cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.901870
title: POS336 raw data of SB1050 multibeam echosounder (bathymetry & beam time series)

description: Between 28.04.2006 and 17.05.2006, bathymetric data was acquired in the Eastern Mediterranean Sea during the R/V POSEIDON cruise P336. The expedition was dedicated to studying slope instability and related geohazardous processes at the northern Cretan Margin and the slopes of the Aegean volcanic islands. The cruise aimed at an understanding of parameters controlling sediment physics, and ultimately geohazards such as landslides and other mass wasting events. Bathymetric mapping with the multibeam echosounder (MBES) ELAC SEABEAM 1050 was used to survey approximately 2450 km² of the study area and identify landslide and mass wasting deposits. Based on hydroacoustic and seismic data, these deposits were characterised by in-situ measurements, such as Cone Penetrating Testing and sub-surface heat flow measurements, and sampling, such as gravity coring and laboratory studies on board. CI Citation: Paul Wintersteller (seafloor-imaging@marum.de) as responsible party for bathymetry raw data ingest and approval. Description of the data source: During the P336 cruise, the multibeam echosounder (MBES) ELAC SEABEAM 1050 was used for continuous mapping of the seafloor. The transducer array is fixed in a Mills cross configuration and transmits a frequency of approximately 12 kHz with an angular coverage sector of up to 150°. The signal is formed into 191 beams, where the beam spacing can be set to equidistant or equiangular. During this cruise, the opening angle was set to 60-70°, depending on the state of the sea, which restricted the coverage to gain a more continuous beam spacing on the seafloor. For further information on the system, consult: http://www.angelopodesta.com/documenti/SeaBeam_1050-1055.pdf Responsible person during this cruise / PI: Ingo Kock (Ingo.Kock@grs.de), Melanie Reichelt & Sebastian Krastel-Gudegast (sebastian.krastel@ifg.uni-kiel.de) Chief Scientist: Achim Kopf (akopf@marum.de) CR: https://elib.suub.uni-bremen.de/ip/docs/00010106.pdf CSR: https://www2.bsh.de/aktdat/dod/fahrtergebnis/2006/20130246.htm
DOI: 10.1594/pangaea.902084
title: Holocene bulk proxies of sediment core GeoB16601-5
DOI: 10.1594/pangaea.902188
title: Stable isotopes from tubular carbonate conduits of rock-sediment sample GeoB11319-1

description: Tubular carbonate conduits (TCC) are exposed on a secondary terrace at the SW Peak of Athina mud volcanoes Anaximander Mountains, eastern Mediterranean Sea. Three carbonatic phases compose the TCC sampled at Athina mud volcano: the micritic high-Mg-calcite, the clotted and fibrous aragonite and the detrital infilling. The stable isotopes of carbon and oxygen data from the sample studied show the influence of the anaerobic oxydation of methane in the formation of TCC.
DOI: 10.1594/pangaea.902242
title: X-ray diffraction (XRD) measurements of rock-sediment sample GeoB11319-1

description: Sample powders for X-ray diffraction (XRD) and for stable isotope measurements were obtained from surfaces of the polished slabs, using a handheld microdrill. The XRD measurements were performed on a X'PERT PRO diffractometer equipped with a copper anode λ=1.54 Å at 40 mA and 40 kV current. Qualitative and quantitative analyses were carried out applying the Rietveld method using EXPGUI-GSAS (Rietveld, 1969; Larson and von Dreele, 1994; Toby, 2001). The accuracy was estimated±1 wt.-%. The Mg-content in calcite was determined using the method of Titschack et al. (2011).Values in parentheses represent the deviation in units of last digits. Rp, Rwp and χ2 are agreement factors indicative of the goodness of the Rietweld analyses (Toby, 2006)
DOI: 10.1594/pangaea.902244
title: Organism annotations of pelagic video transects at Senghor flank NW: observations
DOI: 10.1594/pangaea.902245
title: Organism annotations of pelagic video transects at Senghor flank NW: transect lengths
DOI: 10.1594/pangaea.902256
title: Sea ice draft, surface water temperature, salinity and chlorophyl a from SUIT measurements during POLARSTERN cruise PS106

