cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.711935
title: Pollen profile MUCKROSS, Muckross, Ireland

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.911083
title: Other measurements at 10 m from station Southern Great Plains (1997-04)

description: Version 2, 2020-01-21, with better quality control applied.
DOI: 10.1594/pangaea.778493
title: (Appendix A3) Major element concentration in ODP Hole 129-802A sediments
DOI: 10.1594/pangaea.498723
title: Physical oceanography from BT during cruise U90X007573B_1976
DOI: 10.1594/pangaea.763338
title: Weekly growth of mussel Mytilus edulis, 2010
DOI: 10.1594/pangaea.749378
title: Meteorological observations during GARLAND cruise from Spithead to St. Johns started at 1779-10-25
DOI: 10.1594/pangaea.875288
title: Snow height on sea ice and sea ice drift from autonomous measurements from buoy 2016S37, deployed during POLARSTERN cruise PS96 (ANT-XXXI/2)

description: Snow height was measured by the Snow Depth Buoy 2016S37, an autonomous platform, drifting on Antarctic sea ice, during POLARSTERN cruise PS96 (ANT-XXXI/2). The resulting time series describes the evolution of snow depth as a function of place and time between 18 Jan 2016 and 24 Dec 2016 in sample intervals of 1 hour. The Snow Depth Buoy consists of four independent sonar measurements representing the area (approx. 10 m**2) around the buoy. The buoy was installed on multi year ice. In addition to snow depth, geographic position (GPS), barometric pressure, air temperature, and an internal ice temperature were measured. Negative values of snow depth occur if surface ablation continues into the sea ice. Thus, these measurements describe the position of the sea ice surface relative to the original snow-ice interface. Differences between single sensors indicate small-scale variability of the snow pack around the buoy. The data set has been processed, including the removal of obvious inconsistencies (missing values). Records without any snow depth may still be used for sea ice drift analyses.
DOI: 10.1594/pangaea.738367
title: (Table 5) Chemical composition of different size fractions from clastic rocks

description: SiO2 to P2O5 contents have been determined by E.V. Cherkasova and N.L. Kalashnikova, Cr to Mo - by A.I. Gusarova (Geological Institute, USSR Acad. Sci.), Zn to Ce - by Yu.I. Pronin (Institute of Mineralogy, Geochemistry and Crystallochemistry of Rare Elements)
DOI: 10.1594/pangaea.916703
title: 1-Hz PPP displacements at GEONET station 0507 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.695807
title: Documentation of sediment core GIK12558-2
DOI: 10.1594/pangaea.870143
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_IX_09
DOI: 10.1594/pangaea.859770
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE404
DOI: 10.1594/pangaea.885985
title: Basic measurements of radiation at station Billings (2012-03)

description: Version 2, 2018-02-06, including temperature, humidity and pressure data.
DOI: 10.1594/pangaea.763152
title: Mineralogy of serpentine muds of ODP Leg 125 holes (Table 1)

