Subglacial plant remains from the Omnsbreen glacier area, south Norway
Plant remains have been found on ground recently deglaciated from the Omnsbreen glacier. They consist of Salix herbacea, Salix spp., Silene acaulis, Polytrichum norvegicum, Kiaeria of. starkei, and some unidentified species. Their age has been determined by the radiocarbon method to approx. 550 year...
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Language: | English |
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Online Access: | http://dx.doi.org/10.1111/j.1502-3885.1978.tb00266.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1978.tb00266.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1978.tb00266.x |
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crwiley:10.1111/j.1502-3885.1978.tb00266.x 2024-10-13T14:07:28+00:00 Subglacial plant remains from the Omnsbreen glacier area, south Norway ELVEN, REIDAR 1978 http://dx.doi.org/10.1111/j.1502-3885.1978.tb00266.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1978.tb00266.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1978.tb00266.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 7, issue 2, page 83-89 ISSN 0300-9483 1502-3885 journal-article 1978 crwiley https://doi.org/10.1111/j.1502-3885.1978.tb00266.x 2024-09-23T04:36:52Z Plant remains have been found on ground recently deglaciated from the Omnsbreen glacier. They consist of Salix herbacea, Salix spp., Silene acaulis, Polytrichum norvegicum, Kiaeria of. starkei, and some unidentified species. Their age has been determined by the radiocarbon method to approx. 550 years, indicating that the present Omnsbreen glacier emerged as late as the clima deterioration in the late Middle Ages. The past vegetation was similar to the present, but slightly more thermophilous, indicating a rapid clima deterioration in the fourteenth century. Article in Journal/Newspaper glacier Salix herbacea Silene acaulis Wiley Online Library Norway Boreas 7 2 83 89 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
Plant remains have been found on ground recently deglaciated from the Omnsbreen glacier. They consist of Salix herbacea, Salix spp., Silene acaulis, Polytrichum norvegicum, Kiaeria of. starkei, and some unidentified species. Their age has been determined by the radiocarbon method to approx. 550 years, indicating that the present Omnsbreen glacier emerged as late as the clima deterioration in the late Middle Ages. The past vegetation was similar to the present, but slightly more thermophilous, indicating a rapid clima deterioration in the fourteenth century. |
format |
Article in Journal/Newspaper |
author |
ELVEN, REIDAR |
spellingShingle |
ELVEN, REIDAR Subglacial plant remains from the Omnsbreen glacier area, south Norway |
author_facet |
ELVEN, REIDAR |
author_sort |
ELVEN, REIDAR |
title |
Subglacial plant remains from the Omnsbreen glacier area, south Norway |
title_short |
Subglacial plant remains from the Omnsbreen glacier area, south Norway |
title_full |
Subglacial plant remains from the Omnsbreen glacier area, south Norway |
title_fullStr |
Subglacial plant remains from the Omnsbreen glacier area, south Norway |
title_full_unstemmed |
Subglacial plant remains from the Omnsbreen glacier area, south Norway |
title_sort |
subglacial plant remains from the omnsbreen glacier area, south norway |
publisher |
Wiley |
publishDate |
1978 |
url |
http://dx.doi.org/10.1111/j.1502-3885.1978.tb00266.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1978.tb00266.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1978.tb00266.x |
geographic |
Norway |
geographic_facet |
Norway |
genre |
glacier Salix herbacea Silene acaulis |
genre_facet |
glacier Salix herbacea Silene acaulis |
op_source |
Boreas volume 7, issue 2, page 83-89 ISSN 0300-9483 1502-3885 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1502-3885.1978.tb00266.x |
container_title |
Boreas |
container_volume |
7 |
container_issue |
2 |
container_start_page |
83 |
op_container_end_page |
89 |
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1812813764888625152 |