description: Measured surface water properties (temperature, salinity, chl a), and derived sea-ice thickness and draft for each haul. Data are interpolated on a 0.5 m grid along the transect.
DOI: 10.1594/pangaea.902333
title: Irradiance from SUIT measurements during POLARSTERN cruise PS106

description: Measured under-ice irradiance and derived transmittance for each haul. The associated ice draft values are the values from the corresponding TSC file resampled at the frequency of the RAMSES irradiance measurements.
DOI: 10.1594/pangaea.902337
title: Radiance from SUIT measurements during POLARSTERN cruise PS106

description: Measured under-ice radiance and derived transflectance for each haul. The associated ice draft values are the values from the corresponding TSC file resampled at the frequency of the RAMSES radiance measurements.
DOI: 10.1594/pangaea.902712
title: MM74/2 raw data of EM710 multibeam echosounder (bathymetry, beam time series & amplitudes)

description: Between 07.10.2007 and 28.10.2007, bathymetric data was acquired in the Makran region during the R/V METEOR cruise M74/2. The subduction of the Eurasian plate beneath the Arab plate in the Makran region is associated with continuous sediment input, active mud volcanism and fluid venting. The expedition was dedicated to the investigation of known seeps and the location of new venting sites. Furthermore, the scientists focused on the influence of extreme sediment thickness on the nature of vents and the relationship between local tectonics and spatial distribution of seeps. The multibeam echosounders (MBES) KONGSBERG SIMRAD EM120 and EM710 were utilized for large-scale mapping of vent-related structures on the seafloor. In order to visualize vent-related structures in the shallow subsurface, a deep-tow sidescan sonar, sediment echosounder, and high-resolution multichannel equipment were utilized. These acoustic methods were supplemented by video observations and gravity corer and multicorer samples, which yielded detailed information at many locations. CI Citation: Paul Wintersteller (seafloor-imaging@marum.de) as responsible party for bathymetry raw data ingest and approval. Description of the data source: During the M74/2 cruise, the hull-mounted multibeam ecosounder (MBES) KONGSBERG SIMRAD EM710 was utilized to perform bathymetric mapping. The system is optimised to survey with high resolution in water depths of maximum 1,000 m depth and uses a frequency range from 70 to 100 kHz. 256 beams with an acoustical 1°(TX)/1°(RX) footprint are formed for each ping. Combining phase and amplitude bottom detection algorithms allows achieving best possible accuracy. For further information, consult: https://epic.awi.de/id/eprint/26726/1/Kon2007b.pdf. The position and depth of the water column is estimated for each beam by using the detected two-way-travel time and the beam angle known for each beam and taking ray bending due to refraction in the water column by sound speed into account. As most of the working area during M74/2 was deeper than 1,000m water depths, the EM 710 was used sporadically as an addition to the EM120. Systematically biased outer beams produced problems in areas with large overlap of parallel profiles. The applied sound velocity profile and a roll bias were tested as possible error sources, but no significant error was found. As the effect seems to be strongest on steep slopes, it might be a problem in yaw, which was not corrected for so far. Responsible person during this cruise / PI: Markus Brüning Chief Scientist: Volkhard Spiess (vspiess@uni-bremen.de) CR: https://www.tib.eu/en/search/id/awi%3Adoi~10.2312%252Fcr_m74/ CSR: https://www2.bsh.de/aktdat/dod/fahrtergebnis/2007/20080085.htm
DOI: 10.1594/pangaea.902749
title: M74/3 raw data of EM710 multibeam echosounder (bathymetry, beam time series & amplitudes)

