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  3. Palynological Studies of a Peat Deposit in Front of the Thompson Glacier (Progress Report)
 

Palynological Studies of a Peat Deposit in Front of the Thompson Glacier (Progress Report)

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BORIS DOI
10.48350/151448
Date of Publication
1963
Publication Type
Book Section
Division/Institute

Institut für Pflanzen...

Contributor
Hegg, Otto
Institut für Pflanzenwissenschaften (IPS)
Editor
Müller, Fritz
Subject(s)

500 - Science::580 - ...

Publisher
McGill University
Language
English
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.
Handle
https://boris-portal.unibe.ch/handle/20.500.12422/201370
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File(s)
FileFile TypeFormatSizeLicensePublisher/Copright statementContent
1963_AxelHeibergIsland_PrelimRep_217.pdftextAdobe PDF225.99 KBpublisherpublished restricted
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