cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.477740
title: Hydrochemistry measured on water bottle samples at station SPac_1967_ET_43S/37

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.922913
title: Survival traits of plants in experimental plots in a coastal grassland in California (2018-2019)
DOI: 10.1594/pangaea.751037
title: Meteorological observations during PALLAS cruise from Plymouth to Falmouth started at 1825-06-08
DOI: 10.1594/pangaea.759331
title: Basic and other measurements of radiation at Neumayer Station (1999-03)
DOI: 10.1594/pangaea.681281
title: Radiosonde measurements from station Ny-Ålesund (1991-10)
DOI: 10.1594/pangaea.773327
title: Aerosol measurements at station Ny-Ålesund in 2011, raw data

description: for KFM values see doi:10.1594/PANGAEA.743342
DOI: 10.1594/pangaea.743097
title: Aerosol measurements at station Ny-Ålesund in 2005, raw data

description: for KFM values see doi:10.1594/PANGAEA.743342
DOI: 10.1594/pangaea.730385
title: (Table 51) Minerals of interstice and fissure fillings in basalts of alkaline series from the Emperor Mount Chain, DSDP Holes 55-430A, 432A, and 433A

description: X - mineral dominates, + - mineral occurs in minor amount or as admixture.
DOI: 10.1594/pangaea.919152
title: Ultra-violet measurements from station Desert Rock (2019-12)
DOI: 10.1594/pangaea.694442
title: Temperature and salinity in the water column of the Aegean Sea at Station FEBR-1999-IR50

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.832981
title: Basic geochemical data of DSDP Site 80-550, from the latest Paleocene to the late Early Eocene, including PETM, ETM2 and ETM3

description: Calculated ages relative to the onset of the PETM (based on Westerhold et al., 2009, EPSL and our age model) are shown as are linear sedimentation rates (LSRs) and mass accumulation rates (MARs).
DOI: 10.1594/pangaea.919155
title: Ultra-violet measurements from station Desert Rock (2020-01)
DOI: 10.1594/pangaea.667169
title: (Table S3) Barium intensities of the measured split core sediment surface area from XRF core scanning of Site 690
DOI: 10.1594/pangaea.734199
title: Inventory of SINOPS project data sets

description: During the SINOPS project, an optimal state of the art simulation of the marine silicon cycle is attempted employing a biogeochemical ocean general circulation model (BOGCM) through three particular time steps relevant for global (paleo-) climate. In order to tune the model optimally, results of the simulations are compared to a comprehensive data set of 'real' observations. SINOPS' scientific data management ensures that data structure becomes homogeneous throughout the project. Practical work routine comprises systematic progress from data acquisition, through preparation, processing, quality check and archiving, up to the presentation of data to the scientific community. Meta-information and analytical data are mapped by an n-dimensional catalogue in order to itemize the analytical value and to serve as an unambiguous identifier. In practice, data management is carried out by means of the online-accessible information system PANGAEA, which offers a tool set comprising a data warehouse, Graphical Information System (GIS), 2-D plot, cross-section plot, etc. and whose multidimensional data model promotes scientific data mining. Besides scientific and technical aspects, this alliance between scientific project team and data management crew serves to integrate the participants and allows them to gain mutual respect and appreciation.
description: Supplement to: Dittert, Nicolas; Corrin, Lydie; Diepenbroek, Michael; Grobe, Hannes; Heinze, Christoph; Ragueneau, Olivier (2002): Management of (pale-)oceanographic data sets using the PANGAEA information system: the SINOPS example. Computers & Geosciences, 28(7), 789-798
DOI: 10.1594/pangaea.736359
title: Radiosonde measurements from Neumayer Station (2009-02)
DOI: 10.1594/pangaea.736408
title: Basic and other measurements of radiation at Neumayer Station (2009-12)
DOI: 10.1594/pangaea.667171
title: (Table S4) Ba intensities of the measured split core sediment surface area from XRF core scanning of Site 1262 splice
DOI: 10.1594/pangaea.704484
title: δ¹⁸O of ice core DML94C07_38
DOI: 10.1594/pangaea.922916
title: Survival traits per plot and year of plants in experimental plots in a coastal grassland in California (2017-2019)
DOI: 10.1594/pangaea.924897
title: Daily mean water discharge in Bretjørna river in the Grønfjorden area
DOI: 10.1594/pangaea.667422
title: (Table 5) Composition of whole rocks, magnesium oxide enriched trends from DSDP Hole 51-417D
DOI: 10.1594/pangaea.751018
title: Meteorological observations during PALEMBANG cruise from Nederland to Padang started at 1833-09-04
DOI: 10.1594/pangaea.667423
title: (Table 5) Composition of whole rocks, magnesium oxide enriched trends from DSDP Hole 52-418A
DOI: 10.1594/pangaea.923954
title: Hydrogen isotopic composition of leaf waxes at IODP Site 361-U1478
DOI: 10.1594/pangaea.484457
title: Hydrochemistry measured on water bottle samples at station SAVE2/89-1

