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      Secular Evolution of Continents and the Earth System

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          Nature and composition of the continental crust: A lower crustal perspective

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            On the Relative Importance of the Driving Forces of Plate Motion

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              A neoproterozoic snowball earth

              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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                Author and article information

                Contributors
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                Journal
                Reviews of Geophysics
                Reviews of Geophysics
                American Geophysical Union (AGU)
                8755-1209
                1944-9208
                December 2022
                December 15 2022
                December 2022
                : 60
                : 4
                Affiliations
                [1 ]School of Earth, Atmosphere & Environment Monash University VIC Melbourne Australia
                [2 ]School of Earth & Planetary Sciences National Institute of Science Education and Research HBNI Bhubaneswar India
                [3 ]Department of Earth Sciences The University of Adelaide SA Adelaide Australia
                [4 ]School of Earth Sciences University of Bristol Bristol UK
                Article
                10.1029/2022RG000789
                45dc1b0b-045f-4f78-ae9f-91e951e32122
                © 2022

                http://creativecommons.org/licenses/by/4.0/

                http://creativecommons.org/licenses/by/4.0/

                http://doi.wiley.com/10.1002/tdm_license_1.1

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