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...

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Published in:Journal of Quaternary Science
Main Authors: Bennike, O, Björck, Svante
Format: Article in Journal/Newspaper
Language:English
Published: John Wiley & Sons Inc. 2002
Subjects:
Online Access:https://lup.lub.lu.se/record/334113
https://doi.org/10.1002/jqs.670
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spelling 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
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