cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.853935
title: Phenotypical responses of Fucus vesiculosus germlings to warming, acidification, nutrient enrichment and local upwelling under natural fluctuations (July - September 2014) - Carbon and nitrogen OAW x N experiment

description: Kiel Outdoor Benthocosms OAW- N-: ambient Temperature, pCO2 and nutrient conditionsOAW- N+ : ambient Temperature, ambient pCO2 and high nutrient conditions Carbon, nitrogen content (% DW) and C:N ratios were measured after the exposure of ambient and high nutrient levels
DOI: 10.1594/pangaea.511209
title: Radiosonde at Georg-Forster station on 1991-04-05 00:00h

description: Height of tropopause 8573 m, total ozone 314.1 DU
DOI: 10.1594/pangaea.761159
title: (Table 3) Lanthanum and scandium contents in phosphorites from seamounts and submarine rises

description: Scandium and lanthanum were analyzed using neutron activation and ICP-MS methods in 60 samples of oceanic phosphorites of various composition and age recovered from continental margins and seamounts in the Atlantic and Pacific Oceans. In the samples studied scandium content ranges from 0.1 to 60 ppm, lanthanum content ranges from 0.4 to 513 ppm, and La/Sc ratio varies from 1.1 to 114. The lowest scandium content occurs in recent phosphorite nodules, intermediate - in Pleistocene phosphatic sand, and the highest - in ancient seamount phosphorites. Process of scandium accumulation in the phosphorites is mainly controlled by their specific surface area and duration of their contact with ocean water. Lanthanum concentrates in the phosphorites much more intensely than scandium. Correlation between scandium and lanthanum distribution is weak, and it appears only when average concentrations of these elements in various groups of samples are compared.
description: Supplement to: Baturin, Gleb N (1999): Scandium and lanthanum in oceanic phosphorites. Translated from Okeanologiya, 1999, 39(3), 430-439, Oceanology, 39(3), 391-400
DOI: 10.1594/pangaea.908884
title: Radiosonde measurements from station Lindenberg (2017-09)
DOI: 10.1594/pangaea.905485
title: Data Set S12 - PC1 and PC2 loadings of the PCA (IODP Site 342-U1410)
DOI: 10.1594/pangaea.911213
title: Other measurements at 10 m from station Southern Great Plains (2017-12)
DOI: 10.1594/pangaea.739073
title: Pollen profile BSCUL, Ballyscullion East, United Kingdom

description: Method: Faegri and Iversen, 1989.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.911250
title: Tidal phase and amplitude of gauge station N-Joulters
DOI: 10.1594/pangaea.807093
title: (Table 2) Seroprevalence against Trichinella spp. in Ursus maritimus from Svalbard and Barents Sea pack ice

description: Blood samples of live-caught polar bears (Ursus maritimus) from Svalbard collected 1991-2000 (Period 1) and 2006-2008 (Period 2) and from the pack ice of the Barents Sea collected in Period 1, were assayed for antibodies against Trichinella spp. by ELISA. Of 54 cubs-of-the-year included in the Period 1 sample, 53 were seronegative, indicating that exposure to Trichinella infected meat is uncommon during the first months of life for polar bears in the Svalbard region. Of 30 mother-offspring pairs, 18 mothers were seropositive with seronegative offspring (n = 27), suggesting (1) that maternal antibodies had dropped to levels below detection limit by the time of capture in April (offspring approximately 4 months old), and (2) supporting experimental studies in other animal models showing that vertical transmission of Trichinella spp. is uncommon. Bear 1 year and older had higher prevalence in Svalbard (78%) than in the Barents Sea (51%). There was no temporal change in prevalence for bears from Svalbard during the time between the two periods. The prevalence increased with age in both sexes. A positive correlation was found between anti-Toxoplasma gondii and anti-Trichinella spp. antibodies.
description: Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
description: Supplement to: Asbakk, Kjetil; Aars, Jon; Derocher, Andrew E; Wiig, Øystein; Oksanen, Antti; Born, Erik W; Dietz, Rune; Sonne, Christian; Godfroid, Jacques; Kapel, Christian M O (2010): Serosurvey for Trichinella in polar bears (Ursus maritimus) from Svalbard and the Barents Sea. Veterinary Parasitology, 172(3-4), 256-263
DOI: 10.1594/pangaea.670359
title: Present day and paleo-geographic coordinates, thicknesses and isopach area of the Early Eocene +19 ash layer (Table 1)

