Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/75871
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Type: Journal article
Title: The Paleocene-Eocene thermal maximum: a perturbation of carbon cycle, climate, and biosphere with implications for the future
Author: McInerney, F.
Wing, S.
Citation: Annual Review of Earth and Planetary Sciences, 2011; 39(1):489-516
Publisher: Annual Reviews
Issue Date: 2011
ISSN: 0084-6597
1545-4495
Statement of
Responsibility: 
Francesca A. McInerney and Scott L. Wing
Abstract: During the Paleocene-Eocene Thermal Maximum (PETM), ~56 Mya, thousands of petagrams of carbon were released into the ocean-atmosphere system with attendant changes in the carbon cycle, climate, ocean chemistry, and marine and continental ecosystems. The period of carbon release is thought to have lasted <20 ka, the duration of the whole event was ~200 ka, and the global temperature increase was 5–8°C. Terrestrial and marine organisms experienced large shifts in geographic ranges, rapid evolution, and changes in trophic ecology, but few groups suffered major extinctions with the exception of benthic foraminifera. The PETM provides valuable insights into the carbon cycle, climate system, and biotic responses to environmental change that are relevant to long-term future global changes.
Keywords: PETM; global warming; paleoclimate; paleoecology; carbon cycle
Rights: © 2011 by Annual Reviews
RMID: 0020122906
DOI: 10.1146/annurev-earth-040610-133431
Appears in Collections:Earth and Environmental Sciences publications
Environment Institute publications

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