cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.974127
title: IMAU Antarctic automatic weather station data, including surface radiation balance (AWS17, Scar Inlet, Larsen B remnants)

description: The authors thank all the persons involved in the transport, installation, servicing and dismantling of the weather stations. The technical staff of the IMAU is acknowledged for the design of the weather stations. The Alfred Wegener Institute (AWI) is acknowledged for the support regarding the weather stations at Kohnen Base (AWS9), on Berkner Island (AWS10) and on the Halvfarryggen ice rise (AWS11). The installations of weather stations on Plateau station B (AWS12), and the Pole of inaccessibility (AWS13) were carried out under the umbrella of the project Trans-Antarctic Scientific Traverse Expeditions – Ice Divide of East Antarctica (TASTE-IDEA), funded by the Norwegian Polar Institute, the U.S. National Science Foundation (NSF), and the Research Council of Norway within the framework of TASTE-IDEA project 152 of IPY 2007–2008. The installations of AWS1-3 were carried out at a traverse during the Norwegian Antarctic Research Expedition (NARE) 1996/97 organized by the Norwegian Polar Institute. The traverse was a contribution to the "European Project for Ice Coring in Antarctica" (EPICA), a joint ESF (European Science Foundation)/EC scientific programme, funded by the European Commission under the Environment and Climate Programme (1994-1998) contract ENV4-CT95-0074 and by national contributions from Belgium, Denmark, France, Germany, Italy, The Netherlands, Norway, Sweden, Switzerland and the United Kingdom. The Finnish Antarctic Research Program, (FINNARP) at the Finnish Meteorological Institute (FMI) is acknowledged for the support with the operation of the weather station at Wasa/Aboa Camp Maudheimvida (AWS5). The Royal Meteorological Institute of Belgium (KMI) and the KU Leuven are acknowledged for the support regarding the weather station at the Princess Elisabeth station (AWS16) and On the King Baudouin ice shelf (AWS19). The British Antarctic survey is acknowledged for the support with the operations of the weather stations on the Larsen C ice shelf: North (AWS14), South (AWS15) and Cabinet inlet (AWS18), and on the remnants of the Larsen B ice shelf on Scar inlet (AWS17). The Swedish Antarctic Research Programme (SWEDARP) is acknowledged for the support with the operations of the weather station at the Rampen site 1090 (AWS4), Wasa/Aboa Camp Maudheimvida (AWS5), Svea (AWS6), Scharffenbergbotnen (AWS7), and Camp Victoria (AWS8) in Dronning Maud Land. The weather station on Roi Baudouin ice shelf (AWS19) was installed in the framework of the BENEMELT project, funded by the InBev-Baillet Latour Antarctica Fellowship, a joint initiative of the InBev-Baillet Latour Fund and the International Polar Foundation (IPF).
DOI: 10.1594/pangaea.974128
title: IMAU Antarctic automatic weather station data, including surface radiation balance (AWS18, Cabinet Inlet, Larsen C West)

