Isotopic composition of syngenetic ice wedges and palaeoclimatic reconstruction, western Taymyr, Russian Arctic
Recent, Holocene and Late Weichselian (Sartan) generations of syngenetic ice wedges developed in loess‐like and alluvial sediments were investigated along the coast of the Yenisey Bay from Sopochnaya Karga Cape (71°88'N, 82°68'E) to Dikson (73°31'N, 80°34'E). Ages of about 3.4 −...
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Online Access: | https://doi.org/10.1002/ppp.707 |
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ftrepec:oai:RePEc:wly:perpro:v:22:y:2011:i:1:p:101-106 2023-05-15T15:05:35+02:00 Isotopic composition of syngenetic ice wedges and palaeoclimatic reconstruction, western Taymyr, Russian Arctic Irina Streletskaya Alexander Vasiliev Hanno Meyer https://doi.org/10.1002/ppp.707 unknown https://doi.org/10.1002/ppp.707 article ftrepec https://doi.org/10.1002/ppp.707 2020-12-04T13:31:25Z Recent, Holocene and Late Weichselian (Sartan) generations of syngenetic ice wedges developed in loess‐like and alluvial sediments were investigated along the coast of the Yenisey Bay from Sopochnaya Karga Cape (71°88'N, 82°68'E) to Dikson (73°31'N, 80°34'E). Ages of about 3.4 − 4.6 ka BP were determined for peat layer and wood fragments in ice‐rich deposits surrounding ice wedges near Dikson. The isotopic composition of these wedges reflects relatively cold winter temperatures in the Holocene. The lightest isotope composition characterises older ice wedges near Dikson and Sopochnaya Karga Cape. A warming trend between ice wedges of different generations was indicated by a distinct increase in O (4 − 5 ‰) and H (35 − 40‰) stable isotopes. Palaeotemperature reconstruction based on the data shows that winter temperatures during the formation of older generation ice wedges were lower than Holocene winter temperatures, indicating that they developed in the Late Weichselian (MIS2). The presence of syngenetic ice wedges strongly suggests that the coast of western Taymyr was not ice‐covered at this time. Copyright © 2011 John Wiley & Sons, Ltd. Article in Journal/Newspaper Arctic Taymyr RePEc (Research Papers in Economics) Arctic Taymyr ENVELOPE(89.987,89.987,68.219,68.219) Yenisey ENVELOPE(82.680,82.680,71.828,71.828) Dikson ENVELOPE(80.529,80.529,73.508,73.508) Karga ENVELOPE(139.579,139.579,74.811,74.811) Permafrost and Periglacial Processes 22 1 101 106 |
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Open Polar |
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RePEc (Research Papers in Economics) |
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description |
Recent, Holocene and Late Weichselian (Sartan) generations of syngenetic ice wedges developed in loess‐like and alluvial sediments were investigated along the coast of the Yenisey Bay from Sopochnaya Karga Cape (71°88'N, 82°68'E) to Dikson (73°31'N, 80°34'E). Ages of about 3.4 − 4.6 ka BP were determined for peat layer and wood fragments in ice‐rich deposits surrounding ice wedges near Dikson. The isotopic composition of these wedges reflects relatively cold winter temperatures in the Holocene. The lightest isotope composition characterises older ice wedges near Dikson and Sopochnaya Karga Cape. A warming trend between ice wedges of different generations was indicated by a distinct increase in O (4 − 5 ‰) and H (35 − 40‰) stable isotopes. Palaeotemperature reconstruction based on the data shows that winter temperatures during the formation of older generation ice wedges were lower than Holocene winter temperatures, indicating that they developed in the Late Weichselian (MIS2). The presence of syngenetic ice wedges strongly suggests that the coast of western Taymyr was not ice‐covered at this time. Copyright © 2011 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Irina Streletskaya Alexander Vasiliev Hanno Meyer |
spellingShingle |
Irina Streletskaya Alexander Vasiliev Hanno Meyer Isotopic composition of syngenetic ice wedges and palaeoclimatic reconstruction, western Taymyr, Russian Arctic |
author_facet |
Irina Streletskaya Alexander Vasiliev Hanno Meyer |
author_sort |
Irina Streletskaya |
title |
Isotopic composition of syngenetic ice wedges and palaeoclimatic reconstruction, western Taymyr, Russian Arctic |
title_short |
Isotopic composition of syngenetic ice wedges and palaeoclimatic reconstruction, western Taymyr, Russian Arctic |
title_full |
Isotopic composition of syngenetic ice wedges and palaeoclimatic reconstruction, western Taymyr, Russian Arctic |
title_fullStr |
Isotopic composition of syngenetic ice wedges and palaeoclimatic reconstruction, western Taymyr, Russian Arctic |
title_full_unstemmed |
Isotopic composition of syngenetic ice wedges and palaeoclimatic reconstruction, western Taymyr, Russian Arctic |
title_sort |
isotopic composition of syngenetic ice wedges and palaeoclimatic reconstruction, western taymyr, russian arctic |
url |
https://doi.org/10.1002/ppp.707 |
long_lat |
ENVELOPE(89.987,89.987,68.219,68.219) ENVELOPE(82.680,82.680,71.828,71.828) ENVELOPE(80.529,80.529,73.508,73.508) ENVELOPE(139.579,139.579,74.811,74.811) |
geographic |
Arctic Taymyr Yenisey Dikson Karga |
geographic_facet |
Arctic Taymyr Yenisey Dikson Karga |
genre |
Arctic Taymyr |
genre_facet |
Arctic Taymyr |
op_relation |
https://doi.org/10.1002/ppp.707 |
op_doi |
https://doi.org/10.1002/ppp.707 |
container_title |
Permafrost and Periglacial Processes |
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22 |
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1 |
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101 |
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106 |
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1766337255061848064 |