Bulk sedimentology of the Batagay thaw slump, Northeastern Siberia ...
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...
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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 |
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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 |