Hostname: page-component-cd9895bd7-jn8rn Total loading time: 0 Render date: 2024-12-26T04:51:55.499Z Has data issue: false hasContentIssue false

Lower Mississippian crinoid (Echinodermata) fauna from Utah County, Utah

Published online by Cambridge University Press:  20 May 2016

William I. Ausich*
Affiliation:
Department of Geological Sciences, 155 South Oval Mall, The Ohio State University, Columbus 43210,

Abstract

A low-diversity crinoid fauna is described from the Fitchville Formation, Lower Mississippian (Late Devonian to Early Mississippian) of Utah County, Utah. Based on the crinoid fauna, composed of Nunnacrinus olsoni new species, Paracosmetocrinus lundi new species, and Platycrinites sp., this fauna is interpreted as being from the Kinderhookian, Upper Fitchville Formation. This occurrence of Nunnacrinus extends the geographic and facies range of this genus in western North America and the geographic range of Paracosmetocrinus within western North America.

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

Ausich, W. I. 1997. Regional encrinites: a vanished lithofacies, p. 509519. In Brett, C. E. and Baird, G. C. (eds.), Paleontological Events: Stratigraphic, Ecologic and Evolutionary Implications. Columbia University Press, New York.Google Scholar
Ausich, W. I. 1998a. Early phylogeny and subclass division of the Crinoidea (Phylum Echinodermata). Journal of Paleontology, 72:499510.CrossRefGoogle Scholar
Ausich, W. I. 1998b. Phylogeny of Arenig to Caradoc crinoids (Phylum Echinodermata) and suprageneric classification of the Crinoidea. University of Kansas Paleontological Contributions, New Series, 9, 36 p.Google Scholar
Ausich, W. I., and Lane, N. G. 1982. Crinoids from the Edwardsville Formation (Lower Mississippian) of southern Indiana. Journal of Paleontology, 56:13431361.Google Scholar
Ausich, W. I., and Sevastopulo, G. D. 2001. The Lower Carboniferous (Tournaisian) crinoids from Hook Head, County Wexford, Ireland. Palaeontographical Society Monograph, 617, 136 p.Google Scholar
Austin, T. Sr., and Austin, T. Jr. 1842. Proposed arrangement of the Echinodermata, particularly as regards the Crinoidea, and a subdivision of the class Adelostella (Echinidae). Annals and Magazine of Natural History, series 1, 10:106113.CrossRefGoogle Scholar
Beach, G. A. 1961. Late Devonian and Mississippian biostratigraphy of central Utah. Brigham Young University Geology Studies, 8:3754.Google Scholar
Bowsher, A. L. 1955. New genera of Mississippian camerate crinoids. University of Kansas Paleontological Contributions, Echinodermata, 1, 23 p.Google Scholar
Bronn, H. G. 1848–1849. Index palaeontologicus, unter Mitwirkung der Herren Prof. H. T. Göppert und H. von Meyer. Handbuch einer Geschichte der Natur, 5(1, 2), Pt. 3, 1381 p.Google Scholar
Brower, J. C. 1970. Chapter 12, p. 475543. In McKee, E. D. and Gutschick, R. C. (eds.), History of the Redwall Limestone. Geological Society of America Memoir, 114.Google Scholar
Clark, D. L., and Beach, G. A. 1961. Late Devonian—Early Mississippian biostratigraphy, central Utah. Geological Society of America Special Paper, 68:150.Google Scholar
Greenhalgh, B. R. 1980. The Fitchville Formation: a study of the biostratigraphy and depositional environments in West Central Utah County, Utah. Brigham Young University Geology Studies, 27:929.Google Scholar
Gutschick, R. C., Sandberg, C. A., and Sando, W. J. 1980. Mississippian shelf margin and carbonate platform from Montana to Nevada, p. 111147. In Fouch, T. D. and Magathan, E. R. (eds.), Paleozoic Paleogeography of the West-central United States. Rocky Mountain Paleogeography Symposium, 1. Rocky Mountain Section of Society of Economic Paleontologists and Mineralogists, Denver.Google Scholar
