cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.696326
title: Basic measurements of radiation at station Ilorin (1999-12)

description: Some additional quality control will be performed during summer 2013 for the LW data. For further infos contact Rachel T. Pinker
DOI: 10.1594/pangaea.694852
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station JUNE-1998-IR02

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.726827
title: (Table 4) Stable carbon and oxygen isotope ratios of foraminifera from DSDP Leg 10
DOI: 10.1594/pangaea.871792
title: Temperature and precipitation measurements in Mendoza, Argentina from October 1875- December 1880 and March- December 1886, digitized version

description: The data of this dataset might have been revised during the review process. This might therefore be an old version. To be sure, please check the respective dataset at doi:10.1594/PANGAEA.871480
DOI: 10.1594/pangaea.705768
title: Documentation of sediment core GIK13532-2
DOI: 10.1594/pangaea.696374
title: Basic measurements of radiation at station Ilorin (2004-01)

description: Some additional quality control will be performed during summer 2013 for the LW data. For further infos contact Rachel T. Pinker
DOI: 10.1594/pangaea.688644
title: Chlorophyll concentration in three subfractions at bottle station SEPT-1999-K9

description: Separate filtration through polycarbonate Millipore filters having porosities 0.2 (total stock), 1.2 and 3.0µm.
DOI: 10.1594/pangaea.744073
title: (Table 1) Concentration of major components from ODP Hole 175-1085A
DOI: 10.1594/pangaea.780383
title: (Table 3) Chemical composition of low-K glasses from ODP Hole 125-782A fallout tephra

description: Cations based on 4 oxygens. Numerical ages of tephra are based on calcareous nannofossil stratigraphy Xu and Wise (1992, doi:10.2973/odp.proc.sr.125.142.1992)
DOI: 10.1594/pangaea.787446
title: (Table T7) Geochemical composition of amphibole from ODP Hole 176-735B gabbros
DOI: 10.1594/pangaea.696385
title: Basic measurements of radiation at station Ilorin (2004-12)

description: Some additional quality control will be performed during summer 2013 for the LW data. For further infos contact Rachel T. Pinker
DOI: 10.1594/pangaea.816354
title: (Appendix) Major element composition of ODP Site 202-1233 sediments

description: Sediment depth is given in mcd.
DOI: 10.1594/pangaea.827760
title: Physical oceanography measured on water bottle samples during Charles Darwin cruise CD53

description: University of Edinburgh Department of Geology and Geophysics (now University of Edinburgh School of GeoSciences). Authorship was originally "BODC" and was changed by request of the BODC.
DOI: 10.1594/pangaea.876835
title: Continuous light intensity observations at station BEFmate_S3low (2014-09)
DOI: 10.1594/pangaea.748175
title: Hydrography on standard level calculated from water bottle samples of RV Mihail Krupskiy in 1980
DOI: 10.1594/pangaea.665951
title: Oceanography at CTD/bottle station IFREMER_2777
DOI: 10.1594/pangaea.856088
title: Growth during feeding of Scophthalmus maximus first feeding larvae with beta-glucan (MacroGard)
DOI: 10.1594/pangaea.673567
title: Radiosonde measurements from station Bermuda (2005-01)

description: Start location: Bermuda; Distance from radiation site: 2 km
DOI: 10.1594/pangaea.859550
title: (Table S2) Single non-normalized electron probe analyses of all glass shard samples from the Seward Peninsula (core Kit-1)
DOI: 10.1594/pangaea.701503
title: Water temperature profiles from 8 XBT drops along the track of cruise SK115
DOI: 10.1594/pangaea.686243
title: (Table A4) Distribution of Pleistocene calcareous nannofossil marker species and morphotypes at ODP Hole 177-1091A from Meteor Rise, South Atlantic

