Facies logs and age determinations of 8 sites from Taymyr Peninsula ...
The Taymyr Peninsula constitutes the eastern delimitation of a possible Kara Sea basin ice sheet. The existence of such an ice sheet during the last global glacial maximum (LGM), i.e. during the Late Weichselian/Upper Zyryansk, is favoured by some Russian scientists. However, a growing number of stu...
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ftdatacite:10.1594/pangaea.727407 2024-09-15T18:12:19+00:00 Facies logs and age determinations of 8 sites from Taymyr Peninsula ... Möller, Per Bolshiyanov, Dimitry Yu Bergsten, Helene 1999 application/zip https://dx.doi.org/10.1594/pangaea.727407 https://doi.pangaea.de/10.1594/PANGAEA.727407 en eng PANGAEA https://dx.doi.org/10.1111/j.1502-3885.1999.tb00208.x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 agedetermination facieslogs Outcrop sample RU-Land_1996_Taymyr AWI Arctic Land Expedition Quaternary Environment of the Eurasian North QUEEN article Collection Supplementary Publication Series of Datasets 1999 ftdatacite https://doi.org/10.1594/pangaea.72740710.1111/j.1502-3885.1999.tb00208.x 2024-08-01T10:58:30Z The Taymyr Peninsula constitutes the eastern delimitation of a possible Kara Sea basin ice sheet. The existence of such an ice sheet during the last global glacial maximum (LGM), i.e. during the Late Weichselian/Upper Zyryansk, is favoured by some Russian scientists. However, a growing number of studies point towards a more minimalistic view concerning the areal extent of Late Weichselian/Upper Zyryansk Siberian glaciation. Investigations carried out by us along the central Byrranga Mountains and in the Taymyr Lake basin south thereof, reject the possibility of a Late Weichselian/Upper Zyryansk glaciation of this area. Our conclusion is based on the following: Dating of a continuous lacustrine sediment sequence at Cape Sabler on the Taymyr Lake shows that it spans at least the period 39-17 ka BP. Even younger ages have been reported, suggesting that this lacustrine environment prevailed until shortly before the Holocene. The distribution of these sediments indicates the existence of a paleo-Taymyr lake ... : Supplement to: Möller, Per; Bolshiyanov, Dimitry Yu; Bergsten, Helene (1999): Weichselian geology and palaeoenvironmental history of the central Taymyr Peninsula, Siberia, indicating no glaciation during the last global glacial maximum. Boreas, 28(1), 92-114 ... Article in Journal/Newspaper Ice Sheet Kara Sea Taymyr Taymyr Peninsula Siberia DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
agedetermination facieslogs Outcrop sample RU-Land_1996_Taymyr AWI Arctic Land Expedition Quaternary Environment of the Eurasian North QUEEN |
spellingShingle |
agedetermination facieslogs Outcrop sample RU-Land_1996_Taymyr AWI Arctic Land Expedition Quaternary Environment of the Eurasian North QUEEN Möller, Per Bolshiyanov, Dimitry Yu Bergsten, Helene Facies logs and age determinations of 8 sites from Taymyr Peninsula ... |
topic_facet |
agedetermination facieslogs Outcrop sample RU-Land_1996_Taymyr AWI Arctic Land Expedition Quaternary Environment of the Eurasian North QUEEN |
description |
The Taymyr Peninsula constitutes the eastern delimitation of a possible Kara Sea basin ice sheet. The existence of such an ice sheet during the last global glacial maximum (LGM), i.e. during the Late Weichselian/Upper Zyryansk, is favoured by some Russian scientists. However, a growing number of studies point towards a more minimalistic view concerning the areal extent of Late Weichselian/Upper Zyryansk Siberian glaciation. Investigations carried out by us along the central Byrranga Mountains and in the Taymyr Lake basin south thereof, reject the possibility of a Late Weichselian/Upper Zyryansk glaciation of this area. Our conclusion is based on the following: Dating of a continuous lacustrine sediment sequence at Cape Sabler on the Taymyr Lake shows that it spans at least the period 39-17 ka BP. Even younger ages have been reported, suggesting that this lacustrine environment prevailed until shortly before the Holocene. The distribution of these sediments indicates the existence of a paleo-Taymyr lake ... : Supplement to: Möller, Per; Bolshiyanov, Dimitry Yu; Bergsten, Helene (1999): Weichselian geology and palaeoenvironmental history of the central Taymyr Peninsula, Siberia, indicating no glaciation during the last global glacial maximum. Boreas, 28(1), 92-114 ... |
format |
Article in Journal/Newspaper |
author |
Möller, Per Bolshiyanov, Dimitry Yu Bergsten, Helene |
author_facet |
Möller, Per Bolshiyanov, Dimitry Yu Bergsten, Helene |
author_sort |
Möller, Per |
title |
Facies logs and age determinations of 8 sites from Taymyr Peninsula ... |
title_short |
Facies logs and age determinations of 8 sites from Taymyr Peninsula ... |
title_full |
Facies logs and age determinations of 8 sites from Taymyr Peninsula ... |
title_fullStr |
Facies logs and age determinations of 8 sites from Taymyr Peninsula ... |
title_full_unstemmed |
Facies logs and age determinations of 8 sites from Taymyr Peninsula ... |
title_sort |
facies logs and age determinations of 8 sites from taymyr peninsula ... |
publisher |
PANGAEA |
publishDate |
1999 |
url |
https://dx.doi.org/10.1594/pangaea.727407 https://doi.pangaea.de/10.1594/PANGAEA.727407 |
genre |
Ice Sheet Kara Sea Taymyr Taymyr Peninsula Siberia |
genre_facet |
Ice Sheet Kara Sea Taymyr Taymyr Peninsula Siberia |
op_relation |
https://dx.doi.org/10.1111/j.1502-3885.1999.tb00208.x |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.72740710.1111/j.1502-3885.1999.tb00208.x |
_version_ |
1810449896861335552 |