description: Large serpentinite seamounts are common in the forearc regions between the trench axis and the active volcanic fronts of the Mariana and Izu-Bonin intraoceanic arcs. The seamounts apparently form both as mud volcanoes, composed of unconsolidated serpentine mud flows that have entrained metamorphosed ultramafic and mafic rocks, and as horst blocks, possibly diapirically emplaced, of serpentinized ultramafics partially draped with unconsolidated serpentine slump deposits and mud flows. The clayand silt-sized serpentine recovered from three sites on Conical Seamount on the Mariana forearc region and from two sites on Torishima Forearc Seamount on the Izu-Bonin forearc region is composed predominantly of chrysotile, brucite, chlorite, and clays. A variety of accessory minerals attest to the presence of unusual pore fluids in some of the samples. Aragonite, unstable at the depths at which the serpentine deposits were drilled, is present in many of the surficial cores from Conical Seamount. Sjogrenite minerals, commonly found as weathering products of serpentine resulting from interaction with groundwater, are found in most of the samples. The presence of aragonite and carbonate-hydroxide hydrate minerals argues for interaction of the serpentine deposits with fluids other than seawater.There are numerous examples of sedimentary serpentinite deposits exposed on land that are very similar to the deposits recovered from the serpentine seamounts drilled on ODP Leg 125. We suggest that Conical Seamount may be a type locality for the study of in situ formation of many of these sedimentary serpentinite bodies. Further, we suggest that both the deposits drilled on Conical Seamount and on Torishima Forearc Seamount demonstrate that serpentinization can continue in situ within the seamounts through interaction of the serpentine deposits with both seawater and subduction-related fluids.
description: X = definitely present, x = probably present, ?x = possible present, ? = questionable, - = absent. Analysed on bulk samples.
description: Supplement to: Fryer, Patricia B; Mottl, Michael J (1992): Lithology, mineralogy, and origin of serpentine muds recovered from Conical and Torishima Forearc Seamounts: Results of Leg 125 drilling. In: Fryer, P; Pearce, JA; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 125, 343-362
DOI: 10.1594/pangaea.778672
title: Helicopter-borne sea ice thickness measurements from the CASIMBO field program in spring 2010 from flight HEM_CAS10_01b
DOI: 10.1594/pangaea.718478
title: Radiosonde measurements from station Boulder, SURFRAD (2000-01)

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; Version 2, 2009-06-12
DOI: 10.1594/pangaea.721572
title: Ultra-violet measurements from station Fort Peck (2002-01)

description: Version 2, 2009-06-19. 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 2017-02-03.
DOI: 10.1594/pangaea.694970
title: Concentrations of chlorophyll-alpha in water of the Ionian Sea at Station SEPT-2000-IRI32

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore filters. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).
DOI: 10.1594/pangaea.872121
title: Water temperature at time series station Liliguapi, Paso Comau, Patagonia, Chile in 2016/2017

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de).
DOI: 10.1594/pangaea.854518
title: Glacier mass balance Vernagtferner, Schwarzwand area, Austria, 1976/1977
DOI: 10.1594/pangaea.895600
title: Distribution of soil n-alkane δD along an altitudinal transect in the Jimma zone of the southwest Ethiopian highlands
DOI: 10.1594/pangaea.840545
title: (Tables 5-8) Concentrations of heavy metals in earthworms, in vegetation and in wood mice kidneys obtained from Heteren and Plateaux, The Netherlands

description: All concentrations are given in mg/kg dry weight.
DOI: 10.1594/pangaea.885986
title: Basic measurements of radiation at station Billings (2012-04)

description: Version 2, 2018-02-06, including temperature, humidity and pressure data.
DOI: 10.1594/pangaea.739245
title: Pollen profile GAMPERF, Gamperfin, Switzerland

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.896034
title: Arsenic content of porewater samples in two lakes in the Puget Sound lowland (2016-2018)
DOI: 10.1594/pangaea.760135
title: (Table 8) Bio- and magnetostratigraphic events of ODP Hole 120-751A
DOI: 10.1594/pangaea.778425
title: (Table 3) Bulk mineralogical composition of the sediments from ODP Hole 129-800A

description: Sediment depth is given in mbsf. T = traces, P = present, X = relative abundance, M = mixture of volcanic minerals (with feldspar, pyroxenes and olivines)
DOI: 10.1594/pangaea.734218
title: (Table 18) Chemical composition of Mesozoic and Cenozoic deposits from DSDP Holes 62-465 and 62-465A (on terrigenous-free carbonate-free silica-free basis)

description: Empty cells = not found.
DOI: 10.1594/pangaea.907276
title: Track of GPS very-near surface drifter ISMER_20150805_spot700
DOI: 10.1594/pangaea.933480
title: Meteorological synoptical observations from station Toravere (2020-11)
DOI: 10.1594/pangaea.587145
title: Physical oceanography at CTD station M1_CTD263 of the Persian Gulf
DOI: 10.1594/pangaea.849441
title: Ground-penetrating radar (GPR) point measurements of ice thickness on Gaisskarferner in 1995
DOI: 10.1594/pangaea.902046
title: Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at station ALERT2018_08_1
DOI: 10.1594/pangaea.872155
title: Water temperature at time series station X-Huinay, Comau Fjord, Patagonia, Chile in 2016/2017

