cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.966060
title: Airborne sea ice parameters during aircraft flight P6_217_ICEBIRD_2019_1904071201, Version 2

description: Airborne multi-instrument measurements of sea ice were made in April 2019 during the winter campaign of the AWI IceBird campaign series. The data consist of five surveys spanning sea-ice covered areas in the Lincoln Sea, Central Arctic Ocean, as well as the Beaufort Sea. For each flight, the geolocated total (ice+snow) thickness data from an airborne electromagnetic (EM) induction sensor are provided with a point spacing of approximately 5-6 meters. Larger gaps in the trajectories arise from high-altitude calibrations of the EM sensor. The data are combined with collocated and simultaneous snow depth measurements from an airborne frequency-modulated continuous-wave ultrawideband radar, snow freeboard measurements from an airborne near-infrared laser scanner, and surface temperature measurements from an airborne infrared radiation pyrometer. Each value represents the average within the approximately 40 m diameter footprint of the EM sensor, thus representing a smoothed representation. These values are then used to derive further sea ice parameters such as sea ice bulk density. The trajectory data contain the full and unfiltered data record with quality flags.
DOI: 10.1594/pangaea.966059
title: Airborne sea ice parameters during aircraft flight P6_217_ICEBIRD_2019_1904051001, Version 2

description: Airborne multi-instrument measurements of sea ice were made in April 2019 during the winter campaign of the AWI IceBird campaign series. The data consist of five surveys spanning sea-ice covered areas in the Lincoln Sea, Central Arctic Ocean, as well as the Beaufort Sea. For each flight, the geolocated total (ice+snow) thickness data from an airborne electromagnetic (EM) induction sensor are provided with a point spacing of approximately 5-6 meters. Larger gaps in the trajectories arise from high-altitude calibrations of the EM sensor. The data are combined with collocated and simultaneous snow depth measurements from an airborne frequency-modulated continuous-wave ultrawideband radar, snow freeboard measurements from an airborne near-infrared laser scanner, and surface temperature measurements from an airborne infrared radiation pyrometer. Each value represents the average within the approximately 40 m diameter footprint of the EM sensor, thus representing a smoothed representation. These values are then used to derive further sea ice parameters such as sea ice bulk density. The trajectory data contain the full and unfiltered data record with quality flags.
DOI: 10.1594/pangaea.866951
title: (Table 1) Collection dates for the upper (1290 m) and lower (3439 m) traps, bulk mass fluxes and composition, molar C:N ratios of organic matter and d15N (only lower trap) of CVOO-3 time-series site
DOI: 10.1594/pangaea.938146
title: Morphotype counts of Emiliania huxleyi coccoliths from surface sediment samples in the Drake Passage
DOI: 10.1594/pangaea.901243
title: Coccolithophores abundance across the Drake Passage from CTD stations during POLARSTERN cruise PS97 (ANT-XXXI/3)
DOI: 10.1594/pangaea.783478
title: (Fig. 4) Lithology of sediment core GeoB11035-1
DOI: 10.1594/pangaea.704633
title: (Table 3) Morphometric measurements of Neogloboquadrina pachyderma sin. from ODP Site 151-907 on the Iceland Plateau

description: sampling size fraction 125-500 µm
DOI: 10.1594/pangaea.937988
title: Water isotope time series (March 2020 - March 2021) of samples collected along the Zingster Bodden chain

description: Time series of stable isotopes (δ2H and δ18O) were analyzed in water samples collected at the Zingster Bodden chain in biweekly to monthly intervals between March 2020 and March 2021. Herefore, a Limnos sampler was used to obtain water from 0.5 to 1 m below surface. In the laboratory, a WTW 1970i conductivity meter and TetraCon 325 measuring cell were used to analyse electrical conductivity. Sub-samples were transferred into measurement vials before isotope analysis was conducted at IGB Berlin, using a Picarro L2130-i cavity ring-down spectrometer. Water chemical parameters were measured with regularly calibrated WTW multiparameter devices.The data give information about the seasonal isotope amplitude at the sampled locations and about spatial variability along the transects.
DOI: 10.1594/pangaea.937986
title: Water isotope time series (March 2020 - March 2021) of samples collected at A. P. Møller Skolen, Kleine Breite, Schlei