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.752494
title: Meteorological observations during TIGRIS cruise from Motherbank to Madras started at 1814-06-11
DOI: 10.1594/pangaea.713274
title: (Table 1) Sea surface temperature reconstruction from alkenones of sediment core W8809A-29GC
DOI: 10.1594/pangaea.834343
title: Ceilometer raw data measured at Neumayer Station (2010-01), links to files
DOI: 10.1594/pangaea.904391
title: Table SM-4: Offsets of ODP Site 138-851

description: These are the offsets for Holes 851A, 851B, 851C, 851D and 851E between m CSF (metres core depth below seafloor) and revised m CCSF (revised metres core composite depth below sea floor) for each core.The relevant core for each row is given in the lefthand "Core number" columnAdd the core-specific offset to the CSF scale to convert to the CCSF scale.
DOI: 10.1594/pangaea.925108
title: Meteorological synoptical observations from station Tamanrasset (2020-10)
DOI: 10.1594/pangaea.511777
title: Bivalve abundance of surface sediments of the Atlantic continental shelf off Southern Spanish Sahara, West Africa (Table 2)

description: a = abundant, c = common, f = fragments, r = rare, () = fossil reworked material, * = living and well preserved
DOI: 10.1594/pangaea.925110
title: Ozone measurements from station Tamanrasset (2020-10)
DOI: 10.1594/pangaea.748701
title: Meteorological observations during DROMEDARY cruise from Spithead to Barbados started at 1798-01-10
DOI: 10.1594/pangaea.784287
title: Laser profiles of sea ice surface roughness during ARANDA cruise IRIS 2005 from flight IRIS2005_200503160832
DOI: 10.1594/pangaea.819120
title: Physical oceanography at time series station Brandal in the Kongsfjorden (Spitsbergen, Arctic), 2012-09 to 2013-09
DOI: 10.1594/pangaea.681347
title: Radiosonde measurements from Georg-von-Neumayer Station (1984-12)
DOI: 10.1594/pangaea.784316
title: Laser profiles of sea ice surface roughness during campaign IRIS 2004 from flight IRIS2004_200402100902
DOI: 10.1594/pangaea.477521
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_OC_10S/208

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.511454
title: Dive depth profile of Weddell seal DRE1998_wed_a_f_04 from Drescher Inlet

description: Time-depth profile at 8 s resolution
DOI: 10.1594/pangaea.925113
title: Ultra-violet measurements from station Izaña (2020-10)
DOI: 10.1594/pangaea.925114
title: Radiosonde measurements from station Izaña (2020-10)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.748516
title: Meteorological observations during DIANA cruise from Jamaica to Spithead started at 1792-04-26
DOI: 10.1594/pangaea.682936
title: Continuous meteorological observations at Georg-von-Neumayer station (1987-10)

description: Geocode DATE/TIME has centered values.
DOI: 10.1594/pangaea.925115
title: Ozone measurements from station Izaña (2020-10)
DOI: 10.1594/pangaea.748041
title: Hydrography on standard level calculated from water bottle samples of RV Akademik Mstislav Keldysh from 1982 to 1983
DOI: 10.1594/pangaea.511198
title: Radiosonde at Georg-Forster station on 1989-12-07 00:00h

description: Height of tropopause 8966 m, total ozone 299.9 DU
DOI: 10.1594/pangaea.511199
title: Radiosonde at Georg-Forster station on 1989-12-14 00:00h

description: Height of tropopause 8303 m, total ozone 407.6 DU
DOI: 10.1594/pangaea.664246
title: Oceanography at CTD/bottle station IFREMER_1087
DOI: 10.1594/pangaea.751168
title: Meteorological observations during PHAETON cruise from Hampton Road to Madras started at 1804-01-29
DOI: 10.1594/pangaea.786577
title: (Table 1) Pore-water chemistry, mineralogy and stable isotope ratios for ODP Leg 133 holes

