cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.774742
title: ADCP current meter data from mooring TR_LF_ADCP_3 at Tisler Cold-Water Coral Reef, Norway
DOI: 10.1594/pangaea.774568
title: Physical oceanography and current meter data from mooring TR_RCM1a at Tisler Cold-Water Coral Reef, Norway
DOI: 10.1594/pangaea.774574
title: Physical oceanography and current meter data from mooring TR_RCM4 at Tisler Cold-Water Coral Reef, Norway
DOI: 10.1594/pangaea.912492
title: Hydrocarbon composition (C1/(C2-C5), stable carbon isotopic composition of methane (d13C-CH4), and stable hydrogen isotopic composition of methane (d2H-CH4) in hydrate-bound gas of sediment core GMGC17
DOI: 10.1594/pangaea.784319
title: Laser profiles of sea ice surface roughness during campaign IRIS 2004 from flight IRIS2004_200402291206
DOI: 10.1594/pangaea.751654
title: Meteorological observations during Queen Charlotte cruise from York Factory to Gravesend started at 1797-09-28
DOI: 10.1594/pangaea.928246
title: Dentoglobigerina altispira Mg/Ca and stable oxygen isotopes of ODP Hole 130-806B
DOI: 10.1594/pangaea.912502
title: Hydrocarbon composition (C1/(C2-C5), stable carbon isotopic composition of methane (d13C-CH4), and stable hydrogen isotopic composition of methane (d2H-CH4) in hydrate-bound gas of sediment core GMMB07
DOI: 10.1594/pangaea.691292
title: Mesozooplankton average length during Professor Vodyanitskiy cruise PV20, Part I

description: Mesozooplankton was sampled by JUDAY net with a 37 cm ring diameter and mesh sizes of 125 µm. Integrated hauls (0-200 m) were usually taken. 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.912269
title: Methane concentrations of MeBo sediment core GMMB11

description: Methane concentrations (uncorrected for sediment porosity and Bunsen coefficient) in headspace gas prepared from MeBo sediment cores recovered in the area of Pockmark A.
DOI: 10.1594/pangaea.729167
title: (Table T75) Secondary minerals in basalts of Ninetyeast Ridge, Leg 121, Hole 757C

description: In the column Comment: 1 = data of mineral determinations from description of thin sections (Frey et al., 1991, doi:10.2973/odp.proc.sr.121.163.1991); 2 = data of mineral determinations from XRD analyses (Peirce, Weissel, et al., 1989, doi:10.2973/odp.proc.ir.121.1989).
DOI: 10.1594/pangaea.943110
title: Radiosonde measurements from station Lindenberg (2019-12)
DOI: 10.1594/pangaea.890553
title: Age determination of V34_core1 peat core
DOI: 10.1594/pangaea.912495
title: Hydrocarbon composition (C1/(C2-C5), stable carbon isotopic composition of methane (d13C-CH4), and stable hydrogen isotopic composition of methane (d2H-CH4) in hydrate-bound gas of sediment core GMGC30
DOI: 10.1594/pangaea.827376
title: Spatially explicit estimates of length and biomass of Micromesistius poutassou (Blue Whiting) from acoustic and trawl surveys in the North-East Atlantic in May 2008

description: Acoustic estimates of herring and blue whiting abundance were obtained during the surveys using the Simrad ER60 scientific echosounder. The allocation of NASC-values to herring, blue whiting and other acoustic targets were based on the composition of the trawl catches and the appearance of echo recordings. To estimate the abundance, the allocated NASC -values were averaged for ICES-squares (0.5° latitude by 1° longitude). For each statistical square, the unit area density of fish (rA) in number per square nautical mile (N*nm-2) was calculated using standard equations (Foote et al., 1987; Toresen et al., 1998). To estimate the total abundance of fish, the unit area abundance for each statistical square was multiplied by the number of square nautical miles in each statistical square and then summed for all the statistical squares within defined subareas and over the total area. Biomass estimation was calculated by multiplying abundance in numbers by the average weight of the fish in each statistical square then summing all squares within defined subareas and over the total area. The Norwegian BEAM soft-ware (Totland and Godø 2001) was used to make estimates of total biomass.
description: The research leading to these results received (partial/full) funding from the European Commission FP7 EURO-BASIN (European Basin-Scale Anal ysis, Synthesis, and Integration; Grant Agreement 264 933).
DOI: 10.1594/pangaea.890554
title: Age determination of Vasyugan_coreV21 peat core
DOI: 10.1594/pangaea.496989
title: Physical oceanography from BT during cruise M90BF00007B_1987
DOI: 10.1594/pangaea.757272
title: Phytoplankton pigments during Professor Vodyanitskiy cruise PV23
DOI: 10.1594/pangaea.758563
title: (Table 6) Chemistry of Cr-spinel and ilmenite/magnetite minerals of ODP Hole 120-748C
DOI: 10.1594/pangaea.854612
title: Glacier mass balance Vernagtferner, Austria, 1988/1989
DOI: 10.1594/pangaea.854648
title: Description of manganese nodules collected in a sandstone formation near Dillon, Montana

