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The extinction of the dinosaurs
Authors:Paul M. Barrett  Matthew T. Carrano  David C. Evans  Graeme T. Lloyd  Philip D. Mannion  Mark A. Norell  Daniel J. Peppe  Paul Upchurch  Thomas E. Williamson
Affiliation:1. Department of Earth Sciences, Natural History Museum, London SW7 5BD, U.K.;2. Department of Paleobiology, Smithsonian Institution, Washington, DC 20013, U.S.A.;3. Department of Natural History, Royal Ontario Museum, Toronto, Ontario M5S 2C6, Canada;4. Department of Earth Sciences, University of Oxford, Oxford OX1 3AN, U.K.;5. Department of Earth Science and Engineering, Imperial College London, London SW7 2AZ, U.K.;6. Division of Paleontology, American Museum of Natural History, New York, NY 10024, U.S.A.;7. Department of Geology, Baylor University, Waco, TX 76706, U.S.A.;8. Department of Earth Sciences, University College London, London WC1E 6BT, U.K.;9. New Mexico Museum of Natural History and Science, Albuquerque, NM 87104, U.S.A.
Abstract:Non‐avian dinosaurs went extinct 66 million years ago, geologically coincident with the impact of a large bolide (comet or asteroid) during an interval of massive volcanic eruptions and changes in temperature and sea level. There has long been fervent debate about how these events affected dinosaurs. We review a wealth of new data accumulated over the past two decades, provide updated and novel analyses of long‐term dinosaur diversity trends during the latest Cretaceous, and discuss an emerging consensus on the extinction's tempo and causes. Little support exists for a global, long‐term decline across non‐avian dinosaur diversity prior to their extinction at the end of the Cretaceous. However, restructuring of latest Cretaceous dinosaur faunas in North America led to reduced diversity of large‐bodied herbivores, perhaps making communities more susceptible to cascading extinctions. The abruptness of the dinosaur extinction suggests a key role for the bolide impact, although the coarseness of the fossil record makes testing the effects of Deccan volcanism difficult.
Keywords:dinosaurs  end‐Cretaceous  mass extinction  Cretaceous–  Paleogene  extinctions  macroevolution  Chicxulub impact  Deccan Traps  global change  palaeontology
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