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Conodont biostratigraphy and depositional history of strata comprising the Niagaran sequence (Silurian) in the northern part of the Cincinnati Arch region, west-central Ohio, and evolution of Kockelella walliseri (Helfrich)

Published online by Cambridge University Press:  20 May 2016

Mark A. Kleffner
Mark A. Kleffner*
Affiliation:
Department of Geological Sciences, The Ohio State University at Lima, Lima 45804
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Abstract

The Dayton, Osgood, and Laurel Formations and the Euphemia, Springfield, and basal part of the Cedarville Dolomites near the axis of the Cincinnati Arch in northeast Preble County, Ohio, belong in the uppermost part of the Ozarkodina sagitta rhenana to lower part of the Ozarkodina? crassa Chronozone and are late early to middle Wenlockian in age. The Dayton–Cedarville succession on the eastern flank of the Cincinnati Arch in north-central Greene County, Ohio, belongs in the uppermost part of the Pterospathodus celloni to upper part of the Ancoradella ploeckensis Chronozone and is late Llandoverian to early middle Ludlovian in age.

The sea transgressed across the exposed and eroded Brassfield Formation to begin deposition of the Dayton Formation on the eastern flank of the Cincinnati Arch in Greene County, Ohio, during the late Llandoverian and completely flooded all of west-central Ohio by the late early Wenlockian. The region remained covered by a sea of fluctuating depth during deposition of the Dayton Formation–Cedarville Dolomite succession from the Wenlockian through early middle Ludlovian.

Kockelella walliseri (Helfrich) evolved from K. ranuliformis (Walliser) during the middle Wenlockian (upper part of Ozarkodina sagitta rhenana Chronozone) by development of a lateral process adjacent to the cusp on the Pa element and by minor modification of the Pb element and some of the ramiform elements. Specimens from upper Llandoverian and lower Wenlockian strata previously assigned to K. walliseri belong to a different species, Kockelella sp. A Fordham, 1991. The evolutionary trends in the K. walliseri lineage, progressive restriction of the basal cavity and increasing development of the length of the lateral processes in the Pa element, parallel the trends in the K. amsdeni–K. stauros–K. variabilis lineage and resulted in the divergence of Kockelella cf. K. stauros Bischoff, 1986, from the main lineage in the middle Wenlockian.

Type
Research Article
Information
Journal of Paleontology , Volume 68 , Issue 1 , January 1994 , pp. 141 - 153
Copyright
Copyright © The Paleontological Society 