description: 23 layers of altered volcanic ash (bentonites) originating from the North Atlantic Igneous Province have been recorded in early Eocene deposits of the Austrian Alps, about 1,900 km away from the source area. The Austrian bentonites are distal equivalents of the ''main ash-phase'' in Denmark and the North Sea basin. We have calculated the total eruption volume of this series as 21,000 km**3, which occurred in 600,000 years. The most powerful single eruption of this series took place 54.0 million years ago (Ma) and ejected ca. 1,200 km**3 of ash material, which makes it one of the largest basaltic pyroclastic eruptions in geological history. The clustering of eruptions must have significantly affected the incoming solar radiation in the early Eocene by the continuous production of stratospheric dust and aerosol clouds. This hypothesis is corroborated by oxygen isotope values, which indicate a global decrease of sea surface temperatures between 1 and 2 C during this major phase of explosive volcanism.
description: #0.00: samples with low foraminiferal amount / Age: Calendar age
description: Supplement to: Egger, Hans; Brückl, Ewald (2006): Gigantic volcanic eruptions and climatic change in the early Eocene. International Journal of Earth Sciences, 95, 1065-1070
DOI: 10.1594/pangaea.761750
title: Physical oceanography during KAPITAN DRANITSYN cruise Transdrift-III to the Laptev Sea, Arctic Ocean

description: The TRANSDRIFT III expedition was part of the joint Russian-German cooperation and the Laptev Sea System project. The Arctic and Antarctic Research Institute (AARI) in St. Petersburg and the GEOMAR Research Center for Marine Geosciences were jointly responsible for the organization and coordination of the TRANSDRIFT III expedition, which was funded by the Russian Ministry for Research and Technology and the German Ministry for Research and Technology.The TRANSDRIFT III expedition was carried out aboard the Russian icebreaker KAPITAN DRANITSYN in the Laptev Sea from October 1 to 30, 1995. In this shelf region a multi-disciplinary working program investigated the causes and effects of annual freeze-up. Unlike our previous expeditions to the Laptev Sea, which focused on oceanographical, hydrochemical, ecological and sedimentological processes during the brief ice-fee period in summer, this expedition studied these processes during the extreme physical change through the onset of ice formation in autumn. This was the first study of its kind under these conditions, and gave important clues to the rapid (14 to 40 days) freeze-up, which has significant year-round effects on the Laptev Sea and global environment.The working program was carried out in bilateral cooperation. CTD data were retrieved at a total number of 75 positions in the Laptev Sea. Hydrochemical sampling with oxygen, silicate and phosphate analysis was carried out at 65 of these stations.
DOI: 10.1594/pangaea.907221
title: Track of GPS very-near surface drifter ISMER_20141022_spot063
DOI: 10.1594/pangaea.911249
title: Tidal phase and amplitude of gauge station Joulters
DOI: 10.1594/pangaea.907261
title: Track of GPS very-near surface drifter ISMER_20150615_spot035
DOI: 10.1594/pangaea.907292
title: Track of GPS very-near surface drifter ISMER_20150811_spot721
DOI: 10.1594/pangaea.907303
title: Track of GPS very-near surface drifter ISMER_20150924_spot714
DOI: 10.1594/pangaea.907305
title: Track of GPS very-near surface drifter ISMER_20150924_spot912
DOI: 10.1594/pangaea.822831
title: Meteorological measurements in the upper air at station Aachen, 1920-02-20 to 1920-08-25, ERA-CLIM ID 5630

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.828619
title: Thermal conductivity of IODP Hole 323-U1341B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.870220
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_VIII_07
DOI: 10.1594/pangaea.828620
title: Thermal conductivity of IODP Hole 323-U1341C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.832034
title: (Table S01) Carbonate content of sediment core RC11-84
DOI: 10.1594/pangaea.911251
title: Tidal phase and amplitude of gauge station NW_Andros
DOI: 10.1594/pangaea.815866
title: Length changes of Austrian glaciers 2011/2012
DOI: 10.1594/pangaea.843909
title: Hydrochemistry measured on water bottle samples in the Arctic Ocean during ODEN cruise SWERUS-C3 (77DN20140705)
DOI: 10.1594/pangaea.822800
title: Meteorological measurements in the upper air at station Bushehr, 1949-07-03 to 1952-04-08, ERA-CLIM ID 5535

