Abstract
Spruce migrated into the area at least 9000 radiocarbon years ago. From 9000 yr BP to 5000 yr BP the area supported a sparse Picea-Salix-Betula forest-tundra vegetation. By 5000 yr BP local environmental change created a different habitat primarily affecting the local taxa. Alnus invaded the general area shortly after 5000 yr BP. A local Betula-dominated community replaced the previous Cyperaceae-dominated one at about 3000 yr BP. A Cyperaceae-dominated community again occupied the area at 1900 yr BP. The present regional forest-tundra vegetation has had little change during the last 9000 radiocarbon years. -from Authors
Cite
CITATION STYLE
Xia-Cheng Wang, & Geurts, M. A. (1991). Post-glacial vegetation history of the Ittlemit Lake basin, southwest Yukon Territory. Arctic, 44(1), 23–30. https://doi.org/10.14430/arctic1514
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