Exceptional Record of Mid-Pleistocene Vertebrates Helps Differentiate Climatic from Anthropogenic Ecosystem Perturbations

Mid-Pleistocene vertebrates in North America are scarce but important for recognizing the ecological effects of climatic change in the absence of humans. We report on a uniquely rich mid-Pleistocene vertebrate sequence from Porcupine Cave, Colorado, which records at least 127 species and the earlies...

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Published in:Proceedings of the National Academy of Sciences - PNAS Vol. 101; no. 25; pp. 9297 - 9302
Main Authors: Barnosky, Anthony D., Bell, Christopher J., Emslie, Steven D., Goodwin, H. Thomas, Mead, Jim I., Repenning, Charles A., Scott, Eric, Shabel, Alan B., Leopold, Estella B.
Format: Journal Article
Language:English
Published: United States National Academy of Sciences 22-06-2004
National Acad Sciences
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Summary:Mid-Pleistocene vertebrates in North America are scarce but important for recognizing the ecological effects of climatic change in the absence of humans. We report on a uniquely rich mid-Pleistocene vertebrate sequence from Porcupine Cave, Colorado, which records at least 127 species and the earliest appearances of 30 mammals and birds. By analyzing >20,000 mammal fossils in relation to modern species and independent climatic proxies, we determined how mammal communities reacted to presumed glacial-interglacial transitions between 1,000,000 and 600,000 years ago. We conclude that climatic warming primarily affected mammals of lower trophic and size categories, in contrast to documented human impacts on higher trophic and size categories historically. Despite changes in species composition and minor changes in small-mammal species richness evident at times of climatic change, overall structural stability of mammal communities persisted >600,000 years before human impacts.
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To whom correspondence should be addressed: E-mail: barnosky@socrates.berkeley.edu.
Communicated by Estella B. Leopold, University of Washington, Seattle, WA, April 12, 2004
ISSN:0027-8424
1091-6490
DOI:10.1073/pnas.0402592101