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      Remote Sensing of Planetary Properties and Biosignatures on Extrasolar Terrestrial Planets

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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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            Runaway and moist greenhouse atmospheres and the evolution of Earth and Venus

            James F. Kasting (1988)
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              Thermal and albedo mapping of Mars during the Viking primary mission

              Alan Peterfreund, Frank Palluconi, Ellis Miner … (1977)
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                Author and article information

                Journal
                Title: Astrobiology
                Abbreviated Title: Astrobiology
                Publisher: Mary Ann Liebert Inc
                ISSN (Print): 1531-1074
                ISSN (Electronic): 1557-8070
                Publication date Created: June 2002
                Publication date (Print): June 2002
                Volume: 2
                Issue: 2
                Pages: 153-181
                Article
                DOI: 10.1089/15311070260192246
                PubMed ID: 12469366
                SO-VID: e39be4ed-d281-49e7-8323-79de0afb350d
                Copyright © © 2002
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