description: The occurrence of dolomite in young Pleistocene sediments off the northeastern coast of Australia offers a special opportunity to examine dolomite formation relative to the original mineralogy and the remineralization of organic material through the processes of sulfate reduction and methanogenesis. The four cores examined in this study form a transect from shallow to deep water (Sites 821, 820, 819, and 822). At all sites, dolomite occurs in sediments of Pleistocene age and is more abundant closer to the continental margin (Site 821) than in sediments found in deeper water (Sites 819 and 822). In spite of the fact that the classic diagenetic zones of sulfate reduction and methanogenesis were all well developed at Sites 819, 820, 821, and 822, the d13C of the interstitial dissolved inorganic carbon (DIC) showed no evidence of these diagenetic processes. The dolomites retrieved from sediments showed d13C values similar to that of the DIC. The isotopic composition of the dolomite revealed no evidence of having been formed in either the sulfate reduction zone or the zone of methanogenesis. The Leg 133 sites differ from other anoxic hemipelagic areas in which extensive sulfate reduction and methanogenesis have been documented in that the sediments are dominated by CaCO3. Recrystallization of calcium carbonate apparently buffers the isotopic composition of the system, masking large isotopic changes that might be induced by additions of isotopically light or heavy CO2 derived from the processes of sulfate reduction and methanogenesis. The dolomite does not appear to be preferentially located in the portion of the cores in which sulfate is absent. Based on the association between the abundance of high-Mg calcite (HMC) and dolomite, it is thought that dolomites formed in response to the dissolution of HMC.
description: Supplement to: Swart, Peter K (1993): The formation of dolomite in sediments from the Continental Margin of northeastern Queensland. In: McKenzie, JA; Davies, PJ; Palmer-Julson, A; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 133, 513-523
DOI: 10.1594/pangaea.834367
title: Ceilometer raw data measured at Neumayer Station (2012-01), links to files
DOI: 10.1594/pangaea.771685
title: Physical oceanography during Walther Herwig III cruise WH272
DOI: 10.1594/pangaea.498129
title: Physical oceanography from BT during cruise U58XX01050B_1941
DOI: 10.1594/pangaea.511251
title: Radiosonde at Georg-Forster station on 1991-12-18 12:00h

description: Height of tropopause 9266 m
DOI: 10.1594/pangaea.510974
title: Radiosonde at Georg-Forster station on 1986-01-19 12:00h

description: Height of tropopause 8675 m
DOI: 10.1594/pangaea.894790
title: Gradient measurements of air and dewpoint temperature, relative humidity and wind speed, in the Djankuat research basin in 2015
DOI: 10.1594/pangaea.895734
title: Water column nutrient, chlorophyll and dissolved organic carbon concentrations and dissolved organic matter characteristics in Roskilde Fjord, Denmark

description: Anthropogenic nutrient enrichment is changing the structure and the function of coastal ecosystems. These coastal zones are transitions between freshwater and marine systems where multiple biogeochemical processes remove, produce and transform organic matter. The extent to which the coastal zone is merely a conduit for terrestrial (allochthonous) organic matter, versus a distinct source of autochthonous organic matter fueled by eutrophication, is unclear. To address this issue, we characterized the freshwater and marine dissolved organic matter (DOM) pools in an eutrophic estuary with a long water residence time (Roskilde Fjord, Denmark) over an annual cycle. We combined elemental, optical (absorbance and fluorescence) and isotopic analyses to obtain insight about the bulk properties of the DOM pool during this period. We also used sediment traps to analyze the changes related to the exchange of organic matter between the particulate (POM) and dissolved (DOM) fractions. The results showed that labile autochthonous DOM from in situ primary production was rapidly transformed to more recalcitrant DOM that accumulated in the estuary despite continuous exchange with the open sea. Also, parts of the POM pool were degraded rapidly (within 24h) and transformed into the DOM pool. Accumulated DOM was characterized by relatively low molecular size and stable carbon isotopic value, and by high protein-like fluorescence. These results indicate that autotrophic material can be a major source of specific recalcitrant DOM in eutrophic coastal waters, contributing significantly to the flux of organic carbon to the ocean.
description: Supplement to: Asmala, Eero; Haraguchi, Lumi; Markager, Stiig; Massicotte, Philippe; Riemann, Bo; Staehr, Peter A; Carstensen, Jacob (2018): Eutrophication leads to accumulation of recalcitrant autochthonous organic matter in coastal environment. Global Biogeochemical Cycles, 32(11), 1673-1687
DOI: 10.1594/pangaea.510977
title: Radiosonde at Georg-Forster station on 1986-02-01 12:00h

