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Chemostratigraphic Evidence of Deccan Volcanism from the Marine Osmium Isotope Record

Ravizza, G., Peucker-Ehrenbrink, B.·2003·Science
DOI 10.1126/science.1089209
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Abstract

Continental flood basalt (CFB) volcanism is hypothesized to have played a causative role in global climate change and mass extinctions. Uncertainties associated with radiometric dating preclude a clear chronological assessment of the environmental consequences of CFB volcanism. Our results document a 25% decline in the marine 187 Os/ 188 Os record that predates the Cretaceous-Tertiary boundary (KTB) and coincides with late Maastrichtian warming. We argue that this decline provides a chemostratigraphic marker of Deccan volcanism and thus constitutes compelling evidence that the main environmental consequence of Deccan volcanism was a transient global warming event of 3° to 5°C that is fully resolved from the KTB mass extinction.

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Metadata

Authors
Ravizza, G., & Peucker-Ehrenbrink, B.
Affiliations
Department of Geology and Geophysics, University of Hawaii, Honolulu, HI 96822–2225, USA.
Venue
Science
Publisher
American Association for the Advancement of Science (AAAS)
Published
2003-11-21
Volume
302
Issue
5649
Pages
1392-1395
ISSN
  • 0036-8075
  • 1095-9203
DOI
10.1126/science.1089209
Cited by
156
References
1
Language
en

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