cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.861316
title: Physical oceanography from CVOO mooring KPO_1094

description: CVOO: Cape Verde Ocean Observatory ProjectLabel:kpo_1094_01 Type:Seabird Microcat SN:2809Label:kpo_1094_02 Type:Seabird Microcat SN:1717Label:kpo_1094_03 Type:Seabird Microcat SN:7472Label:kpo_1094_04 Type:Aanderaa Optode SN:938Label:kpo_1094_05 Type:GEOMAR Mini T-D Logger SN:70Label:kpo_1094_06 Type:Seabird Microcat SN:2934Label:kpo_1094_08 Type:Seabird Microcat SN:960Label:kpo_1094_09 Type:Seabird Microcat SN:1520Label:kpo_1094_10 Type:Aanderaa Optode SN:939Label:kpo_1094_11 Type:Sunburst SAMI CO2-Sensor SN:NaNLabel:kpo_1094_12 Type:Teledyne RDI ADCP SN:1972Label:kpo_1094_13 Type:Seabird Microcat SN:2265Label:kpo_1094_14 Type:Seabird Microcat SN:1721Label:kpo_1094_15 Type:Aanderaa RCM-8 SN:10555Label:kpo_1094_16 Type:Seabird Microcat SN:2492Label:kpo_1094_17 Type:Seabird Microcat SN:381Label:kpo_1094_18 Type:Seabird Microcat SN:3413Label:kpo_1094_20 Type:Aanderaa RCM-8 SN:12005Label:kpo_1094_21 Type:Seabird Microcat SN:2264Label:kpo_1094_22 Type:Seabird Microcat SN:53Label:kpo_1094_23 Type:GEOMAR Mini T-D Logger SN:34Label:kpo_1094_24 Type:Seabird Microcat SN:957Label:kpo_1094_25 Type:GEOMAR Mini T-D Logger SN:46Label:kpo_1094_26 Type:Seabird Microcat SN:938Label:kpo_1094_27 Type:GEOMAR Mini T-D Logger SN:27Label:kpo_1094_29 Type:Aanderaa RCM-8 SN:11622Label:kpo_1094_30 Type:Seabird Microcat SN:1162Label:kpo_1094_31 Type:GEOMAR Mini T-D Logger SN:24Label:kpo_1094_32 Type:Seabird Microcat SN:1320Label:kpo_1094_33 Type:GEOMAR Mini T-D Logger SN:20
DOI: 10.1594/pangaea.946835
title: Ground temperature data of a tundra polygonal lake near the WWF station Kytalyk at the Berelekh River in the Indigirka lowland (NE Siberia) from 2011-2012

description: Patterned ground of the polygonal tundra yields sensitive indicators of environmental and climate change. Polygon ponds, mires and cryosoils are typical components of Arctic Siberian wetlands underlain by permafrost. Field studies of recent environmental dynamics were carried out in the Indigirka lowland in summer 2011 and 2012. Using a multidisciplinary approach, several stages of polygonal systems were studied as modern tundra habitats in the surrounding of the WWF station Kytalyk at the Berelekh River, a tributary of the Indigirka River. The floral and faunal associations of the polygonal tundra landscape were described. Ecological, hydrological, meteorological, limnological and cryological features were analyzed in order to evaluate modern environmental conditions and their essential controlling parameters. A monitoring program was carried out to measure changes of air, water and ground temperatures as well as water conductivity, water level and soil moisture and to collect water, diatom, zooplankton, zoobenthos, tecamoebae, phytoplankton and ostracod samples. These data sets contain environmental field data, logger data, various ecological data, and analyses of sediments and water.This dataset comprises ground temperature measurements at different depth at the center and wall of a polygonal lake from 2011-2012.
DOI: 10.1594/pangaea.664381
title: Oceanography at CTD/bottle station IFREMER_1222
DOI: 10.1594/pangaea.837363
title: (Table 2) Stomach content of anadromous Arctic char (Salvelinus alpinus) sampled in inner Frobisher Bay, Canada

