Pollen Diagrams from Sub-Arctic Central Canada
- 31 March 1967
- journal article
- research article
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 155 (3770), 1665-1668
- https://doi.org/10.1126/science.155.3770.1665
Abstract
Peat from Keewatin and Manitoba contained macrofossil and palynological evidence of former latitudinal movements of the forest-tundra boundary in response to the changing location of the mean summer position of the Arctic front. Radiocarbon dating demonstrates the synchroneity of these climatic changes with those registered in northwest Europe during the past 6000 years.This publication has 9 references indexed in Scilit:
- University of Wisconsin Radiocarbon Dates IIRadiocarbon, 1966
- University of Wisconsin Radiocarbon Dates IRadiocarbon, 1965
- The Vegetation of the Ennadai Lake Area, N.W.T.: Studies in Subarctic and Arctic BioclimatologyEcological Monographs, 1965
- Radiocarbon and Soil Evidence of Former Forest in the Southern Canadian TundraScience, 1965
- Studies on Southern Pennine Peats: III. The Behaviour of SphagnumJournal of Ecology, 1964
- CONTRIBUTIONS TO THE HOLOCENE PALEOECOLOGY OF WESTCENTRAL CANADA: I. THE RIDING MOUNTAIN AREACanadian Journal of Botany, 1964
- NOTES ON LATE‐QUATERNARY CLIMATIC CHANGES IN CANADA *Annals of the New York Academy of Sciences, 1961
- A Radiocarbon Date of Peat from James Bay in QuebecScience, 1954
- A Radiocarbon Date of Peat from James Bay in QuebecScience, 1954