Difference between revisions of "Paleocene-Eocene Thermal Maximum"
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Revision as of 08:34, 21 April 2008
Paleocene-Eocene Thermal Maximum
The Paleocene–Eocene Thermal Maximum was a 'blip' in the smooth running of Earth's environment and climate that took place about 55 million years ago.
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- Zachos JC et al. (2005) Rapid Acidification of the Ocean During the Paleocene-Eocene Thermal Maximum. Science, 308: 1611-1615.
- Zeebe RE & Zachos JC (2007) Reversed deep-sea carbonate ion basin gradient during Paleocene-Eocene thermal maximum. Paleoceanography, 22: PA3201, doi:10.1029/2006PA001395.