description: Observed at a magnification of 1000X. Abundance of taxa: V = very abundant (&gt;50%), A = abundant (&gt;20-&lt;50 %), C = common (&gt;10-&lt;20%), F = few (&gt;1-&lt;10%), R = rare (&lt;1%), - = absent
DOI: 10.1594/pangaea.749400
title: Meteorological observations during George IV cruise from Java Head to The Downs started at 1829-02-01
DOI: 10.1594/pangaea.748363
title: Hydrography on standard level calculated from water bottle samples of RV Vema from 1958 to 1962
DOI: 10.1594/pangaea.495839
title: Water temperature IBT profiles from cruise U90CQ85011I_1985
DOI: 10.1594/pangaea.701529
title: Water temperature profiles from 13 XBT drops along the track of cruise SOIREE
DOI: 10.1594/pangaea.701550
title: Water temperature profiles from 9 XBT drops along the track of cruise HOT-20
DOI: 10.1594/pangaea.818754
title: Body size, clutch mass and genetic information of a fragmented lizard population of Lerma, Spain
DOI: 10.1594/pangaea.707575
title: Meteorological synoptical observations from station Payerne (1999-02)
DOI: 10.1594/pangaea.723208
title: Description of profile 7136-111
DOI: 10.1594/pangaea.818888
title: Elevation zones Hintereisferner, Ötztal Alps, Austria, 2001/2002
DOI: 10.1594/pangaea.770880
title: (Table 5) Selected analyses of chromium-spinels in peridotites from ODP Leg 125 samples

description: Fe2O3 and Fe3+ are calculated on the basis of AB2O4 stoichiometry. Cation proportions on the basis of O = 32.
DOI: 10.1594/pangaea.678061
title: Expanded measurements from Neumayer Station (2005-12)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.782656
title: (Table S4) Clinopyroxene compositions of Pito Deep samples
DOI: 10.1594/pangaea.846552
title: Documentation of sediment core LOMROG07-GC02
DOI: 10.1594/pangaea.774278
title: (Table 5) Basement andesite Cr-spinel representative composition, ODP Hole 126-793B
DOI: 10.1594/pangaea.671786
title: Basic measurements of radiation at station Regina (1995-06)
DOI: 10.1594/pangaea.723852
title: Basic measurements of radiation at station Billings (2008-06)
DOI: 10.1594/pangaea.913065
title: Seawater carbonate chemistry parameters model simulation results for Santa Barbara Basin, link to xlsx file

description: The 2013-2014 model‐based estimates of the carbonate system variables (total alankinity (TA), dissolved inorganic carbon (DIC), and saturation state of araongite and calcite (Ω)) and water column parameters (temperature, salinity, and nitrate concentration) near the site of the sediment trap in the Santa Barbara Basin stem from the simulations described in detail by Turi et al. (2016). Simulated water column parameters span from the sea surface (0 meters) to approximately 275 meters water depth. Based on these simulated values, the carbonate system calculation program, CO2SYS was used to estimate the remaining components of the carbonate system, including pH the fugacity, partial pressure, and concentration of CO2, bicarbonate ion, carbonate ion. The model is based on the UCLA‐ETH version of the Regional Oceanic Modeling System (Shchepetkin & McWilliams, 2005) and includes a nitrogen‐based nutrient‐phytoplankton zooplankton‐detritus model (Gruber et al., 2006) that was extended with a carbon module (Gruber et al., 2012; Hauri et al., 2013). The CalCS model setup employed here has a horizontal resolution of 5 km and 34 levels in the vertical and spans the entire U.S. coast from about 30°N to 50°N and extends more than 1,300 km into the Pacific. The boundary conditions at the lateral boundaries of the model consisted of a combination of climatological fields based on observations and time‐varying anomaly fields derived from a global hindcast simulation with the NCAR CCSM3 model (Graven et al., 2012).
DOI: 10.1594/pangaea.753526
title: Documentation of sediment core GeoB14608-1
DOI: 10.1594/pangaea.838753
title: Lithology of sediment core SA12A, Knízecí pláne, Czech Republic

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.787358
title: (Table 7) Major element analysis of ODP Site 134-833 volcaniclastic sediments
DOI: 10.1594/pangaea.787471
title: (Table T14) Major element oxides and cations of titanite from ODP Hole 176-735B veins

description: Number of ions is calculated on the basis of 4 Si atoms.
DOI: 10.1594/pangaea.773397
title: (Table 1) Chemical analyses of olivines in ODP Leg 126 backarc samples

description: Atomic formulas calculated on the basis of 4 oxygens.
DOI: 10.1594/pangaea.805906
title: (Table 1) Geochemistry of clinopyroxene in ODP Hole 140-504B
DOI: 10.1594/pangaea.677768
title: Ozone measurements from station South Pole (1997-10)
DOI: 10.1594/pangaea.779001
title: (Table 4) Geochemistry of apatite from ODP Hole 129-800A samples
DOI: 10.1594/pangaea.787125
title: (Tab. S4) individual amphibole analyses from Ni-Cu-PGE-bearing mafic and ultramafic intrusions from the Portneuf-Mauricie Domain, Grenville Province, Canada
DOI: 10.1594/pangaea.787654
title: (Table 4) Analyses of pyroxenes from ODP Leg 135 sites
DOI: 10.1594/pangaea.807694
title: (Table 1) Climate and soil characteristics of study sites on Anchorage, Signy and Falkland Islands