description: Between 30.10.2007 and 28.11.2007, bathymetric data was acquired on the continental margin of Pakistan in the Makran subduction zone during R/V METEOR cruise M74/3. This expedition builds on the findings of the previous cruise M74/2, which was dedicated to a systematic seep search in the working area, where several bubble flares, backscatter anomalies and distinct seismic records were detected by using sidescan sonar, multi-channel seismics and a sediment echosounder. These findings provided the basis for detailed surveying during the cruise M74/3. The multibeam echosounders (MBES) KONGSBERG SIMRAD EM120 and EM710 were utilized for extensive mapping of the working area, which is essential for most investigations. Furthermore, bathymetric mapping during M74/3 significantly increased the resolution of previous bathymetry grids and provided information for the deployment of the remotely operated vehicle (ROV) MARUM-QUEST. The ROV was utilized to map the seafloor, take samples at potential seep sites and deploy and recover autonomous tools, such as a bubble-meter and in-situ pore water sampler. CI Citation: Paul Wintersteller (seafloor-imaging@marum.de) as responsible party for bathymetry raw data ingest and approval. Description of the data source: During the M74/2 cruise, the hull-mounted multibeam ecosounder (MBES) KONGSBERG SIMRAD EM710 was utilized to perform bathymetric mapping. The system is optimised to survey with high resolution in water depths of maximum 1,000 m depth and uses a frequency range from 70 to 100 kHz. 256 beams with an acoustical 1°(TX)/1°(RX) footprint are formed for each ping. Combining phase and amplitude bottom detection algorithms allows achieving best possible accuracy. For further information, consult: https://epic.awi.de/id/eprint/26726/1/Kon2007b.pdf. The position and depth of the water column is estimated for each beam by using the detected two-way-travel time and the beam angle known for each beam and taking ray bending due to refraction in the water column by sound speed into account. As most of the working area during M74/3 was deeper than 1,000m water depths, the EM710 was used sporadically as an addition to the EM120. Systematically biased outer beams produced problems in areas with large overlap of parallel profiles. The applied sound velocity profile and a roll bias were tested as possible error sources, but no significant error was found. As the effect seems to be strongest on steep slopes, it might be a problem in yaw, which was not corrected for so far. Responsible person during this cruise / PI: Markus Brüning Chief Scientist: Gerhard Bohrmann (gbohrmann@marum.de) CR: https://www.tib.eu/en/search/id/awi%3Adoi~10.2312%252Fcr_m74/ CSR: https://www2.bsh.de/aktdat/dod/fahrtergebnis/2007/20070155.htm
DOI: 10.1594/pangaea.902932
title: Pore water trace metal geochemistry from gravity corer SO242/1_38-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.902933
title: Pore water trace metal geochemistry from gravity corer SO242/1_51-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.902934
title: Pore water trace metal geochemistry from gravity corer SO242/1_84-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.902964
title: Pore water trace metal geochemistry from gravity corer SO242/1_89-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.902965
title: Pore water trace metal geochemistry from gravity corer SO242/1_100-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.902966
title: Pore water trace metal geochemistry from gravity corer SO242/1_123-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.902967
title: Pore water trace metal geochemistry from gravity corer SO242/1_132-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.903028
title: Solid phase trace metal geochemistry from gravity corer SO242/1_84-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.903388
title: Profile of vertical fish echo sounding with Simrad EK60 during Helmer Hanssen cruise CAGE 14.1 with links to raw data files
DOI: 10.1594/pangaea.902991
title: Solid phase trace metal geochemistry from gravity corer SO242/1_38-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.902992
title: Solid phase trace metal geochemistry from gravity corer SO242/1_51-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.902994
title: Solid phase trace metal geochemistry from gravity corer SO242/1_132-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.902998
title: Solid phase trace metal geochemistry from gravity corer SO242/1_100-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.903008
title: Solid phase trace metal geochemistry from gravity corer SO242/1_123-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.903027
title: Solid phase trace metal geochemistry from gravity corer SO242/1_89-1 of SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: LOQ = Limit of quantification
DOI: 10.1594/pangaea.903517
title: CaCO3 corrected metal geochemistry data of gravity cores from SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: In order to account for dilution effects of carbonate layers, metal data has been CaCO3 corrected for better comparison within and between the cores.
description: Decimal places are set by PANGAEA standards. Therefore three significant figures are not possible for all values shown here and are sometimes rounded.
DOI: 10.1594/pangaea.903843
title: Physical oceanography from mooring KPO_1092