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de).
DOI: 10.1594/pangaea.495944
title: Water temperature MBT profiles from cruise U90M_1988
DOI: 10.1594/pangaea.739466
title: Pollen profile LLYN-JL, Llyn Gwernan, United Kingdom

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.885989
title: Basic measurements of radiation at station Billings (2012-11)
DOI: 10.1594/pangaea.854470
title: Glacier mass balance Vernagtferner, Brochkogel area, Austria, 1969/1970
DOI: 10.1594/pangaea.854487
title: Glacier mass balance Vernagtferner, Brochkogel area, Austria, 1986/1987
DOI: 10.1594/pangaea.465137
title: Physical properties of sediment core MD03-2659
DOI: 10.1594/pangaea.465143
title: (Table 1) Lithofacies interpretation and distribution in sediment core CRP-3

description: Seven hundred and nineteen samples from throughout the Cainozoic section in CRP-3 were analysed by a Malvern Mastersizes laser particle analyser, in order to derive a stratigraphic distribution of grain-size parameters downhole. Entropy analysis of these data (using the method of Woolfe & Michibayashi, 1995) allowed recognition of four groups of samples, each group characterised by a distinctive grain-size distribution. Group 1, which shows a multi-modal distribution, corresponds to mudrocks, interbedded mudrock/sandstone facies, muddy sandstones and diamictites. Group 2, with a sand-grade mode but showing wide dispersion of particle size, corresponds to muddy sandstones, a few cleaner sandstones and some conglomerates. Group 3 and Group 4 are also sand-dominated, with better grain-size sorting, and correspond to clean, well-washed sandstones of varying mean grain-size (medium and fine modes, respectively). The downhole disappearance of Group 1, and dominance of Groups 3 and 4 reflect a concomitant change from mudrock- and diamictite-rich lithology to a section dominated by clean, well-washed sandstones with minor conglomerates. Progressive downhole increases in percentage sand and principal mode also reflect these changes. Significant shifts in grain-size parameters and entropy group membership were noted across sequence boundaries and seismic reflectors, as recognised in other studies.
description: Modification of the facies scheme constructed for CRP-2/2A
DOI: 10.1594/pangaea.854488
title: Glacier mass balance Vernagtferner, Brochkogel area, Austria, 1987/1988
DOI: 10.1594/pangaea.901672
title: Downward spectral solar irradiance as measured in different depths under sea ice (transmitted irradiance) at station ALERT2018_08_2

description: Measurements of transmitted solar radiation under sea ice have been performed on First-Year-Ice (FYI) and Multi-Year-Ice (MYI) during the ALERT2018 campaign (Multidisciplinary Arctic Program (MAP) - Last Ice) off Alert, Nunavut, Canada in the Lincoln Sea between 07 May and 23 May 2018. The radiation measurements have been performed with Ramses spectral radiometes (TriOS, Rastede, Germany). All data are given in full spectral resolution interpolated to 1.0 nm, and integrated over the entire wavelength range (broadband, total: 320 to 950 nm). The irradiance sensor (cos-collector) for energy budget calculations was installed on the ROV. All times are given in UTC.
DOI: 10.1594/pangaea.854531
title: Glacier mass balance Vernagtferner, Schwarzwand area, Austria, 1989/1990
DOI: 10.1594/pangaea.846078
title: Basic measurements of radiation at station Boulder (2013-02)
DOI: 10.1594/pangaea.854543
title: Glacier mass balance Vernagtferner, Schwarzwand area, Austria, 2001/2002
DOI: 10.1594/pangaea.465136
title: Physical properties of sediment core MD03-2658G
DOI: 10.1594/pangaea.711164
title: (Fig. 3j) Clay mineral content of sediment core JR104-GC380
DOI: 10.1594/pangaea.680195
title: Other measurements at 300 m from station Boulder (1993-12)
DOI: 10.1594/pangaea.717167
title: Documentation of sediment core JR104-GC371
DOI: 10.1594/pangaea.756156
title: (Table 1a) Generation times of zooflagellates in samples taken at various times of a day at Station DM25-2189b1
DOI: 10.1594/pangaea.465127
title: Physical properties of sediment core MD03-2641
DOI: 10.1594/pangaea.880250
title: Time series of hydrofluorocarbon HFC-134a concentration at MteCimone in 2011
DOI: 10.1594/pangaea.465135
title: Physical properties of sediment core MD03-2657G
DOI: 10.1594/pangaea.776898
title: Core-section summary from IODP Hole 331-C0017B
DOI: 10.1594/pangaea.695045
title: Concentrations of particulate organic carbon in water of the Aegean Sea at Station MAY-1997-S09

