Palynological Studies of a Peat Deposit in Front of the Thompson Glacier (Progress Report)
It appears that the area on Axel Heiberg Island in which the profile discussed above was studied has not been inundated by the sea or overrun by glaciers since 2,500 B. C. Between 2,000 and 1,000 B. C., the climate was apparently more favourable for the formation of vegetation than it is at present....
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McGill University
1963
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ftdatacite:10.48350/151448 2023-05-15T15:34:45+02:00 Palynological Studies of a Peat Deposit in Front of the Thompson Glacier (Progress Report) Hegg, Otto 1963 https://dx.doi.org/10.48350/151448 https://boris.unibe.ch/151448/ unknown McGill University restricted access publisher holds copyright http://purl.org/coar/access_right/c_16ec 580 Plants Botany Text article-journal book part ScholarlyArticle 1963 ftdatacite https://doi.org/10.48350/151448 2021-11-05T12:55:41Z It appears that the area on Axel Heiberg Island in which the profile discussed above was studied has not been inundated by the sea or overrun by glaciers since 2,500 B. C. Between 2,000 and 1,000 B. C., the climate was apparently more favourable for the formation of vegetation than it is at present. This change in climate is not apparent from evidence of more species in the region at that time than there are now, but rather by quantitative changes within the species present on Axel Heiberg Island today. Book Part Axel Heiberg Island DataCite Metadata Store (German National Library of Science and Technology) Heiberg ENVELOPE(13.964,13.964,66.424,66.424) Axel Heiberg Island ENVELOPE(-91.001,-91.001,79.752,79.752) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
580 Plants Botany |
spellingShingle |
580 Plants Botany Hegg, Otto Palynological Studies of a Peat Deposit in Front of the Thompson Glacier (Progress Report) |
topic_facet |
580 Plants Botany |
description |
It appears that the area on Axel Heiberg Island in which the profile discussed above was studied has not been inundated by the sea or overrun by glaciers since 2,500 B. C. Between 2,000 and 1,000 B. C., the climate was apparently more favourable for the formation of vegetation than it is at present. This change in climate is not apparent from evidence of more species in the region at that time than there are now, but rather by quantitative changes within the species present on Axel Heiberg Island today. |
format |
Book Part |
author |
Hegg, Otto |
author_facet |
Hegg, Otto |
author_sort |
Hegg, Otto |
title |
Palynological Studies of a Peat Deposit in Front of the Thompson Glacier (Progress Report) |
title_short |
Palynological Studies of a Peat Deposit in Front of the Thompson Glacier (Progress Report) |
title_full |
Palynological Studies of a Peat Deposit in Front of the Thompson Glacier (Progress Report) |
title_fullStr |
Palynological Studies of a Peat Deposit in Front of the Thompson Glacier (Progress Report) |
title_full_unstemmed |
Palynological Studies of a Peat Deposit in Front of the Thompson Glacier (Progress Report) |
title_sort |
palynological studies of a peat deposit in front of the thompson glacier (progress report) |
publisher |
McGill University |
publishDate |
1963 |
url |
https://dx.doi.org/10.48350/151448 https://boris.unibe.ch/151448/ |
long_lat |
ENVELOPE(13.964,13.964,66.424,66.424) ENVELOPE(-91.001,-91.001,79.752,79.752) |
geographic |
Heiberg Axel Heiberg Island |
geographic_facet |
Heiberg Axel Heiberg Island |
genre |
Axel Heiberg Island |
genre_facet |
Axel Heiberg Island |
op_rights |
restricted access publisher holds copyright http://purl.org/coar/access_right/c_16ec |
op_doi |
https://doi.org/10.48350/151448 |
_version_ |
1766365038628569088 |