description: instrument = Label:kpo_1092_01 File:kpo_1092_instr_01.nc Type:GEOMAR TD-Logger SN:72instrument = Label:kpo_1092_02 File:kpo_1092_instr_02.nc Type:Aanderaa Optode 3830 SN:01470 depth/pressure data was derived not measuredinstrument = Label:kpo_1092_03 File:kpo_1092_instr_03.nc Type:Seabird MicroCat 37-SM mit P SN:06854instrument = Label:kpo_1092_04 File:kpo_1092_instr_04.nc Type:Aanderaa Optode 4330 SN:00375 depth/pressure data was derived not measuredinstrument = Label:kpo_1092_05 File:kpo_1092_instr_05.nc Type:Seabird MicroCat 37-SM SN:01599 depth/pressure data was derived not measuredinstrument = Label:kpo_1092_06 File:kpo_1092_instr_06.nc Type:Aanderaa Optode 3830 SN:01465 depth/pressure data was derived not measuredinstrument = Label:kpo_1092_07 File:kpo_1092_instr_07.nc Type:Seabird MicroCat 37-SM mit P SN:06855instrument = Label:kpo_1092_08 File:kpo_1092_instr_08.nc Type:Aanderaa Optode 3830 SN:00940 depth/pressure data was derived not measuredinstrument = Label:kpo_1092_09 File:kpo_1092_instr_09.nc Type:Seabird MicroCat 37-SM SN:02048 depth/pressure data was derived not measuredinstrument = Label:kpo_1092_10 File:kpo_1092_instr_10.nc Type:Aanderaa Optode 3830 SN:00219 depth/pressure data was derived not measuredinstrument = Label:kpo_1092_11 File:kpo_1092_instr_11.nc Type:Seabird MicroCat 37-SM SN:02249 depth/pressure data was derived not measuredinstrument = Label:kpo_1092_12 File:kpo_1092_instr_12.nc Type:Aanderaa Optode 4330 SN:00214 depth/pressure data was derived not measuredinstrument = Label:kpo_1092_13 File:kpo_1092_instr_13.nc Type:Seabird MicroCat 37-SM mit P SN:06858instrument = Label:kpo_1092_14 File:kpo_1092_instr_14.nc Type:Aanderaa Optode 3830 SN:01463 depth/pressure data was derived not measuredinstrument = Label:kpo_1092_15 File:kpo_1092_instr_15.nc Type:Seabird MicroCat 37-SM SN:02279 depth/pressure data was derived not measuredinstrument = Label:kpo_1092_16 File:kpo_1092_instr_16.nc Type:Teledyne RDI LongRanger 75 SN:17590instrument = Label:kpo_1092_17 File:kpo_1092_instr_17.nc Type:Aanderaa Optode 4330 SN:00379 depth/pressure data was derived not measuredinstrument = Label:kpo_1092_18 File:kpo_1092_instr_18.nc Type:Seabird MicroCat 37-SM SN:03144 depth/pressure data was derived not measured
DOI: 10.1594/pangaea.903518
title: Pore water rare earth element data of sediment cores SO242/1_80-1, SO242/1_89-1 and SO242/1_100-1 from SONNE cruise SO242/1 at the DISCOL area, Peru Basin
DOI: 10.1594/pangaea.903848
title: Physical oceanography from mooring KPO_1093

