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Geology; March 1999; v. 27; no. 3; p. 215-218; DOI: 10.1130/0091-7613(1999)027<0215:LOMEAN>2.3.CO;2
© 1999 Geological Society of America
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Late Ordovician mass extinction: A new perspective from stratigraphic sections in central Nevada

Stanley C. Finney1, William B. N. Berry2, John D. Cooper3, Robert L. Ripperdan4, Walter C. Sweet5, Stephen R. Jacobson5, Azzedine Soufiane6, Aicha Achab6 and Paula J. Noble7

1 Department of Geological Sciences, California State University, Long Beach, California 90840, USA
2 Department of Geology and Geophysics, University of California, Berkeley, California 94720, USA
3 Department of Geological Sciences, California State University, Fullerton, California 92834, USA
4 Department of Geology, University of Puerto Rico, Mayagüez, Puerto Rico 00681
5 Department of Geological Sciences, Ohio State University, Columbus, Ohio 43210, USA
6 Centre Géoscientifique de Québec, Ste-Foy, Québec, G1V 4C7 Canada
7 Department of Geological Sciences, University of Nevada, Reno, Nevada 89557, USA

Integrated sequence stratigraphic, biostratigraphic, and chemostratigraphic analyses of three stratigraphic sections in central Nevada indicate that Late Ordovician glaciation-induced sea-level fall produced diachronous, stepwise faunal turnover in graptolites, conodonts, chitinozoans, and radiolarians, and also triggered a strong, but transient, positive {delta}13C excursion. This pattern is very different from that described for most mass extinction events.




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