimir M; Cheshko, Andrey L (1981): Uranium in North Atlantic surface waters. Oceanology, 21(6), 708-711
DOI: 10.1594/pangaea.898945
title: Temperature percentiles thresholds in Lisbon, Portugal, for the base period 1961-1990
DOI: 10.1594/pangaea.900455
title: Radiosonde raw data from Neumayer Station (2018-02), links to files

description: A software update on the sounding system results in different file formats, namely "dc3db" for the old software and "mwx" for the new software.
DOI: 10.1594/pangaea.834346
title: Ceilometer raw data measured at Neumayer Station (2010-04), links to files
DOI: 10.1594/pangaea.898410
title: Water level and storage changes of Ake Sayi lake during 2000‒2017

description: Following information is included:1) Date of the data acquisition time in the form of yyyy-mm-dd.2) Lake water levels are orthometric heights with respect to EGM08, WGS84, in the unit of meter.3) Uncertainty of the lake water level in the unit of meter, if it is altimetry water level. The uncertainty of optical water levels was not calculated and set to 0.4) Lake water storage changes with respect to the baseline (lake water storage of the water level baseline H0, which is a value we do not exactly know; see https://doi.pangaea.de/10.1594/PANGAEA.898409) in the unit of km^3.5) The source of the data, 0 - Landsat, 1 - Envisat, 2 - ICESat, 3 - CryoSat, 4 - Jason-1/2/3.