description: The authors thank all the persons involved in the transport, installation, servicing and dismantling of the weather stations. The technical staff of the IMAU is acknowledged for the design of the weather stations. The Alfred Wegener Institute (AWI) is acknowledged for the support regarding the weather stations at Kohnen Base (AWS9), on Berkner Island (AWS10) and on the Halvfarryggen ice rise (AWS11). The installations of weather stations on Plateau station B (AWS12), and the Pole of inaccessibility (AWS13) were carried out under the umbrella of the project Trans-Antarctic Scientific Traverse Expeditions – Ice Divide of East Antarctica (TASTE-IDEA), funded by the Norwegian Polar Institute, the U.S. National Science Foundation (NSF), and the Research Council of Norway within the framework of TASTE-IDEA project 152 of IPY 2007–2008. The installations of AWS1-3 were carried out at a traverse during the Norwegian Antarctic Research Expedition (NARE) 1996/97 organized by the Norwegian Polar Institute. The traverse was a contribution to the "European Project for Ice Coring in Antarctica" (EPICA), a joint ESF (European Science Foundation)/EC scientific programme, funded by the European Commission under the Environment and Climate Programme (1994-1998) contract ENV4-CT95-0074 and by national contributions from Belgium, Denmark, France, Germany, Italy, The Netherlands, Norway, Sweden, Switzerland and the United Kingdom. The Finnish Antarctic Research Program, (FINNARP) at the Finnish Meteorological Institute (FMI) is acknowledged for the support with the operation of the weather station at Wasa/Aboa Camp Maudheimvida (AWS5). The Royal Meteorological Institute of Belgium (KMI) and the KU Leuven are acknowledged for the support regarding the weather station at the Princess Elisabeth station (AWS16) and On the King Baudouin ice shelf (AWS19). The British Antarctic survey is acknowledged for the support with the operations of the weather stations on the Larsen C ice shelf: North (AWS14), South (AWS15) and Cabinet inlet (AWS18), and on the remnants of the Larsen B ice shelf on Scar inlet (AWS17). The Swedish Antarctic Research Programme (SWEDARP) is acknowledged for the support with the operations of the weather station at the Rampen site 1090 (AWS4), Wasa/Aboa Camp Maudheimvida (AWS5), Svea (AWS6), Scharffenbergbotnen (AWS7), and Camp Victoria (AWS8) in Dronning Maud Land. The weather station on Roi Baudouin ice shelf (AWS19) was installed in the framework of the BENEMELT project, funded by the InBev-Baillet Latour Antarctica Fellowship, a joint initiative of the InBev-Baillet Latour Fund and the International Polar Foundation (IPF).
DOI: 10.1594/pangaea.974129
title: IMAU Antarctic automatic weather station data, including surface radiation balance (AWS19, King Baudouin ice shelf)

description: The authors thank all the persons involved in the transport, installation, servicing and dismantling of the weather stations. The technical staff of the IMAU is acknowledged for the design of the weather stations. The Alfred Wegener Institute (AWI) is acknowledged for the support regarding the weather stations at Kohnen Base (AWS9), on Berkner Island (AWS10) and on the Halvfarryggen ice rise (AWS11). The installations of weather stations on Plateau station B (AWS12), and the Pole of inaccessibility (AWS13) were carried out under the umbrella of the project Trans-Antarctic Scientific Traverse Expeditions – Ice Divide of East Antarctica (TASTE-IDEA), funded by the Norwegian Polar Institute, the U.S. National Science Foundation (NSF), and the Research Council of Norway within the framework of TASTE-IDEA project 152 of IPY 2007–2008. The installations of AWS1-3 were carried out at a traverse during the Norwegian Antarctic Research Expedition (NARE) 1996/97 organized by the Norwegian Polar Institute. The traverse was a contribution to the "European Project for Ice Coring in Antarctica" (EPICA), a joint ESF (European Science Foundation)/EC scientific programme, funded by the European Commission under the Environment and Climate Programme (1994-1998) contract ENV4-CT95-0074 and by national contributions from Belgium, Denmark, France, Germany, Italy, The Netherlands, Norway, Sweden, Switzerland and the United Kingdom. The Finnish Antarctic Research Program, (FINNARP) at the Finnish Meteorological Institute (FMI) is acknowledged for the support with the operation of the weather station at Wasa/Aboa Camp Maudheimvida (AWS5). The Royal Meteorological Institute of Belgium (KMI) and the KU Leuven are acknowledged for the support regarding the weather station at the Princess Elisabeth station (AWS16) and On the King Baudouin ice shelf (AWS19). The British Antarctic survey is acknowledged for the support with the operations of the weather stations on the Larsen C ice shelf: North (AWS14), South (AWS15) and Cabinet inlet (AWS18), and on the remnants of the Larsen B ice shelf on Scar inlet (AWS17). The Swedish Antarctic Research Programme (SWEDARP) is acknowledged for the support with the operations of the weather station at the Rampen site 1090 (AWS4), Wasa/Aboa Camp Maudheimvida (AWS5), Svea (AWS6), Scharffenbergbotnen (AWS7), and Camp Victoria (AWS8) in Dronning Maud Land. The weather station on Roi Baudouin ice shelf (AWS19) was installed in the framework of the BENEMELT project, funded by the InBev-Baillet Latour Antarctica Fellowship, a joint initiative of the InBev-Baillet Latour Fund and the International Polar Foundation (IPF).
DOI: 10.1594/pangaea.974877
title: Pressure-induced leakage of dissolved organic matter (DOM) from different diatom species

