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      Cyanobacterial blooms tied to volcanism during the 5 m.y. Permo-Triassic biotic crisis

      , , , , , , ,
      Geology
      Geological Society of America

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          Oceanic Anoxia and the End Permian Mass Extinction

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            Large perturbations of the carbon cycle during recovery from the end-permian extinction.

            High-resolution carbon isotope measurements of multiple stratigraphic sections in south China demonstrate that the pronounced carbon isotopic excursion at the Permian-Triassic boundary was not an isolated event but the first in a series of large fluctuations that continued throughout the Early Triassic before ending abruptly early in the Middle Triassic. The unusual behavior of the carbon cycle coincides with the delayed recovery from end-Permian extinction recorded by fossils, suggesting a direct relationship between Earth system function and biological rediversification in the aftermath of Earth's most devastating mass extinction.
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              Paleophysiology and end-Permian mass extinction

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                Author and article information

                Journal
                Geology
                Geology
                Geological Society of America
                0091-7613
                1943-2682
                April 30 2010
                April 30 2010
                : 38
                : 5
                : 447-450
                Article
                10.1130/G30769.1
                27b5bb53-7242-4552-8070-c0e21219bb05
                © 2010
                History

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