The circumboreal tundra-taiga interface: late Pleistocene and Holocene changes.

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Summary

A scenario of a continuous but modest occupation of eastern Beringia by spruce during the late-Pleistocene is proposed instead of an exceptionally rapid spread of conifers from the glacial refugium south of the Laurentide ice sheet, which typically has been assumed.

Type
article
Published
2002-08-01
Cited by
59
References
96

Keywords

Macrofossil, Beringia, Deglaciation, Holocene, Glacial period

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