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Journal of Paleontology; January 2009; v. 83; no. 1; p. 70-79; DOI: 10.1666/08-058R.1
© 2009 Paleontological Society
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ARTICLE

Protosalvinia Dawson and Associated Conodonts of the Upper Trachytera Zone, Famennian, Upper Devonian, in the Eastern United States

D. Jeffrey Over1, Remus Lazar2, Gordon C. Baird3, Juergen Schieber4 and Frank R. Ettensohn5

1 Department of Geological Sciences, State University of New York College at Geneseo, Geneseo, 14454, <over{at}geneseo.edu>
2 Exxonmobil Upstream Research Co., Houston, Texas 77027
3 Department of Geological Sciences, State University of New York College at Fredonia, Fredonia, 14063
4 Department of Geological Sciences, Indiana University, Bloomington, 47405
5 Department of Earth and Environmental Sciences, University of Kentucky, Lexington, 40506

Protosalvinia first occur in association with conodonts of the Upper trachytera Zone and below the Three Lick Bed in the Ohio Shale and the Ellicott Shale of the central and northern Appalachian Basin, as well as in the Clegg Creek Member of the New Albany Shale of the Illinois Basin. In the Chattanooga Shale of the southern Appalachian Basin, Protosalvinia are found no lower than the Upper marginifera Zone or associated with obviously reworked conodonts in the Middle expansa Zone. Regionally Protosalvinia are associated with a disconformity and may be found with conodonts of the Lower expansa Zone.




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[Abstract] [Full Text] [PDF]


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