Late Quaternary history of the Kap Mackenzie area, northeast Greenland

Wagner, B., Bennike, O., Cremer, H. & Klug, M. 2010: Late Quaternary history of the Kap Mackenzie area, northeast Greenland. Boreas , Vol. 39, pp. 492–504. 10.1111/j.1502‐3885.2010.00148.x. ISSN 0300‐9483. The Kap Mackenzie area on the outer coast of northeast Greenland was glaciated during the...

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Published in:Boreas
Main Authors: WAGNER, BERND, BENNIKE, OLE, CREMER, HOLGER, KLUG, MARTIN
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2010
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Online Access:http://dx.doi.org/10.1111/j.1502-3885.2010.00148.x
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spelling crwiley:10.1111/j.1502-3885.2010.00148.x 2024-09-15T18:08:49+00:00 Late Quaternary history of the Kap Mackenzie area, northeast Greenland WAGNER, BERND BENNIKE, OLE CREMER, HOLGER KLUG, MARTIN 2010 http://dx.doi.org/10.1111/j.1502-3885.2010.00148.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.2010.00148.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.2010.00148.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 39, issue 3, page 492-504 ISSN 0300-9483 1502-3885 journal-article 2010 crwiley https://doi.org/10.1111/j.1502-3885.2010.00148.x 2024-08-09T04:22:29Z Wagner, B., Bennike, O., Cremer, H. & Klug, M. 2010: Late Quaternary history of the Kap Mackenzie area, northeast Greenland. Boreas , Vol. 39, pp. 492–504. 10.1111/j.1502‐3885.2010.00148.x. ISSN 0300‐9483. The Kap Mackenzie area on the outer coast of northeast Greenland was glaciated during the last glacial stage, and pre‐Holocene shell material was brought to the area. Dating of marine shells indicates that deglaciation occurred in the earliest Holocene, before 10 800 cal. a BP. The marine limit is around 53 m a.s.l. In the wake of the deglaciation, a glaciomarine fauna characterized the area, but after c . one millennium a more species‐rich marine fauna took over. This fauna included Mytilus edulis and Mysella sovaliki , which do not live in the region at present; the latter is new to the Holocene fauna of northeast Greenland. The oldest M. edulis sample is dated to c . 9500 cal. a BP, which is the earliest date for the species from the region and indicates that the Holocene thermal maximum began earlier in the region than previously documented. This is supported by driftwood dated to c . 9650 cal. a BP, which is the earliest driftwood date so far from northeastern Greenland and implies that the coastal area was at least partly free of sea ice in summer. As indicated by former studies, the Storegga tsunami hit the Kap Mackenzie area at c . 8100 cal. a BP. Loon Lake, at 18 m a.s.l., was isolated from the sea at c . 6200 cal. a BP, which is distinctly later than expected from existing relative sea‐level curves for the region. Article in Journal/Newspaper Greenland Sea ice Wiley Online Library Boreas
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Wagner, B., Bennike, O., Cremer, H. & Klug, M. 2010: Late Quaternary history of the Kap Mackenzie area, northeast Greenland. Boreas , Vol. 39, pp. 492–504. 10.1111/j.1502‐3885.2010.00148.x. ISSN 0300‐9483. The Kap Mackenzie area on the outer coast of northeast Greenland was glaciated during the last glacial stage, and pre‐Holocene shell material was brought to the area. Dating of marine shells indicates that deglaciation occurred in the earliest Holocene, before 10 800 cal. a BP. The marine limit is around 53 m a.s.l. In the wake of the deglaciation, a glaciomarine fauna characterized the area, but after c . one millennium a more species‐rich marine fauna took over. This fauna included Mytilus edulis and Mysella sovaliki , which do not live in the region at present; the latter is new to the Holocene fauna of northeast Greenland. The oldest M. edulis sample is dated to c . 9500 cal. a BP, which is the earliest date for the species from the region and indicates that the Holocene thermal maximum began earlier in the region than previously documented. This is supported by driftwood dated to c . 9650 cal. a BP, which is the earliest driftwood date so far from northeastern Greenland and implies that the coastal area was at least partly free of sea ice in summer. As indicated by former studies, the Storegga tsunami hit the Kap Mackenzie area at c . 8100 cal. a BP. Loon Lake, at 18 m a.s.l., was isolated from the sea at c . 6200 cal. a BP, which is distinctly later than expected from existing relative sea‐level curves for the region.
format Article in Journal/Newspaper
author WAGNER, BERND
BENNIKE, OLE
CREMER, HOLGER
KLUG, MARTIN
spellingShingle WAGNER, BERND
BENNIKE, OLE
CREMER, HOLGER
KLUG, MARTIN
Late Quaternary history of the Kap Mackenzie area, northeast Greenland
author_facet WAGNER, BERND
BENNIKE, OLE
CREMER, HOLGER
KLUG, MARTIN
author_sort WAGNER, BERND
title Late Quaternary history of the Kap Mackenzie area, northeast Greenland
title_short Late Quaternary history of the Kap Mackenzie area, northeast Greenland
title_full Late Quaternary history of the Kap Mackenzie area, northeast Greenland
title_fullStr Late Quaternary history of the Kap Mackenzie area, northeast Greenland
title_full_unstemmed Late Quaternary history of the Kap Mackenzie area, northeast Greenland
title_sort late quaternary history of the kap mackenzie area, northeast greenland
publisher Wiley
publishDate 2010
url http://dx.doi.org/10.1111/j.1502-3885.2010.00148.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.2010.00148.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.2010.00148.x
genre Greenland
Sea ice
genre_facet Greenland
Sea ice
op_source Boreas
volume 39, issue 3, page 492-504
ISSN 0300-9483 1502-3885
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1111/j.1502-3885.2010.00148.x
container_title Boreas
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