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Mississippian (middle Osagean) ammonoids from the Nada Member of the Borden Formation, Kentucky

Published online by Cambridge University Press:  20 May 2016

David M. Work  and
Charles E. Mason
David M. Work
Affiliation:
Geier Collections and Research Center, Cincinnati Museum Center, 1301 Western Avenue, Cincinnati, Ohio 45203
Charles E. Mason
Affiliation:
Department of Physical Sciences, Morehead State University, Morehead, Kentucky 40351
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Extract

The borden formation in northeastern Kentucky contains a significant, largely undescribed, Osagean (upper Tournaisian to lower Viséan) ammonoid succession. Lower Osagean strata in the Nancy Member contain a diverse Pericyclus Zone assemblage characterized by Muensteroceras oweni (Hall), M. parallelum (Hall), Kazakhstania colubrella (Morton), Imitoceras ixion (Hall), and Masonoceras kentuckiense Work and Manger. This interval, which ranges into the basal Cowbell Member, was referred to the Muensteroceras oweni Assemblage Zone by Gordon and Mason (1985) and Gordon (1986) and indicates correlation to the lower Ivorian Stage of the Belgian Tournaisian succession. The succeeding middle Osagean interval in the middle and upper part of the Cowbell Member contains Merocanites drostei Collinson and Dzhaprakoceras which presumably represent the lower, or Tournaisian (upper Courceyan or lower Chadian), portion of the Fascipericyclus–Ammonellipsites Zone. An even higher middle Osagean assemblage with Polaricyclus bordenensis new species and Winchelloceras allei (Winchell, 1862) occurs in the upper part of the Nada Member, near the top of the Borden Formation, and is the basis for the current report.

Type
Paleontological Notes
Information
Journal of Paleontology , Volume 77 , Issue 3 , May 2003 , pp. 593 - 596
Copyright
Copyright © The Paleontological Society