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References

Aldridge, R. J. 1975. The stratigraphic distribution of conodonts in the British Silurian. Journal of the Geological Society, 131:607–618.Google Scholar
Aldridge, R. J. 1985. Conodonts of the Silurian System from the British Isles, p. 68–92. In Higgins, A. C. and Austin, R. L. (eds.), A Stratigraphical Index of Conodonts. Ellis Horwood Limited, Chichester, England.Google Scholar
Aldridge, R. J., Dorning, K. J., and Siveter, D. J. 1981. Distribution of microfossil groups across the Wenlock Shelf of the Welsh Basin, p. 18–30. In Neale, J. W. and Brasier, M. D. (eds.), Microfossils from Recent and Fossil Shelf Seas. Ellis Horwood Limited, Chichester, England.Google Scholar
Aldridge, R. J., and Mabillard, J. E. 1981. Local variations in the distribution of Silurian conodonts: an example from the amorphognathoides interval of the Welsh Basin, p. 10–17. In Neale, J. W. and Brasier, M. D. (eds.), Microfossils from Recent and Fossil Shelf Seas. Ellis Horwood Limited, Chichester, England.Google Scholar
Aldridge, R. J., and Schönlaub, H.-P. 1989. Conodonts, p. 274–279. In Holland, C. H. and Bassett, M. G. (eds.), A Global Standard for the Silurian System. National Museum of Wales, Geological Series No. 9, Cardiff.Google Scholar
Ausich, W. I. 1987. John Bryan State Park, Ohio: Silurian stratigraphy, p. 419–422. In Biggs, D. L. (ed.), DNAG Centennial Field Guides, North-Central Section. Geological Society of America, Boulder, Colorado.Google Scholar
Barrick, J. E. 1983. Wenlockian (Silurian) conodont biostratigraphy, biofacies, and carbonate lithofacies, Wayne Formation, central Tennessee. Journal of Paleontology, 57:208–239.Google Scholar
Barrick, J. E., and Klapper, G. 1976. Multielement Silurian (late Llandoverian–Wenlockian) conodonts of the Clarita Formation, Arbuckle Mountains, and phylogeny of Kockelella. Geologica et Palaeontologica, 10:59–100.Google Scholar
Berry, W. B. N., and Boucot, A. J. 1970. Correlation of the North American Silurian rocks. Geological Society of America, Special Paper 102, 289 p.Google Scholar
Berry, W. B. N., and Murphy, M. 1975. Silurian and Devonian graptolites of central Nevada. University of California Publications in Geological Sciences 110, 109 p.Google Scholar
Bischoff, G. C. O. 1986. Early and Middle Silurian conodonts from midwestern New South Wales. Courier Forschungsinstitut Senckenberg, 89, 337 p.Google Scholar
Busch, D. A. 1939. The stratigraphy and paleontology of the Niagaran strata of west-central Ohio and adjacent northern Indiana. Unpubl. Ph.D. dissertation, The Ohio State University, Columbus, 233 p.Google Scholar
Cooper, B. J. 1980. Toward an improved Silurian conodont biostratigraphy. Lethaia, 13:209–227.Google Scholar
Droste, J. B., and Shaver, R. H. 1983. Atlas of early and middle Paleozoic paleogeography of the southern Great Lakes area. Indiana Geological Survey Special Report, 32, 32 p.Google Scholar
Dzik, J. 1976. Remarks on the evolution of Ordovician conodonts. Acta Palaeontologica Polonica, 21:395–455.Google Scholar
Foerste, A. F. 1935. Correlation of the Silurian formations in southwestern Ohio, southeastern Indiana, Kentucky, and western Tennessee. Bulletin of the Scientific Laboratories of Denison University, 30:119–205.Google Scholar
Fordham, B. 1991. A literature-based phylogeny and classification of Silurian conodonts. Palaeontographica, Abt. A, 217, 136 p.Google Scholar
Gnoli, M., Leone, F., Olivieri, R., and Serpagli, E. 1988. The Mason Porcus section as reference section for uppermost Silurian–Lower Devonian in SW Sardinia. Bullettino della Societa Paleontologica Italiana, 27:323–334.Google Scholar
Helfrich, C. T. 1975. Silurian Conodonts from Wills Mountain Anticline, Virginia, West Virginia, and Maryland. Geological Society of America, Special Paper 161, 82 p.Google Scholar
Helfrich, C. T. 1980. Late Llandovery–early Wenlock conodonts from the upper part of the Rose Hill and the basal part of the Mifflintown Formations, Virginia, West Virginia, and Maryland. Journal of Paleontology, 54 557–569.Google Scholar
Horvath, A. L., and Sparling, D. 1967. Silurian geology of western Ohio: guide to the 42nd Annual Field Conference of the Section of Geology of the Ohio Academy of Science. University of Dayton, Dayton, 25 p.Google Scholar
Jeppsson, L. 1983. Silurian conodont faunas from Gotland. Fossils and Strata, 15:121–144.Google Scholar
Kahle, C. 1988. Surface and subsurface paleokarst, Silurian Lockport and Peebles Dolomites, western Ohio, p. 229–255. In James, N. P. and Choquette, P. W. (eds.), Paleokarst. Springer-Verlag, Inc., New York.Google Scholar
