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dc.contributor.authorKnoll, Andrew
dc.contributor.authorBambach, Richard
dc.contributor.authorCanfield, Donald E.
dc.contributor.authorGrotzinger, John P.
dc.date.accessioned2009-08-18T19:49:59Z
dc.date.issued1996
dc.identifier.citationKnoll, 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.en
dc.identifier.issn1095-9203en
dc.identifier.issn0036-8075en
dc.identifier.urihttp://nrs.harvard.edu/urn-3:HUL.InstRepos:3210662
dc.description.abstractThe 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.en
dc.description.sponsorshipOrganismic and Evolutionary Biologyen
dc.language.isoen_USen
dc.publisherAmerican Association for the Advancement of Scienceen
dc.relation.isversionofhttp://dx.doi.org/10.1126/science.273.5274.452en
dash.licenseMETA_ONLY
dc.titleComparative Earth History and Late Permian Mass Extinctionen
dc.relation.journalScienceen
dash.depositing.authorKnoll, Andrew
dash.embargo.until10000-01-01
dc.identifier.doi10.1126/science.273.5274.452*
dash.contributor.affiliatedBambach, Richard
dash.contributor.affiliatedKnoll, Andrew


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