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Research ArticleARTICLES

The Weathering of Sedimentary Organic Matter as a Control on Atmospheric O2: II. Theoretical Modeling

Edward W. Bolton, Robert A. Berner and Steven T. Petsch
American Journal of Science October 2006, 306 (8) 575-615; DOI: https://doi.org/10.2475/08.2006.01
Edward W. Bolton
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Robert A. Berner
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Steven T. Petsch
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American Journal of Science
Vol. 306, Issue 8
October 2006
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The Weathering of Sedimentary Organic Matter as a Control on Atmospheric O2: II. Theoretical Modeling
Edward W. Bolton, Robert A. Berner, Steven T. Petsch
American Journal of Science Oct 2006, 306 (8) 575-615; DOI: 10.2475/08.2006.01

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The Weathering of Sedimentary Organic Matter as a Control on Atmospheric O2: II. Theoretical Modeling
Edward W. Bolton, Robert A. Berner, Steven T. Petsch
American Journal of Science Oct 2006, 306 (8) 575-615; DOI: 10.2475/08.2006.01
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    • Abstract
    • INTRODUCTION
    • THE MODEL
    • RESULTS AND DISCUSSION
    • SUMMARY AND CONCLUSIONS
    • APPENDIX A
    • APPENDIX B
    • Acknowledgments
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  • Carbon cycle evolution before and after the Great Oxidation of the atmosphere
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  • Reply to comment by Thomas M. Blattmann on "Carbon dioxide emissions by rock organic carbon oxidation and the next geochemical carbon budget of the Mackenzie River Basin", v. 319, n. 6, p. 473-499.
  • Carbon dioxide emissions by rock organic carbon oxidation and the net geochemical carbon budget of the Mackenzie River Basin
  • On the geological and scientific legacy of petrogenic organic carbon
  • Model based Paleozoic atmospheric oxygen estimates: a revisit to GEOCARBSULF
  • Microbial oxidation of lithospheric organic carbon in rapidly eroding tropical mountain soils
  • Mountain glaciation drives rapid oxidation of rock-bound organic carbon
  • Biotic effects on oxygen consumption during weathering: Implications for the second rise of oxygen
  • A model for the decrease in amplitude of carbon isotope excursions across the Phanerozoic
  • Hypothesized link between Neoproterozoic greening of the land surface and the establishment of an oxygen-rich atmosphere
  • Dynamic model constraints on oxygen-17 depletion in atmospheric O2 after a snowball Earth
  • Efficient transport of fossil organic carbon to the ocean by steep mountain rivers: An orogenic carbon sequestration mechanism
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