description: Sample amount N = 58. Frequency of occurrence is expressed relative to the total number of stomachs containing food (N = 56).
DOI: 10.1594/pangaea.826961
title: (Table 2) 210Pb and 137Cs activity ratios from bulk sediment from sediment core JM06-WP-16-MCB
DOI: 10.1594/pangaea.752935
title: Meteorological observations during YARMOUTH cruise from Barbuda to Barbados started at 1778-02-21
DOI: 10.1594/pangaea.831454
title: Photograph frames taken for monitoring coral reef conditions during and after a severe bleaching event in 2010 in the Andaman Sea
DOI: 10.1594/pangaea.919647
title: Biovolume of Ceratium longipes and Ceratium fusus in the KOSMOS Experiment Bergen 2015
DOI: 10.1594/pangaea.857513
title: Phenotypical responses of Fucus vesiculosus germlings to warming, acidification, nutrient enrichment and local upwelling under natural fluctuations (July - September 2014) - Nutrients

description: Kiel Outdoor Benthocosms
DOI: 10.1594/pangaea.767358
title: (Table 1) Depth and ages of the chronolostratigraphical boundaries from IODP Sites 303-U1305, U1302 and U1303

description: Cores raised during IODP Expedition 303 off southern Greenland (Eirik Ridge site 1305) and off the Labrador Coast (Orphan Knoll site 1302/1303) were analyzed to establish an isotope stratigraphy, respectively for the "inner" and "outer" basins of the Labrador Sea (LS). These isotopic data also provide information on the Atlantic Meridional Overturning Circulation (AMOC), notably with regard to the intensity of the Western Boundary Under Current (WBUC), which is tightly controlled by the production of Denmark Strait Overflow Water (DSOW), and the production of Labrador Sea Water (LSW) in the inner basin through winter cooling and convection. The upper 184 m of sediment at Eirik Ridge spans marine isotope stages (MIS) 32 to 1. At this site, two distinct regimes are observed: prior to MIS 20, the isotopic record resembles that of the open North Atlantic records of the interval, whereas a more site-specific pattern is observed afterwards. This later pattern was characterized by i) high DSOW production rates and strong WBUC during interglacial stages, as indicated by sedimentation rates, ii) large amplitude d18O-shifts from glacial stages to interglacial stages (&gt; 2.5 per mil) and iii) an overall range of d18O-values significantly more positive than before. At Orphan Knoll, the 105 m record spans approximately 800 ka and provides direct information on linkages between the northeastern sector of the Laurentide Ice Sheet and the North Atlantic. At this site, a shift towards larger amplitude glacial/interglacial ranges of d18O-values occurred after MIS 13, although isotopic records bear a typical North Atlantic signature, particularly during MIS 5, in contradiction to those of Eirik Ridge, where substages 5a to 5c are barely recognized. Closer examination of d18O-records in planktic and benthic foraminifera demonstrates the presence of distinct deep-water masses in the inner vs. outer LS basins during MIS 11 and more particularly MIS 5e. Data confirm that the modern AMOC, with LSW formation, seems mostly exclusive to the present interglacial, and also suggest some specificity of each interglacial with respect to the production rate of DSOW and the AMOC, in general.
description: Sediment depth is given in mcd. The authors compilated Site 303-U1303 and Site 303-U1302, this composite core is given here as Site 303-U1302.
description: Supplement to: Hillaire-Marcel, Claude; de Vernal, Anne; McKay, Jennifer L (2011): Foraminifer isotope study of the Pleistocene Labrador Sea, northwest North Atlantic (IODP Sites 1302/03 and 1305), with emphasis on paleoceanographical differences between its “inner” and “outer” basins. Marine Geology, 279(1-4, 188-198
DOI: 10.1594/pangaea.906318
title: Nitrogen isotope and element concentration data for core Tarfaya SN4
DOI: 10.1594/pangaea.909911
title: Physical oceanography (ADCP) from mooring KPO_1107