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore filters. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).
DOI: 10.1594/pangaea.730150
title: (Table 15) Trace element contents in a vein and altered zones of basalts from the California Gulf, DSDP Hole 65-485A
DOI: 10.1594/pangaea.730382
title: (Table 47) Distribution of petrogenic components in coarce-pored olivine tholeiites from the Emperor Mount Chain, DSDP Hole 55-433C

description: Analyses have been carried out by T.N. Bortina in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences.
DOI: 10.1594/pangaea.849411
title: Abundance of mesozooplankton in central Adriatic Sea from 1959 to 1991 at Stoncica Station

description: The dataset is composed of 50 years of approximately monthly mesozooplankton sampling at station Stončica. The volume of filtered water was estimated assuming 70% efficiency of the Hensen 330 micrometer mesh size net according to Laevastu (1958). Subsamples amounting to 1/20 of the catch were counted for the most representative groups. The whole catch was examined for rare species.The results in the datatables are recalculated to (#/m**3).
DOI: 10.1594/pangaea.730032
title: (Table 58) Mineral composition of clay sediments from the Central American Trench at DSDP Site 67-496
DOI: 10.1594/pangaea.806062
title: Basic measurements of radiation at station Nauru Island (2001-06)

description: Version 3, 2013-01-25
DOI: 10.1594/pangaea.694981
title: Concentrations of particulate organic carbon in water of the Aegean Sea at Station FEBR-1998-IR30
DOI: 10.1594/pangaea.687222
title: Particulate organic carbon and nitrogen from bottle APRIL-2000-K1

description: POC/PON measured on a EA 1108 CHN Fisons Instruments CHN analyser according to the methodology suggested by Cutter, G.A. & J. Radford-Knoery (1991) and Verardo et al (1990).
DOI: 10.1594/pangaea.694870
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station JUNE-1998-IR64

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore filters. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).
DOI: 10.1594/pangaea.465129
title: Physical properties of sediment core MD03-2648
DOI: 10.1594/pangaea.901616
title: Beach profile data for the Elwha River Delta, 2016-11-18

description: Data were collected using GNSS survey methods, with a differential GPS operating in Real Time Kinematic (RTK) mode. Data from prior to 2013 were typically collected with a Magellan ProMark 3 traditional RKT-DGPS system (i.e. local base station and rover), with the base station sited on survey control markers installed in 1996, with survey control coordinates referenced to NAD83(CORS91). Starting in 2013 survey data were typically collected with an AshTech ProMark 200 RTK-DGPS system connected to the Washington State Reference Network. Survey data collected between January and November 2013 are referenced to NAD83(CORS96), and after November 2013 to NAD83(2011). Vertical data for surveys in 2012 and 2013 are referenced to NAVD88, presumably using Geoid96 (the survey control documentation does not specific a geoid). For all subsequent surveys the vertical data are referenced to NAVD88(Geoid09). No conversion were applied to these data to account for variations in horizontal or vertical coordinate system adjustments through time, but an error analysis suggests a standard deviation for the elevation data of between 0.03 and 0.05 m across the entire sampling period (2011-2018). All survey data were collected with the GNSS system mounted on a 2.05 m rover pole, held level as a transect line was traced in a cross-shore orientation on the beach. The associated text files include the horizontal (HRMS) and vertical (VRMS) root-mean-square errors estimated by the GNSS system, as well as the RTK-DGPS status reported by the GNSS system at the time each point was collected. Times are referenced to local Pacific time (either PST or PDT).
DOI: 10.1594/pangaea.465130
title: Physical properties of sediment core MD03-2649G
DOI: 10.1594/pangaea.921511
title: Total dissolved solids and major ions in ice-wedge ice of the laida of Belyy Island
DOI: 10.1594/pangaea.901620
title: Beach profile data for the Elwha River Delta, 2017-03-05

