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      Eocene vegetation patterns reconstructed from plant diversity — A global perspective

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      Palaeogeography, Palaeoclimatology, Palaeoecology
      Elsevier BV

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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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            Evolution of Early Cenozoic marine temperatures

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              Some Aspects of Plant Geography of the Northern Hemisphere During the Late Cretaceous and Tertiary

              Jack Wolfe (1975)
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                Author and article information

                Journal
                Palaeogeography, Palaeoclimatology, Palaeoecology
                Palaeogeography, Palaeoclimatology, Palaeoecology
                Elsevier BV
                00310182
                April 2007
                April 2007
                : 247
                : 3-4
                : 243-271
                Article
                10.1016/j.palaeo.2006.10.022
                c417d30c-f906-4411-aa79-d9a5802156a1
                © 2007

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

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