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GSA Today, v. 9, no. 8, August 1999
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Table of Contents
Science Article: (View Abstract)
The Late Cretaceous Vertebrate Fauna of Madagascar: Implications for Gondwanan Paleobiogeography
by David W. Krause, Raymond R. Rogers, Catherine A. Forster, Joseph H. Hartman,
Gregory A. Buckley, Scott D. Sampson
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SAGE Remarks: Earth Systems Science: An Interdisciplinary Approach |
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New CEO |
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Washington Report: Meet Charles Groat |
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Exxon Short Course at the 1999 GSA Annual Meeting |
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Call for Papers for 2000 GSA Section and Annual Meetings |
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Rock Stars Preston Cloud |
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Letters |
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Birdsall-Dreiss Distinguished Lecturer for 2000 Announced |
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GSAF Update |
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Student News and Views: The Best Student |
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Bulletin and Geology Contents |
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Call For GSA Short Course Proposals for Future Meeting |
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The Late Cretaceous Vertebrate Fauna of
Madagascar: Implications for Gondwanan Paleobiogeography
David W. Krause, Department
of Anatomical Sciences, State University of New York, Stony Brook, NY 11794
Raymond R. Rogers, Department
of Geology, Macalester College, 1600 Grand Avenue, St. Paul, MN 55105
Catherine A. Forster,
Department of Anatomical Sciences, State University of New York, Stony Brook,
NY 11794
Joseph H. Hartman, Energy
and Environmental Research Center, University of North Dakota, Grand Forks, ND
58202
Gregory A. Buckley, Roosevelt
University, Evelyn T. Stone University College, Chicago, IL 60605
Scott D. Sampson, Utah Museum
of Natural History and Department of Geology and Geophysics, University of Utah,
Salt Lake City, UT 84112
ABSTRACT
A rich, newly discovered assemblage of exquisitely preserved vertebrate fossils
from the Late Cretaceous of Madagascar provides an unparalleled opportunity to
investigate the paleobiogeography of Gondwanan landmasses. Most current plate
tectonic models depict widespread fragmentation of Gondwana prior to the Late
Cretaceous. The discovery of mammals, dinosaurs, and crocodiles in the latest
Cretaceous (Maastrichtian) of Madagascar that are closely related to forms in
India and South America reveals a cosmopolitanism at or near the close of the
Cretaceous that is paradoxical in the context of these models.
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