description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
DOI: 10.1594/pangaea.890470
title: Maximum annual precipitation reconstruction at successive 500-year intervals in South America
DOI: 10.1594/pangaea.943145
title: Basic measurements of radiation at station Cener (2022-01)
DOI: 10.1594/pangaea.552471
title: Oxygen profile of the water column of site M1_CTD049, Red Sea (Table 4)
DOI: 10.1594/pangaea.907353
title: Abundances of stream benthic macroinvertebrates influenced by four typical land cover types of the European Alps during an annual investigation in South Tyrol (Italy)

description: Stream benthic macroinvertebrates have been collected at 14 sites in South Tyrol, on three different sampling occasions (May, July, September), year 2017.Considering the entire hydrological network of South Tyrol, sampling sites were selected according to the following requirements: 1) each sampling site had a homogeneous land cover type at reach scale (buffer area used of 1,000 m x 300 m), one among the types rocks (R), high alpine grasslands (G), coniferous forest (F), valley-bottom pastures (P); 2) the sampling sites had no glacial water source; 3) the sampling sites were situated max. 500 m from any road or trail (for access purpose); 4) for each of the four land cover types mentioned above, the most similar points in regards to landscape composition and topography calculated at the catchment scale were chosen.Organisms were collected through Surber samplings (0.0506 squared metres, mesh size 500 µm) in 3 rocks (R-5, R-29, R-52) and high alpine grasslands (G-133, G-188, G-193) sites, and in 4 coniferous forests (F-51, F-178, F-391, F-621) and valley bottom pastures (P-9, P-37, P-50, P-53) sites.Further details regarding the site selection and their characteristics are explained in the publication resulting from the analysis of this abundances data (see "Supplement to:").
description: Supplement to: Scotti, Alberto; Füreder, L; Marsoner, Thomas; Tappeiner, Ulrike; Stawinoga, A E; Bottarin, Roberta (2020): Effects of land cover type on community structure and functional traits of alpine stream benthic macroinvertebrates. Freshwater Biology, 65(3), 524-539
DOI: 10.1594/pangaea.912488
title: Hydrocarbon composition (C1/(C2-C5), stable carbon isotopic composition of methane (d13C-CH4), and stable hydrogen isotopic composition of methane (d2H-CH4) in hydrate-bound gas of sediment core GMGC01
DOI: 10.1594/pangaea.924467
title: Meteorological synoptical observations from station Tateno (2020-06)
DOI: 10.1594/pangaea.912267
title: Methane concentrations of MeBo sediment core GMMB08

description: Methane concentrations (uncorrected for sediment porosity and Bunsen coefficient) in headspace gas prepared from MeBo sediment cores recovered in the area of Pockmark A.
DOI: 10.1594/pangaea.943066
title: Radiosonde measurements from station Lindenberg (2019-06)
DOI: 10.1594/pangaea.890526
title: Minimum annual precipitation reconstruction at successive 500-year intervals in South America
DOI: 10.1594/pangaea.909239
title: Soil moisture time-series estimated from networks of 5TE capacitance sensors at Voulund Farmland, Harrild Heathland and Gludsted Plantation, Denmark, in 2013-2019

description: Time-series of soil column soil moisture (down to 22.5 cm depth) estimated from networks of 5TE capacitance sensors at the three field site locations. Data is available from 2013-2019 for Voulund Farmland and Gludsted Plantation, and from 2014-2019 at Harrild Heathland.
description: Equipment: Networks of 5TE capacitance sensors (Decagon Devices Inc., 2014); 6 stations and 2-3 measurements depths (litter layer and/or 2.5 cm and 22.5 cm depths)
DOI: 10.1594/pangaea.912268
title: Methane concentrations of MeBo sediment core GMMB10