description: Four diatom strains obtained from different culture collections were grown to stationary phase in L1 medium plus silicate (Guillard & Hargraves 1993) at 15°C under a light/dark regime of 14/10 h. For experimentation, the diatom strains were incubated at either atmospheric pressure (0.1 MPa = control treatment) or at gradually increasing hydrostatic pressure (0.1-100 MPa = pressure treatment) throughout 21 days in darkness and at 3°C. The pressure treatment simulated the sinking of particle-associated diatoms from the ocean surface down into a hadal trench of 10 km depth. Pressure-induced leakage of dissolved organic matter (DOM) was followed throughout the incubations. Both ambient concentrations and intracellular concentrations of different DOM components were measured: Dissolved organic carbon (DOC), total dissolved nitrogen (TDN), protein-like and humic-like DOM fluorescence, total proteins, total polysaccharides, laminarin, and dimethylsulfoniopropionate (DMSP). The cell abundance of the different diatom strains was followed throughout the incubations.
description: Information about the used cultured organisms:Skeletonema marinoi, Bigelow National Center for Marine Algae and Microbiota, Strain No. CCMP1332, isolated from Long Island Sound (41.2264 N, -73.0639 W) (isolation date is unknown); https://ncma.bigelow.org/CCMP1332Thalassiosira weissflogii, Bigelow National Center for Marine Algae and Microbiota, Strain No. CCMP1336, isolated from Long Island Sound (41.11 N, -72.1 W) (isolation date is unknown); https://ncma.bigelow.org/CCMP1336Chaetoceros socialis, Roscoff Culture Collection, Strain No. RCC6904, isolated from Gulf of Naples (40.7344 N, 14.2718 E) in 2016; https://roscoff-culture-collection.org/rcc-strain-details/6904Phaeodactylum tricornutum, Algal Bank GUMACC (University of Gothenburg), Strain No. 2, isolated from Gullmarsfjorden (58.2934 N, 11.5096 E) in 2004; https://fmprod27.it.gu.se/fmi/webd/GUMACC
DOI: 10.1594/pangaea.974878
title: Pressure-induced leakage of dissolved organic matter (DOM) from diatom-bacteria aggregates

description: Model diatom aggregates were produced from the diatom Skeletonema marinoi and the natural microbial community of seawater collected in Oeresund (Stief et al. 2023), Central Arctic Ocean, and Japan Trench. S. marinoi was grown to stationary phase in L1 medium plus silicate (Guillard & Hargraves 1993) at 15°C under a light/dark regime of 14/10 h. The diatom aggregates were individually incubated at either atmospheric pressure (0.1 MPa = control treatment) or at gradually increasing hydrostatic pressure (0.1-100 MPa = pressure treatment) throughout 20 days in darkness and at 3°C. The pressure treatment simulated the sinking of diatom-bacteria aggregates from the ocean surface down into a hadal trench of 10 km depth. Pressure-induced leakage of dissolved organic matter (DOM) was followed throughout the incubations. Ambient concentrations of different DOM components were measured: Dissolved organic carbon (DOC), total dissolved nitrogen (TDN), protein-like and humic-like DOM fluorescence.
description: Information about the used cultured organisms:Skeletonema marinoi, Bigelow National Center for Marine Algae and Microbiota, Strain No. CCMP1332, isolated from Long Island Sound (41.2264 N, -73.0639 W) (isolation date is unknown); https://ncma.bigelow.org/CCMP1332
DOI: 10.1594/pangaea.974879
title: Degradation of diatom-derived dissolved organic matter (DOM) in surface seawater

description: Stored surface seawater originally collected in the North Sea was amended with dissolved organic matter (DOM) obtained from the diatom Skeletonema marinoi by exposing the diatom culture to a hydrostatic pressure level of 40 MPa for 24 h. To this end, S. marinoi had been grown to stationary phase in L1 medium plus silicate (Guillard & Hargraves 1993) at 15°C under a light/dark regime of 14/10 h. Diatom-cell-free DOM was added to aliquoted seawater samples at initial concentrations of 250 µmol C/L. The microbial degradation of the added DOM and the microbial response to DOM-amendment at 15°C and in darkness was followed for 2 weeks. The seawater was subsampled at defined time intervals to analyze a number of variables.
description: Information about the used cultured organisms:Skeletonema marinoi, Bigelow National Center for Marine Algae and Microbiota, Strain No. CCMP1332, isolated from Long Island Sound (41.2264 N, -73.0639 W) (isolation date is unknown); https://ncma.bigelow.org/CCMP1332
DOI: 10.26180/30026032
title: SHARE2024 Conference Abstract Booklet

