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Crinoid assemblages from the Fort Payne Formation (late Osagean, early Viséan, Mississippian) from Kentucky, Tennessee, and Alabama

Published online by Cambridge University Press:  14 July 2015

Elyssa B. Krivicich ,
William I. Ausich  and
David L. Meyer
Elyssa B. Krivicich
Affiliation:
School of Earth Sciences, 125 South Oval Mall, The Ohio State University, Columbus, OH 43210, USA, ;
William I. Ausich
Affiliation:
School of Earth Sciences, 125 South Oval Mall, The Ohio State University, Columbus, OH 43210, USA, ;
David L. Meyer
Affiliation:
Department of Geology, University of Cincinnati, Cincinnati, OH 45221, USA,
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Abstract

The Mississippian Fort Payne Formation of Kentucky, Tennessee, and Alabama is well known for its abundant crinoids and a diverse array of autochthonous and allochthonous carbonate and siliciclastic facies. Using Principal Coordinate Analysis and Non-Metric Multidimensional Scaling, it is demonstrated that distinct, contemporaneous, and geographically adjacent autochthonous facies in south-central Kentucky supported distinct crinoid assemblages. The two carbonate buildup facies had different assemblages dominated by camerate crinoids, carbonate channel-fill deposits were dominated by advanced cladid crinoids and the camerate Elegantocrinus hemisphaericus, and green shale facies supported a fauna dominated by disparids and primitive cladid crinoids. Allochthonous facies contain neither distinctive nor exotic taxa. Thus, these transported assemblages are considered a mixture of elements from the recognized, autochthonous facies. Faunal assemblages from Dale Hollow Reservoir are allochthonous; and faunas in north-central Alabama and south-central Tennessee are different from others, which may reflect slight biogeographic distinctions.

Type
Research Article
Information
Journal of Paleontology , Volume 88 , Issue 6 , November 2014 , pp. 1154 - 1162
Copyright
Copyright © The Paleontological Society 