description: Methane concentrations (uncorrected for sediment porosity and Bunsen coefficient) in headspace gas prepared from MeBo sediment cores recovered in the area of Pockmark A.
DOI: 10.1594/pangaea.781230
title: (Table T5) Presence of contamination tracers in rock samples from ODP Leg 187 sites

description: Table shows presence ("+") and absence ("-") of microspheres. Blank space = no thin section was made to examine the interior of the rock for microspheres.
DOI: 10.1594/pangaea.777025
title: Core-section summary from IODP Hole 331-C0015C
DOI: 10.1594/pangaea.912337
title: Pore water sulfate and chloride concentrations in pressurized sediment core GMDA03 collected in the area of Pockmark A
DOI: 10.1594/pangaea.943072
title: Radiosonde measurements from station Lindenberg (2019-07)
DOI: 10.1594/pangaea.793264
title: (Appendix B Table 12) Calcareous nannofossil biohorizons of ODP Hole 167-1022A

description: DEPTH, sediment is given in mcd.
DOI: 10.1594/pangaea.943086
title: Radiosonde measurements from station Lindenberg (2019-08)
DOI: 10.1594/pangaea.943148
title: Basic measurements of radiation at station Reunion Island, University (2022-03), Version 1
DOI: 10.1594/pangaea.810524
title: Virtual geomagnetic pole reconstruction at Site 320-U1336

description: Depth [m] = Depth (CCSF-A)
DOI: 10.1594/pangaea.930344
title: Meteorological records of the Malaspina Expedition (1789-1794)

description: Meteorological observations made in the Malaspina Expedition from 1789 to 1794 have been retrieved. Variables such as air temperature, atmospheric pressure, wind direction and intensity, and weather conditions, were recorded in these observations. In total, nearly 17000 instrumental data were digitized.
DOI: 10.1594/pangaea.854859
title: Daily polynya area from passive microwave satellite sensors AMSR-E and AMSR2 in the North Water polynya region in 2002/2003
DOI: 10.1594/pangaea.912504
title: Hydrocarbon composition (C1/(C2-C5), stable carbon isotopic composition of methane (d13C-CH4), and stable hydrogen isotopic composition of methane (d2H-CH4) in hydrate-bound gas of sediment core GMMB11
DOI: 10.1594/pangaea.854965
title: Annotated record of the detailed examination of Mn deposits from NORTHERN HOLIDAY Expedition stations

description: The cores described in this report were taken on the NORTHERN HOLIDAY Expedition in August to September 1951 by the Scripps Institution of Oceanography from the R/V Horizon. A total of 19 cores and dredges were recovered and are available at Scripps for sampling and study.
description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
DOI: 10.1594/pangaea.912489
title: Hydrocarbon composition (C1/(C2-C5), stable carbon isotopic composition of methane (d13C-CH4), and stable hydrogen isotopic composition of methane (d2H-CH4) in hydrate-bound gas of sediment core GMGC02
DOI: 10.1594/pangaea.943147
title: Basic measurements of radiation at station Cener (2022-03)
DOI: 10.1594/pangaea.894762
title: Storstrømmen, Northeast Greenland - speed - grounding lines - ice fronts

description: The datasets describe the ice speed, grounding line positions and ice fronts of Storstrømmen and L. Bistrup Bræ located in Northeast Greenland. This data set consists of GeoTIFF (.tif) for the speed maps and ESRI shapefiles (.shp, .shx, .dbf, .prj) for the grounding lines and ice fronts.Surface ice velocity derived from feature or speckle tracking using declassified CORONA images from August 1967 and March 1968, Landsat-1&2/MSS images between 1973 and 1976, orthorectified American HEXAGON spy image acquired in1978 and 1982, Landsat-4&5/TM image pairs between 1984 and 1991, ERS-1/2 in 1993. GeoTIFF speed data are provided on polar stereographic projection. The file naming convention is first acquisition date (date1) followed by the second acquisition date (date2) and velocity component along x or y axis. (vx or v). Example : 19931231-19940118_vy.tif where date1=19931231, date2=19940118 and vy is the displacement along the y-axis.Grounding Lines position using InSAR data from the European Earth Remote Sensing (ERS-1/2) radar satellite collected in 1992 (3-day repeat cycle), in 1996 (1-day apart) and Sentinel-1a/b in Nov. 2015 and Apr. 2017. To digitize the grounding lines, we pick the inward limit of detection of vertical motion, where the glacier becomes afloat with a precision of about 50 m, as in Rignot et al., 2011.Ice fronts position between 1907 and 2015 from historical maps, aerial and satellite imagery.
description: Supplement to: Mouginot, Jeremie P; Bjørk, Anders Anker; Millan, Romain; Scheuchl, Bernd; Rignot, Eric (2018): Insights on the surge behavior of Storstrømmen and L. Bistrup Brae, Northeast Greenland, over the last century. Geophysical Research Letters, 45(20), 11,197-11,205
DOI: 10.1594/pangaea.893551
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018022812