description: Height of tropopause 9555 m, total ozone 193.0 DU
DOI: 10.1594/pangaea.510978
title: Radiosonde at Georg-Forster station on 1986-02-05 12:00h

description: Height of tropopause 8556 m, total ozone 280.3 DU
DOI: 10.1594/pangaea.862158
title: GPS-derived precipitable water vapor content calculated for station ALIC
DOI: 10.1594/pangaea.911820
title: Elemental composition of sediment core MD03-2611G measured by X-ray fluorescence
DOI: 10.1594/pangaea.476244
title: Hydrochemistry measured on water bottle samples at station NAtl_1962_ER_59N/294

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.862159
title: GPS-derived precipitable water vapor content calculated for station ALRT
DOI: 10.1594/pangaea.862198
title: GPS-derived precipitable water vapor content calculated for station CEDU
DOI: 10.1594/pangaea.684637
title: Particulate organic carbon and nitrogen concentrations in water samples collected at Station MARCH-1997-GN36199704601MSB02 in the Aegean Sea

description: For determining POC and PON concentrations 1 to 5 litres (depending on the distance of the station from the coast and the depth layer sampled) were filtered through Whatman GF/F filters (2.5 cm diam.). Then these filters were wrapped in aluminium foil and stored at -22°C until analysing in the laboratory.
DOI: 10.1594/pangaea.862201
title: GPS-derived precipitable water vapor content calculated for station CHAN
DOI: 10.1594/pangaea.759473
title: Ozone measurements from Neumayer Station (2010-10)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.772930
title: (Table 1) Petrography of Alborán Island igneous rocks
DOI: 10.1594/pangaea.911822
title: Sea surface temperature from sediment cores MD03-2611G and MUC-3 reconstructed by modern analogue technique
DOI: 10.1594/pangaea.805873
title: (Table 1) Oxygen and hydrogen isotope ratios of hydrothermal altered dolerites from ODP Holes 137-504B and 140-504B

description: Dolerite samples, recovered in the dike complex between 1589 and 1991 meters below seafloor in Hole 504B during Legs 137/140, have been altered by hydrothermal fluids as shown by the intense replacement of igneous minerals by secondary amphiboles, chlorites, albite, and anorthite. These rocks display a negative correlation between alteration extent and density. This is interpreted in terms of the development of secondary light minerals and an increase in porosity.For hydrogen, secondary hydroxyl groups (amphibole) dominate over igneous volatiles and control the dD(whole-rock) (-53 per mil to -40 per mil mean = -44 per mil), the D/H fractionation between amphibole (actinolite) and water being about -44 per mil ± 3 per mil at 350°C assuming the fluid has a sea water D/H ratio (dD(fluid) = 0 per mil).The d18O(whole-rock) values, ranging from 4.7 per mil to 2.7 per mil (mean = 4.1 per mil), are negatively correlated with the abundance of secondary amphiboles, chlorites, and albite (alteration percent) determined by point counting. The comparison of halos related to veins or patches with less altered adjacent parts shows that the process of alteration produces an increase in the amphibole content related to a decrease in the d18O(halo/patch). The halos/patches from the deepest samples in Hole 504B have the lowest d18O(whole-rock) values. This feature can be explained by the progressively decreasing proportion of albite with depth in the dike section. According to Taylor's model, the depletion in 18O of these dolerites (relative to fresh magmatic values: d18O(whole-rock) ~5.7 per mil) is explained by seawater-rock interaction in which the seawater/rock ratio is higher than 0.15 in atomic proportion (~0.3 in mass). Consequently, we deduce that large quantities of seawater-derived fluids have circulated deep in the lower part of the sheeted dike complex of Hole 504B.The d18O profile in Hole 504B shows a net disequilibrium in the 18O exchange between seawater and the oceanic crust in favor of enrichment in 18O in the seawater. This can be explained by a particular strong expression of high-temperature hydrothermal interaction with seawater-derived fluids at shallow depths (i.e., in Layer 2).
description: Supplement to: Agrinier, Pierre; Laverne, Christine; Tartarotti, Paola (1995): Stable isotope ratios (oxygen, hydrogen) and petrology of hydrothermally altered dolerites at the bottom of the sheeted dike complex of Hole 504B. In: Erzinger, J; Becker, K; Dick, HJB; Stokking, LB (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 137, 99-106
DOI: 10.1594/pangaea.911866
title: Sea surface temperature from sediment core SS0206-GC15 reconstructed by modern analogue technique
DOI: 10.1594/pangaea.663509
title: Oceanography at CTD/bottle station IFREMER_0349
DOI: 10.1594/pangaea.921401
title: Macro-ice content of permafrost of the high floodplain at the estuary section of the Tambey River
DOI: 10.1594/pangaea.692288
title: Particulate organic carbon and nitrogen concentrations in water samples collected at Station SEPT-1997-GN36199704605MSB02 in the Aegean Sea

