The subfossil occurrence of Mytilus edulis L. in central East Greenland
The subfossil occurrence of Mytilus edulis in central East Greenland has been C 14 ‐dated to roughly between 8000 B.P. and 5500 B.P.; compared with other areas this is a short period. Its immigration coincides with the final deglaciation of the innermost fjords, and its disappearance is contemporane...
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crwiley:10.1111/j.1502-3885.1974.tb00664.x 2024-06-02T08:05:54+00:00 The subfossil occurrence of Mytilus edulis L. in central East Greenland HJORT, CHRISTIAN FUNDER, SVEND 1974 http://dx.doi.org/10.1111/j.1502-3885.1974.tb00664.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1974.tb00664.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1974.tb00664.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 3, issue 1, page 23-33 ISSN 0300-9483 1502-3885 journal-article 1974 crwiley https://doi.org/10.1111/j.1502-3885.1974.tb00664.x 2024-05-06T07:00:53Z The subfossil occurrence of Mytilus edulis in central East Greenland has been C 14 ‐dated to roughly between 8000 B.P. and 5500 B.P.; compared with other areas this is a short period. Its immigration coincides with the final deglaciation of the innermost fjords, and its disappearance is contemporaneous with an increase in cold‐climate plants, as shown by pollen spectra. It is suggested that it immigrated from the Svalbard area rather than from southeast Greenland, and that the central East Greenland fjord zone forms an isolated oasis, where more southerly species like Mytilus and Chlamys islandica can or could live, even if this was not possible along the surrounding and more hostile outer coasts. The reason for the absence of Mytilus edalis from the region today is probably not the local climate. Article in Journal/Newspaper East Greenland Greenland Svalbard Wiley Online Library Svalbard Greenland Boreas 3 1 23 33 |
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Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
The subfossil occurrence of Mytilus edulis in central East Greenland has been C 14 ‐dated to roughly between 8000 B.P. and 5500 B.P.; compared with other areas this is a short period. Its immigration coincides with the final deglaciation of the innermost fjords, and its disappearance is contemporaneous with an increase in cold‐climate plants, as shown by pollen spectra. It is suggested that it immigrated from the Svalbard area rather than from southeast Greenland, and that the central East Greenland fjord zone forms an isolated oasis, where more southerly species like Mytilus and Chlamys islandica can or could live, even if this was not possible along the surrounding and more hostile outer coasts. The reason for the absence of Mytilus edalis from the region today is probably not the local climate. |
format |
Article in Journal/Newspaper |
author |
HJORT, CHRISTIAN FUNDER, SVEND |
spellingShingle |
HJORT, CHRISTIAN FUNDER, SVEND The subfossil occurrence of Mytilus edulis L. in central East Greenland |
author_facet |
HJORT, CHRISTIAN FUNDER, SVEND |
author_sort |
HJORT, CHRISTIAN |
title |
The subfossil occurrence of Mytilus edulis L. in central East Greenland |
title_short |
The subfossil occurrence of Mytilus edulis L. in central East Greenland |
title_full |
The subfossil occurrence of Mytilus edulis L. in central East Greenland |
title_fullStr |
The subfossil occurrence of Mytilus edulis L. in central East Greenland |
title_full_unstemmed |
The subfossil occurrence of Mytilus edulis L. in central East Greenland |
title_sort |
subfossil occurrence of mytilus edulis l. in central east greenland |
publisher |
Wiley |
publishDate |
1974 |
url |
http://dx.doi.org/10.1111/j.1502-3885.1974.tb00664.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1974.tb00664.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1974.tb00664.x |
geographic |
Svalbard Greenland |
geographic_facet |
Svalbard Greenland |
genre |
East Greenland Greenland Svalbard |
genre_facet |
East Greenland Greenland Svalbard |
op_source |
Boreas volume 3, issue 1, page 23-33 ISSN 0300-9483 1502-3885 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1502-3885.1974.tb00664.x |
container_title |
Boreas |
container_volume |
3 |
container_issue |
1 |
container_start_page |
23 |
op_container_end_page |
33 |
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1800750788144791552 |