description: Newly processed version with Mooring toolbox version 2019.
DOI: 10.1594/pangaea.860335
title: Freshwater mesocosm experiment 2012 in Vancouver, Canada: average temperature

description: P=Phytoplankton; PZ=Phytoplankton+Zooplankton, PZN=Phytoplankton + Zooplankton+Notonectids
DOI: 10.1594/pangaea.860337
title: Freshwater mesocosm experiment 2012 in Vancouver, Canada: zooplankton size

description: P=Phytoplankton; PZ=Phytoplankton+Zooplankton, PZN=Phytoplankton + Zooplankton+Notonectids
DOI: 10.1594/pangaea.860336
title: Freshwater mesocosm experiment 2012 in Vancouver, Canada: oxygen

description: P=Phytoplankton; PZ=Phytoplankton+Zooplankton, PZN=Phytoplankton + Zooplankton+Notonectids
DOI: 10.1594/pangaea.860338
title: Freshwater mesocosm experiment 2012 in Vancouver, Canada: zooplankton species

description: P=Phytoplankton; PZ=Phytoplankton+Zooplankton, PZN=Phytoplankton + Zooplankton+Notonectids
DOI: 10.1594/pangaea.860339
title: Freshwater mesocosm experiment 2012 in Vancouver, Canada: phytoplankton

description: P=Phytoplankton; PZ=Phytoplankton+Zooplankton, PZN=Phytoplankton + Zooplankton+Notonectids
DOI: 10.1594/pangaea.912478
title: XRF core scanning data from Core LB1 (La Bedoule, southern France)
DOI: 10.1594/pangaea.919632
title: Phytoplankton and microzooplankton biomass in the KOSMOS Experiment Bergen 2015
DOI: 10.1594/pangaea.906319
title: Iron speciation measured on core Tarfaya SN4
DOI: 10.1594/pangaea.912479
title: XRF core scanning data from Core LB3 (La Bedoule, southern France)
DOI: 10.1594/pangaea.948275
title: Ultra-violet measurements from station Izaña (2022-08)
DOI: 10.1594/pangaea.924690
title: Physical oceanography from mooring KPO_0612

description: The processing was done as described in Bunge et al. (2008) and in Bourlès Bernard et al (2020): French PIRATA cruises: MOORING ADCP data. SEANOE. https://doi.org/10.17882/51557
description: instrument = Label:kpo_0612_01 File:kpo_0612_instr_01.nc Type:Teledyne RDI Workhorse 300 SN:508instrument = Label:kpo_0612_02 File:kpo_0612_instr_02.nc Type:Teledyne RDI LongRanger 75 SN:3173instrument = Label:kpo_0612_03 File:kpo_0612_instr_03.nc Type:Aanderaa RCM 4 SN:05486instrument = Label:kpo_0612_05 File:kpo_0612_instr_05.nc Type:Aanderaa RCM 4 SN:05450instrument = Label:kpo_0612_06 File:kpo_0612_instr_06.nc Type:Aanderaa RCM 4 SN:05893instrument = Label:kpo_0612_07 File:kpo_0612_instr_07.nc Type:Aanderaa RCM 4 SN:05446instrument = Label:kpo_0612_08 File:kpo_0612_instr_08.nc Type:Aanderaa RCM 4 SN:05894comment = flag_meaningscomment = 0:unknowncomment = 1:good_datacomment = 2:probably_good_datacomment = 3:potentially_correctable_bad_datacomment = 4:bad_datacomment = 5:not_usedcomment = 6:not_usedcomment = 7:nominal_value
DOI: 10.1594/pangaea.674067
title: Radiosonde measurements from station Camborne (2003-04)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.924244
title: Physical oceanography from mooring KPO_1026

