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      The abundance of 13C in marine organic matter and isotopic fractionation in the global biogeochemical cycle of carbon during the past 800 Ma

      Author(s): , ,
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      Journal: Chemical Geology
      Publisher: Elsevier BV

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          A neoproterozoic snowball earth

          Hoffman, Kaufman, Halverson … (1998)
          Negative carbon isotope anomalies in carbonate rocks bracketing Neoproterozoic glacial deposits in Namibia, combined with estimates of thermal subsidence history, suggest that biological productivity in the surface ocean collapsed for millions of years. This collapse can be explained by a global glaciation (that is, a snowball Earth), which ended abruptly when subaerial volcanic outgassing raised atmospheric carbon dioxide to about 350 times the modern level. The rapid termination would have resulted in a warming of the snowball Earth to extreme greenhouse conditions. The transfer of atmospheric carbon dioxide to the ocean would result in the rapid precipitation of calcium carbonate in warm surface waters, producing the cap carbonate rocks observed globally.
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            87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater

            Jan Veizer, Davin Ala, Karem Azmy … (1999)
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              The distribution of 13C of ΣCO2 in the world oceans

              P.M. Kroopnick (1985)
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                Author and article information

                Journal
                Title: Chemical Geology
                Abbreviated Title: Chemical Geology
                Publisher: Elsevier BV
                ISSN (Print): 00092541
                Publication date Created: September 1999
                Publication date (Print): September 1999
                Volume: 161
                Issue: 1-3
                Pages: 103-125
                Article
                DOI: 10.1016/S0009-2541(99)00083-2
                SO-VID: 4cb7364a-4a1c-42f3-95d6-4a2039bd795e
                Copyright © © 1999
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                http://www.elsevier.com/tdm/userlicense/1.0/

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