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Late-Quaternary Vegetational Dynamics and Community Stability Reconsidered

Published online by Cambridge University Press:  20 January 2017

Paul A. Delcourt
Affiliation:
Program for Quaternary Studies of the Southeastern United States, Department of Geological Sciences, and Graduate Program in Ecology, University of Tennessee, Knoxville, Tennessee 37996 USA
Hazel R. Delcourt
Affiliation:
Program for Quaternary Studies of the Southeastern United States, Department of Botany, University of Tennessee, Knoxville, Tennessee 37996 USA

Abstract

Defining the spatial and temporal limits of vegetational processes such as migration and invasion of established communities is a prerequisite to evaluating the degree of stability in plant communities through the late Quaternary. The interpretation of changes in boundaries of major vegetation types over the past 20,000 yr offers a complementary view to that provided by migration maps for particular plant taxa. North of approximately 43°N in eastern North America, continual vegetational disequilibrium has resulted from climatic change, soil development, and species migrations during postglacial times. Between 33° and 39°N, stable full-glacial vegetation was replaced by a relatively unstable vegetation during late-glacial climatic amelioration; stable interglacial vegetation developed there after about 9000 yr B.P. Late-Quaternary vegetation has been in dynamic equilibrium, with a relatively constant flora, south of 33°N on upland interfluves along the northern Gulf Coastal Plain, peninsular Florida, and west-central Mexico.

Type
Original Articles
Copyright
University of Washington

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