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.809990
title: (Table 5) Major ion composition of seggregated ice from Herschel Island and Komakuk Beach

description: The percentages of individual anion and cation species are given as per cent of the total anion or cation population.
DOI: 10.1594/pangaea.908572
title: (Table S1) Bulk stable isotopes of ODP Hole 114-702B

description: Error (‰): (Solnhofen limestone) 0.04‰ for d13C; 0.07‰ for d18O.
DOI: 10.1594/pangaea.894820
title: (Figure 02) Meteorological time series at Princess Elisabeth Station in 2013-2016
DOI: 10.1594/pangaea.730060
title: Meteorological synoptical observations from station Tamanrasset (2009-08)
DOI: 10.1594/pangaea.894821
title: (Figure 02) Daily precipitation at Princess Elisabeth Station in 2013-2016
DOI: 10.1594/pangaea.433071
title: Age and alkenone-derived Holocene sea-surface temperature records of sediment core 167-1012B

description: This dataset shows only a subset of the published version.
DOI: 10.1594/pangaea.894822
title: (Figure 05) Total monthly particle number concentration between 2012-2016
DOI: 10.1594/pangaea.691514
title: Sea-bed photographs (benthos) from the Magellan region (South America) along profile VH1094_0871

description: Photos represent approx. 1m**2 each, taken vertically by Hasselblad 500EL/M with two strobes Metz mecablitz 45; Kodak Ektachrome 64; Minolta Dimage Scan Multi II; JPEG compression: 300 dpi, 21.4 x 20.0 cm; J. Gutt: mailto:Julian.Gutt@awi.de
DOI: 10.1594/pangaea.911380
title: Radiosonde measurements from station Southern Great Plains (2017-12)

description: Launches may be at irregular time intervals. The radiosonde measurements from station Southern Great Plains are used for Billings and E13
DOI: 10.1594/pangaea.754362
title: (Table 2) Sr/Ca and Mn/Ca ratios of ODP Hole 113-690C
DOI: 10.1594/pangaea.894827
title: (Figure 06) Condensation nuclei concentrations measured by LAS (first season)
DOI: 10.1594/pangaea.691515
title: Sea-bed photographs (benthos) from the Magellan region (South America) along profile VH1094_0879

description: Photos represent approx. 1m**2 each, taken vertically by Hasselblad 500EL/M with two strobes Metz mecablitz 45; Kodak Ektachrome 64; Minolta Dimage Scan Multi II; JPEG compression: 300 dpi, 21.4 x 20.0 cm; J. Gutt: mailto:Julian.Gutt@awi.de
DOI: 10.1594/pangaea.774857
title: (Table 27) Concentrations of particulate total silica in waters of the Southern Atlantic Ocean
DOI: 10.1594/pangaea.870224
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_VIII_11
DOI: 10.1594/pangaea.822965
title: Meteorological measurements in the upper air at station Santa Ana, 1946-02-09 to 1946-02-09, ERA-CLIM ID 5975

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.838203
title: Pollen profile VERNAY, France

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.842036
title: Other measurements at 10 m from station Darwin (2003-03)

description: Version 3, 2015-01-28
DOI: 10.1594/pangaea.691516
title: Sea-bed photographs (benthos) from the Magellan region (South America) along profile VH1094_0880

description: Photos represent approx. 1m**2 each, taken vertically by Hasselblad 500EL/M with two strobes Metz mecablitz 45; Kodak Ektachrome 64; Minolta Dimage Scan Multi II; JPEG compression: 300 dpi, 21.4 x 20.0 cm; J. Gutt: mailto:Julian.Gutt@awi.de
DOI: 10.1594/pangaea.899793
title: Whole-rock major element and select trace element analyses (XRF) of rock samples used for mapping in the northern Semail ophiolite (Oman)

description: Anhydrous compositions closed to 100wt% oxides, total Fe calculated as Fe2O3, LOI determined after heating in air for 2 h at 1050˚C.
DOI: 10.1594/pangaea.548291
title: Physical oceanography at CTD station Bm_1997-09-01_6, Bajo Molle, Chile
DOI: 10.1594/pangaea.822417
title: Meteorological measurements in the upper air at station Kara-Kul, 1957-08-31 to 1957-09-24, ERA-CLIM ID 4674
DOI: 10.1594/pangaea.839873
title: Splice tie points for IODP Hole 347-M0066
DOI: 10.1594/pangaea.497200
title: Physical oceanography from BT during cruise M90PS00012B_1962
DOI: 10.1594/pangaea.838507
title: Lithology of sediment core BAJONDI, Bajondillo, Spain