description: Time series of stable isotopes (δ2H and δ18O) were analyzed in water samples collected near the A. P. Møller Skolen, Schleswig (Kleine Breite, Schlei), in biweekly to monthly intervals between March 2020 and March 2021. Water was sampled with a pipette from ca. 0.5 m below water surface and directly transferred into a measurement vial. Isotope analysis was conducted at IGB Berlin, using a Picarro L2130-i cavity ring-down spectrometer. Water chemical parameters were measured in-situ with a modular WTW 3440 multiparameter devices and regularly calibrated conductivity cells (MPP 930 IDS, TetraCon® 925-P). The data give information about the seasonal isotope amplitude at the sampled locations and about spatial variability along the transects.
DOI: 10.1594/pangaea.937989
title: Water isotope time series (March 2020 - March 2021) of samples collected in Kloster, Hiddensee

description: Time series of stable isotopes (δ2H and δ18O) were analyzed in water samples taken near the harbour of Kloster (Hiddensee), in biweekly to monthly intervals between March 2020 and March 2021. Water was sampled with a pipette from ca. 0.5 m below water surface and directly transferred into a measurement vial. Isotope analysis was conducted at IGB Berlin, using a Picarro L2130-i cavity ring-down spectrometer. Water chemical parameters were measured in-situ with WTW multiparameter measurement devices.The data give information about the seasonal isotope amplitude at the sampled locations and about spatial variability along the transects.
DOI: 10.15468/dl.y7atvx
title: Occurrence Download

description: A dataset containing 55338 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Felis silvestris Schreber, 1777"
 ]
}

 The dataset includes 55338 records from 487 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000205-250123221155621/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.206401
title: Sedimentology and age control parameter of core PS51/038-4
DOI: 10.1594/pangaea.901375
title: Carbon and carbonate concentrations of ODP Site 162-982 in the North Atlantic
DOI: 10.1594/pangaea.704635
title: (Table 3) Morphometric measurements of Neogloboquadrina pachyderma sin. from ODP Site 162-985 in the Norway Basin

description: sampling size fraction 125-500 µm
DOI: 10.1594/pangaea.890337
title: Isotopic analysis (δ¹⁸O & δ¹³C) of benthic foraminifera from IODP Hole 306-U1313D
DOI: 10.1594/pangaea.875166
title: Coccolith fraction Sr/Ca of sediment core GeoB12613-1 from the western Indian Ocean (off Tanzania)
DOI: 10.1594/pangaea.932663
title: Airborne low-altitude snow depth on sea ice during aircraft flight P5_205_PAMARCMIP_2017_1704021401, Version 1

description: Airborne observations of snow depth on sea ice were made in March and April 2017 as part of the Polar Airborne Measurements and Arctic Regional Climate Model Simulation Project (PAMARCMIP) under the AWI IceBird campaign series. The data consist of six surveys spanning sea-ice covered areas in the Lincoln Sea, Central Arctic Ocean, as well as the Beaufort and Chukchi Seas. For each flight, the geolocated snow depth data from an airborne frequency-modulated continuous-wave ultrawideband radar using an algorithm based on signal peakiness are provided with a point spacing of approximately 4-5 meters. The trajectory data contain the full and unfiltered data record with quality flags. Longer sections of altitude-flagged data arise from calibrations of an EM sensor. Each snow depth value represents the average depth within the radar footprint that has a theoretical smooth surface cross-/along-track diameter of 2.6/1.0 m.
DOI: 10.1594/pangaea.959926
title: Stable oxygen and hydrogen isotopic composition of pore water (δ18O; δD) of sediment core GeoB24343-1

description: The samples are retrieved from sediment core GeoB24343-1 (Monza MV; 0-318 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary complex. Hydrogen (δD) and oxygen (δ18O) isotopes were analysed in the sediment geochemistry laboratory at MARUM using a Picarro 2130i CRD System. Approximately 2 mL of the onboard extracted pore water was used per measurement. The results are an average of at least three injections, while a total of 9 injections of 7 µL each have been analysed per sample. Results are reported in delta notation (‰) relative to V-SMOW2 -SLAP2 with nominal standard (std) deviation of 0.03 for δ18O and 0.3 for δD. Actual std deviation is between 0.02 and 0.29 for δ18O and between 0.04 and 1.68 for δD.
DOI: 10.1594/pangaea.959927
title: Stable oxygen and hydrogen isotopic composition of pore water (δ18O; δD) of sediment core GeoB24346-2