description: GEOMAR moorings are typically equipped with instruments recording pressure, temperature, conductivity, dissolved oxygen and current velocity. Instruments with pressure, temperature, conductivity and oxygen sensors were calibrated in situ immediately prior to and after a mooring deployment period by attaching them to the CTD frame during CTDO casts. Correction terms were then developed from the difference between the sensor readings and the calibrated CTDO data during several minute long calibration stops. These correction terms were then applied to the full deployment periods. This ensured best data quality with recognition of potential sensor drifts and also allowed for the estimation of calibration and measurement errors (Hahn et al. 2014, Bittig et al. 2018, Berx et al. 2019).
description: instrument = Label:kpo_1026_02 File:kpo_1026_instr_02.nc Type:Seabird Microcat SN:2247instrument = Label:kpo_1026_04 File:kpo_1026_instr_04.nc Type:Aanderaa RCM-8 SN:9345instrument = Label:kpo_1026_05 File:kpo_1026_instr_05.nc Type:Seabird Microcat SN:3196Quality flags:1:good_data7:nominal_value
DOI: 10.1594/pangaea.857323
title: (Table 1, page 106) Chemical composition of Lake George (New York) iron-manganese nodules

description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
DOI: 10.1594/pangaea.924245
title: Physical oceanography from mooring KPO_1027

description: GEOMAR moorings are typically equipped with instruments recording pressure, temperature, conductivity, dissolved oxygen and current velocity. Instruments with pressure, temperature, conductivity and oxygen sensors were calibrated in situ immediately prior to and after a mooring deployment period by attaching them to the CTD frame during CTDO casts. Correction terms were then developed from the difference between the sensor readings and the calibrated CTDO data during several minute long calibration stops. These correction terms were then applied to the full deployment periods. This ensured best data quality with recognition of potential sensor drifts and also allowed for the estimation of calibration and measurement errors (Hahn et al. 2014, Bittig et al. 2018, Berx et al. 2019).
description: instrument = Label:kpo_1027_02 File:kpo_1027_instr_02.nc Type:Seabird Microcat SN:2245instrument = Label:kpo_1027_04 File:kpo_1027_instr_04.nc Type:Aanderaa RCM-8 SN:9727instrument = Label:kpo_1027_05 File:kpo_1027_instr_05.nc Type:Seabird Microcat SN:2248Quality flags:1:good_data7:nominal_value
DOI: 10.1594/pangaea.876749
title: Continuous light intensity observations at station BEFmate_I3low (2015-09)
DOI: 10.1594/pangaea.948278
title: Ozone measurements from station Izaña (2022-08)
DOI: 10.1594/pangaea.943783
title: Physicochemical parameters of the water column for the sample stations of the Weser river campaign 2016

description: A key task in understanding and mapping the complex mass transport pathways and potential transformation processes of contaminants in coastal regions such as the German Bight is to determine and evaluate the most significant contribution sources into coastal areas. Rivers represent one key input source within this context. As part of a river campaign in June 2016, sediment and freshwater samples were taken from the Weser river and its tributaries to identify their elemental and isotopic fingerprint and to investigate potential inputs to the German Bight. At every sampling station physicochemical parameters of the water column were measured directly after sampling with respective probes of a multimeter covering pH, dissolved oxygen, temperature and conductivity.
DOI: 10.1594/pangaea.948342
title: Ozone measurements from station Tamanrasset (2022-08)
DOI: 10.1594/pangaea.948367
title: Radiosonde measurements from station Tateno (2022-06)
DOI: 10.1594/pangaea.948276
title: Radiosonde measurements from station Izaña (2022-08)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.930579
title: Temperature and precipitation reconstruction for western North America samples from the Northern Hemisphere Harmonized Pollen Archive
DOI: 10.1594/pangaea.876755
title: Continuous light intensity observations at station BEFmate_I3low (2016-09)
DOI: 10.1594/pangaea.943671
title: Physicochemical parameters of the water column for the sample stations of the Ems river campaign 2016

