CLIMATE PREDICTORS OF LATE QUATERNARY EXTINCTIONS
Article first published online: 14 APR 2010
DOI: 10.1111/j.1558-5646.2010.01009.x
© 2010 The Author(s). Journal compilation © 2010 The Society for the Study of Evolution
Additional Information
How to Cite
Nogués-Bravo, D., Ohlemüller, R., Batra, P. and Araújo, M. B. (2010), CLIMATE PREDICTORS OF LATE QUATERNARY EXTINCTIONS. Evolution, 64: 2442–2449. doi: 10.1111/j.1558-5646.2010.01009.x
Publication History
- Issue published online: 3 AUG 2010
- Article first published online: 14 APR 2010
- Received May 27, 2009Accepted March 2, 2010
Keywords:
- Body size;
- climate change;
- climate footprint;
- genetic diversity;
- global extinctions;
- Late Quaternary;
- phylogeography;
- refugia;
- species richness
Between 50,000 and 3,000 years before present (BP) 65% of mammal genera weighing over 44 kg went extinct, together with a lower proportion of small mammals. Why species went extinct in such large numbers is hotly debated. One of the arguments proposes that climate changes underlie Late Quaternary extinctions, but global quantitative evidence for this hypothesis is still lacking. We test the potential role of global climate change on the extinction of mammals during the Late Quaternary. Our results suggest that continents with the highest climate footprint values, in other words, with climate changes of greater magnitudes during the Late Quaternary, witnessed more extinctions than continents with lower climate footprint values, with the exception of South America. Our results are consistent across species with different body masses, reinforcing the view that past climate changes contributed to global extinctions. Our model outputs, the climate change footprint dataset, provide a new research venue to test hypotheses about biodiversity dynamics during the Late Quaternary from the genetic to the species richness level.

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