description: Soil surface temperature (n = 3), photosynthetically active radiation (PAR) (n = 2), soil moisture (n = 3 with the exception of the moss community at Anchorage Island where n = 2) and relative humidity (n = 3) in the vegetation communities of the three study locations. Analyses were based on the mean of the hourly data for the period December 2004-November 2005 for each community.
DOI: 10.1594/pangaea.694745
title: Temperature and salinity in the water column of the Ionian Sea at Station MARCH-2000-IRI31

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.793060
title: (Table 2) Major element oxides of olivine in rocks obtained from the Gorely volcanic center
DOI: 10.15468/dl.c4rndq
title: Occurrence Download

description: A dataset containing 17076 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Türkiye",
 "Geometry POLYGON((30.3333 37.3,31.55 37.3,31.55 38.5,30.3333 38.5,30.3333 37.3))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Animalia"
 ]
}

 The dataset includes 17076 records from 112 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031236-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.870966
title: Geochemistry of heavy minerals of sediment sample LOMROG07-PC04_92.4-94.4cm
DOI: 10.1594/pangaea.665618
title: Oceanography at CTD/bottle station IFREMER_2458
DOI: 10.1594/pangaea.793061
title: (Table 3) Major element oxides of plagioclase in rocks obtained from the Gorely volcanic center
DOI: 10.1594/pangaea.793059
title: (Table 1) Major element oxides of rocks obtained from the Gorely volcanic center
DOI: 10.1594/pangaea.836902
title: (Table 1) Water chemistry of groundwater and snow samples from three sites in Ontario, Canada

description: Snow samples collected from hand-dug pits at two sites in Simcoe County, Ontario, Canada were analysed for major and trace elements using the clean lab methods established for polar ice. Potentially toxic, chalcophile elements are highly enriched in snow, relative to their natural abundance in crustal rocks, with enrichment factor (EF) values (calculated using Sc) in the range 107 to 1081 for Ag, As, Bi, Cd, Cu, Mo, Pb, Sb, Te, and Zn. Relative to M/Sc ratios in snow, water samples collected at two artesian flows in this area are significantly depleted in Ag, Al, Be, Bi, Cd, Cr, Cu, Ni, Pb, Sb, Tl, V, and Zn at both sites, and in Co, Th and Tl at one of the sites. The removal from the waters of these elements is presumably due to such processes as physical retention (filtration) of metal-bearing atmospheric aerosols by organic and mineral soil components as well as adsorption and surface complexation of ionic species onto organic, metal oxyhydroxide and clay mineral surfaces. In the case of Pb, the removal processes are so effective that apparently ''natural'' ratios of Pb to Sc are found in the groundwaters. Tritium measurements show that the groundwater at one of the sites is modern (ie not more than 30 years old) meaning that the inputs of Pb and other trace elements to the groundwaters may originally have been much higher than they are today; the M/Sc ratios measured in the groundwaters today, therefore, represent a conservative estimate of the extent of metal removal along the flow path. Lithogenic elements significantly enriched in the groundwaters at both sites include Ba, Ca, Li, Mg, Mn, Na, Rb, S, Si, Sr, and Ti. The abundance of these elements can largely be explained in terms of weathering of the dominant silicate (plagioclase, potassium feldspar, amphibole and biotite) and carbonate minerals (calcite, dolomite and ankerite) in the soils and sediments of the watershed. Arsenic, Mo, Te, and especially U are also highly enriched in the groundwaters, due to chemical weathering: these could easily be explained if there are small amounts of sulfides (As, Mo, Te) and apatite (U) in the soils of the source area. Elements neither significantly enriched nor depleted at both sites include Fe, Ga, Ge, and P.
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: Shotyk, William; Krachler, Michael; Aeschbach-Hertig, Werner; Hillier, Stephen; Zheng, Jiancheng (2010): Trace elements in recent groundwater of an artesian flow system and comparison with snow: enrichments, depletions, and chemical evolution of the water. Journal of Environmental Monitoring, 12(1), 208
DOI: 10.1594/pangaea.804621
title: (Table 1) Major element content of glass fragments from ODP Site 136-842
DOI: 10.1594/pangaea.751620
title: Meteorological observations during PYLADES cruise from Fayal to Motherbank started at 1815-06-15
DOI: 10.1594/pangaea.477599
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_OC_22S/89