description: instrument = Label:kpo_1093_01 File:kpo_1093_instr_01.nc Type:GEOMAR TD-Logger SN:64instrument = Label:kpo_1093_02 File:kpo_1093_instr_02.nc Type:Aanderaa Optode 3830 SN:01144 depth/pressure data was derived not measuredinstrument = Label:kpo_1093_03 File:kpo_1093_instr_03.nc Type:Seabird MicroCat 37-SM mit P SN:06863instrument = Label:kpo_1093_04 File:kpo_1093_instr_04.nc Type:Aanderaa Optode 3830 SN:01468 depth/pressure data was derived not measuredinstrument = Label:kpo_1093_05 File:kpo_1093_instr_05.nc Type:Seabird MicroCat 37-SM SN:02251 depth/pressure data was derived not measuredinstrument = Label:kpo_1093_06 File:kpo_1093_instr_06.nc Type:Aanderaa Optode 3830 SN:1467 depth/pressure data was derived not measuredinstrument = Label:kpo_1093_07 File:kpo_1093_instr_07.nc Type:Seabird MicroCat 37-SM mit P SN:06857instrument = Label:kpo_1093_08 File:kpo_1093_instr_08.nc Type:Aanderaa Optode 3830 SN:00944 depth/pressure data was derived not measured instrument = Label:kpo_1093_09 File:kpo_1093_instr_09.nc Type:Seabird MicroCat 37-SM SN:02250 depth/pressure data was derived not measuredinstrument = Label:kpo_1093_10 File:kpo_1093_instr_10.nc Type:Aanderaa Optode 3830 SN:01138 depth/pressure data was derived not measuredinstrument = Label:kpo_1093_11 File:kpo_1093_instr_11.nc Type:Seabird MicroCat 37-SM SN:02246 depth/pressure data was derived not measuredinstrument = Label:kpo_1093_12 File:kpo_1093_instr_12.nc Type:Aanderaa Optode 3830 SN:01469 depth/pressure data was derived not measuredinstrument = Label:kpo_1093_13 File:kpo_1093_instr_13.nc Type:Seabird MicroCat 37-SM mit P SN:06856instrument = Label:kpo_1093_14 File:kpo_1093_instr_14.nc Type:Aanderaa Optode 3830 SN:01462 depth/pressure data was derived not measuredinstrument = Label:kpo_1093_15 File:kpo_1093_instr_15.nc Type:Seabird MicroCat 37-SM SN:02245 depth/pressure data was derived not measuredinstrument = Label:kpo_1093_16 File:kpo_1093_instr_16.nc Type:Teledyne RDI LongRanger 75 SN:17570instrument = Label:kpo_1093_17 File:kpo_1093_instr_17.nc Type:Aanderaa Optode 3830 SN:01133 depth/pressure data was derived not measuredinstrument = Label:kpo_1093_18 File:kpo_1093_instr_18.nc Type:Seabird MicroCat 37-SM SN:01550 depth/pressure data was derived not measured
DOI: 10.1594/pangaea.904050
title: Links to master tracks in different resolutions of POLARSTERN cruise PS119, Punta Arenas - Port Stanley, 2019-04-13 - 2019-05-31
DOI: 10.1594/pangaea.903436
title: Profile of vertical fish echo sounding with Simrad EK60 during Helmer Hanssen cruise CAGE 14.5 with links to raw data files
DOI: 10.1594/pangaea.904603
title: Heat flow data at station HF1650
DOI: 10.1594/pangaea.904163
title: Winter sea ice concentrations derived from diatom transfer functions on sediment core PS69/274-1 from the western Amundsen Sea, Antarctic

description: Via a transfer function, we reconstructed winter sea ice concentrations derived from diatom assemblages on sediment core PS69/274-1 from the western Amundsen Sea, Antarctica. Those data were compared to sea ice reconstructions based on biomarker data.
DOI: 10.1594/pangaea.904202
title: Physical oceanography from mooring KPO_1090

