Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extincti...
Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extinction
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Publisher
United States: The American Association for the Advancement of Science
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Language
English
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Publisher
United States: The American Association for the Advancement of Science
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Scope and Contents
Contents
Rapid climate change at the end of the Permian Period (~252 million years ago) is the hypothesized trigger for the largest mass extinction in Earth's history. We present model simulations of the Permian/Triassic climate transition that reproduce the ocean warming and oxygen (O
) loss indicated by the geologic record. The effect of these changes...
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Full title
Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extinction
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TN_cdi_proquest_miscellaneous_2155927330
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_2155927330
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ISSN
0036-8075
E-ISSN
1095-9203
DOI
10.1126/science.aat1327