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References

Chaplin, J. R., Lierman, R. T., and Mason, C. E. 1986. Field guide to the stratigraphy and depositional environments of the Carboniferous (Mississippian and lowermost Pennsylvanian) deposits of northeastern Kentucky; STOP 6: Hilltop Church section, p. 115–128. In Haban, S. M. (ed.), Carboniferous of Eastern Kentucky. Sixth Gondwana Symposium (19–23 August, 1985), Field Excursion 6, Guidebook [Institute of Polar Studies, The Ohio State University, Miscellaneous Publication 228].Google Scholar
Gordon, M. 1957. Mississippian cephalopods of northern and eastern Alaska. United States Geological Survey, Professional Paper, 283, 61 p.Google Scholar
Gordon, M. 1965. Carboniferous cephalopods of Arkansas. United States Geological Survey, Professional Paper, 460, 322 p. (Imprinted 1964)Google Scholar
Gordon, M. 1986. Late Kinderhookian (Early Mississippian) ammonoids of the western United States. Paleontological Society Memoir 19, Journal of Paleontology, 60(3) supplement, 36 p.Google Scholar
Gordon, M., and Mason, C. E. 1985. Progradation of the Borden Formation in Kentucky, U.S.A., demonstrated by successive Early Mississippian (Osagean) ammonoid faunas. Dixième Congrès International de Stratigraphie et de Géologie du Carbonifère, Compte Rendu, 1:191–198.Google Scholar
Hyatt, A. 1884. Genera of fossil cephalopods. Boston Society of Natural History, Proceedings, 22:253–338.Google Scholar
Hyatt, A. 1900. Cephalopods, p. 502–604. In Zittel-Eastman Textbook of Paleontology. I. MacMillan and Co., New York.Google Scholar
Kammer, T. W. 1985. Basinal and prodeltaic communities of the Early Carboniferous Borden Formation in northern Kentucky and southern Indiana (U.S.A.). Palaeogeography, Palaeoclimatology, Palaeoecology, 49:79–121.CrossRefGoogle Scholar
Kusina, L. F. 1971. New and little-known Viséan (Saourian) ammonoids. Paleontologicheskii Zhurnal, 1971(1):37–48. (In Russian)Google Scholar
Lane, H. R. 1974. Mississippian of southeastern New Mexico and West Texas—a wedge-on-wedge relation. American Association of Petroleum Geologists Bulletin, 58:269–282.Google Scholar
Lane, H. R., and Brenckle, P. L. 2001. Type Mississippian subdivisions and biostratigraphic succession, p. 83–107. In Heckel, P. H. (ed.), Stratigraphy and Biostratigraphy of the Mississippian Subsystem (Carboniferous System) in its Type Region, the Mississippi River Valley of Illinois, Missouri, and Iowa. I.U.G.S. Subcommission on Carboniferous Stratigraphy Guidebook for Field Conference, September 8–13, 2001.Google Scholar
Lane, H. R., and Ormiston, A. 1982. Waulsortian Facies, Sacramento Mountains, New Mexico, p. 115–182. In Bolton, K., Lane, H. R., and LeMone, D. V. (eds.), Symposium on the Paleoenvironmental Setting and Distribution of the Waulsortian Facies. El Paso Geological Society and University of Texas at El Paso, International Field Seminar Guide, March 2–6, 1982.Google Scholar
Lane, H. R., Sandberg, C. A., and Ziegler, W. 1980. Taxonomy and phylogeny of some Lower Carboniferous conodonts and preliminary standard post-Siphonodella zonation. Geologica et Palaeontologica, 14:117–164.Google Scholar
Miller, A. K., and Garner, H. F. 1955. Lower Mississippian cephalopods of Michigan, Pt. III, Ammonoids and summary. Contributions from the Museum of Paleontology, The University of Michigan, 12(8):113–173.Google Scholar
Riley, N. J. 1991. A global review of mid-Dinantian ammonoid biostratigraphy, p. 133–143. In Brenckle, P. L. and Manger, W. L. (eds.), Intercontinental Correlation and Division of the Carboniferous System. Courier Forschungsinstitut Senckenberg, 130. (Imprinted 1990)Google Scholar
Ruzhencev, V. E. 1965. Principal ammonoid assemblages of the Carboniferous. International Geology Review, 8:48–59.CrossRefGoogle Scholar
Smith, J. P. 1903. Carboniferous ammonoids of America. United States Geological Survey, Monograph 42, 211 p.Google Scholar
Wedekind, R. 1918. Die Genera der Palaeoammonoidea (Goniatiten). Mit Ausschluss der Mimoceratidae, Glyphioceratidae und Prolecanitidae. Palaeontographica, 62:85–184.Google Scholar
Weyer, D. 1972. Zum Alter der Ammonoideen-Faunen des Marshall-Sandsteins (Unterkarbon; Michigan, USA). Deutsche Gesellschaft für Geologische Wissenschaften Berichte, Reihe A, Geologie und Paläontologie, 17:325–350.Google Scholar
Winchell, A. 1862. Notice of the rocks lying between the Carboniferous Limestone of the lower peninsula of Michigan and the limestones of the Hamilton Group, with descriptions of some cephalopods supposed to be new to science. American Journal of Science and Arts, Series 2, 33:352–366.Google Scholar
Winchell, A. 1865. Descriptions of new species of fossils from the Marshall Group of Michigan and its supposed equivalents in other states, with notes on some fossils of the same age previously described. Proceedings of the Philadelphia Academy of Natural Sciences, 1865, p. 109–133.Google Scholar
Winchell, A. 1870. Notices and descriptions of fossils from the Marshall Group of the western states, with notes on fossils from other formations. Proceedings of the American Philosophical Society, 11:245–260.Google Scholar
Work, D. M., Nassichuk, W. W., and Richards, B. C. 2000. Lower Viséan ammonoids from the lower Mount Head Formation, east-central British Columbia. Geological Survey of Canada, Bulletin 541, 71 p.CrossRefGoogle Scholar