description: This is the booklet of submitted and peer reviewed abstracts for the 2024 SHARE Conference held in November 2024. This hybrid event (the second running of it) was held over 2 days - onsite in Melbourne and on Zoom around the rest of Australia, and across the broader Indo-Pacific and South-East Asian regions)
DOI: 10.26180/30026032.v1
title: SHARE2024 Conference Abstract Booklet

description: This is the booklet of submitted and peer reviewed abstracts for the 2024 SHARE Conference held in November 2024. This hybrid event (the second running of it) was held over 2 days - onsite in Melbourne and on Zoom around the rest of Australia, and across the broader Indo-Pacific and South-East Asian regions)
DOI: 10.1594/pangaea.982322
title: Hyperspectral camera raw data (SPECIM_IQ_01) of the Antarctic sea ice cover during the PS140 EASIS cruise in 2024

description: The data consists of 2D hyperspectral images 512x512 pixels in 204 bands in the wavengths range between 400 - 900nm with 2.5 nm step, obtained with the SPECIM IQ hyperspectral camera. The observed surfaces comprise open water, snow covered ice floes, flooded sea ice, overturned ice floes with visible algae layers, under variable illumination conditions. The data are raw data in the original SPECIM IQ format. Within the field of view of each scene, there is a white reference plate, which can be used for image calibration to obtain the hemispheric-directional surface reflectances. Out-of-focus white reference still can be used for calibration as the spectral properties are not affected. Each data record is a folder (compressed as one file) readable by the Specim IQ software, which is downloadable free of charge from the manufacturer (Specim) after registration. This dataset is an experimental setup to explore the use of spatially resolved hyperspectral imaging of Antarctic sea ice obtained from onboard the research vessel.
DOI: 10.1594/pangaea.983878
title: Oceanographic data of Time Series Station Spiekeroog for 2018

description: The Time Series Station Spiekeroog (TSS) was setup in 2002, in the tidal inlet between the East Frisian Islands of Langeoog and Spiekeroog in the Southern German Bight, at position 53°45′01.0″ N, 007°40′16.3″ E. The aim was to ensure the continuous measurement of physical, biological, chemical and meteorological parameters, even under extreme weather conditions such as storms, ice, and storm surges. The TSS was financed as part of the Deutsche Forschungsgemeinschaft (DFG) research unit BioGeoChemistry of Tidal Flats and the Ministry for Science and Culture of the Land of Lower Saxony (MWK). Here, sea level, water temperature and conductivity were measured in the year 2018. All raw data were revised and corrected for steps as range, outliers and stationarity checks. Water temperature and conductivity were measured in five different depths (4 m, 5.5 m, 7.5 m, 9.5 m, 11.5 m below MSL). Due to marine biofouling at the sensors and accompanying drift of instruments, the measured water temperature and conductivity data were corrected via linear regression by using reference data. As the water column in this region is well mixed and the water depth of the measurements varies with the tide, data from all five depths were averaged and referenced to a water depth of 4 m. Absolute salinity was derived from conductivity, temperature and pressure data according to TEOS 10. Data were smoothed and a quality flag was assigned for water temperature and salinity. The quality flags refer to the standard for data quality control of SeaDataNet https://www.seadatanet.org/ (0 = raw data, 1 = good data, 2 = probably good data, 3 = questionable data). A detailed description of the Time Series Station Spiekeroog, its structure and instrumentation can be found in Zielinski et al. (2022) and in Reuter et al. (2009).
DOI: 10.1594/pangaea.983889
title: Oceanographic data of Time Series Station Spiekeroog for 2019

