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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Main Author: Hegg, Otto
Format: Book Part
Language:unknown
Published: McGill University 1963
Subjects:
Online Access:https://dx.doi.org/10.48350/151448
https://boris.unibe.ch/151448/
id ftdatacite:10.48350/151448
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spelling 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
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