Radiocarbon age, stable isotope composition of Holocene ice wedges and mean January air temperatures in the Kolyma Lowland region ...
Ice wedges visible in natural alas and floodplain exposures have been studied in 1983-2018 years in the Kolyma Lowland region. Most ice wedges have been found within alases dated between 11 and 4.2 cal kyr BP, corresponding to the Greenlandian and Northgrippian stages of the Holocene. The greatest i...
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ftdatacite:10.1594/pangaea.943185 2024-09-15T18:17:00+00:00 Radiocarbon age, stable isotope composition of Holocene ice wedges and mean January air temperatures in the Kolyma Lowland region ... Vasil'chuk, Yurij K Budantseva, Nadine A 2022 application/zip https://dx.doi.org/10.1594/pangaea.943185 https://doi.pangaea.de/10.1594/PANGAEA.943185 en eng PANGAEA https://dx.doi.org/10.1002/ppp.2128 https://dx.doi.org/10.3402/tellusa.v16i4.8993 https://dx.doi.org/10.2458/azu_js_rc.55.16947 https://dx.doi.org/10.21782/ec2541-9994-2019-2(12-24) https://dx.doi.org/10.21782/kz1560-7496-2018-5(3-19) Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Holocene ice wedge January air paleotemperature lower Kolyma River radiocarbon dates stable oxygen and hydrogen isotopes article Bundled Publication of Datasets Collection 2022 ftdatacite https://doi.org/10.1594/pangaea.94318510.1002/ppp.212810.3402/tellusa.v16i4.899310.2458/azu_js_rc.55.1694710.21782/ec2541-9994-2019-2(12-24)10.21782/kz1560-7496-2018-5(3-19) 2024-07-03T10:20:00Z Ice wedges visible in natural alas and floodplain exposures have been studied in 1983-2018 years in the Kolyma Lowland region. Most ice wedges have been found within alases dated between 11 and 4.2 cal kyr BP, corresponding to the Greenlandian and Northgrippian stages of the Holocene. The greatest intensity of ice wedge growth occurred during 10.5-6 cal kyr BP. A decrease in their growth was mainly caused by alas draining and reduced sedimentation. In the last 4-4.5 cal kyr BP (Meghalayan stage of the Holocene), ice wedges continued to grow in old alases, sometimes as a younger generation, as well as within young alases and floodplains of the Kolyma River and its tributaries. Stable oxygen isotope values of ice-wedge ice have been successfully used as a basis for winter paleotemperature reconstructions. Obtained paleotemperature information shows that during the Holocene, mean January air temperature did not fluctuate significantly in the Kolyma Lowland region, with a slight decrease during the Meghalayan ... : Data was submitted and proofread by Yurij K Vasil'chuk and Lyubov Bludushkina at the faculty of Geography, Department of Landscape Geochemistry and Soil Geography, Lomonosov Moscow State University. ... Article in Journal/Newspaper kolyma river DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Holocene ice wedge January air paleotemperature lower Kolyma River radiocarbon dates stable oxygen and hydrogen isotopes |
spellingShingle |
Holocene ice wedge January air paleotemperature lower Kolyma River radiocarbon dates stable oxygen and hydrogen isotopes Vasil'chuk, Yurij K Budantseva, Nadine A Radiocarbon age, stable isotope composition of Holocene ice wedges and mean January air temperatures in the Kolyma Lowland region ... |
topic_facet |
Holocene ice wedge January air paleotemperature lower Kolyma River radiocarbon dates stable oxygen and hydrogen isotopes |
description |
Ice wedges visible in natural alas and floodplain exposures have been studied in 1983-2018 years in the Kolyma Lowland region. Most ice wedges have been found within alases dated between 11 and 4.2 cal kyr BP, corresponding to the Greenlandian and Northgrippian stages of the Holocene. The greatest intensity of ice wedge growth occurred during 10.5-6 cal kyr BP. A decrease in their growth was mainly caused by alas draining and reduced sedimentation. In the last 4-4.5 cal kyr BP (Meghalayan stage of the Holocene), ice wedges continued to grow in old alases, sometimes as a younger generation, as well as within young alases and floodplains of the Kolyma River and its tributaries. Stable oxygen isotope values of ice-wedge ice have been successfully used as a basis for winter paleotemperature reconstructions. Obtained paleotemperature information shows that during the Holocene, mean January air temperature did not fluctuate significantly in the Kolyma Lowland region, with a slight decrease during the Meghalayan ... : Data was submitted and proofread by Yurij K Vasil'chuk and Lyubov Bludushkina at the faculty of Geography, Department of Landscape Geochemistry and Soil Geography, Lomonosov Moscow State University. ... |
format |
Article in Journal/Newspaper |
author |
Vasil'chuk, Yurij K Budantseva, Nadine A |
author_facet |
Vasil'chuk, Yurij K Budantseva, Nadine A |
author_sort |
Vasil'chuk, Yurij K |
title |
Radiocarbon age, stable isotope composition of Holocene ice wedges and mean January air temperatures in the Kolyma Lowland region ... |
title_short |
Radiocarbon age, stable isotope composition of Holocene ice wedges and mean January air temperatures in the Kolyma Lowland region ... |
title_full |
Radiocarbon age, stable isotope composition of Holocene ice wedges and mean January air temperatures in the Kolyma Lowland region ... |
title_fullStr |
Radiocarbon age, stable isotope composition of Holocene ice wedges and mean January air temperatures in the Kolyma Lowland region ... |
title_full_unstemmed |
Radiocarbon age, stable isotope composition of Holocene ice wedges and mean January air temperatures in the Kolyma Lowland region ... |
title_sort |
radiocarbon age, stable isotope composition of holocene ice wedges and mean january air temperatures in the kolyma lowland region ... |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://dx.doi.org/10.1594/pangaea.943185 https://doi.pangaea.de/10.1594/PANGAEA.943185 |
genre |
kolyma river |
genre_facet |
kolyma river |
op_relation |
https://dx.doi.org/10.1002/ppp.2128 https://dx.doi.org/10.3402/tellusa.v16i4.8993 https://dx.doi.org/10.2458/azu_js_rc.55.16947 https://dx.doi.org/10.21782/ec2541-9994-2019-2(12-24) https://dx.doi.org/10.21782/kz1560-7496-2018-5(3-19) |
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.94318510.1002/ppp.212810.3402/tellusa.v16i4.899310.2458/azu_js_rc.55.1694710.21782/ec2541-9994-2019-2(12-24)10.21782/kz1560-7496-2018-5(3-19) |
_version_ |
1810454988998049792 |