description: The Time Series Station Spiekeroog (TSS) was setup in 2002, in the tidal inlet between the East Frisian Islands of Langeoog and Spiekeroog in the Southern German Bight, at position 53°45′01.0″ N, 007°40′16.3″ E. The aim was to ensure the continuous measurement of physical, biological, chemical and meteorological parameters, even under extreme weather conditions such as storms, ice, and storm surges. The TSS was financed as part of the Deutsche Forschungsgemeinschaft (DFG) research unit BioGeoChemistry of Tidal Flats and the Ministry for Science and Culture of the Land of Lower Saxony (MWK). Here, sea level, water temperature and conductivity were measured in the year 2019. All raw data were revised and corrected for steps as range, outliers and stationarity checks. Water temperature and conductivity were measured in five different depths (4 m, 5.5 m, 7.5 m, 9.5 m, 11.5 m below MSL). Due to marine biofouling at the sensors and accompanying drift of instruments, the measured water temperature and conductivity data were corrected via linear regression by using reference data. As the water column in this region is well mixed and the water depth of the measurements varies with the tide, data from all five depths were averaged and referenced to a water depth of 4 m. Absolute salinity was derived from conductivity, temperature and pressure data according to TEOS 10. Data were smoothed and a quality flag was assigned for water temperature and salinity. The quality flags refer to the standard for data quality control of SeaDataNet https://www.seadatanet.org/ (0 = raw data, 1 = good data, 2 = probably good data, 3 = questionable data). A detailed description of the Time Series Station Spiekeroog, its structure and instrumentation can be found in Zielinski et al. (2022) and in Reuter et al. (2009).
DOI: 10.15468/dl.y6gtys
title: Occurrence Download

description: A dataset containing 16 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Bujurquina huallagae)",
 "BasisOfRecord is one of (Specimen, Literature Occurrence, Human Observation, Observation)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "Year is greater than or equal to 1991",
 "Year is less than or equal to 2025"
 ]
}

 The dataset includes 16 records from 7 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0017416-250827131500795/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.983890
title: Oceanographic data of Time Series Station Spiekeroog for 2020

description: The Time Series Station Spiekeroog (TSS) was setup in 2002, in the tidal inlet between the East Frisian Islands of Langeoog and Spiekeroog in the Southern German Bight, at position 53°45′01.0″ N, 007°40′16.3″ E. The aim was to ensure the continuous measurement of physical, biological, chemical and meteorological parameters, even under extreme weather conditions such as storms, ice, and storm surges. The TSS was financed as part of the Deutsche Forschungsgemeinschaft (DFG) research unit BioGeoChemistry of Tidal Flats and the Ministry for Science and Culture of the Land of Lower Saxony (MWK). Here, sea level, water temperature and conductivity were measured in the year 2020. All raw data were revised and corrected for steps as range, outliers and stationarity checks. Water temperature and conductivity were measured in five different depths (4 m, 5.5 m, 7.5 m, 9.5 m, 11.5 m below MSL). Due to marine biofouling at the sensors and accompanying drift of instruments, the measured water temperature and conductivity data were corrected via linear regression by using reference data. As the water column in this region is well mixed and the water depth of the measurements varies with the tide, data from all five depths were averaged and referenced to a water depth of 4 m. Absolute salinity was derived from conductivity, temperature and pressure data according to TEOS 10. Data were smoothed and a quality flag was assigned for water temperature and salinity. The quality flags refer to the standard for data quality control of SeaDataNet https://www.seadatanet.org/ (0 = raw data, 1 = good data, 2 = probably good data, 3 = questionable data). A detailed description of the Time Series Station Spiekeroog, its structure and instrumentation can be found in Zielinski et al. (2022) and in Reuter et al. (2009).
DOI: 10.15468/dl.kgjgyt
title: Occurrence Download

description: A dataset containing 14358 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "TaxonKey is Arrhenatherum elatius bulbosum"
 ]
}

 The dataset includes 14358 records from 372 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0017417-250827131500795/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.5281/zenodo.17032352
title: Data files and figures for arXiv:2508.20237 (Chiral restoration temperature at finite spin density in QCD)

description: Data files, plot scripts and figures for the paper titled „Chiral restoration temperature at finite spin density in QCD” (arXiv:2508.20237).
DOI: 10.5281/zenodo.17032353
title: Data files and figures for arXiv:2508.20237 (Chiral restoration temperature at finite spin density in QCD)

description: Data files, plot scripts and figures for the paper titled „Chiral restoration temperature at finite spin density in QCD” (arXiv:2508.20237).
DOI: 10.15468/dl.zbv96z
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is China",
 "BasisOfRecord is Fossil",
 "TaxonKey is Plantae",
 "Preparations ~*pollen*"
 ]
}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0017419-250827131500795/datasets/export for details.
DOI: 10.15468/dl.tfuvef
title: Occurrence Download

description: A dataset containing 37279 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "TaxonKey is Bromus rubens"
 ]
}

 The dataset includes 37279 records from 473 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0017418-250827131500795/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.