Klapper, G. 1981a. Family Kockelellidae, p. W157. In Robison, R. A. (ed.), Treatise on Invertebrate Paleontology, Part W Miscellanea Supplement 2, Conodonta. The Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Klapper, G. 1981b. Kockelella ranuliformis, p. 171–173. In Ziegler, W. (ed.), Catalogue of Conodonts–Volume IV. E. Schweizerbart'sche Verlagsbuchhandlung, Stuttgart.Google Scholar
Klapper, G. 1981c. Kockelella walliseri, p. 187–189. In Ziegler, W. (ed.), Catalogue of Conodonts–Volume IV. E. Schweizerbart'sche Verlagsbuchhandlung, Stuttgart.Google Scholar
Klapper, G., and Murphy, M. A. 1975. Silurian–Lower Devonian conodont sequence in the Roberts Mountain Formation of central Nevada. University of California Publications in Geological Sciences, 111, 62 p.Google Scholar
Kleffner, M. A. 1985. Conodont biostratigraphy of the Stray “Clinton” and “Packer Shell” (Silurian, Ohio subsurface) and its bearing on correlation, p. 219–231. In Gray, J., Maslowski, A., McCullough, W., and Shafer, W. E. (eds.), The New Clinton Collection—1985. Ohio Geological Society, Columbus.Google Scholar
Kleffner, M. A. 1986. Silurian (Llandovery–Ludlow) conodont biostratigraphy of west-central Ohio and its bearing on correlation. Geological Society of America, Abstracts with Programs, 18:250.Google Scholar
Kleffner, M. A. 1987. Conodonts of the Estill Shale and Bisher Formation (Silurian, southern Ohio): biostratigraphy and distribution. Ohio Journal of Science, 87:78–89.Google Scholar
Kleffner, M. A. 1988. Taxonomy and biostratigraphic significance of Wenlockian and Ludlovian (Silurian) conodonts in the midcontinent outcrop area, North America. Unpubl. Ph.D. dissertation, The Ohio State University, Columbus, 251 p.Google Scholar
Kleffner, M. A. 1989. A conodont-based Silurian chronostratigraphy. Geological Society of America Bulletin, 101:904–912.Google Scholar
Kleffner, M. A. 1990. Wenlockian (Silurian) conodont biostratigraphy, depositional environments, and depositional history along the eastern flank of the Cincinnati Arch in southern Ohio. Journal of Paleontology, 64:319–328.Google Scholar
Kleffner, M. A. 1991. Conodont biostratigraphy of the upper part of the Clinton Group and the Lockport Group (Silurian) in the Niagara Gorge region, New York and Ontario. Journal of Paleontology, 65:500–511.Google Scholar
Kleffner, M. A. 1992. Recognition of the Wenlock/Ludlow boundary in regions with and without graptolite-bearing strata. Geological Society of America, Abstracts with Programs, 24:26.Google Scholar
Kleffner, M. A., and Ausich, W. I. 1988. Lower and Middle Silurian of the eastern flank of the Cincinnati Arch and the Appalachian Basin margin, Ohio. Field Trip 1, Society of economic Paleontologists and Mineralogists, Fifth Midyear Meeting, Columbus, Ohio, August, 1988, 25 p.Google Scholar
Kovach, J. 1974. Stratigraphy and paleontology of the pentamerid brachiopods of the Niagaran rocks of western Ohio and eastern Indiana. Unpubl. Ph.D. dissertation, The Ohio State University, Columbus, 366 p.Google Scholar
Niooll, R. S., and Rexroad, C. B. 1969. Stratigraphy and conodont paleontology of the Salamonie Dolomite and Lee Creek Member of the Brassfield Limestone (Silurian) in southeastern Indiana and adjacent Kentucky. Indiana Geological Survey Bulletin 40, 73 p.Google Scholar
Nowlan, G. S. 1983. Early Silurian conodonts of eastern Canada. Fossils and Strata, 15:95–110.Google Scholar
Over, J. D., and Chatterton, B. D. E. 1987. Silurian conodonts from the southern Mackenzie Mountains, Northwest Territories, Canada. Geologica et Palaeontologica, 21:1–49.Google Scholar
Savage, N. M. 1985. Silurian (Llandovery–Wenlock) conodonts from the base of the Heceta Limestone, southeastern Alaska. Canadian Journal of Earth Sciences, 22:711–727.Google Scholar
Shaw, A. B. 1964. Time in Stratigraphy. McGraw-Hill, New York, 365 p.Google Scholar
Sweet, W. C. 1988. The Conodonta: Morphology, Taxonomy, Paleoecology, and Evolutionary History of a Long-Extinct Animal Phylum. Oxford University Press, New York, 212 p.Google Scholar
Uyeno, T. T., and Barnes, C. R. 1983. Conodonts of the Jupiter and Chicotte Formations (Lower Silurian), Anticosti Island, Quebec. Geological Survey of Canada Bulletin 355, 49 p.Google Scholar
Walliser, O. H. 1957. Conodonten aus dem oberen Gotlandium Deutschlands und der Karnischen Alpen. Notizblatt des hessischen Landesamtes für Bodenforschung zu Wiesbaden, 85:28–52.Google Scholar
Walliser, O. H. 1964. Conodonten des Silurs. Abhandlungen des Hessisches Landesamt für Bodenforschung, Wiesbaden, No. 41, 106 p.Google Scholar