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.911386
title: Weekly monitoring of pH, food resources and copepod traits and performance in a year-round upwelling system, Antofagasta (23°S), during 2015

description: Weekly monitoring of hydrographic and carbonate system parameters were assessed in a year-round upwelling in conjunction with morphometric (body size) and physiological (ingestion and egg production) traits of a numerically dominant copepod species.
DOI: 10.1594/pangaea.903890
title: Peat parameters from the Laphroaig Peat Bog, Islay, Southwestern Scotland
DOI: 10.1594/pangaea.849463
title: Ground-penetrating radar (GPR) point measurements of ice thickness on Nillkees in 2006
DOI: 10.1594/pangaea.778621
title: Dissolution of a spatially variable DNAPL (dense non aqueous phase liquid) source

description: Dissolution of non-aqueous phase liquids (NAPLs) or gases into groundwater is a key process, both for contamination problems originating from organic liquid sources, and for dissolution trapping in geological storage of CO2. Dissolution in natural systems typically will involve both high and low NAPL saturations and a wide range of pore water flow velocities within the same source zone for dissolution to groundwater. To correctly predict dissolution in such complex systems and as the NAPL saturations change over time, models must be capable of predicting dissolution under a range of saturations and flow conditions.To provide data to test and validate such models, an experiment was conducted in a two-dimensional sand tank, where the dissolution of a spatially variable, 5x5 cm**2 DNAPL tetrachloroethene source was carefully measured using x-ray attenuation techniques at a resolution of 0.2x0.2 cm**2. By continuously measuring the NAPL saturations, the temporal evolution of DNAPL mass loss by dissolution to groundwater could be measured at each pixel. Next, a general dissolution and solute transport code was written and several published rate-limited (RL) dissolution models and a local equilibrium (LE) approach were tested against the experimental data. It was found that none of the models could adequately predict the observed dissolution pattern, particularly in the zones of higher NAPL saturation. Combining these models with a model for NAPL pool dissolution produced qualitatively better agreement with experimental data, but the total matching error was not significantly improved. A sensitivity study of commonly used fitting parameters further showed that several combinations of these parameters could produce equally good fits to the experimental observations. The results indicate that common empirical model formulations for RL dissolution may be inadequate in complex, variable saturation NAPL source zones, and that further model developments and testing is desirable.
description: Data in each text file are given in three columns:1) horizontal coordinate x [cm],2) vertical coordinate y [cm],3) NAPL (non aqueous phase liquid) saturation [unitless].The origin for the spatial coordinates is the lower left corner of the fine, white Unimin # 50 sand as shown in Figure 1 of the paper. The file named "NAPLsat_1day" is the initial condition and considered time=0, consequently, NAPLsat_2days refers to measured NAPL saturations after 1 day of dissolution since time zero and so on. The files having an extension "_3x3filer" contain data that have been filtered using a 3 by 3 median filter. The data are given at 2 mm x 2 mm scale. The user can chose to aggregate to a larger scale if desired.
description: Supplement to: Fagerlund, Fritjof; Yang, Zhenjing; Illangasekare, T H; Niemi, A; Phenrat, T; Lowry, G V (submitted): Dissolution of a spatially variable non-aqueous phase liquid source: generation of an experimental dataset and comparison of models. Computers & Geosciences
DOI: 10.1594/pangaea.854974
title: (Table 1) Iceberg characteristics and start and end date and location of iceberg buoys in the Weddell Sea

