The Post-glacial history of vegetation and climate at Ennadai Lake, Keewatin, and Lynn Lake, Manitoba (Canada)

Peat from Keewatin and Manitoba contained macrofossil and palynological evidence of former latitudinal movements of the forest — tundra boundary probably in response to the changing location of the mean summer position of the Arctic front. There was very rapid melting of the large late-Wisconsin ice...

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Bibliographic Details
Published in:E&G Quaternary Science Journal
Main Author: H. Nichols
Format: Article in Journal/Newspaper
Language:German
English
Published: Copernicus Publications 1967
Subjects:
Online Access:https://doi.org/10.3285/eg.18.1.12
https://doaj.org/article/107d1c52e9284ea8ba0a5fcff6fc4ed7