Deglaciation chronology, sea-level changes and environmental changes from Holocene lake sediments of Germania Havn Sø, Sabine Ø, northeast Greenland

Abstract Germania Havn Sø is located at the outermost coast of northeastern Greenland. According to radiocarbon dating, the lake basin was deglaciated in the early Holocene, around 11,000 cal yr BP. At that time the lake was a marine bay, but the lake was isolated soon after deglaciation at ~ 10,600...

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Published in:Quaternary Research
Main Authors: Bennike, Ole, Wagner, Bernd
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2012
Subjects:
Online Access:http://dx.doi.org/10.1016/j.yqres.2012.03.004
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spelling crcambridgeupr:10.1016/j.yqres.2012.03.004 2024-06-23T07:52:05+00:00 Deglaciation chronology, sea-level changes and environmental changes from Holocene lake sediments of Germania Havn Sø, Sabine Ø, northeast Greenland Bennike, Ole Wagner, Bernd 2012 http://dx.doi.org/10.1016/j.yqres.2012.03.004 http://api.elsevier.com/content/article/PII:S0033589412000300?httpAccept=text/xml http://api.elsevier.com/content/article/PII:S0033589412000300?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400008425 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 78, issue 1, page 103-109 ISSN 0033-5894 1096-0287 journal-article 2012 crcambridgeupr https://doi.org/10.1016/j.yqres.2012.03.004 2024-06-05T04:03:21Z Abstract Germania Havn Sø is located at the outermost coast of northeastern Greenland. According to radiocarbon dating, the lake basin was deglaciated in the early Holocene, around 11,000 cal yr BP. At that time the lake was a marine bay, but the lake was isolated soon after deglaciation at ~ 10,600 cal yr BP. The marine fauna was species-poor, indicating harsh conditions with a high sedimentation rate and lowered salinity due to glacial meltwater supply. The pioneer vegetation around the lake was dominated by mosses and herbs. Deposition of relatively coarse sediments during the early Holocene indicates erosion of the newly deglaciated terrain. Remains of the first woody plant ( Salix herbacea) appear at 7600 cal yr BP and remains of other woody plants ( Salix arctica , Dryas octopetala , Cassiope tetragona and Empetrum nigrum ) appear around one millennium later. Declining concentrations of D. octopetala and the caddis fly Apatania zonella in the late Holocene probably imply falling summer temperatures. Only moderate changes in the granulometric and geochemical record during the Holocene indicate relatively stable environmental settings in the lake, which can probably be explained by its location at the outer coast and the buffering effect of the neighboring ocean. Article in Journal/Newspaper Cassiope tetragona Dryas octopetala Empetrum nigrum Greenland Salix herbacea Cambridge University Press Germania Havn ENVELOPE(-18.827,-18.827,74.537,74.537) Greenland Sabine Ø ENVELOPE(-18.945,-18.945,74.595,74.595) Quaternary Research 78 1 103 109
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Germania Havn Sø is located at the outermost coast of northeastern Greenland. According to radiocarbon dating, the lake basin was deglaciated in the early Holocene, around 11,000 cal yr BP. At that time the lake was a marine bay, but the lake was isolated soon after deglaciation at ~ 10,600 cal yr BP. The marine fauna was species-poor, indicating harsh conditions with a high sedimentation rate and lowered salinity due to glacial meltwater supply. The pioneer vegetation around the lake was dominated by mosses and herbs. Deposition of relatively coarse sediments during the early Holocene indicates erosion of the newly deglaciated terrain. Remains of the first woody plant ( Salix herbacea) appear at 7600 cal yr BP and remains of other woody plants ( Salix arctica , Dryas octopetala , Cassiope tetragona and Empetrum nigrum ) appear around one millennium later. Declining concentrations of D. octopetala and the caddis fly Apatania zonella in the late Holocene probably imply falling summer temperatures. Only moderate changes in the granulometric and geochemical record during the Holocene indicate relatively stable environmental settings in the lake, which can probably be explained by its location at the outer coast and the buffering effect of the neighboring ocean.
format Article in Journal/Newspaper
author Bennike, Ole
Wagner, Bernd
spellingShingle Bennike, Ole
Wagner, Bernd
Deglaciation chronology, sea-level changes and environmental changes from Holocene lake sediments of Germania Havn Sø, Sabine Ø, northeast Greenland
author_facet Bennike, Ole
Wagner, Bernd
author_sort Bennike, Ole
title Deglaciation chronology, sea-level changes and environmental changes from Holocene lake sediments of Germania Havn Sø, Sabine Ø, northeast Greenland
title_short Deglaciation chronology, sea-level changes and environmental changes from Holocene lake sediments of Germania Havn Sø, Sabine Ø, northeast Greenland
title_full Deglaciation chronology, sea-level changes and environmental changes from Holocene lake sediments of Germania Havn Sø, Sabine Ø, northeast Greenland
title_fullStr Deglaciation chronology, sea-level changes and environmental changes from Holocene lake sediments of Germania Havn Sø, Sabine Ø, northeast Greenland
title_full_unstemmed Deglaciation chronology, sea-level changes and environmental changes from Holocene lake sediments of Germania Havn Sø, Sabine Ø, northeast Greenland
title_sort deglaciation chronology, sea-level changes and environmental changes from holocene lake sediments of germania havn sø, sabine ø, northeast greenland
publisher Cambridge University Press (CUP)
publishDate 2012
url http://dx.doi.org/10.1016/j.yqres.2012.03.004
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long_lat ENVELOPE(-18.827,-18.827,74.537,74.537)
ENVELOPE(-18.945,-18.945,74.595,74.595)
geographic Germania Havn
Greenland
Sabine Ø
geographic_facet Germania Havn
Greenland
Sabine Ø
genre Cassiope tetragona
Dryas octopetala
Empetrum nigrum
Greenland
Salix herbacea
genre_facet Cassiope tetragona
Dryas octopetala
Empetrum nigrum
Greenland
Salix herbacea
op_source Quaternary Research
volume 78, issue 1, page 103-109
ISSN 0033-5894 1096-0287
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1016/j.yqres.2012.03.004
container_title Quaternary Research
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