id ftdatacite:10.1594/pangaea.877343
record_format openpolar
spelling ftdatacite:10.1594/pangaea.877343 2024-09-09T19:44:37+00:00 Bulk sedimentology of the Batagay thaw slump, Northeastern Siberia ... Ashastina, Kseniia Schirrmeister, Lutz Scheidemann, Dyke Fuchs, Margret C Kienast, Frank 2017 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.877343 https://doi.pangaea.de/10.1594/PANGAEA.877343 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.877346 https://dx.doi.org/10.5194/cp-13-795-2017 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Sample ID DEPTH, sediment/rock Ice content Nitrogen, total Carbon, total Carbon, organic, total Carbon, organic, total/Nitrogen, total ratio Calcium carbonate Grain size, mean Size fraction < 0.002 mm, clay Size fraction 0.020-0.002 mm Size fraction 0.063-0.020 mm, coarse silt Size fraction 0.200-0.063 mm, fine sand Size fraction > 0.200 mm Susceptibility, specific, low-field mass-normalized Susceptibility, specific, high-field mass-normalized δ13C Unit Outcrop sample Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Vario EL III Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Elementar Vario MAX Cube Calculated Bartington MS2B bulk sensor Mass spectrometer Finnigan Delta-S dataset Dataset 2017 ftdatacite https://doi.org/10.1594/pangaea.87734310.1594/pangaea.87734610.5194/cp-13-795-2017 2024-06-17T09:47:39Z We described the Batagay permafrost sequence during the June 2014 field campaign. The 60m high outcrop was sampled from top to bottom along its height, ideally in 1m steps, but depending on its accessibility. The sampling procedure was carried out as follows: (1) the cryolithological characteristics at each sampling point were described and photographed, (2) the sampling zone was cleaned, and (3) frozen deposits were taken using a hammer and a chisel and placed into plastic bags. The wet sediments were air-dried in the field and split into subsamples for sedimentological and biogeochemical analysis in the laboratories of the Alfred Wegener Institute in Potsdam.Total carbon (TC) and total nitrogen (TN) were measured with a vario EL III element analyser and the total organic carbon (TOC) content was measured with a vario MAX analyser. Using the TOC and TN values, the TOC = TN (C = N) ratio was calculated to deduce the degree of organic matter decomposition. The lower the C/N ratio is, the higher the ... Dataset Ice permafrost Siberia DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Sample ID
DEPTH, sediment/rock
Ice content
Nitrogen, total
Carbon, total
Carbon, organic, total
Carbon, organic, total/Nitrogen, total ratio
Calcium carbonate
Grain size, mean
Size fraction < 0.002 mm, clay
Size fraction 0.020-0.002 mm
Size fraction 0.063-0.020 mm, coarse silt
Size fraction 0.200-0.063 mm, fine sand
Size fraction > 0.200 mm
Susceptibility, specific, low-field mass-normalized
Susceptibility, specific, high-field mass-normalized
δ13C
Unit
Outcrop sample
Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Vario EL III
Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Elementar Vario MAX Cube
Calculated
Bartington MS2B bulk sensor
Mass spectrometer Finnigan Delta-S
spellingShingle Sample ID
DEPTH, sediment/rock
Ice content
Nitrogen, total
Carbon, total
Carbon, organic, total
Carbon, organic, total/Nitrogen, total ratio
Calcium carbonate
Grain size, mean
Size fraction < 0.002 mm, clay
Size fraction 0.020-0.002 mm
Size fraction 0.063-0.020 mm, coarse silt
Size fraction 0.200-0.063 mm, fine sand
Size fraction > 0.200 mm
Susceptibility, specific, low-field mass-normalized
Susceptibility, specific, high-field mass-normalized
δ13C
Unit
Outcrop sample
Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Vario EL III
Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Elementar Vario MAX Cube
Calculated
Bartington MS2B bulk sensor
Mass spectrometer Finnigan Delta-S
Ashastina, Kseniia
Schirrmeister, Lutz
Scheidemann, Dyke
Fuchs, Margret C
Kienast, Frank
Bulk sedimentology of the Batagay thaw slump, Northeastern Siberia ...
topic_facet Sample ID
DEPTH, sediment/rock
Ice content
Nitrogen, total
Carbon, total
Carbon, organic, total
Carbon, organic, total/Nitrogen, total ratio
Calcium carbonate
Grain size, mean
Size fraction < 0.002 mm, clay
Size fraction 0.020-0.002 mm
Size fraction 0.063-0.020 mm, coarse silt
Size fraction 0.200-0.063 mm, fine sand
Size fraction > 0.200 mm
Susceptibility, specific, low-field mass-normalized
Susceptibility, specific, high-field mass-normalized
δ13C
Unit
Outcrop sample
Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Vario EL III
Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Elementar Vario MAX Cube
Calculated
Bartington MS2B bulk sensor
Mass spectrometer Finnigan Delta-S
description We described the Batagay permafrost sequence during the June 2014 field campaign. The 60m high outcrop was sampled from top to bottom along its height, ideally in 1m steps, but depending on its accessibility. The sampling procedure was carried out as follows: (1) the cryolithological characteristics at each sampling point were described and photographed, (2) the sampling zone was cleaned, and (3) frozen deposits were taken using a hammer and a chisel and placed into plastic bags. The wet sediments were air-dried in the field and split into subsamples for sedimentological and biogeochemical analysis in the laboratories of the Alfred Wegener Institute in Potsdam.Total carbon (TC) and total nitrogen (TN) were measured with a vario EL III element analyser and the total organic carbon (TOC) content was measured with a vario MAX analyser. Using the TOC and TN values, the TOC = TN (C = N) ratio was calculated to deduce the degree of organic matter decomposition. The lower the C/N ratio is, the higher the ...
format Dataset
author Ashastina, Kseniia
Schirrmeister, Lutz
Scheidemann, Dyke
Fuchs, Margret C
Kienast, Frank
author_facet Ashastina, Kseniia
Schirrmeister, Lutz
Scheidemann, Dyke
Fuchs, Margret C
Kienast, Frank
author_sort Ashastina, Kseniia
title Bulk sedimentology of the Batagay thaw slump, Northeastern Siberia ...
title_short Bulk sedimentology of the Batagay thaw slump, Northeastern Siberia ...
title_full Bulk sedimentology of the Batagay thaw slump, Northeastern Siberia ...
title_fullStr Bulk sedimentology of the Batagay thaw slump, Northeastern Siberia ...
title_full_unstemmed Bulk sedimentology of the Batagay thaw slump, Northeastern Siberia ...
title_sort bulk sedimentology of the batagay thaw slump, northeastern siberia ...
publisher PANGAEA
publishDate 2017
url https://dx.doi.org/10.1594/pangaea.877343
https://doi.pangaea.de/10.1594/PANGAEA.877343
genre Ice
permafrost
Siberia
genre_facet Ice
permafrost
Siberia
op_relation https://dx.doi.org/10.1594/pangaea.877346
https://dx.doi.org/10.5194/cp-13-795-2017
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.87734310.1594/pangaea.87734610.5194/cp-13-795-2017
_version_ 1809914286031503360