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References

Ausich, W. I. 1980. A model for niche differentiation in Lower Mississippian crinoid communities. Journal of Paleontology, 54:273–288.Google Scholar
Ausich, W. I. 1983. Component concept for the study of paleocommunities with an example from the Early Carboniferous of southern Indiana. Palaeogeography, Palaeoclimatology, Palaeoecology, 44:251–282.Google Scholar
Ausich, W. I. and Baumiller, T. K. 1993. Method for determining muscular articulations in fossil crinoids. PALAIOS, 8:477–484.Google Scholar
Ausich, W. I. and Kammer, T. W. 1990. Systematics and phylogeny of the late Osagean and Meramecian crinoids Platycrinites and Eucladocrinus from the Mississippian stratotype region. Journal of Paleontology, 64:759–778.Google Scholar
Ausich, W. I. and Kammer, T. W. 1991a. Systematic revisions to Aorocrinus, Dorycrinus, Macrocrinus, Paradichocrinus, Strotocrinus, and Uperocrinus: Mississippian camerate crinoids from the stratotype region (Echinodermata). Journal of Paleontology, 65:936–944.Google Scholar
Ausich, W. I. and Kammer, T. W. 1991b. Late Osagean and Meramecian Actinocrinites from the Mississippian stratotype region (Echinodermata: Crinoidea). Journal of Paleontology, 65:485–499.Google Scholar
Ausich, W. I. and Kammer, T. W. 1992. Dizygocrinus: Mississippian camerate crinoid from the midcontinental United States (Echinodermata). Journal of Paleontology, 66:637–658.CrossRefGoogle Scholar
Ausich, W. I. and Kammer, T. W. 2008. Generic concepts in the Amphoracrinidae Bather, 1899 (Class Crinoidea) and evaluation of generic assignments of North American species. Journal of Paleontology, 82:1130–1149.CrossRefGoogle Scholar
Ausich, W. I. and Kammer, T. W. 2009. Generic concepts in the Platycrinitidae Austin and Austin (Class Crinoidea). Journal of Paleontology, 83:694–717.Google Scholar
Ausich, W. I. and Kammer, T. W. 2010. Generic concepts in the Batocrinidae Wachsmuth and Springer, 1881 (Class Crinoidea). Journal of Paleontology, 84:32–50.Google Scholar
Ausich, W. I. and Lane, N. G. 1985. Crinoid assemblages and geographic endemism in the Lower Mississippian (Carboniferous) crinoids of the continental interior, p. 216–224. In Dutro, J. T. Jr. and Pfefferkorn, H. W. (eds.), Neuvième Congres International de Stratigraphie et de Gèologie du Carbonifère, Compte Rendu, vol. 5: Paleontology, Paleoecology, Paleogeography.Google Scholar
Ausich, W. I. and Meyer, D. L. 1990. Origin and composition of carbonate buildups and associated facie in the Fort Payne Formation (Lower Mississippian, south- central Kentucky): An integrated sedimentologic and paleoecologic analysis. Geological Society of America Bulletin, 102:129–146.2.3.CO;2>CrossRefGoogle Scholar
Ausich, W. I. and Meyer, D. L. 1992. Crinoidea Flexibilia (Echinodermata) from the Fort Payne Formation (Lower Mississippian; Kentucky and Tennessee). Journal of Paleontology, 66:825–838.Google Scholar
Ausich, W. I., Goldstein, A., and Yates, R. 2000. Crinoids from the Muldraugh Member of the Borden Formation in north-central Kentucky (Echinodermata, Lower Mississippian). Journal of Paleontology, 74:1072–1082.Google Scholar
Ausich, W. I., Kammer, T. W., and Lane, N. G. 1979. Fossil communities of the Borden (Mississippian) delta in Indiana and northern Kentucky. Journal of Paleontology, 53:1182–1196.Google Scholar
Ausich, W. I., Kammer, T. W., and Meyer, D. L. 1997. Middle Mississippian disparid crinoids from the east-central United States. Journal of Paleontology, 71:131–148.CrossRefGoogle Scholar
Chowns, T. M. and Elkins, J. E. 1974. The origin of quartz geodes and cauliflower cherts through the silicification of anhydrite nodules. Journal of Sedimentary Petrology, 44:885–903.Google Scholar
Greb, S. F., Potter, P. E., Meyer, D. L., and Ausich, W. I. 2008. Mud mounds, paleoslumps, crinoids, and more; the geology of the Fort Payne Formation at Lake Cumberland, south-central Kentucky: Field trip for the Kentucky Chapter of the American Institute of Professional Geologists. Kentucky Geological Survey Online Publication, <http://www.ky.aipg.org/GUIDEBOOKS/2008%20Guidebook.pdf>..>Google Scholar
Hammer, Ø., Harper, D. A. T., and Ryan, P. D. 2001. PAST: Paleontological Statistics Software Package for Education and Data Analysis: Palaeontologia Electronica, v. 4, no. 1, 178 kb, <http://palaeo-electronica.org/20011/past/issue101.html>..>Google Scholar
Hammer, Ø. and Harper, D. A. T. 2006. Paleontological Data Analysis. Blackwell Publishing, Oxford, U.K., p. 351.Google Scholar
Johnson, K. 2003. Depositional architecture and processes of the Fort Payne Formation, south-central Kentucky. Unpublished M.S. thesis, The Ohio State University, Columbus, 162 p.Google Scholar
Kammer, T. W. 1984. Crinoid from the New Providence Shale Member of the Borden (Mississippian) delta in Kentucky and Indiana. Journal of Paleontology, 58:115–130.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
Kammer, T. W. and Ausich, W. I. 1987. Aerosol suspension feeding and current velocities: Distributional controls for late Osagean crinoids. Paleobiology, 13:379–395.Google Scholar
Kammer, T. W. and Ausich, W. I. 1992. Advanced cladid crinoids from the middle Mississippian of the East-Central United States: Primitive-grade calyces. Journal of Paleontology, 66:461–480.Google Scholar
Kammer, T. W. and Ausich, W. I. 1993. Advanced cladid crinoids from the middle Mississippian of the East-Central United States: Intermediate-grade calyces. Journal of Paleontology, 67:614–639.Google Scholar