description: The samples are retrieved from sediment core GeoB24346-2 (Milano MV; 0-274 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary complex. Hydrogen (δD) and oxygen (δ18O) isotopes were analysed in the sediment geochemistry laboratory at MARUM using a Picarro 2130i CRD System. Approximately 2 mL of the onboard extracted pore water was used per measurement. The results are an average of at least three injections, while a total of 9 injections of 7 µL each have been analysed per sample. Results are reported in delta notation (‰) relative to V-SMOW2 -SLAP2 with nominal standard (std) deviation of 0.03 for δ18O and 0.3 for δD. Actual std deviation is between 0.02 and 0.29 for δ18O and between 0.04 and 1.68 for δD.
DOI: 10.1594/pangaea.959922
title: Stable oxygen and hydrogen isotopic composition of pore water (δ18O; δD) of sediment core GeoB24310-1

description: The samples are retrieved from sediment core GeoB24310-1 (Napoli MV; 0-280 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary complex. Hydrogen (δD) and oxygen (δ18O) isotopes were analysed in the sediment geochemistry laboratory at MARUM using a Picarro 2130i CRD System. Approximately 2 mL of the onboard extracted pore water was used per measurement. The results are an average of at least three injections, while a total of 9 injections of 7 µL each have been analysed per sample. Results are reported in delta notation (‰) relative to V-SMOW2 -SLAP2 with nominal standard (std) deviation of 0.03 for δ18O and 0.3 for δD. Actual std deviation is between 0.02 and 0.29 for δ18O and between 0.04 and 1.68 for δD.
DOI: 10.1594/pangaea.959923
title: Stable oxygen and hydrogen isotopic composition of pore water (δ18O; δD) of sediment core GeoB24311-1

description: The samples are retrieved from sediment core GeoB24311-1 (Bergamo MV; 0-356 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary complex. Hydrogen (δD) and oxygen (δ18O) isotopes were analysed in the sediment geochemistry laboratory at MARUM using a Picarro 2130i CRD System. Approximately 2 mL of the onboard extracted pore water was used per measurement. The results are an average of at least three injections, while a total of 9 injections of 7 µL each have been analysed per sample. Results are reported in delta notation (‰) relative to V-SMOW2 -SLAP2 with nominal standard (std) deviation of 0.03 for δ18O and 0.3 for δD. Actual std deviation is between 0.02 and 0.29 for δ18O and between 0.04 and 1.68 for δD.
DOI: 10.1594/pangaea.959928
title: Stable oxygen and hydrogen isotopic composition of pore water (δ18O; δD) of sediment core GeoB24348-2

description: The samples are retrieved from sediment core GeoB24348-2 (Brine pool; 0-537 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary complex. Hydrogen (δD) and oxygen (δ18O) isotopes were analysed in the sediment geochemistry laboratory at MARUM using a Picarro 2130i CRD System. Approximately 2 mL of the onboard extracted pore water was used per measurement. The results are an average of at least three injections, while a total of 9 injections of 7 µL each have been analysed per sample. Results are reported in delta notation (‰) relative to V-SMOW2 -SLAP2 with nominal standard (std) deviation of 0.03 for δ18O and 0.3 for δD. Actual std deviation is between 0.02 and 0.29 for δ18O and between 0.04 and 1.68 for δD.
DOI: 10.1594/pangaea.933841
title: Airborne sea ice parameters during aircraft flight P5_205_PAMARCMIP_2017_1704021401, Version 1

description: Airborne multi-instrument measurements of sea ice were made in April 2017 as part of the Polar Airborne Measurements and Arctic Regional Climate Model Simulation Project (PAMARCMIP) under the AWI IceBird campaign series. The data consist of four surveys spanning sea-ice covered areas in the Beaufort and Chukchi Seas. For each flight, the geolocated total (ice+snow) thickness data from an airborne electromagnetic (EM) induction sensor are provided with a point spacing of approximately 5-6 meters. Larger gaps in the trajectories arise from high-altitude calibrations of the EM sensor. The data are combined with collocated and simultaneous snow depth measurements from an airborne frequency-modulated continuous-wave ultrawideband radar, snow freeboard measurements from an airborne near-infrared laser scanner, and surface temperature measurements from an airborne infrared radiation pyrometer. Each value represents the average within the approximately 40 m diameter footprint of the EM sensor, thus representing a smoothed representation. These values are then used to derive further sea ice parameters such as sea ice bulk density. The trajectory data contain the full and unfiltered data record with quality flags.
DOI: 10.1594/pangaea.959929
title: Stable oxygen and hydrogen isotopic composition of pore water (δ18O; δD) of sediment core GeoB24351-1

