Comparative Earth History and Late Permian Mass Extinction

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Comparative Earth History and Late Permian Mass Extinction

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Title: Comparative Earth History and Late Permian Mass Extinction
Author: Knoll, Andrew; Canfield, Donald E.; Grotzinger, John P.; Bambach, Richard

Note: Order does not necessarily reflect citation order of authors.

Citation: Knoll, Andrew H., Richard K. Bambach, Donald E. Canfield, and John P. Grotzinger. 1996. Comparative earth history and Late Permian mass extinction. Science 273(5274): 452-457.
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Abstract: The repeated association during the late Neoproterozoic Era of large carbon-isotopic excursions, continental glaciation, and stratigraphically anomalous carbonate precipitation provides a framework for interpreting the reprise of these conditions on the Late Permian Earth. A paleoceanographic model that was developed to explain these stratigraphically linked phenomena suggests that the overturn of anoxic deep oceans during the Late Permian introduced high concentrations of carbon dioxide into surficial environments. The predicted physiological and climatic consequences for marine and terrestrial organisms are in good accord with the observed timing and selectivity of Late Permian mass extinction.
Published Version: http://dx.doi.org/10.1126/science.273.5274.452
Citable link to this page: http://nrs.harvard.edu/urn-3:HUL.InstRepos:3210662

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  • FAS Scholarly Articles [7106]
    Peer reviewed scholarly articles from the Faculty of Arts and Sciences of Harvard University
 
 

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