EA40CH05-Payne ARI 23 March 2012 10:24 End-Permian Mass Extinction in the Oceans: An Ancient Analog for the Twenty-First Century? Jonathan L. Payne1 and Matthew E. Clapham2 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305; email:
[email protected] 2Department of Earth and Planetary Sciences, University of California, Santa Cruz, California 95064; email:
[email protected] Annu. Rev. Earth Planet. Sci. 2012. 40:89–111 Keywords First published online as a Review in Advance on ocean acidification, evolution, isotope geochemistry, volcanism, January 3, 2012 biodiversity The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract This article’s doi: The greatest loss of biodiversity in the history of animal life occurred at the 10.1146/annurev-earth-042711-105329 end of the Permian Period (∼252 million years ago). This biotic catastro- Annu. Rev. Earth Planet. Sci. 2012.40:89-111. Downloaded from www.annualreviews.org Copyright c 2012 by Annual Reviews. phe coincided with an interval of widespread ocean anoxia and the eruption All rights reserved of one of Earth’s largest continental flood basalt provinces, the Siberian by Stanford University - Main Campus Robert Crown Law Library on 06/04/12. For personal use only. 0084-6597/12/0530-0089$20.00 Traps. Volatile release from basaltic magma and sedimentary strata dur- ing emplacement of the Siberian Traps can account for most end-Permian paleontological and geochemical observations. Climate change and, per- haps, destruction of the ozone layer can explain extinctions on land, whereas changes in ocean oxygen levels, CO2, pH, and temperature can account for extinction selectivity across marine animals.