description: The samples are retrieved from sediment core GeoB24351-1(Gelendzhik MV; 0-284 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary complex. Hydrogen (δD) and oxygen (δ18O) isotopes were analysed in the sediment geochemistry laboratory at MARUM using a Picarro 2130i CRD System. Approximately 2 mL of the onboard extracted pore water was used per measurement. The results are an average of at least three injections, while a total of 9 injections of 7 µL each have been analysed per sample. Results are reported in delta notation (‰) relative to V-SMOW2 -SLAP2 with nominal standard (std) deviation of 0.03 for δ18O and 0.3 for δD. Actual std deviation is between 0.02 and 0.29 for δ18O and between 0.04 and 1.68 for δD.
DOI: 10.1594/pangaea.933875
title: Airborne sea ice parameters during aircraft flight P5_205_PAMARCMIP_2017_1704061801, Version 1

description: Airborne multi-instrument measurements of sea ice were made in April 2017 as part of the Polar Airborne Measurements and Arctic Regional Climate Model Simulation Project (PAMARCMIP) under the AWI IceBird campaign series. The data consist of four surveys spanning sea-ice covered areas in the Beaufort and Chukchi Seas. For each flight, the geolocated total (ice+snow) thickness data from an airborne electromagnetic (EM) induction sensor are provided with a point spacing of approximately 5-6 meters. Larger gaps in the trajectories arise from high-altitude calibrations of the EM sensor. The data are combined with collocated and simultaneous snow depth measurements from an airborne frequency-modulated continuous-wave ultrawideband radar, snow freeboard measurements from an airborne near-infrared laser scanner, and surface temperature measurements from an airborne infrared radiation pyrometer. Each value represents the average within the approximately 40 m diameter footprint of the EM sensor, thus representing a smoothed representation. These values are then used to derive further sea ice parameters such as sea ice bulk density. The trajectory data contain the full and unfiltered data record with quality flags.
DOI: 10.1594/pangaea.933890
title: Airborne sea ice parameters during aircraft flight P5_205_PAMARCMIP_2017_1704082001, Version 1

description: Airborne multi-instrument measurements of sea ice were made in April 2017 as part of the Polar Airborne Measurements and Arctic Regional Climate Model Simulation Project (PAMARCMIP) under the AWI IceBird campaign series. The data consist of four surveys spanning sea-ice covered areas in the Beaufort and Chukchi Seas. For each flight, the geolocated total (ice+snow) thickness data from an airborne electromagnetic (EM) induction sensor are provided with a point spacing of approximately 5-6 meters. Larger gaps in the trajectories arise from high-altitude calibrations of the EM sensor. The data are combined with collocated and simultaneous snow depth measurements from an airborne frequency-modulated continuous-wave ultrawideband radar, snow freeboard measurements from an airborne near-infrared laser scanner, and surface temperature measurements from an airborne infrared radiation pyrometer. Each value represents the average within the approximately 40 m diameter footprint of the EM sensor, thus representing a smoothed representation. These values are then used to derive further sea ice parameters such as sea ice bulk density. The trajectory data contain the full and unfiltered data record with quality flags.
DOI: 10.1594/pangaea.961250
title: Stable water isotope data 2021-2023 from Lobor village (near Zlatar town)

description: Measured values of δ18O and δ2H, associated d-excess values, and amount of collected precipitation from Lobor village, near Zlatar town
description: The precipitation collector has been installed on 2021-02-24.The sample collected on 2022-06-14 (with δ18O = -2.76 ‰, δD = -20.88 ‰, precipitation = 32 mm) has been excluded due to evaporation of the sample.
DOI: 10.1594/pangaea.961248
title: Stable water isotope data 2021-2023 from Petrov vrh (Daruvar)

description: Measured values of δ18O and δ2H, associated d-excess values, and amount of collected precipitation from Petrov vrh (Daruvar)
description: The precipitation collector has been installed on 2021-03-09.
DOI: 10.1594/pangaea.704634
title: (Table 3) Morphometric measurements of Neogloboquadrina pachyderma sin. from ODP Site 151-909 in the Fram Strait

description: sampling size fraction 125-500 µm
DOI: 10.1594/pangaea.937985
title: Water isotope values in samples collected June 2019, March 2020 and July 2020 along estuarine systems at the Baltic Sea coast

