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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Published in:Boreas
Main Author: ELVEN, REIDAR
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1978
Subjects:
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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spelling 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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