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Terminal Pleistocene change in mammal communities in southeastern Washington State, USA

Published online by Cambridge University Press:  20 January 2017

R. Lee Lyman
R. Lee Lyman*
Affiliation:
Department of Anthropology, 107 Swallow Hall, University of Missouri, Columbia, MO 65211, USA
*
*Fax: + 1 573 884 5450. E-mail address:lymanr@missouri.edu.
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Abstract

Small mammal communities in western North America experienced declines in taxonomic richness across the late Pleistocene to Holocene transition (PHT), a recent natural global warming event. One community also experienced a decline in evenness and others replaced one species with a congener. Variability in response of small mammal communities to PHT warming is apparent. At the presently arid and xeric Marmes site in the Columbia Basin of southeastern Washington State, megafauna were absent by about 13,000 cal yr BP, evenness of small mammals declined about 11,700 cal yr BP and again about 11,400 cal yr BP whereas richness declined about 11,400 cal BP. Regional faunal turnover was, however, minimal among small-bodied taxa. Local mammal communities are depauperate as a result of megafaunal extinctions and subsequent decreases in small-mammal richness and evenness. The latter chronologically corresponds with a decrease in primary productivity driven by increasing warmth and aridity. More faunas must be studied in order to fully document the range of variability in the responses of mammalian communities to PHT warming. Documentation of patterns in those responses will facilitate understanding and enhance predictive accuracy with respect to responses of mammalian communities to modern global warming.

Keywords

Climate changeColumbia BasinConservation paleozoologyEastern Washington stateMammalsPaleoecologyPleistocene–Holocene transition
Type
Research Article
Information
Quaternary Research , Volume 81 , Issue 2 , March 2014 , pp. 295 - 304
Copyright
University of Washington

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