Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ...

Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedges polygonal massives of Russian permafrost zone is represented. Dating of Late Pleistocene syngenetic ice wedges is possible with using of radiocarbon dates of the host sediments indirectly. Formation of syngenetic ice wedges is a...

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Bibliographic Details
Main Authors: Vasil'chuk, Yurij K, Vasil'chuk, Alla Constantinovna
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
AGE
Ice
Online Access:https://dx.doi.org/10.1594/pangaea.939682
https://doi.pangaea.de/10.1594/PANGAEA.939682
id ftdatacite:10.1594/pangaea.939682
record_format openpolar
spelling ftdatacite:10.1594/pangaea.939682 2024-09-09T19:44:20+00:00 Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ... Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.939682 https://doi.pangaea.de/10.1594/PANGAEA.939682 en eng PANGAEA https://dx.doi.org/10.1016/s0012-821x(00)00122-9 https://dx.doi.org/10.1016/s0168-583x(00)00212-3 https://dx.doi.org/10.3103/s0145875218010131 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/10.1017/s0033822200041199 https://dx.doi.org/10.1134/s1028334x19110096 https://dx.doi.org/10.1134/s1028334x20020154 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Late Pleistocene organic organic accumulation Permafrost radiocarbon dating syngenetic ice-wedges Event label Latitude of event Longitude of event Sample ID Sample comment Location AGE Age, error ELEVATION Age, dated material Reference/source Multiple investigations Age, radiocarbon dataset Dataset 2022 ftdatacite https://doi.org/10.1594/pangaea.93968210.1016/s0012-821x(00)00122-910.1016/s0168-583x(00)00212-310.3103/s014587521801013110.21782/kz1560-7496-2018-5(3-19)10.21782/ec2541-9994-2020-2(3-13)10.1017/s003382220004119910.1134/s1028334x1911009610.1134/s1028334x2 2024-08-01T10:50:55Z Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedges polygonal massives of Russian permafrost zone is represented. Dating of Late Pleistocene syngenetic ice wedges is possible with using of radiocarbon dates of the host sediments indirectly. Formation of syngenetic ice wedges is a cyclically-interrupted process. Fluvial origin of syngenetic sediments formed of ice wedge thickness determines presence of allochthonous and autochthonous organic material there. This is the main cause of age inversions or disturbances in the radiocarbon date series from syngenetic permafrost cross-sections. ... : The ¹⁴C measurements were made in the Geological Institute of the Russian Academy of Sciences (L. Sulerzhitsky). ... Dataset Ice permafrost wedge* DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Late Pleistocene
organic
organic accumulation
Permafrost
radiocarbon dating
syngenetic ice-wedges
Event label
Latitude of event
Longitude of event
Sample ID
Sample comment
Location
AGE
Age, error
ELEVATION
Age, dated material
Reference/source
Multiple investigations
Age, radiocarbon
spellingShingle Late Pleistocene
organic
organic accumulation
Permafrost
radiocarbon dating
syngenetic ice-wedges
Event label
Latitude of event
Longitude of event
Sample ID
Sample comment
Location
AGE
Age, error
ELEVATION
Age, dated material
Reference/source
Multiple investigations
Age, radiocarbon
Vasil'chuk, Yurij K
Vasil'chuk, Alla Constantinovna
Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ...
topic_facet Late Pleistocene
organic
organic accumulation
Permafrost
radiocarbon dating
syngenetic ice-wedges
Event label
Latitude of event
Longitude of event
Sample ID
Sample comment
Location
AGE
Age, error
ELEVATION
Age, dated material
Reference/source
Multiple investigations
Age, radiocarbon
description Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedges polygonal massives of Russian permafrost zone is represented. Dating of Late Pleistocene syngenetic ice wedges is possible with using of radiocarbon dates of the host sediments indirectly. Formation of syngenetic ice wedges is a cyclically-interrupted process. Fluvial origin of syngenetic sediments formed of ice wedge thickness determines presence of allochthonous and autochthonous organic material there. This is the main cause of age inversions or disturbances in the radiocarbon date series from syngenetic permafrost cross-sections. ... : The ¹⁴C measurements were made in the Geological Institute of the Russian Academy of Sciences (L. Sulerzhitsky). ...
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 Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ...
title_short Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ...
title_full Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ...
title_fullStr Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ...
title_full_unstemmed Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ...
title_sort radiocarbon dating of the late pleistocene thick syngenetic ice-wedge polygonal massives of russian permafrost zone ...
publisher PANGAEA
publishDate 2022
url https://dx.doi.org/10.1594/pangaea.939682
https://doi.pangaea.de/10.1594/PANGAEA.939682
genre Ice
permafrost
wedge*
genre_facet Ice
permafrost
wedge*
op_relation https://dx.doi.org/10.1016/s0012-821x(00)00122-9
https://dx.doi.org/10.1016/s0168-583x(00)00212-3
https://dx.doi.org/10.3103/s0145875218010131
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/10.1017/s0033822200041199
https://dx.doi.org/10.1134/s1028334x19110096
https://dx.doi.org/10.1134/s1028334x20020154
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.93968210.1016/s0012-821x(00)00122-910.1016/s0168-583x(00)00212-310.3103/s014587521801013110.21782/kz1560-7496-2018-5(3-19)10.21782/ec2541-9994-2020-2(3-13)10.1017/s003382220004119910.1134/s1028334x1911009610.1134/s1028334x2
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