Jaekel, O. 1918. Phylogenie und System der Pelmatozoen. Paläontologische Zeitschrift, 3:1128.CrossRefGoogle Scholar
Laudon, L. R., Parks, J. M., and Spreng, A. C. 1952. Mississippian crinoid fauna from the Banff Formation, Sunwapta Pass, Alberta. Journal of Paleontology, 26:544575.Google Scholar
Laudon, L. R., and Severson, J. L. 1953. New crinoid fauna, Mississippian Lodgepole Formation, Montana. Journal of Paleontology, 27:505536.Google Scholar
Meek, F. B., and Worthen, A. H. 1865. Descriptions of new Crinoidea, &c., from the Carboniferous rocks of Illinois and some of the adjoining states. Philadelphia Academy of Natural Science, Proceedings, series 1, 17(3):155166.Google Scholar
Miller, J. S. 1821. A natural history of the Crinoidea or lily-shaped animals, with observations on the genera Asteria, Euryale, Comatula, and Marsupites . Bryan and Co., Bristol, 150 p.Google Scholar
Moore, R. C. 1952. Crinoids, p. 604652. In Moore, R. C., Lalicker, C. G., and Fischer, A. G. (eds.), Invertebrate Fossils. McGraw-Hill, New York.Google Scholar
Moore, R. C., and Laudon, L. 1943. Evolution and classification of Paleozoic crinoids. Geological Society of America Special Paper, 46, 153 p.Google Scholar
Moore, R. C., and Teichert, C. (eds.). 1978. Treatise on Invertebrate Paleontology, Pt. T, Echinodermata 2. Geological Society of America and The University of Kansas Press, Lawrence, 1027 p.Google Scholar
Morris, H. T., and Lovering, T. S. 1961. Stratigraphy of the east Tintic Mountains, Utah. U.S. Geological Survey Professional Paper, 361, 145 p.Google Scholar
Newman, G. J. 1980. Conodonts and biostratigraphy of the Lower Mississippian in western Utah and eastern Nevada. Brigham Young University Geology Studies, 27:103121.Google Scholar
Rigby, J. K., and Clark, D. L. 1962. Devonian and Mississippian Systems in central Utah. Brigham Young University Geology Studies, 9:1725.Google Scholar
Strimple, H. L. 1967. Aphelecrinidae, a new family of inadunate crinoids. Oklahoma Geology Notes, 27:8185.Google Scholar
Ubaghs, G. 1978a. Skeletal morphology of fossil crinoids, p. T58T216. In Moore, R. C. and Teichert, C. (eds.), Treatise on Invertebrate Paleontology, Pt. T, Echinodermata 2(2). Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Ubaghs, G. 1978b. Suborder Compsocrinina, p. T440T487. In Moore, R. C. and Teichert, C. (eds.), Treatise on Invertebrate Paleontology, Pt. T, Echinodermata 2(2). Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Wachsmuth, C., and Springer, F. 1885. Revision of the Palaeocrinoidea, Pt. 3, Sec. 1. Proceedings of the Academy of Natural Sciences of Philadelphia for 1885:223364 (1–139).Google Scholar
Wachsmuth, C., and Springer, F. 1897. The North American Crinoidea Camerata. Harvard College Museum of Comparative Zoology, Memoir 21–22, 897 p.CrossRefGoogle Scholar
Webster, G. D., 1991. Tournaisian and early Visean crinoid faunas of western North America. Eleventh International Geological Congress of Carboniferous Stratigraphy and Geology, 2:376381.Google Scholar
Webster, G. D. 1997. Lower Carboniferous echinoderms from northern Utah and western Wyoming. Utah Geological Survey Bulletin, 128, 65 p.Google Scholar
Webster, G. D., and Lane, N. G. 1970. Carboniferous echinoderms from the southwestern United States. Journal of Paleontology, 44:276296.Google Scholar
Webster, G. D., and Lane, N. G. 1987. Crinoids from the Anchor Limestone (Lower Mississippian) of the Monte Cristo Group southern Nevada. University of Kansas Paleontological Contributions Paper, 119, 56 p.Google Scholar
Witkind, I. J., and Weiss, M. P. 1991. Geologic map of the Nephi 30′ × 60′ Quadrangle, Carbon, Emery, Juab, Sanpete, Utah, and Wasatch Counties, Utah. U.S. Geological Survey Miscellaneous Investigations Series Map, I-1937.Google Scholar