Kammer, T. W. and Ausich, W. I. 1994. Advanced cladid crinoids from the middle Mississippian of the east-central United States: Advanced-grade calyces. Journal of Paleontology, 68:339–351.CrossRefGoogle Scholar
Kammer, T. W., Baumiller, T. K., and Ausich, W. I. 1997. Species longevity as a function of niche breadth: Evidence from fossil crinoids. Geology, 25:219–222.Google Scholar
Kammer, T. W., Baumiller, T. K., and Ausich, W. I. 1998. Evolutionary significance of differential species longevity in Osagean-Meramecian (Mississippian) crinoid clades. Paleobiology, 24:155–176.Google Scholar
Kidwell, S. M., Fürsich, F. T., and Aigner, T. 1986. Conceptual framework for the analysis and classification of fossil concentrations. Palaios, 1:228–238.CrossRefGoogle Scholar
Khetani, A. B. and Read, J. F. 2002. Sequence development of a mixed carbonate- siliciclastic high-relief ramp, Mississippian, Kentucky, U.S.A. Journal of Sedimentary Research, 72:657–672.Google Scholar
Krause, R. A. and Meyer, D. L. 2004. Sequence stratigraphy and depositional dynamics of carbonate buildups and associated facies from the lower Mississippian Fort Payne Formation of southern Kentucky, U.S.A. Journal of Sedimentary Research, 74:831–844.CrossRefGoogle Scholar
Krause, R. A. Jr., Meyer, D. L., and Ausich, W. I. 2002. Carbonate buildups in the Fort Payne Formation (Lower Mississippian) Cumberland County, Kentucky, p. 1–13. In Ettensohn, F. R. and Smath, M. L. (eds.), Guidebook for Geology Field Trips in Kentucky and Adjacent Areas, 2002 Joint Meeting of the North-Central Section and Southeastern Section of the Geological Society of America, Lexington; University of Kentucky, Lexington.Google Scholar
Krivicich, E. B. 2011. Paleocommunity analysis of crinoids from the Fort Payne Formation (late Osagean) with localities in Kentucky, Tennessee, and Alabama. Unpublished M.S. Thesis, The Ohio State University, Columbus, 189 p.Google Scholar
Krivicich, E. B., Ausich, W. I., and Keyes, R. G. 2013. Crinoidea from the Fort Payne Chert of north-central Alabama and south-central Tennessee (Phylum Echinodermata; Mississippian). Southeastern Geology, 49:133–143.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 Paleontologica, 14:117–164.Google Scholar
Lane, N. G. 1973. Paleontology and paleoecology of the Crawfordsville fossil site (upper Osagian: Indiana) with sections by J. L. Matthews, E. G. Driscoll, and E. L. Yochelson. University of California Publications in Geological Sciences, 99, 147 p.Google Scholar
Leslie, S. A., Ausich, W. I., and Meyer, D. L. 1996. Lower Mississippian Sedimentation Dynamics and Conodont Biostratigraphy (lowermost Fort Payne Formation along the southeastern margin of the Eastern Interior Seaway). Southeastern Geology, 36:27–35.Google Scholar
Lewis, R. Q. and Potter, P. E. 1978. Surface rocks in the western Lake Cumberland area, Clinton, Russell, and Wayne Counties, Kentucky. Geological Society of Kentucky, Kentucky Geological Survey, Annual Field Conference, 41 p.Google Scholar
MacQuown, W. C. and Perkins, J. H. 1982. Stratigraphy and petrology of petroleum producing Waulsortian-type carbonate mounds in Fort Payne Formation (Lower Mississippian) of north-central Tennessee. American Association of Petroleum Geologists, Bulletin, 66:1055–1075.Google Scholar
Meyer, D. L. and Ausich, W. I. 1992. Fort Payne carbonate facies (Mississippian) of south-central Kentucky. Geological Society of America, Annual Meeting 1992, Field Trip 14 Guidebook, 20 p.Google Scholar
Meyer, D. L. and Ausich, W. I. 1997. Morphologic variation within and between populations of the camerate crinoid Agaricocrinus (Lower Mississippian, Kentucky and Tennessee): breaking the spell of the mushroom. Journal of Paleontology, 71:896–917.Google Scholar
Meyer, D. L., Ausich, W. I., and Terry, R. E. 1989. Comparative taphonomy of echinoderms in carbonate facies: Fort Payne Formation (Lower Mississippian) of Kentucky and Tennessee. Palaios, 4:533–572.Google Scholar
Meyer, D. L., Ausich, W. I., Bohl, D. T., Norris, W. A., and Potter, P. E. 1995. Carbonate mud-mounds in the Fort Payne Formation (lower Carboniferous), Cumberland Saddle region, Kentucky and Tennessee, U.S.A. Special Publications International Association of Sedimentologists, 23:273–287.Google Scholar
Meyer, D. L., Ausich, W. I., and Potter, P. E. 1992. Mississippian Clinoform—lithologic and paleoecologic diversity amid slopes, slides and mounds. Palaios, 7:335–336.Google Scholar
Norris, W. A. 1991. Paleoecology and paleocommunuity analysis of green shale faunas from the Fort Payne Formation (Lower Mississippian) of south-central Kentucky and northcentral Tennessee. Unpublished M.S. thesis, University of Cincinnati, 226 p.Google Scholar
Pryor, W. A. and Sable, E. G. 1974. Carboniferous of the Eastern Interior Basin. In G. Briggs, Carboniferous of the southeastern United States. Geological Society of America Special Paper, 148:281–313.Google Scholar
Ruppel, S. C. 1979. Conodonts from the lower Mississippian Fort Payne and Tuscumbia Formations of Northern Alabama. Journal of Paleontology, 53:55–70.Google Scholar
Smith, E. A. 1890. Geological structure and descriptions of the valley regions adjacent to the Cahaba coal field. Alabama Geological Survey Special Publication, 2:133–180.Google Scholar
Terry, R. E. 1989. Echinoderm paleoecology and taphonomy of carbonate debris flows, Fort Payne Formation (late Osagean, lower Mississippian), Dale Hollow Reservoir, Tennessee. Unpublished M.S. thesis, University of Cincinnati, 180 p.Google Scholar
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