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.870184
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_VII_01
DOI: 10.1594/pangaea.909962
title: Table 6 - Alternative orbital tuning schemes for Falconara section

description: Results of alternate tuning experiments using (1) the original sapropel midpoints only, (2) sapropel mid-points and Pb isotope 'peaks' based on the 206Pb/204Pb record, and (3) based on only the 206Pb/204Pb 'peaks.'
description: Empty age column means there are no new tuning point data. Comment parameter meaning: Star - samples not run for Pb isotopes, used here for age-depth comparison; MP - sapropel mid-point: Contact - contact between two lithologies, used in time series figures to draw lithological boundaries.
DOI: 10.1594/pangaea.737495
title: (Table 2.2.1.4) Individual width of sympagic meiofauna in sections of sea-ice core IO-3

description: sea-ice core diameter 9 cm; DEPTH ice/snow represents the middle of the ice-core section measured from ice surface; width gives the median of individuals in each ice-core section
DOI: 10.1594/pangaea.848213
title: Basic measurements of radiation at station Kwajalein (2013-04)
DOI: 10.1594/pangaea.911792
title: Radiosonde measurements from station Tateno (2019-11)
DOI: 10.1594/pangaea.897698
title: Atmospheric pCO2 compilation from pedogenic carbon for the Late Cretaceous-Early Paleogene
DOI: 10.1594/pangaea.755472
title: Geochemical analyses of secondary minerals from ODP Leg 115 basalts (Tables 1+2)

description: Basalts recovered along the Reunion hotspot track on Ocean Drilling Program (ODP) Leg 115 range in age from 34 Ma at Site 706 to 64 Ma at Site 707. They have undergone various degrees of secondary alteration. Within single holes the amount of alteration can vary from a few percent to near complete replacement of phenocrysts and groundmass by secondary minerals. Olivine appears to be the most susceptible to alteration and in some sections it is the only mineral altered. In other sections, olivine, pyroxene and plagioclase phenocrysts, and groundmass have been completely replaced by secondary minerals.Clays are the predominant form of secondary mineralization. In addition to replacing olivine, pyroxene, glass, and groundmass, clays have filled veins, vesicles, and voids. Minor amounts of calcite, zeolites, and K-feldspar were also detected. The clays that filled vesicles and veins often show color zonations of dark, opaque bands near the edges that grade into tan or green transparent regions in the centers of the veins. The electron microprobe was used to obtain chemical analyses of these veins as well as to characterize isolated clays that replaced specific minerals and filled voids and vesicles.
description: Supplement to: Fisk, Martin R; Howard, Katherine J (1990): Chemistry of basalt alteration from Leg 115. In: Duncan, RA; Backmann, J; Peterson, LC; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 115, 791-793
DOI: 10.1594/pangaea.911432
title: Silt/clay ratio of the decarbonated fraction of borehole PRGL1-4 from the Gulf of Lion, Mediterranean Sea
DOI: 10.1594/pangaea.911437
title: Decarbonated silt/clay ratio from sediment core MD99-2348 from the Gulf of Lion, Mediterranean Sea
DOI: 10.1594/pangaea.911830
title: Radiosonde measurements from station Minamitorishima (2019-11)
DOI: 10.1594/pangaea.690670
title: Documentation of sediment core GIK12517-1
DOI: 10.1594/pangaea.737512
title: (Table 2.2.1.5) Individual carbon content of sympagic meiofauna in sections of sea-ice core IO-8

description: sea-ice core diameter 9 cm; DEPTH ice/snow represents the middle of the ice-core section measured from ice surface; C-content gives the calculated value per individual, calculated from median length and width in the respective ice-core section
DOI: 10.1594/pangaea.901533
title: Beach profile data for the Elwha River Delta, 2012-12-26

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).
description: Portions of these data have been published previously, including in Gelfenbaum et al. 2015.
DOI: 10.1594/pangaea.901566
title: Beach profile data for the Elwha River Delta, 2014-05-17

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).
description: Portions of these data have been published previously, including in Gelfenbaum et al. 2015.
DOI: 10.1594/pangaea.911796
title: Nitrogen isotope ratio and oxygen isotope ratio from Arabian Sea IODP Site 355-U1456
DOI: 10.1594/pangaea.495558
title: Water temperature MBT profiles from cruise U7424620M_1955
DOI: 10.1594/pangaea.901591
title: Beach profile data for the Elwha River Delta, 2015-08-27

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).
description: Portions of these data have been published previously, including in Gelfenbaum et al. 2015.