Hostname: page-component-586b7cd67f-r5fsc Total loading time: 0 Render date: 2024-11-30T19:54:30.458Z Has data issue: false hasContentIssue false
  • English
  • Français

New flexible crinoids from the Bangor Limestone (Mississippian) of Tennessee

Published online by Cambridge University Press:  14 July 2015

Larry W. Knox  and
G. Wayne Kendrick
Larry W. Knox
Affiliation:
Department of Earth Sciences, Box 5125, Tennessee Technological University, Cookeville 38505
G. Wayne Kendrick
Affiliation:
202 Oldwood Road, Huntsville, Alabama 35811
Get access Rights & Permissions [Opens in a new window]

Abstract

New flexible crinoids referable to Taxocrinus Phillips and Onychocrinus Lyon and Casseday are made known from Carboniferous (Mississippian, Chesterian) strata of Tennessee. Taxocrinus strimplei n. sp. and Onychocrinus sp. A are reported from a single locality in the Bangor Limestone in Cumberland County, east-central Tennessee. Specimens of both species are characterized by having fewer numbers of brachials than any species yet referred to either genus. Both the evolutionary development of their brachial series and their stratigraphic position suggest that these species are at or near the end of lineages of these two genera.

Type
Research Article
Information
Journal of Paleontology , Volume 61 , Issue 1 , January 1987 , pp. 122 - 129
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

Burdick, D. W. and Strimple, H. L. 1971. Crinoids from the Beech Creek Limestone, Lower Golconda Group, St. Clair County, Illinois. University of Kansas Paleontological Contributions, Paper 51:15–47.Google Scholar
Burdick, D. W. and Strimple, H. L. 1973. Flexible crinoids from the Fayetteville Formation (Chesterian) of northeastern Oklahoma. Journal of Paleontology, 47:226–230.Google Scholar
Burdick, D. W. and Strimple, H. L. 1982. Genevievian and Chesterian crinoids of Alabama. Geological Survey of Alabama Bulletin 121, 277 p.Google Scholar
Burwell, H. B. 1967. Well sample descriptions and drillers' logs, Scott County, Tennessee. Tennessee Department of Conservation, Division of Geology Report of Investigations 21, 201 p.Google Scholar
Horowitz, A. S. 1965. Crinoids from the Glen Dean Limestone (Middle Chester) of southern Indiana and Kentucky. Indiana Department of Conservation, Geological Survey Bulletin 34, 52 p.Google Scholar
Horowitz, A. S. et al. 1979. Carboniferous paleontological zonation and intercontinental correlation of the Fowler No. 1 Traders core, Scott County, Tennessee, U.S.A. Southeastern Geology, 20:205–228.Google Scholar
Horowitz, A. S. et al. and Strimple, H. L. 1974. Chesterian echinoderm zonation in eastern United States, p. 207–220. In Seventh International Congress of Carboniferous Stratigraphy and Geology, Krefeld, 1971, Compte Rendu, 3.Google Scholar
Mamet, B. L. and Skipp, B. 1970. Lower Carboniferous calcareous foraminifera: preliminary zonation and stratigraphic implications for the Mississippian of North America, p. 1129–1146. In Sixth International Congress of Carboniferous Stratigraphy and Geology, Sheffield, 1967, Compte Rendu, 3.Google Scholar
Milici, R. C. et al. 1979. The Mississippian and Pennsylvanian (Carboniferous) Systems in the United States—Tennessee. U.S. Geological Survey Professional Paper 1110-G, 38 p.Google Scholar
Springer, F. 1920. The Crinoidea Flexibilia. Smithsonian Institution Publication 2501, 486 p.Google Scholar
Stearns, R. G. 1954. The Cumberland Plateau overthrust and geology of the Crab Orchard Mountains area, Tennessee. Tennessee Department of Conservation, Division of Geology Bulletin 60, 47 p.Google Scholar
Strimple, H. L. 1978. Flexible crinoids from Pitkin Formation (Chesterian) of Oklahoma and Arkansas. Oklahoma Geology Notes, 38:61–65.Google Scholar
Taylor, A. R., Lewis, R. Q. Sr. and Smith, J. H. 1975. Geologic map of the Burnside Quadrangle, south-central Kentucky. United States Geological Survey, Geological Quadrangle Map GQ–1253, scale 1:24,000.Google Scholar