Hegg, Otto (1963). Palynological Studies of a Peat Deposit in Front of the Thompson Glacier (Progress Report). In: Müller, Fritz (ed.) Preliminary Report 1961-1962. Axel Heiberg Island Research Reports: Vol. 14 (pp. 217-219). Montreal: McGill University
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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.
Item Type: |
Book Section (Report Section) |
|---|---|
Division/Institute: |
08 Faculty of Science > Department of Biology > Institute of Plant Sciences (IPS) 08 Faculty of Science > Department of Biology > Institute of Plant Sciences (IPS) > Vegetation Science [discontinued] |
UniBE Contributor: |
Hegg, Otto |
Subjects: |
500 Science > 580 Plants (Botany) |
Series: |
Axel Heiberg Island Research Reports |
Publisher: |
McGill University |
Language: |
English |
Submitter: |
Peter Alfred von Ballmoos-Haas |
Date Deposited: |
21 Jan 2021 17:39 |
Last Modified: |
05 Dec 2022 15:45 |
BORIS DOI: |
10.48350/151448 |
URI: |
https://boris.unibe.ch/id/eprint/151448 |
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