description: The drift of 52 icebergs tagged with GPS buoys in the Weddell Sea since 1999 has been investigated with respect to prevalent drift tracks, sea ice/iceberg interaction, and freshwater fluxes. Buoys were deployed on small- to medium-sized icebergs (edge lengths &lt;= 5 km) in the southwestern and eastern Weddell Sea. The basin-scale iceberg drift of this size class was established. In the western Weddell Sea, icebergs followed a northward course with little deviation and mean daily drift rates up to 9.5 ± 7.3 km/d. To the west of 40°W the drift of iceberg and sea ice was coherent. In the highly consolidated perennial sea ice cover of 95% the sea ice exerted a steering influence on the icebergs and was thus responsible for the coherence of the drift tracks. The northward drift of buoys to the east of 40°W was interrupted by large deviations due to the passage of low-pressure systems. Mean daily drift rates in this area were 11.5 ± 7.2 km/d. A lower threshold of 86% sea ice concentration for coherent sea ice/iceberg movement was determined by examining the sea ice concentration derived from Special Sensor Microwave Imager (SSM/I) and Advanced Microwave Scanning Radiometer for EOS (AMSR-E) satellite data. The length scale of coherent movement was estimated to be at least 200 km, about half the value found for the Arctic Ocean but twice as large as previously suggested. The freshwater fluxes estimated from three iceberg export scenarios deduced from the iceberg drift pattern were highly variable. Assuming a transit time in the Weddell Sea of 1 year, the iceberg meltwater input of 31 Gt which is about a third of the basal meltwater input from the Filchner Ronne Ice Shelf but spreads across the entire Weddell Sea. Iceberg meltwater export of 14.2 × 103 m3 s-1, if all icebergs are exported, is in the lower range of freshwater export by sea ice.
description: Note: Two positions (ordinal number 7 and 51, parameters: latitude 2 and longitude 2) given by the authors seem to be wrong and are therefore labelled with a "?".
description: Supplement to: Schodlok, Michael P; Hellmer, Hartmut H; Rohardt, Gerd; Fahrbach, Eberhard (2006): Weddell Sea iceberg drift: Five years of observations. Journal of Geophysical Research, 111(C6)
DOI: 10.1594/pangaea.916236
title: 1-Hz PPP displacements at GEONET station 0023 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.887544
title: Expanded measurements from Neumayer Station (2017-05)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.694845
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station FEBR-1999-MNB5

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.751099
title: Meteorological observations during PANTHER cruise from Spithead to Fort St. David started at 1760-01-07
DOI: 10.1594/pangaea.788963
title: Documentation of sediment core M40/4_KL66
DOI: 10.1594/pangaea.748253
title: Hydrography on standard level calculated from water bottle samples of RV Saga in 1963
DOI: 10.1594/pangaea.898428
title: Radiosonde measurements from station Eastern North Atlantic (2015-12)

description: Launches may be at irregular time intervals
DOI: 10.1594/pangaea.759655
title: (Table 1) Chemical element contents in ferromanganese encrustations from the Sierra Leone Rise

description: A detailed study of chemical and mineral compositions of ferromanganese encrustations indicated that their variability dependent on composition of host substrate and on geological and oceanological processes.
description: Supplement to: Emelyanov, Emelyan M; Kharin, Gennady S (1994): Ferromanganese encrustations on seamounts of the Sierra Leone Rise (Equatorial Atlantic). Oceanology, 33(4), 537-544
DOI: 10.1594/pangaea.881325
title: Documentation of sediment core K7905-006BC
DOI: 10.1594/pangaea.511078
title: Radiosonde at Georg-Forster station on 1987-10-07 00:00h

description: Height of tropopause 15668 m
DOI: 10.1594/pangaea.876783
title: Continuous light intensity observations at station BEFmate_I3pio (2016-08)
DOI: 10.1594/pangaea.916801
title: 1-Hz PPP displacements at GEONET station 0612 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.869049
title: Documentation of sediment core GIK18384-2
DOI: 10.1594/pangaea.881331
title: Documentation of sediment core K7905-016GC
DOI: 10.1594/pangaea.676693
title: Radiosonde measurements from Neumayer Station (2006-12)
DOI: 10.1594/pangaea.788964
title: Documentation of sediment core M44/1_70KL
DOI: 10.1594/pangaea.748168
title: Hydrography on standard level calculated from water bottle samples of RV Marlin from 1957 to 1977
DOI: 10.1594/pangaea.869067
title: Documentation of sediment core GIK18408-3
DOI: 10.1594/pangaea.817381
title: (Table 7) Major element composition of plagioclase DSDP Hole 67-495
DOI: 10.1594/pangaea.817385
title: (Table 10) Major element compositions of feldspar at DSDP Sites 67-499 and 67-500
DOI: 10.1594/pangaea.908199
title: Stable water isotope composition (δ¹⁸O, δD, d excess) of firn core DOTT-1
DOI: 10.1594/pangaea.910391
title: Basic measurements of radiation at station Eastern North Atlantic (2015-04)