description: INITIALIZATION: 2018022812FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.786707
title: (Table 2) Oxygen isotope ratios of anhydrite from subsurface samples of ODP Sites 193-1188 and 193-1189
DOI: 10.1594/pangaea.815923
title: (Table S3d) Major element compositions of onshore Taupo Volcanic Zone tephras

description: All standard deviations = 2sd.
DOI: 10.1594/pangaea.477307
title: Hydrochemistry measured on water bottle samples at station NPac_1985_TT_47Na/48-1

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.943146
title: Basic measurements of radiation at station Cener (2022-02)

description: On the 14th the thermohygrometer was replaced.
DOI: 10.1594/pangaea.495548
title: Water temperature MBT profiles from cruise U7402373M_1959
DOI: 10.1594/pangaea.805043
title: (Figure 4e) Iron carbonate-free concentrations from powder samples of sediment core GeoB6211-2
DOI: 10.1594/pangaea.669523
title: Horizon at station Payerne
DOI: 10.1594/pangaea.711819
title: (Table 1) 87Sr/86Sr and trace element data for carbonates from ODP Site 115-707
DOI: 10.1594/pangaea.758110
title: (Table 3) Sr, Nd, and Pb isotopic composition of balast from ODP Hole 119-738C
DOI: 10.1594/pangaea.707299
title: (Table 1) Pb, Sr ad Nd isotopic composition of basalts from ODP Hole 136-843B
DOI: 10.1594/pangaea.752052
title: Meteorological observations during SEAFORD cruise from Caicos to Uk started at 1775-02-26
DOI: 10.1594/pangaea.496429
title: Water temperature IBT profiles from cruise U999881011I_1983
DOI: 10.1594/pangaea.855011
title: Trace metal composition of the aerosol at Neumayer Station, Antarctica during the year 2001

description: Aerosol was continuously sampled by sucking ambient air with a flow rate of 120 m**3/h through Whatman 541 filters (diameter 240 mm) using a ventilated electropolished stainless steel inlet stack (total height about 8 m above the snow surface) with a 50% aerodynamic cut-off diameter around 7-10 µm. Trace element analysis was performed by means of inductively coupled plasma - quadrupol mass spectrometry (ICP-QMS, ELAN 6000, Sciex/Perkin Elmer) equipped with a cross-flow nebulizer as sample introduction system. For trace element analyses we chose a total digestion of the samples with a pressurized digestion system (DAS 100, Picotrace) at 200°C in a mixture containing HNO3 (suprapure, 65%, Merck, sub-boiling bi-distilled), HF (suprapure, 40%, Merck, sub-boiling bi-distilled) and H2O2 (suprapure, 30%, Merck). With this device a series of 24 samples could be digested in parallel. Each series included one filter blank and a certified reference sample (NIST 1648 urban particulate matter). For calibration we used commercially available standard solutions (104 ppb multi-element verification standard 1 and 2, Perkin Elmer) which were generally applied in 1 ppb, 10 ppb, and 100 ppb concentrations (1 ppb corresponds to 1 ng of each element in 1 g solute). Each sample was spiked by 10 ppb Rh as internal standard to normalize the signal intensities and compensate instrumental sensitivity variations. We conservatively estimated the method detection limits (MDL) as three times the standard deviation (std) of the overall blank values. Values below the MDL are given as "&lt; respecting MDL value" (e.g.: &lt;0.02) in the table. Concentrations not determined are marked with empty cells. The combined uncertainty of the analyses is approximately between ±8% and ±12% for element concentrations above three times the corresponding MDL. It increased from around ±(15-20)% approaching 3xMDL level to roughly (+50/-100)% close to the MDL. The final atmospheric concentrations (in ng/m**3 = 10**(-9) g/m**3, or pg/m**3 = 10**(-12) g/m**3) were calculated from the blank corrected element amounts and the corrected sampled air volume to standard conditions (273.16 K and 1013 hPa).
DOI: 10.1594/pangaea.774927
title: Continuous meteorological observations at Neumayer station (1996-01)
DOI: 10.1594/pangaea.888418
title: Changes in the processes underpinning the growth of caterpillars
DOI: 10.1594/pangaea.788690
title: (Table T1) Thorium, uranium and protactinium concentrations in ODP Leg 139 and Leg 169 sites
DOI: 10.1594/pangaea.751727
title: Meteorological observations during RELIANCE cruise from Cape of Good Hope to Port Jackson started at 1797-04-13
DOI: 10.1594/pangaea.855350
title: (Table 1, page 605) Chemistry of concretions from Grand Lake (GL) and Ship Harbour Lake (SH), Nova Scotia and Mosque Lake (ML), Ontario