description: Data were collected using GNSS survey methods, with a differential GPS operating in Real Time Kinematic (RTK) mode. Data from prior to 2013 were typically collected with a Magellan ProMark 3 traditional RKT-DGPS system (i.e. local base station and rover), with the base station sited on survey control markers installed in 1996, with survey control coordinates referenced to NAD83(CORS91). Starting in 2013 survey data were typically collected with an AshTech ProMark 200 RTK-DGPS system connected to the Washington State Reference Network. Survey data collected between January and November 2013 are referenced to NAD83(CORS96), and after November 2013 to NAD83(2011). Vertical data for surveys in 2012 and 2013 are referenced to NAVD88, presumably using Geoid96 (the survey control documentation does not specific a geoid). For all subsequent surveys the vertical data are referenced to NAVD88(Geoid09). No conversion were applied to these data to account for variations in horizontal or vertical coordinate system adjustments through time, but an error analysis suggests a standard deviation for the elevation data of between 0.03 and 0.05 m across the entire sampling period (2011-2018). All survey data were collected with the GNSS system mounted on a 2.05 m rover pole, held level as a transect line was traced in a cross-shore orientation on the beach. The associated text files include the horizontal (HRMS) and vertical (VRMS) root-mean-square errors estimated by the GNSS system, as well as the RTK-DGPS status reported by the GNSS system at the time each point was collected. Times are referenced to local Pacific time (either PST or PDT).
DOI: 10.1594/pangaea.668035
title: Basic measurements of radiation at station Boulder (2003-10)
DOI: 10.1594/pangaea.848913
title: Snow temperature measured on Atka Bay landfast sea ice during ANT-Land 2012/2013 season
DOI: 10.1594/pangaea.465131
title: Physical properties of sediment core MD03-2650
DOI: 10.1594/pangaea.664206
title: Oceanography at CTD/bottle station IFREMER_1047
DOI: 10.1594/pangaea.756748
title: (Table 10) Biostratigraphic and paleomagnetic events at ODP Hole 117-724A
DOI: 10.1594/pangaea.712858
title: (Appendix 1) Chemical concentration in particulate matter measured on water bottle samples at station BP97-27
DOI: 10.1594/pangaea.618848
title: Water temperature profile LD99-CR19c
DOI: 10.1594/pangaea.901676
title: Downward spectral solar irradiance as measured in different depths under sea ice (transmitted irradiance) at station ALERT2018_10_1

description: Measurements of transmitted solar radiation under sea ice have been performed on First-Year-Ice (FYI) and Multi-Year-Ice (MYI) during the ALERT2018 campaign (Multidisciplinary Arctic Program (MAP) - Last Ice) off Alert, Nunavut, Canada in the Lincoln Sea between 07 May and 23 May 2018. The radiation measurements have been performed with Ramses spectral radiometes (TriOS, Rastede, Germany). All data are given in full spectral resolution interpolated to 1.0 nm, and integrated over the entire wavelength range (broadband, total: 320 to 950 nm). The irradiance sensor (cos-collector) for energy budget calculations was installed on the ROV. All times are given in UTC.
DOI: 10.1594/pangaea.692197
title: Particulate organic carbon and nitrogen concentrations in water samples collected at Station JANUARY-1995-D2 in the Cretan Sea
DOI: 10.1594/pangaea.806413
title: Hydrographic observations at SIMA station Corumbá reservoir in 2006

description: Quality flags: ? = questionable; / = not valid