description: In order to understand and map the complex mass transport pathways and possible transformation processes of contaminants in coastal regions such as the German Bight, the main coastal contributors must be identified and evaluated. In this context, rivers represent a major input source. In the framework of a river campaign from 20.06.16 till 25.06.2016, sediment and freshwater samples of the Ems and its tributaries were taken to determine their elemental and isotopic fingerprint and to investigate possible inputs into the German Bight. All sediment samples were obtained using a Van Veen grab sampler and were analyzed for their grain size distribution by laser diffraction.
DOI: 10.1594/pangaea.837158
title: (Table 2) d44/40Ca values of planktonic foraminifera from ODP Holes 144-871A and 144-872C
DOI: 10.1594/pangaea.855984
title: (Table 1, page 222) Chemical composition of freshwater concretions from Oneida Lake, New York

description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
DOI: 10.1594/pangaea.948302
title: Expanded measurements from station Ny-Ålesund (2022-08)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.672199
title: Radiosonde measurements from station South Pole (2001-01)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.924266
title: Physical oceanography from mooring KPO_1142 part 1

description: GEOMAR moorings are typically equipped with instruments recording pressure, temperature, conductivity, dissolved oxygen and current velocity. Instruments with pressure, temperature, conductivity and oxygen sensors were calibrated in situ immediately prior to and after a mooring deployment period by attaching them to the CTD frame during CTDO casts. Correction terms were then developed from the difference between the sensor readings and the calibrated CTDO data during several minute long calibration stops. These correction terms were then applied to the full deployment periods. This ensured best data quality with recognition of potential sensor drifts and also allowed for the estimation of calibration and measurement errors (Hahn et al. 2014, Bittig et al. 2018, Berx et al. 2019).
description: instrument = Label:kpo_1142_01 File:kpo_1142_instr_01.nc Type:GEOMAR TD-Logger SN:48instrument = Label:kpo_1142_02 File:kpo_1142_instr_02.nc Type:Seabird MicroCat 37-IM mit P SN:03754instrument = Label:kpo_1142_03 File:kpo_1142_instr_03.nc Type:Aanderaa Optode 3830 SN:00206instrument = Label:kpo_1142_04 File:kpo_1142_instr_04.nc Type:Seabird MicroCat 37-IM SN:02933instrument = Label:kpo_1142_05 File:kpo_1142_instr_05.nc Type:Aanderaa Optode 4330 SN:00215instrument = Label:kpo_1142_06 File:kpo_1142_instr_06.nc Type:Seabird MicroCat 37-SM mit P SN:10609instrument = Label:kpo_1142_07 File:kpo_1142_instr_07.nc Type:Aanderaa Optode 4330 SN:00216instrument = Label:kpo_1142_08 File:kpo_1142_instr_08.nc Type:Seabird MicroCat 37-IM SN:02801Quality flags:0:unknown1:good_data2:probably_good_data3:potentially_correctable_bad_data4:bad_data5:not_used6:not_used7:nominal_value8:interpolated_value
DOI: 10.1594/pangaea.874317
title: Particle export fluxes from sediment traps during METEOR cruise M105: Changes in organic matter composition of particles sinking through the OMZ
DOI: 10.1594/pangaea.924270
title: Physical oceanography from mooring KPO_1142 part 2