description: Studies by optical microscopy, x-ray diffraction, and electron probe techniques of ferromanganese concretions from three Canadian lakes reveal chemical banding of amorphous hydrated iron and manganese oxides. The average ratio of iron to manganese in concretions from these lakes varies from 0.43 to 2.56. The concentrations of cobalt, nickel, copper, and lead are one to two orders of magnitude below those reported for oceanic ferromanganese concretions.
description: The substrate of all concretions sites is coarse-grained quartz sand and pebbles. Core includes slate, sandstone and granite pebbles. Ferromanganese outer rind, 0.5-3.0 cm thick, was separated for analysis.From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: Harriss, Robert C; Troup, Arthur G (1969): Freshwater Ferromanganese Concretions: Chemistry and Internal Structure. Science, 166(3905), 604-606
DOI: 10.1594/pangaea.669524
title: Horizon at station Regina
DOI: 10.1594/pangaea.758902
title: (Table 3) Mixed planktonic foraminifer 87Sr/86Sr isotope ratios of ODP Site 120-748
DOI: 10.1594/pangaea.841946
title: (Table S2) Alkenone unsaturation index and SST reconstruction for ODP Hole 167-1019C

description: Sediment depth is given in mcd.
DOI: 10.1594/pangaea.888893
title: Fecal glucocorticoid metabolites in captive Grévys zebras, and acute shedding of equine Herpesvirus

description: Equine Herpesviruses (EHV) are highly prevalent and often latent pathogens of equids which can be fatal when transmitted to non-equids. Stress and elevated glucocorticoids have been associated with EHV reactivation in domestic horses, but little is known about the correlation of stress and viral reactivation in wild equids. We investigated the effect of environmental stressors (long-distance transport and social group restructuring) on EHV reactivation in captive Grévys zebras. One mare was translocated by road transport from Zoo Mulhouse, France, to join a resident group of three mares in Tierpark Berlin, Germany. We measured fecal glucocorticoid metabolite (fGCM) concentrations daily in each individual from 6 days before the translocation event, to 14 days after translocation. EHV shedding was screened for all animals at Tierpark Berlin using an indirect sampling method. Following the translocation event we found significantly elevated fGCM concentrations in all animals compared to fGCM levels before the translocation event, which coincided with increased rates of EHV shedding. Our results support the hypothesis that environmental stressors induce viral reactivation in wild equids. This finding suggests that potentials stressors such as translocation and group restructuring should be considered in the management of zoological collections to reduce the risk of fatal EHV infections in novel hosts. Moreover, environmental stressors may also play an important role regarding EHV reactivation and spreading in wild equid populations.
description: Supplement to: Seeber, Peter A; Quintard, Benoît; Sicks, Florian; Dehnhard, Martin; Greenwood, Alex D; Franz, Mathias (2018): Environmental stressors may cause equine herpesvirus reactivation in captive Grévy's zebras (Equus grevyi). PeerJ, 6, e5422
DOI: 10.1594/pangaea.496223
title: Water temperature MBT profiles from cruise U90X089256M_1981