δ¹⁸O in ice wedges, ice lenses and snow from Kular, Yakutia (Russia) ...
Variations of δ¹⁸О in Late Pleistocene ice wedges, in structure-forming ice and segregated ice lenses, as well as in snow and water of Burguat River were determined. The studied section of the yedoma strata has been exposed in an outcrop of the slope sediments on a gentle slope in the foothills of K...
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Online Access: | https://dx.doi.org/10.1594/pangaea.926031 https://doi.pangaea.de/10.1594/PANGAEA.926031 |
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ftdatacite:10.1594/pangaea.926031 2024-09-15T18:11:30+00:00 δ¹⁸O in ice wedges, ice lenses and snow from Kular, Yakutia (Russia) ... Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna 2020 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.926031 https://doi.pangaea.de/10.1594/PANGAEA.926031 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.926040 https://dx.doi.org/10.21782/ec2541-9994-2020-3(22-33) https://dx.doi.org/10.21782/kz1560-7496-2018-5(3-19) https://dx.doi.org/10.21782/ec2541-9994-2020-2(3-13) https://dx.doi.org/10.1134/s1028334x19110096 https://dx.doi.org/10.1134/s1028334x20020154 https://dx.doi.org/10.1016/j.apgeochem.2020.104669 https://dx.doi.org/10.1134/s1028334x19080312 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Hydrochemistry Ice wedges Kular Late Pleistocene Northern Yakutia Oxygen isotopes palaeotemperature Permafrost trace elements Yedoma Location Sample ID Sample comment DATE/TIME DEPTH, sediment/rock Treatment δ18O, water dataset Dataset 2020 ftdatacite https://doi.org/10.1594/pangaea.92603110.1594/pangaea.92604010.21782/ec2541-9994-2020-3(22-33)10.21782/kz1560-7496-2018-5(3-19)10.21782/ec2541-9994-2020-2(3-13)10.1134/s1028334x1911009610.1134/s1028334x2002015410.1016/j.apgeochem.2020.10466910.1134/s10283 2024-08-01T10:50:55Z Variations of δ¹⁸О in Late Pleistocene ice wedges, in structure-forming ice and segregated ice lenses, as well as in snow and water of Burguat River were determined. The studied section of the yedoma strata has been exposed in an outcrop of the slope sediments on a gentle slope in the foothills of Kular Ridge, nearby Kular Settlement, on the right bank of the Burguat River, 0.5 kilometers from the mouth of the Emis Creek. ... : In the field, the samples of ice wedges for isotope and chemical analysis were sampled out of the axial parts of the wedges from the main outcrop wall with an interval of 0.2 to 0.5 m using the sampling method elaborated by Yu.K. Vasil'chuk (1992). The isotopic composition of ice wedges has been determined at the Tallinn Institute of Geology. ... Dataset Ice permafrost wedge* Yakutia DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Hydrochemistry Ice wedges Kular Late Pleistocene Northern Yakutia Oxygen isotopes palaeotemperature Permafrost trace elements Yedoma Location Sample ID Sample comment DATE/TIME DEPTH, sediment/rock Treatment δ18O, water |
spellingShingle |
Hydrochemistry Ice wedges Kular Late Pleistocene Northern Yakutia Oxygen isotopes palaeotemperature Permafrost trace elements Yedoma Location Sample ID Sample comment DATE/TIME DEPTH, sediment/rock Treatment δ18O, water Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna δ¹⁸O in ice wedges, ice lenses and snow from Kular, Yakutia (Russia) ... |
topic_facet |
Hydrochemistry Ice wedges Kular Late Pleistocene Northern Yakutia Oxygen isotopes palaeotemperature Permafrost trace elements Yedoma Location Sample ID Sample comment DATE/TIME DEPTH, sediment/rock Treatment δ18O, water |
description |
Variations of δ¹⁸О in Late Pleistocene ice wedges, in structure-forming ice and segregated ice lenses, as well as in snow and water of Burguat River were determined. The studied section of the yedoma strata has been exposed in an outcrop of the slope sediments on a gentle slope in the foothills of Kular Ridge, nearby Kular Settlement, on the right bank of the Burguat River, 0.5 kilometers from the mouth of the Emis Creek. ... : In the field, the samples of ice wedges for isotope and chemical analysis were sampled out of the axial parts of the wedges from the main outcrop wall with an interval of 0.2 to 0.5 m using the sampling method elaborated by Yu.K. Vasil'chuk (1992). The isotopic composition of ice wedges has been determined at the Tallinn Institute of Geology. ... |
format |
Dataset |
author |
Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna |
author_facet |
Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna |
author_sort |
Vasil'chuk, Yurij K |
title |
δ¹⁸O in ice wedges, ice lenses and snow from Kular, Yakutia (Russia) ... |
title_short |
δ¹⁸O in ice wedges, ice lenses and snow from Kular, Yakutia (Russia) ... |
title_full |
δ¹⁸O in ice wedges, ice lenses and snow from Kular, Yakutia (Russia) ... |
title_fullStr |
δ¹⁸O in ice wedges, ice lenses and snow from Kular, Yakutia (Russia) ... |
title_full_unstemmed |
δ¹⁸O in ice wedges, ice lenses and snow from Kular, Yakutia (Russia) ... |
title_sort |
δ¹⁸o in ice wedges, ice lenses and snow from kular, yakutia (russia) ... |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://dx.doi.org/10.1594/pangaea.926031 https://doi.pangaea.de/10.1594/PANGAEA.926031 |
genre |
Ice permafrost wedge* Yakutia |
genre_facet |
Ice permafrost wedge* Yakutia |
op_relation |
https://dx.doi.org/10.1594/pangaea.926040 https://dx.doi.org/10.21782/ec2541-9994-2020-3(22-33) https://dx.doi.org/10.21782/kz1560-7496-2018-5(3-19) https://dx.doi.org/10.21782/ec2541-9994-2020-2(3-13) https://dx.doi.org/10.1134/s1028334x19110096 https://dx.doi.org/10.1134/s1028334x20020154 https://dx.doi.org/10.1016/j.apgeochem.2020.104669 https://dx.doi.org/10.1134/s1028334x19080312 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.92603110.1594/pangaea.92604010.21782/ec2541-9994-2020-3(22-33)10.21782/kz1560-7496-2018-5(3-19)10.21782/ec2541-9994-2020-2(3-13)10.1134/s1028334x1911009610.1134/s1028334x2002015410.1016/j.apgeochem.2020.10466910.1134/s10283 |
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1810449087186599936 |