Canfield ocean: Difference between revisions
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[[Ocean anoxia]] |
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[[Mass extinction]] |
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[[Permian-Triassic extinction event]] |
*[[Permian-Triassic extinction event]] |
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==References== |
==References== |
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Revision as of 18:27, 24 August 2012
The Canfield Ocean refers to the Ocean composition theorized by geologist Donald Canfield. In a seminal paper in Nature in 1998, Canfield argued that the Ocean had become partially oxic and sulfidic, causing mass extinction.[1][2]
See also
References
- ^ Canfield, D.E. (1998). "A new model for Proterozoic ocean chemistry". Nature. 396: 450–453. doi:10.1038/24839. Retrieved 2011-12-01.
- ^ Buick, R. (2007). "Did the Proterozoic 'Canfield Ocean'cause a laughing gas greenhouse?". Geobiology. 5.2: 97–100. doi:10.1111/j.1472-4669.2007.00110.x.
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