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      Hydrothermal venting of greenhouse gases triggering Early Jurassic global warming

      , , , , ,
      Earth and Planetary Science Letters
      Elsevier BV

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          Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene

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            Rapid acidification of the ocean during the Paleocene-Eocene thermal maximum.

            The Paleocene-Eocene thermal maximum (PETM) has been attributed to the rapid release of approximately 2000 x 10(9) metric tons of carbon in the form of methane. In theory, oxidation and ocean absorption of this carbon should have lowered deep-sea pH, thereby triggering a rapid ( 100,000 years). These findings indicate that a large mass of carbon (>2000 x 10(9) metric tons of carbon) dissolved in the ocean at the Paleocene-Eocene boundary and that permanent sequestration of this carbon occurred through silicate weathering feedback.
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              Large igneous provinces and mass extinctions

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                Author and article information

                Journal
                Earth and Planetary Science Letters
                Earth and Planetary Science Letters
                Elsevier BV
                0012821X
                April 2007
                April 2007
                : 256
                : 3-4
                : 554-566
                Article
                10.1016/j.epsl.2007.02.013
                c7d68cc9-bce4-4699-aebe-54011bfdf2f7
                © 2007

                http://www.elsevier.com/tdm/userlicense/1.0/

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