description: GEOMAR moorings are typically equipped with instruments recording pressure, temperature, conductivity, dissolved oxygen and current velocity. Instruments with pressure, temperature, conductivity and oxygen sensors were calibrated in situ immediately prior to and after a mooring deployment period by attaching them to the CTD frame during CTDO casts. Correction terms were then developed from the difference between the sensor readings and the calibrated CTDO data during several minute long calibration stops. These correction terms were then applied to the full deployment periods. This ensured best data quality with recognition of potential sensor drifts and also allowed for the estimation of calibration and measurement errors (Hahn et al. 2014, Bittig et al. 2018, Berx et al. 2019). Moored Acoustic Doppler Current Profiler bin depths were corrected using the sound speed at instrument depth following the approach by Shcherbina et al. (2005). Velocities were not corrected, but respective measurement errors were assumed as described in Hahn et al. (2014). For all instruments within a mooring that did not record pressure, full deployment pressure time series were estimated by linearly interpolating between the instruments having a pressure sensor.
description: instrument = Label:kpo_1142_09 File:kpo_1142_instr_09.nc Type:Aanderaa Optode 4330 SN:00375instrument = Label:kpo_1142_10 File:kpo_1142_instr_10.nc Type:Seabird MicroCat 37-SM SN:02247instrument = Label:kpo_1142_11 File:kpo_1142_instr_11.nc Type:Aanderaa Optode 4330 SN:00379instrument = Label:kpo_1142_12 File:kpo_1142_instr_12.nc Type:Seabird MicroCat 37-IM mit P SN:10696instrument = Label:kpo_1142_13 File:kpo_1142_instr_13.nc Type:Aanderaa Optode 3830 SN:00940instrument = Label:kpo_1142_14 File:kpo_1142_instr_14.nc Type:Seabird MicroCat 37-SM SN:01550instrument = Label:kpo_1142_15 File:kpo_1142_instr_15.nc Type:Aanderaa Optode 3830 SN:01074instrument = Label:kpo_1142_16 File:kpo_1142_instr_16.nc Type:Teledyne RDI LongRanger 75 SN:02330Quality flags:0:unknown1:good_data2:probably_good_data3:potentially_correctable_bad_data4:bad_data5:not_used6:not_used7:nominal_value8:interpolated_value
DOI: 10.1594/pangaea.943769
title: Grain size distribution for sediment samples of the campaign Watt2014

description: The German Wadden Sea represents a central sink for the accumulation and further distribution of sediments and SPM originating from the big river systems Elbe, Weser, Ems and Rhine, the German bight as well as from the Wadden Sea area itself. Knowledge about the origin, transport and accumulation of these materials are in particular of importance for coastal protection or the quality status of the German coastal areas in terms of its pollution status.In order to assess the anthropogenic fingerprint of this region also in comparison to previous analysis water and sediment samples were taken between 10.06.2014 and 20.06.2014 at different Wadden Sea areas along the German coast. The surface sediment samples were taken by a box grab or directly using small cores during low tide from the selected Wadden Sea areas representing different sediment properties and were analyzed for their grain size distribution by laser diffraction.
DOI: 10.1594/pangaea.825074
title: Age determination results from site Beaverdam_Creek
DOI: 10.1594/pangaea.877490
title: Urban meteorological data of station 2238 for the city of Amsterdam during the summer of 2015
DOI: 10.1594/pangaea.933125
title: Description of sampling sites in the Indopacific region
DOI: 10.1594/pangaea.932954
title: Description of sampling sites in the African region
DOI: 10.1594/pangaea.933142
title: Description of sampling sites in the NE America region
DOI: 10.1594/pangaea.877491
title: Urban meteorological data of station 2239 for the city of Amsterdam during the summer of 2015
DOI: 10.1594/pangaea.943672
title: Grain size distribution for the sediment sample stations of the Ems river campaign 2016

description: In order to understand and map the complex mass transport pathways and possible transformation processes of contaminants in coastal regions such as the German Bight, the main contributors must be identified and evaluated. In this context, rivers represent a major input source. In the framework of a river campaign from 20.06.16 till 25.06.2016, sediment and freshwater samples of the Ems and its tributaries were taken to determine their elemental and isotopic fingerprint and to investigate possible inputs into the German Bight. At every sampling station physicochemical parameters of the water column were measured directly after sampling with respective probes of a multimeter covering pH, dissolved oxygen, temperature and conductivity.
DOI: 10.1594/pangaea.936263
title: Macrofaunal communities in sediment core LG_3 from Lake Greifen
DOI: 10.1594/pangaea.948341
title: Radiosonde measurements from station Tamanrasset (2022-08)

description: Start location: Tamanrasset; Distance from radiation site: 10 km