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U-Pb geochronology of the Deccan Traps and relation to the end-Cretaceous mass extinction

Schoene, Blair, Samperton, Kyle M., Eddy, Michael P., Keller, Gerta, Adatte, Thierry, Bowring, Samuel A., Khadri, Syed F. R., Gertsch, Brian·2015·Science

Abstract

Dating the influence of Deccan Traps eruptions: The Deccan Traps flood basalts in India represent over a million cubic kilometers of erupted lava. These massive eruptions occurred around the same time as the end-Cretaceous mass extinction some 65 million years ago, which famously wiped out all nonavian dinosaurs. Schoene et al. determined the precise timing and duration of the main phase of the eruptions, which lasted over 750,000 years and occurred just 250,000 years before the Cretaceous-Paleogene boundary. The relative contribution of these eruptions and of the Chicxulub impact in Mexico to the mass extinction remains unclear, but both provide potential kill mechanisms. Science , this issue p. 182

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Metadata

Authors
Schoene, B., Samperton, K. M., Eddy, M. P., Keller, G., Adatte, T., Bowring, S. A., Khadri, S. F. R., & Gertsch, B.
Venue
Science
Published
2015-01-09
Volume
347
Issue
6218
Pages
182-184
ISSN
  • 0036-8075
  • 1095-9203
Cited by
443
References
1
Language
en
Funders
  • Office of International Science and Engineering (EAR-0447171, EAR-1026271)
  • Department of Geosciences Scott Fund at Princeton University
  • U.S. NSF

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CoChat. (2026). Citation check: U-Pb geochronology of the Deccan Traps and relation to the end-Cretaceous mass extinction. https://app.cochat.ai/papers/10.1126/science.aaa0118
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Schoene, B., Samperton, K. M., Eddy, M. P., Keller, G., Adatte, T., Bowring, S. A., Khadri, S. F. R., & Gertsch, B. (2015). U-Pb geochronology of the Deccan Traps and relation to the end-Cretaceous mass extinction. Science. https://doi.org/10.1126/science.aaa0118