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      Expression of the Early Toarcian negative carbon-isotope excursion in separated carbonate microfractions (Jurassic, Paris Basin)

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      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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            Productivity, sedimentation rate, and sedimentary organic matter in the oceans—I. Organic carbon preservation

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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
                January 2009
                January 2009
                : 277
                : 1-2
                : 194-203
                Article
                10.1016/j.epsl.2008.10.013
                5acf969b-dc08-4c3e-97a3-03d05a7e2b6b
                © 2009

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

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