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Ingassing, Storage, and Outgassing of Terrestrial Carbon through Geologic Time

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2013

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Research Article| January 01, 2013 Ingassing, Storage, and Outgassing of Terrestrial Carbon through Geologic Time Rajdeep Dasgupta Rajdeep Dasgupta Department of Earth Science, Rice University, 6100 Main Street, MS 126 Houston, Texas 77005, U.S.A., Rajdeep.Dasgupta@rice.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Rajdeep Dasgupta Department of Earth Science, Rice University, 6100 Main Street, MS 126 Houston, Texas 77005, U.S.A., Rajdeep.Dasgupta@rice.edu Publisher: Mineralogical Society of America First Online: 09 Mar 2017 © 2013 Mineralogical Society of America Reviews in Mineralogy and Geochemistry (2013) 75 (1): 183–229. https://doi.org/10.2138/rmg.2013.75.7 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Rajdeep Dasgupta; Ingassing, Storage, and Outgassing of Terrestrial Carbon through Geologic Time. Reviews in Mineralogy and Geochemistry 2013;; 75 (1): 183–229. doi: https://doi.org/10.2138/rmg.2013.75.7 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search Earth is unique among the terrestrial planets in our solar system in having a fluid envelope that fosters life. The secrets behind Earth's habitable climate are well-tuned cycles of carbon (C) and other volatiles. While on time-scales of ten to thousands of years the chemistry of fluids in the atmosphere, hydrosphere, and biosphere is dictated by fluxes of carbon between near surface reservoirs, over hundreds of millions to billions of years it is maintained by chemical interactions of carbon between Earth's interior, more specifically the mantle, and the exosphere (Berner 1999). This is because of the fact that... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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