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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Main Authors: Möller, Per, Bolshiyanov, Dimitry Yu, Bergsten, Helene
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1999
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.727407
https://doi.pangaea.de/10.1594/PANGAEA.727407
id ftdatacite:10.1594/pangaea.727407
record_format openpolar
spelling 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
institution 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
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