Chronology of the last recession of the Greenland Ice Sheet

Abstract 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, northe...

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Published in:Journal of Quaternary Science
Main Authors: Bennike, Ole, Björck, Svante
Other Authors: Commission for Scientific Research in Greenland., Danish Natural Science Research Council., Carlsberg Foundation.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2002
Subjects:
Online Access:http://dx.doi.org/10.1002/jqs.670
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spelling crwiley:10.1002/jqs.670 2024-06-23T07:52:30+00:00 Chronology of the last recession of the Greenland Ice Sheet Bennike, Ole Björck, Svante Commission for Scientific Research in Greenland. Danish Natural Science Research Council. Carlsberg Foundation. 2002 http://dx.doi.org/10.1002/jqs.670 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.670 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.670 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Quaternary Science volume 17, issue 3, page 211-219 ISSN 0267-8179 1099-1417 journal-article 2002 crwiley https://doi.org/10.1002/jqs.670 2024-06-04T06:45:40Z Abstract 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 © 2002 John Wiley & Sons, Ltd. Article in Journal/Newspaper Ellesmere Island Greenland Ice Sheet Nares strait Wiley Online Library Algae Lake ENVELOPE(100.791,100.791,-66.306,-66.306) Canada Ellesmere Island Greenland Nares ENVELOPE(158.167,158.167,-81.450,-81.450) Journal of Quaternary Science 17 3 211 219
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract 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 © 2002 John Wiley & Sons, Ltd.
author2 Commission for Scientific Research in Greenland.
Danish Natural Science Research Council.
Carlsberg Foundation.
format Article in Journal/Newspaper
author Bennike, Ole
Björck, Svante
spellingShingle Bennike, Ole
Björck, Svante
Chronology of the last recession of the Greenland Ice Sheet
author_facet Bennike, Ole
Björck, Svante
author_sort Bennike, Ole
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 Wiley
publishDate 2002
url http://dx.doi.org/10.1002/jqs.670
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.670
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.670
long_lat ENVELOPE(100.791,100.791,-66.306,-66.306)
ENVELOPE(158.167,158.167,-81.450,-81.450)
geographic Algae Lake
Canada
Ellesmere Island
Greenland
Nares
geographic_facet Algae Lake
Canada
Ellesmere Island
Greenland
Nares
genre Ellesmere Island
Greenland
Ice Sheet
Nares strait
genre_facet Ellesmere Island
Greenland
Ice Sheet
Nares strait
op_source Journal of Quaternary Science
volume 17, issue 3, page 211-219
ISSN 0267-8179 1099-1417
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
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
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