The Last Glacial Maximum on Spitsbergen, Svalbard

Abstract Most scientists have concluded previously that the west coast of Spitsbergen, Svalbard, remained ice-free during the late Weichselian, between 25,000 and 10,000 yr B.P. We conclude that the glaciation was more extensive. Terraces that were postulated to have been ice-free are covered by a t...

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Published in:Quaternary Research
Main Authors: Mangerud, Jan, Bolstad, Magne, Elgersma, Anne, Helliksen, Dag, Landvik, Jon Y., Lønne, Ida, Lycke, Anne Katrine, Salvigsen, Otto, Sandahl, Tom, Svendsen, John Inge
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1992
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Online Access:http://dx.doi.org/10.1016/0033-5894(92)90027-g
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spelling crcambridgeupr:10.1016/0033-5894(92)90027-g 2024-09-15T18:07:57+00:00 The Last Glacial Maximum on Spitsbergen, Svalbard Mangerud, Jan Bolstad, Magne Elgersma, Anne Helliksen, Dag Landvik, Jon Y. Lønne, Ida Lycke, Anne Katrine Salvigsen, Otto Sandahl, Tom Svendsen, John Inge 1992 http://dx.doi.org/10.1016/0033-5894(92)90027-g http://api.elsevier.com/content/article/PII:003358949290027G?httpAccept=text/xml http://api.elsevier.com/content/article/PII:003358949290027G?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400023875 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 38, issue 1, page 1-31 ISSN 0033-5894 1096-0287 journal-article 1992 crcambridgeupr https://doi.org/10.1016/0033-5894(92)90027-g 2024-07-31T04:01:02Z Abstract Most scientists have concluded previously that the west coast of Spitsbergen, Svalbard, remained ice-free during the late Weichselian, between 25,000 and 10,000 yr B.P. We conclude that the glaciation was more extensive. Terraces that were postulated to have been ice-free are covered by a thin, late Weichselian till. Sudden drop in the marine limit and basal radiocarbon dates of raised glaciomarine sediments demonstrates that the glaciers in the main fjords, Isfjorden and Van Mijenfjorden, terminated west (outside) of the fjord mouths. Basal radiocarbon dates from glaciomarine clay above till in cores from the continental shelf west of Spitsbergen yielded ages of about 12,500 yr B.P., from which we conclude that the ice extended to the shelf edge. Based on the extent of amino acid diagenesis in radiocarbon-dated molluscs, the duration of the maximum extension of the late Weichselian glaciation was short, certainly less than 10,000 years. During the ice-free period preceding that glaciation, at least back to 40,000 yr B.P., the glaciers on Svalbard were not significantly larger than at present, as shown by marine deposits close to the glacier snouts. Many radiocarbon dates place deglaciation of the outer coast at about 12,500 yr B.P. At about 10,000 yr B.P., the rest of the archipelago rapidly became ice-free. Article in Journal/Newspaper glacier Isfjord* Isfjord* Isfjorden Isfjorden Svalbard Van Mijenfjorden Spitsbergen Cambridge University Press Quaternary Research 38 1 1 31
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Most scientists have concluded previously that the west coast of Spitsbergen, Svalbard, remained ice-free during the late Weichselian, between 25,000 and 10,000 yr B.P. We conclude that the glaciation was more extensive. Terraces that were postulated to have been ice-free are covered by a thin, late Weichselian till. Sudden drop in the marine limit and basal radiocarbon dates of raised glaciomarine sediments demonstrates that the glaciers in the main fjords, Isfjorden and Van Mijenfjorden, terminated west (outside) of the fjord mouths. Basal radiocarbon dates from glaciomarine clay above till in cores from the continental shelf west of Spitsbergen yielded ages of about 12,500 yr B.P., from which we conclude that the ice extended to the shelf edge. Based on the extent of amino acid diagenesis in radiocarbon-dated molluscs, the duration of the maximum extension of the late Weichselian glaciation was short, certainly less than 10,000 years. During the ice-free period preceding that glaciation, at least back to 40,000 yr B.P., the glaciers on Svalbard were not significantly larger than at present, as shown by marine deposits close to the glacier snouts. Many radiocarbon dates place deglaciation of the outer coast at about 12,500 yr B.P. At about 10,000 yr B.P., the rest of the archipelago rapidly became ice-free.
format Article in Journal/Newspaper
author Mangerud, Jan
Bolstad, Magne
Elgersma, Anne
Helliksen, Dag
Landvik, Jon Y.
Lønne, Ida
Lycke, Anne Katrine
Salvigsen, Otto
Sandahl, Tom
Svendsen, John Inge
spellingShingle Mangerud, Jan
Bolstad, Magne
Elgersma, Anne
Helliksen, Dag
Landvik, Jon Y.
Lønne, Ida
Lycke, Anne Katrine
Salvigsen, Otto
Sandahl, Tom
Svendsen, John Inge
The Last Glacial Maximum on Spitsbergen, Svalbard
author_facet Mangerud, Jan
Bolstad, Magne
Elgersma, Anne
Helliksen, Dag
Landvik, Jon Y.
Lønne, Ida
Lycke, Anne Katrine
Salvigsen, Otto
Sandahl, Tom
Svendsen, John Inge
author_sort Mangerud, Jan
title The Last Glacial Maximum on Spitsbergen, Svalbard
title_short The Last Glacial Maximum on Spitsbergen, Svalbard
title_full The Last Glacial Maximum on Spitsbergen, Svalbard
title_fullStr The Last Glacial Maximum on Spitsbergen, Svalbard
title_full_unstemmed The Last Glacial Maximum on Spitsbergen, Svalbard
title_sort last glacial maximum on spitsbergen, svalbard
publisher Cambridge University Press (CUP)
publishDate 1992
url http://dx.doi.org/10.1016/0033-5894(92)90027-g
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genre glacier
Isfjord*
Isfjord*
Isfjorden
Isfjorden
Svalbard
Van Mijenfjorden
Spitsbergen
genre_facet glacier
Isfjord*
Isfjord*
Isfjorden
Isfjorden
Svalbard
Van Mijenfjorden
Spitsbergen
op_source Quaternary Research
volume 38, issue 1, page 1-31
ISSN 0033-5894 1096-0287
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op_doi https://doi.org/10.1016/0033-5894(92)90027-g
container_title Quaternary Research
container_volume 38
container_issue 1
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