Characteristics of treeline plant communities in Alaska

The treeline in Alaska is usually mapped as the limit of white spruce Picea glauca (Moench) Voss along the south slope of the Brooks Range and in western Alaska and as the limit of Sitka spruce Picea sitchensis (Bong.) Carr. on Kodiak Island and in the Alaska Peninsula. In some localities black spru...

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Bibliographic Details
Published in:Ecography
Main Author: Viereck, Leslie A.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1979
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1600-0587.1979.tb01294.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1600-0587.1979.tb01294.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1600-0587.1979.tb01294.x
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Summary:The treeline in Alaska is usually mapped as the limit of white spruce Picea glauca (Moench) Voss along the south slope of the Brooks Range and in western Alaska and as the limit of Sitka spruce Picea sitchensis (Bong.) Carr. on Kodiak Island and in the Alaska Peninsula. In some localities black spruce Picea mariana (Mill.) B.S.P. and paper birch Betula papyrifera Marsh. form components of the treeline community with white spruce. Of special interest are the groves of balsam poplar Populus balsamifera L. occurring on the north slope of the Brooks Range and to the west and southwest of the spruce treeline. There is some question as to whether trees survived in unglaciated portions of Alaska during the last glacial period. Spruce trees became prevalent about 10000 yr ago and may still be expanding to their climatic limits. In some areas of Alaska the treeline was more expanded during the Hypsithermal period than it is at present, but in other regions evidence for such an expansion is lacking. Treeline in some areas seems to have been stable for the last several centuries, but is has been expanding rapidly for the last 40 yr in central and western Alaska and for a longer period on Kodiak Island.