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New occurrence of Periastron reticulatum Unger emend. Beck, an enigmatic Mississippian fossil plant

Published online by Cambridge University Press:  20 May 2016

Robert A. Gastaldo
Robert A. Gastaldo*
Affiliation:
Department of Geology, Auburn University, Auburn, Alabama 36849-5305
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Abstract

Two new specimens of Periastron reticulatum Unger emend. Beck have been collected from the Erin Slate, Talladega Slate Belt, southern Appalachians. Preserved anatomical features provide a basis for an expanded understanding of the genus and provide a biostratigraphic basis for dating the uppermost unit of the Talladega Slate Belt.

Type
Research Article
Information
Journal of Paleontology , Volume 69 , Issue 2 , March 1995 , pp. 388 - 392
Copyright
Copyright © The Paleontological Society 

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References

Beck, C. B. 1978. Periastron reticulatum Unger and Aerocortex kentuckiensis, N. gen. et sp., from the New Albany Shale of Kentucky. American Journal of Botany, 65:221–235.Google Scholar
Bertrand, P., Böhm, R., and Corsin, P. 1935. Découverte d'une flore dans les Lydiennes du Carbonifére de la Montagne-Noire a Saint-Nazaire-de-Laderez (Hérault). Compte Rendu Academie Science Paris, 200:1344–1345.Google Scholar
Böhm, R. 1935. Etude sur la flore de l'horizon a Lydiennes de la base du Caronifére de la Montagne Noire. Imprimerie de la Charité, Montpellier, p. 1–29.Google Scholar
Galtier, J., Meyer-Berthaud, B., and Rowe, N. 1988. Tournaisian plants from the “Lydiennes” Formation of the Montagne Noire (France). Courier Forschung Institut Senckenberg, 100:109–117.Google Scholar
Gastaldo, R. A., and Cook, R. B. 1982. A reinvestigation of the paleobotanical evidence for the age of the Erin Shale, p. 69–78. In Bearce, D. N., Black, W. W., Kish, S. A., and Tull, J. F. (eds.), Tectonic Studies in the Talladega and Carolina Slate Belts, Southern Appalachian Orogen. Geological Society of America, Special Paper 191.Google Scholar
Gastaldo, R. A., Steltenpohl, M. G., and Guthrie, G. 1993. Mississippian fossils from southern Appalachian metamorphic rocks and their implications for late Paleozoic tectonic evolution. Science, 256(5134):732–734.CrossRefGoogle Scholar
Read, C. B. 1936. A Devonian flora from Kentucky. Journal of Paleontology, 10:215–227.Google Scholar
Scott, D. H., and Jeffrey, E. C. 1914. On fossil plants, showing structure, from the base of the Waverley Shale of Kentucky. Philosophical Transactions Royal Society of London, 205B:315–373.Google Scholar
Tull, J. F., Harris, A. G., Repetski, J. E., McKinney, F. K., Garrett, C. B., and Bearce, D. N. 1988. New paleontologic evidence constraining the age and paleotectonic setting of the Talladega slate belt, southern Appalachians. Geological Society of America Bulletin, 100:1291–1299.Google Scholar
Unger, F. 1856. Zweiter Theil. Schiefer und Sandsteinflora, p. 139–186. In Richter, R. and Unger, F. (eds.); Beitrag zur Paläontologie des Thüringer Waldes. Denkschrift Kaiser Akademie Wissenschaft Wien, 11.Google Scholar