description: Seawater samples (1-5 l depending on distance of a station from a coast and depth of sampling) were filtered through Whatman GF/F filters (diameter 2.5 cm). Then the filters were wrapped in aluminium foil and stored at 22°C until analysis according to Hedges and Stern (Hedges, J.I., Stern, J.H. 1984. Carbon and nitrogen determinations of carbonate-containing solids. Limnol. Oceanogr., 29(3), 657-663; http://www.aslo.org/lo/toc/vol_29/issue_3/0657.pdf)
DOI: 10.1594/pangaea.775037
title: Continuous meteorological observations at Neumayer station (2005-03)
DOI: 10.1594/pangaea.728801
title: Basic measurements of radiation at station Xianghe (2005-08)

description: Version 5, 2009-10-28; The instruments are installed on the roof of the building at about 10 meters from the soil.
DOI: 10.1594/pangaea.674449
title: Radiosonde measurements from Neumayer Station (2000-05)
DOI: 10.1594/pangaea.677199
title: Ozone measurements from Neumayer Station (1993-01)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.692291
title: Particulate organic carbon and nitrogen concentrations in water samples collected at Station SEPT-1997-GN36199704605MSB07 in the Aegean Sea

description: Seawater samples (1-5 l depending on distance of a station from a coast and depth of sampling) were filtered through Whatman GF/F filters (diameter 2.5 cm). Then the filters were wrapped in aluminium foil and stored at 22°C until analysis according to Hedges and Stern (Hedges, J.I., Stern, J.H. 1984. Carbon and nitrogen determinations of carbonate-containing solids. Limnol. Oceanogr., 29(3), 657-663; http://www.aslo.org/lo/toc/vol_29/issue_3/0657.pdf)
DOI: 10.1594/pangaea.759485
title: Expanded measurements from Neumayer Station (2010-12)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.681393
title: Radiosonde measurements from Georg-von-Neumayer Station (1989-01)
DOI: 10.1594/pangaea.908280
title: Geochemical and mineralogical composition of sediment core 4-2 from Inle Lake (Southern Shan State, Myanmar)
DOI: 10.1594/pangaea.510838
title: Radiosonde at Georg-Forster station on 1990-01-11 00:00h

description: Height of tropopause 9596 m, total ozone 260.6 DU
DOI: 10.1594/pangaea.786217
title: Basic measurements of radiation at station Xianghe (2009-07)
DOI: 10.1594/pangaea.510840
title: Radiosonde at Georg-Forster station on 1990-01-25 00:00h

description: Height of tropopause 9983 m, total ozone 310.5 DU
DOI: 10.1594/pangaea.615297
title: Description of the soil of core LD98_t14b

description: For the position of the transects t, v, and w see also figure 3-1
DOI: 10.1594/pangaea.862410
title: GPS-derived precipitable water vapor content calculated for station RIOP
DOI: 10.1594/pangaea.862483
title: GPS-derived precipitable water vapor content calculated for station VESL
DOI: 10.1594/pangaea.907501
title: Organic carbon, nitrogen, sulfur content and stable carbon isotopes for sediment core PG1172
DOI: 10.1594/pangaea.712773
title: (Table A10) Carbonate, total organic carbon and sulphur content of sediment core POS158/1_0020/2
DOI: 10.1594/pangaea.726478
title: (Table 2) Normalized microprobe analyses of volcanic glasses from DSDP Sites 63-468 and 63-469

description: Note that, where there were multiple analyses of the same grain, the average of those analyses is shown. All analyses have been normalized to 100%, but the original total is also shown.
DOI: 10.1594/pangaea.845279
title: Basic measurements of radiation at station Lerwick (2015-03)
DOI: 10.1594/pangaea.723480
title: Basic measurements of radiation at station Billings (1997-01)

description: Version 2, 2009-07-02
DOI: 10.1594/pangaea.848023
title: Basic measurements of radiation at station Camborne (2015-06)