Chronology of the last recession of the Greenland Ice Sheet
A new deglaciation chronology for the ice-free parts of Greenland, the continental shelf and eastern Ellesmere Island (Canada) is proposed. The chronology is based on a new compilation of all published radiocarbon dates from Greenland, and includes crucial new material from southern, northeastern an...
Published in: | Journal of Quaternary Science |
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Format: | Article in Journal/Newspaper |
Language: | English |
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John Wiley & Sons Inc.
2002
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Online Access: | https://lup.lub.lu.se/record/334113 https://doi.org/10.1002/jqs.670 |
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ftulundlup:oai:lup.lub.lu.se:33cc4b75-b6f5-49ab-a065-5284119ff549 2023-05-15T16:05:55+02:00 Chronology of the last recession of the Greenland Ice Sheet Bennike, O Björck, Svante 2002 https://lup.lub.lu.se/record/334113 https://doi.org/10.1002/jqs.670 eng eng John Wiley & Sons Inc. https://lup.lub.lu.se/record/334113 http://dx.doi.org/10.1002/jqs.670 wos:000176602700003 scopus:0036300330 Journal of Quaternary Science; 17(3), pp 211-219 (2002) ISSN: 1099-1417 Geology Last holocene quaternary C-14 dating deglaciation Greenland Glacial Maximum contributiontojournal/article info:eu-repo/semantics/article text 2002 ftulundlup https://doi.org/10.1002/jqs.670 2023-02-01T23:27:22Z A new deglaciation chronology for the ice-free parts of Greenland, the continental shelf and eastern Ellesmere Island (Canada) is proposed. The chronology is based on a new compilation of all published radiocarbon dates from Greenland, and includes crucial new material from southern, northeastern and northwestern Greenland. Although each date provides only a minimum age for the local deglaciation, some of the dates come from species that indicate ice-proximal glaciomarine conditions, and thus may be connected with the actual ice recession. In addition to shell dates, dates from marine algae, lake sediments, peat, terrestrial plants and driftwood also are included. Only offshore and in the far south have secure late-glacial sediments been found. Other previous reports of late-glacial sediments (older than 11.5 cal. kyr BP) from onshore parts of Greenland need to be confirmed. Most of the present ice-free parts of Greenland and Nares Strait between Greenland and Ellesmere Island were not deglaciated until the early Holocene. Copyright (C) 2002 John Wiley Sons, Ltd. Article in Journal/Newspaper Ellesmere Island Greenland Ice Sheet Nares strait Lund University Publications (LUP) Ellesmere Island Canada Greenland Nares ENVELOPE(158.167,158.167,-81.450,-81.450) Algae Lake ENVELOPE(100.791,100.791,-66.306,-66.306) Journal of Quaternary Science 17 3 211 219 |
institution |
Open Polar |
collection |
Lund University Publications (LUP) |
op_collection_id |
ftulundlup |
language |
English |
topic |
Geology Last holocene quaternary C-14 dating deglaciation Greenland Glacial Maximum |
spellingShingle |
Geology Last holocene quaternary C-14 dating deglaciation Greenland Glacial Maximum Bennike, O Björck, Svante Chronology of the last recession of the Greenland Ice Sheet |
topic_facet |
Geology Last holocene quaternary C-14 dating deglaciation Greenland Glacial Maximum |
description |
A new deglaciation chronology for the ice-free parts of Greenland, the continental shelf and eastern Ellesmere Island (Canada) is proposed. The chronology is based on a new compilation of all published radiocarbon dates from Greenland, and includes crucial new material from southern, northeastern and northwestern Greenland. Although each date provides only a minimum age for the local deglaciation, some of the dates come from species that indicate ice-proximal glaciomarine conditions, and thus may be connected with the actual ice recession. In addition to shell dates, dates from marine algae, lake sediments, peat, terrestrial plants and driftwood also are included. Only offshore and in the far south have secure late-glacial sediments been found. Other previous reports of late-glacial sediments (older than 11.5 cal. kyr BP) from onshore parts of Greenland need to be confirmed. Most of the present ice-free parts of Greenland and Nares Strait between Greenland and Ellesmere Island were not deglaciated until the early Holocene. Copyright (C) 2002 John Wiley Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Bennike, O Björck, Svante |
author_facet |
Bennike, O Björck, Svante |
author_sort |
Bennike, O |
title |
Chronology of the last recession of the Greenland Ice Sheet |
title_short |
Chronology of the last recession of the Greenland Ice Sheet |
title_full |
Chronology of the last recession of the Greenland Ice Sheet |
title_fullStr |
Chronology of the last recession of the Greenland Ice Sheet |
title_full_unstemmed |
Chronology of the last recession of the Greenland Ice Sheet |
title_sort |
chronology of the last recession of the greenland ice sheet |
publisher |
John Wiley & Sons Inc. |
publishDate |
2002 |
url |
https://lup.lub.lu.se/record/334113 https://doi.org/10.1002/jqs.670 |
long_lat |
ENVELOPE(158.167,158.167,-81.450,-81.450) ENVELOPE(100.791,100.791,-66.306,-66.306) |
geographic |
Ellesmere Island Canada Greenland Nares Algae Lake |
geographic_facet |
Ellesmere Island Canada Greenland Nares Algae Lake |
genre |
Ellesmere Island Greenland Ice Sheet Nares strait |
genre_facet |
Ellesmere Island Greenland Ice Sheet Nares strait |
op_source |
Journal of Quaternary Science; 17(3), pp 211-219 (2002) ISSN: 1099-1417 |
op_relation |
https://lup.lub.lu.se/record/334113 http://dx.doi.org/10.1002/jqs.670 wos:000176602700003 scopus:0036300330 |
op_doi |
https://doi.org/10.1002/jqs.670 |
container_title |
Journal of Quaternary Science |
container_volume |
17 |
container_issue |
3 |
container_start_page |
211 |
op_container_end_page |
219 |
_version_ |
1766401839228518400 |