This article requires a subscription to view the full text. If you have a subscription you may use the login form below to view the article. Access to this article can also be purchased.
Log in using your username and password
Purchase access
You may purchase access to this article. This will require you to create an account if you don't already have one.
In this issue
The Weathering of Sedimentary Organic Matter as a Control on Atmospheric O2: II. Theoretical Modeling
Jump to section
Related Articles
Cited By...
- Petrographic carbon in ancient sediments constrains Proterozoic Era atmospheric oxygen levels
- Carbon cycle evolution before and after the Great Oxidation of the atmosphere
- Deep abiotic weathering of pyrite
- 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