Hostname: page-component-78c5997874-94fs2 Total loading time: 0 Render date: 2024-11-19T12:09:00.368Z Has data issue: false hasContentIssue false

Upper Devonian (Frasnian) rugose corals from New York State

Published online by Cambridge University Press:  14 July 2015

James E. Sorauf*
Affiliation:
State University of New York, Binghamton 13901

Abstract

West Falls Group strata (Chemung facies) of Upper Devonian (Frasnian) age in New York State reflect sedimentation on a storm dominated sandy shelf. Rugose corals occur in storm deposited coquinites rich in bioclastic debris and are abundant locally, although representing only three species, Tabulophyllum orientale (Stumm), Macgeea ponderosa Stumm, and Disphyllum caespitosum (Goldfuss). The Tabulophyllum and Macgeea species are both characterized by large amounts of stereome (biogenic calcite) in the apical part of the corallite, perhaps useful in stabilizing corallites in the sediment.

Type
Research Article
Copyright
Copyright © The Paleontological Society 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Birenheide, R. 1969. Typen mittel- und oberdevonischer Rugosa aus der Sammlung Goldfuss. Senckenbergiana Lethaea, 50:3755.Google Scholar
Birenheide, R. 1978. Rugose Korallen des Devon. Leitfossilien, No. 2. Gebruder Borntraeger, Berlin, 265 p.Google Scholar
Coen-Aubert, M. 1982. Rugueux solitaires du Frasnien de la Belgique. Bulletin Institut Royale des Sciences Naturelles de la Belgique, 54:165.Google Scholar
Ehrenberg, C. G. 1834. Die Corallenthiere des Rothen Meeres, physiologisch und systematisch Verzeichnet. Berlin, 156 p.Google Scholar
Fenton, C. L., and Fenton, M. A. 1924. The Stratigraphy and Fauna of the Hackberry Stage of the Upper Devonian. Museum of Geology, University of Michigan, Contributions, 1, 260 p.Google Scholar
Goldfuss, G. A. 1826. Petrefacta Germaniae. Leipzig, 252 p.Google Scholar
Hall, J., and Whitfield, R. P. 1873. Description of new species of fossils from the Devonian rocks of Iowa. New York State Cabinet of Natural History, Annual Report, 22:223239.Google Scholar
Hill, D. 1981. Part F, Coelenterata, Supplement 1, Rugosa and Tabulata. Treatise on Invertebrate Paleontology. The Geological Society of America and The University of Kansas Press, Lawrence, 762 p.Google Scholar
Hill, D., and Jell, J. S. 1970. Devonian corals from the Canning Basin, western Australia. Geological Survey of Western Australia, Bulletins, 121, 158 p.Google Scholar
Jell, J. S. 1969. Septal microstructure and classification of the Phillipsastraeidae, p. 5073. In Campbell, K. S. W. (ed.), Stratigraphy and Palaeontology: Essays in Honour of Dorothy Hill. Australian National University Press, Canberra.Google Scholar
Lang, W. D., and Smith, S. 1935. Cyathophyllum caespitosum Goldfuss and other Devonian corals considered in a revision of that species. Quarterly Journal of the Geological Society, 91:538590.CrossRefGoogle Scholar
Middleton, G. V. 1959. Devonian tetracorals from south Devonshire, England. Journal of Paleontology, 33:138160.Google Scholar
Pickett, J. 1967. Untersuchungen zur Phillips-astreidae (Zoantheria: Rugosa). Senckenbergiana Lethaea, 48:189.Google Scholar
Pickett, J. 1969. Comments on the proposed suppression of Pterorhiza Ehrenberg, 1834 (Anthozoa). Z.N.(S.) 1851. Bulletin of Zoological Nomenclature, 26:70.Google Scholar
Rickard, L. V. 1975. Correlation of the Silurian and Devonian rocks in New York State. New York State Museum Map and Chart Series, No. 24.Google Scholar
Rozkowska, M. 1956. Pachyphyllinae from the Middle Devonian of the Holy Cross Mountains. Acta Palaeontologica Polonica, 1:271330.Google Scholar
Rozkowska, M. 1979. Contribution to the Frasnian tetracorals from Poland. Palaeontologica Polonica, 40, 56 p.Google Scholar
Rozkowska, M., and Fedorowski, J. 1972. Genus Disphyllum de Fromentel (Rugosa) in the Devonian of Poland and its distribution. Acta Palaeontologica Polonica, 17:265340.Google Scholar
Semenoff-Tian-Chansky, P. 1974. Recherches sur les Tetracoralliares du Carbonifère du Sahara occidental. Museum Nationale Histoire Naturelle, Mémoires, 21, 316 p.Google Scholar
Semenoff-Tian-Chansky, P., Lafuste, J., and Durand Delga, M. 1961. Madréporaires du Devonien du Chenoua (Algérie). Bulletin de la Société geologique de France, 7 série, 3:290319.Google Scholar
Sloss, L. L. 1939. Devonian rugose corals from the Traverse beds of Michigan. Journal of Paleontology, 13:5273.Google Scholar
Sorauf, J. E. 1978. Upper Devonian Pachyphyllum (rugose coral) from New York State. Journal of Paleontology, 52:818829.Google Scholar
Sorauf, J. E., and Podoff, Nedda. 1977. Skeletal structure in deep water ahermatypic corals. Second Symposium international sur les coraux et recifs coralliens fossiles, Paris, Septembre, 1975. Mémoires du Bureau de Recherches Geologiques et Minières, Nr. 89:211.Google Scholar
Stoll, N. R., et al. 1961. International Code of Zoological Nomenclature adopted by the XV International Congress of Zoology. International Trust for Zoological Nomenclature, London, 176 p.Google Scholar
Stumm, E. C. 1937. The lower Middle Devonian tetracorals of the Nevada Limestone. Journal of Paleontology, 11:423443.Google Scholar
Stumm, E. C. 1960. New rugose corals from the Middle and Upper Devonian of New York. Journal of Paleontology, 34:161163.Google Scholar
Tsien, H. H. 1970. Espèces du genre Disphyllum (Rugosa) dans le Devonien Moyen et le Frasnien de la Belgique. Annales de la Société Geologique de Belgique, 93:159182.Google Scholar
Walther, C. 1928. Untersuchungen über die Mitteldevon–Oberdevongrenze. Deutsche Geologische Gesellschaft, Zeitschrift, 80:97152.Google Scholar
Yoh, S. S. 1937. Die Korallenfauna des Mitteldevons aus der Provinz Kwangsi, Sudchina. Palaeontographica, Abteilung A., 87:4576.Google Scholar