description: instrument = Label:kpo_1090_01 File:kpo_1090_instr_01.nc Type:GEOMAR TD-Logger SN:66instrument = Label:kpo_1090_02 File:kpo_1090_instr_02.nc Type:Aanderaa Optode 4330 SN:00215 depth/pressure data was derived not measuredinstrument = Label:kpo_1090_03 File:kpo_1090_instr_03.nc Type:Seabird MicroCat 37-SM mit P SN:06859instrument = Label:kpo_1090_04 File:kpo_1090_instr_04.nc Type:Aanderaa Optode 3830 SN:01134 depth/pressure data was derived not measuredinstrument = Label:kpo_1090_05 File:kpo_1090_instr_05.nc Type:Seabird MicroCat 37-SM SN:01682 depth/pressure data was derived not measuredinstrument = Label:kpo_1090_06 File:kpo_1090_instr_06.nc Type:Aanderaa Optode 3830 SN:01074 depth/pressure data was derived not measuredinstrument = Label:kpo_1090_07 File:kpo_1090_instr_07.nc Type:Seabird MicroCat 37-SM mit P SN:06860 depth/pressure data was derived not measuredinstrument = Label:kpo_1090_08 File:kpo_1090_instr_08.nc Type:Aanderaa Optode 3830 SN:00206 depth/pressure data was derived not measuredinstrument = Label:kpo_1090_09 File:kpo_1090_instr_09.nc Type:Seabird MicroCat 37-SM SN:08945 depth/pressure data was derived not measuredinstrument = Label:kpo_1090_11 File:kpo_1090_instr_11.nc Type:Seabird MicroCat 37-SM SN:08946 depth/pressure data was derived not measuredinstrument = Label:kpo_1090_12 File:kpo_1090_instr_12.nc Type:Aanderaa Optode 4330 SN:00148 depth/pressure data was derived not measuredinstrument = Label:kpo_1090_13 File:kpo_1090_instr_13.nc Type:Seabird MicroCat 37-SM mit P SN:06861instrument = Label:kpo_1090_14 File:kpo_1090_instr_14.nc Type:Aanderaa Optode 4330 SN:00216 depth/pressure data was derived not measuredinstrument = Label:kpo_1090_15 File:kpo_1090_instr_15.nc Type:Seabird MicroCat 37-IM SN:06779 depth/pressure data was derived not measuredinstrument = Label:kpo_1090_16 File:kpo_1090_instr_16.nc Type:Teledyne RDI LongRanger 75 SN:02395instrument = Label:kpo_1090_17 File:kpo_1090_instr_17.nc Type:Aanderaa Optode 3830 SN:01135 depth/pressure data was derived not measuredinstrument = Label:kpo_1090_18 File:kpo_1090_instr_18.nc Type:Seabird MicroCat 37-SM SN:08947 depth/pressure data was derived not measured
DOI: 10.1594/pangaea.904606
title: Heat flow data at station HF1651
DOI: 10.1594/pangaea.904607
title: Heat flow data at station HF1652
DOI: 10.1594/pangaea.904608
title: Heat flow data at station HF1653
DOI: 10.1594/pangaea.904609
title: Heat flow data at station HF1655
DOI: 10.15468/dl.zg2r7v
title: Occurrence Download

description: A dataset containing 6 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is BOLD:AAB3927"
 ]
}

 The dataset includes 6 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0001340-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.904611
title: Heat flow data at station HF1656
DOI: 10.1594/pangaea.904612
title: Heat flow data at station HF1657
DOI: 10.1594/pangaea.904613
title: Heat flow data at station HF1658
DOI: 10.1594/pangaea.904614
title: Heat flow data at station HF1659
DOI: 10.1594/pangaea.904659
title: Physical oceanography from glider mission IFM12_depl05

description: Netcdf file created from GEOMAR processed glider data. Based on data from file ifm12_depl05_final_gridded.mat . Glider deployment ID : ifm12_depl05 Parameter: Temperature, Salinity, Oxygen, Turbidity, Fluorescence, CDOM
DOI: 10.1594/pangaea.904679
title: Mg/Ca and stable isotopes data of sediment core MSM45-31-1 (MSM45_431-1)
DOI: 10.1594/pangaea.904688
title: Alkenone data of sediment core MSM45-31-1 (MSM45_431-1)
DOI: 10.1594/pangaea.904692
title: Age model of sediment core MSM45-31-1 (MSM45_431-1)
DOI: 10.1594/pangaea.906080
title: Biomarker record of sediment cores 9R and 10R at site PS104_20-2
DOI: 10.1594/pangaea.904262
title: Sedimentological data of sediment core PS69/274-1 from the western Amundsen Sea, Antarctica

description: We analysed TOC and CNS contents on sediment core PS69/274-1 and calculated the C/N-ratio and carbonate content of the individual sample depths. Those data were compared to biomarker data of the same sediment core, in order to give a more accurate environmental reconstruction for the western Amundsen Sea since the last ice age.