Paleontological and sedimentological investigations of a sediment profile from northeast Greenland

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Auteurs principaux: Wagner, Bernd, Bennike, Ole, Cremer, Holger, Klug, Martin
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2010
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author Wagner, Bernd
Bennike, Ole
Cremer, Holger
Klug, Martin
author_facet Wagner, Bernd
Bennike, Ole
Cremer, Holger
Klug, Martin
collection Datos científicos de ciencias marinas y ambientales
contents 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 Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_759229
institution PANGAEA
language en
publishDate 2010
publisher PANGAEA
record_format pangaea
spellingShingle Paleontological and sedimentological investigations of a sediment profile from northeast Greenland
Wagner, Bernd
Bennike, Ole
Cremer, Holger
Klug, Martin
458554; 458555, 458556; 458558, 458559; 458560; 458561, 458562; 458563; 458564; 458565; 458566; 458567; 458568; 458569; 458570; AWI Arctic Land Expedition; COMPCORE; Composite Core; G2003-1; G2003-10; G2003-11; G2003-12; G2003-13; G2003-2; G2003-3; G2003-4; G2003-5; G2003-6; G2003-7; G2003-8; G2003-9; Geological sample; GEOS; GL-Land_2003__EastGreenland; Greenland2003; Loon Lake, Geographical Society Ø, East Greenland; Lz1116
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.
title Paleontological and sedimentological investigations of a sediment profile from northeast Greenland
topic 458554; 458555, 458556; 458558, 458559; 458560; 458561, 458562; 458563; 458564; 458565; 458566; 458567; 458568; 458569; 458570; AWI Arctic Land Expedition; COMPCORE; Composite Core; G2003-1; G2003-10; G2003-11; G2003-12; G2003-13; G2003-2; G2003-3; G2003-4; G2003-5; G2003-6; G2003-7; G2003-8; G2003-9; Geological sample; GEOS; GL-Land_2003__EastGreenland; Greenland2003; Loon Lake, Geographical Society Ø, East Greenland; Lz1116
url https://doi.org/10.1594/PANGAEA.759229