description: Stable isotopes (δ2H and δ18O) were analyzed in water samples collected at 68 spots along the Schlei, the Zingster Bodden chain, and the Rügener and Greifswalder Boddens in June 2019, March 2020, and July 2021. Transect samples were taken at shores from 0.3 to 0.6 m below water surface, using a pipette, and directly transferred into measurement vials. Isotope analysis was conducted at IGB Berlin, using a Picarro L2130-i cavity ring-down spectrometer. Water chemical parameters were measured in-situ with a WTW multiparameter device (Multi 3630 IDS), equipped with a WTW TetraCon 925 electrical conductivity measuring cell. The data give information about the spatial isotope variability along the transects.
DOI: 10.1594/pangaea.206403
title: Grain size analysis of coarse fraction in sediment core PS2178-2
DOI: 10.1594/pangaea.959930
title: Stable oxygen and hydrogen isotopic composition of pore water (δ18O; δD) of sediment core GeoB24352-1

description: The samples are retrieved from sediment core GeoB24352-1 (Heraklion MV; 0-272 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary complex. Hydrogen (δD) and oxygen (δ18O) isotopes were analysed in the sediment geochemistry laboratory at MARUM using a Picarro 2130i CRD System. Approximately 2 mL of the onboard extracted pore water was used per measurement. The results are an average of at least three injections, while a total of 9 injections of 7 µL each have been analysed per sample. Results are reported in delta notation (‰) relative to V-SMOW2 -SLAP2 with nominal standard (std) deviation of 0.03 for δ18O and 0.3 for δD. Actual std deviation is between 0.02 and 0.29 for δ18O and between 0.04 and 1.68 for δD.
DOI: 10.1594/pangaea.206410
title: Beryllium 10 analysis of sediment core PS2178-2 from the Arctic Ocean
DOI: 10.1594/pangaea.959925
title: Stable oxygen and hydrogen isotopic composition of pore water (δ18O; δD) of sediment core GeoB24324-2

description: The samples are retrieved from sediment core GeoB24324-2 (Brine pool; 0-445 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary complex. Hydrogen (δD) and oxygen (δ18O) isotopes were analysed in the sediment geochemistry laboratory at MARUM using a Picarro 2130i CRD System. Approximately 2 mL of the onboard extracted pore water was used per measurement. The results are an average of at least three injections, while a total of 9 injections of 7 µL each have been analysed per sample. Results are reported in delta notation (‰) relative to V-SMOW2 -SLAP2 with nominal standard (std) deviation of 0.03 for δ18O and 0.3 for δD. Actual std deviation is between 0.02 and 0.29 for δ18O and between 0.04 and 1.68 for δD.
DOI: 10.1594/pangaea.206404
title: Grain size analysis of coarse fraction in sediment core PS2178-5
DOI: 10.1594/pangaea.961249
title: Stable water isotope data 2021-2023 from Hrvatsko Žarište village (near Vojnić town)

description: Measured values of δ18O and δ2H, associated d-excess values, and amount of collected precipitation from Hrvatsko Žarište village, near Vojnić town
description: The precipitation collector has been installed on 2021-03-11.
DOI: 10.1594/pangaea.206406
title: Sedimentology and age control parameter of core PS2185-6

description: Georeference age is given in calendar years.
DOI: 10.1594/pangaea.206407
title: Sedimentology and age control parameter of core PS2200-2

description: Georeference age is given in calendar years.
DOI: 10.1594/pangaea.186450
title: Sedimentology on core GIK23065-3
DOI: 10.1594/pangaea.382316
title: Radiosonde PS45/16241 during POLARSTERN cruise ARK-XIII/3 on 1997-08-26 09:56h

description: Height of tropopause 10665 m, precipitable water content 0.6131 cm
DOI: 10.1594/pangaea.783569
title: (Fig. 6) Decarbonated grain size mass frequencies of sediment core GeoB130206-1
DOI: 10.1594/pangaea.783498
title: (Fig. 4) Bulk grain size mass frequencies of sediment core GeoB11035-1
DOI: 10.1594/pangaea.382308
title: Radiosonde PS45/16233 during POLARSTERN cruise ARK-XIII/3 on 1997-08-18 09:58h

description: Height of tropopause 9391 m, precipitable water content 0.8081 cm
DOI: 10.1594/pangaea.186469
title: Geometry of coccolith Calcidiscus leptoporus in sediment core K708-007

description: measured on Calcidiscus leptoporus
DOI: 10.1594/pangaea.783577
title: (Fig. 7) Coccolith species abundance of sediment core GeoB11035-1
DOI: 10.1594/pangaea.198637
title: Geometry of coccolith Gephyrocapsa in ODP Hole 104-643A

description: measured on Gephyrocapsa spp.