Ice‐wedge formation in northern Asia during the Holocene

Abstract The cryostratigraphy of Holocene ice wedges is described from Western Siberia, Yakutia and the Trans‐Baikal region. 14 C dating and oxygen isotope determinations suggest that some of these wedges grew syngenetically during the Holocene climatic optimum. Inferred mean winter and mean January...

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Published in:Permafrost and Periglacial Processes
Main Authors: Vasil'chuk, Yurij K., Vasil'chuk, Alla C.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1995
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.3430060309
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430060309
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430060309
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spelling crwiley:10.1002/ppp.3430060309 2024-06-02T08:13:11+00:00 Ice‐wedge formation in northern Asia during the Holocene Vasil'chuk, Yurij K. Vasil'chuk, Alla C. 1995 http://dx.doi.org/10.1002/ppp.3430060309 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430060309 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430060309 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 6, issue 3, page 273-279 ISSN 1045-6740 1099-1530 journal-article 1995 crwiley https://doi.org/10.1002/ppp.3430060309 2024-05-03T11:57:22Z Abstract The cryostratigraphy of Holocene ice wedges is described from Western Siberia, Yakutia and the Trans‐Baikal region. 14 C dating and oxygen isotope determinations suggest that some of these wedges grew syngenetically during the Holocene climatic optimum. Inferred mean winter and mean January air temperatures for this period are presented. Article in Journal/Newspaper Permafrost and Periglacial Processes Yakutia Siberia Wiley Online Library Permafrost and Periglacial Processes 6 3 273 279
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The cryostratigraphy of Holocene ice wedges is described from Western Siberia, Yakutia and the Trans‐Baikal region. 14 C dating and oxygen isotope determinations suggest that some of these wedges grew syngenetically during the Holocene climatic optimum. Inferred mean winter and mean January air temperatures for this period are presented.
format Article in Journal/Newspaper
author Vasil'chuk, Yurij K.
Vasil'chuk, Alla C.
spellingShingle Vasil'chuk, Yurij K.
Vasil'chuk, Alla C.
Ice‐wedge formation in northern Asia during the Holocene
author_facet Vasil'chuk, Yurij K.
Vasil'chuk, Alla C.
author_sort Vasil'chuk, Yurij K.
title Ice‐wedge formation in northern Asia during the Holocene
title_short Ice‐wedge formation in northern Asia during the Holocene
title_full Ice‐wedge formation in northern Asia during the Holocene
title_fullStr Ice‐wedge formation in northern Asia during the Holocene
title_full_unstemmed Ice‐wedge formation in northern Asia during the Holocene
title_sort ice‐wedge formation in northern asia during the holocene
publisher Wiley
publishDate 1995
url http://dx.doi.org/10.1002/ppp.3430060309
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430060309
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430060309
genre Permafrost and Periglacial Processes
Yakutia
Siberia
genre_facet Permafrost and Periglacial Processes
Yakutia
Siberia
op_source Permafrost and Periglacial Processes
volume 6, issue 3, page 273-279
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.3430060309
container_title Permafrost and Periglacial Processes
container_volume 6
container_issue 3
container_start_page 273
op_container_end_page 279
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