Hostname: page-component-5c6d5d7d68-lvtdw Total loading time: 0 Render date: 2024-08-15T23:34:45.582Z Has data issue: false hasContentIssue false
  • English
  • Français

Late Ordovician rugose corals of the northern Sierra Nevada, California

Published online by Cambridge University Press:  20 May 2016

Robert J. Elias ,
A. W. Potter  and
Rodney Watkins
Robert J. Elias
Affiliation:
Department of Geological Sciences, The University of Manitoba, Winnipeg R3T 2N2, Canada
A. W. Potter
Affiliation:
Department of Geosciences, Oregon State University, Corvallis 97331
Rodney Watkins
Affiliation:
Geology Department, Milwaukee Public Museum, 800 West Wells St., Milwaukee, Wisconsin 53233
Get access Rights & Permissions [Opens in a new window]

Extract

The shoo fly Complex of Late Devonian and older Paleozoic age is a regionally extensive rock assemblage in the northern Sierra Nevada of northern California. It consists chiefly of a coherent unit of phyllite, quartzose sandstone, and chert, and a melange unit (Hannah and Moores, 1986). Several limestone lenses in the Taylorsville area comprise the Montgomery Limestone (Diller, 1892, 1908; McMath, 1958; Figure 1). The Montgomery was long considered to be Silurian, largely on the basis of corals, brachiopods, and cephalopods (Diller, 1892, 1908; McMath, 1958; Berry and Boucot, 1970; Merriam, 1972). However, recent analyses of the biota indicate an Ashgill (middle Maysvillian–Gamachian) age (Boucot and Potter, 1977; Harris, personal commun. cited in Hannah and Moores, 1986, p. 790; Potter et al., 1990b; present study).

Type
Paleontological Notes
Information
Journal of Paleontology , Volume 68 , Issue 1 , January 1994 , pp. 164 - 168
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

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
Boucot, A. J. 1975. Evolution and Extinction Rate Controls (Developments in Palaeontology and Stratigraphy, 1). Elsevier Scientific Publishing Company, Amsterdam, 427 p.Google Scholar
Boucot, A. J., Dean, W. T., Martinsson, A., Potter, A., Rexroad, C., Rohr, D., Savage, N. M., and Wright, A. J. 1973. Pre-late Middle Devonian biostratigraphy of the eastern Klamath belt, northern California. Geological Society of America, Abstracts with Programs, 5:15.Google Scholar
Boucot, A. J., and Potter, A. W. 1977. Middle Devonian orogeny and biogeographical relations in areas along the North American Pacific rim, p. 210–219. In Murphy, M. A., Berry, W. B. N., and Sandberg, C. A. (eds.), Western North America: Devonian. University of California, Riverside Campus, Museum Contribution 4.Google Scholar
D'Allura, J. A., Moores, E. M., and Robinson, L. 1977. Paleozoic rocks of the northern Sierra Nevada: their structural and paleogeographic implications, p. 395–408. In Stewart, J. H., Stevens, C. H., and Fritsche, A. E. (eds.), Paleozoic Paleogeography of the Western United States. Society of Economic Paleontologists and Mineralogists, Pacific Section, Pacific Coast Paleogeography Symposium 1.Google Scholar
Diller, J. S. 1892. Geology of the Taylorville region of California. Geological Society of America Bulletin, 3:369–394.Google Scholar
Diller, J. S. 1908. Geology of the Taylorsville region, California. U.S. Geological Survey, Bulletin 353, 128 p.Google Scholar
Dybowski, W. 1873. Monographie der Zoantharia sclerodermata rugosa aus der Silur-formation Estlands, Nord-Livlands und der Insel Gotland. Archiv für die Naturkunde Liv-, Ehst- und Kurlands, Series I, 5(3):257–414.Google Scholar
Elias, R. J. 1982. Latest Ordovician solitary rugose corals of eastern North America. Bulletins of American Paleontology, 81(314), 116 p.Google Scholar
Elias, R. J. 1989. Extinctions and origins of solitary rugose corals, latest Ordovician to earliest Silurian in North America, p. 319–326. In Jell, P. A. and Pickett, J. W. (eds.), Fossil Cnidaria 5: Proceedings of the Fifth International Symposium on Fossil Cnidaria including Archaeocyatha and Spongiomorphs held in Brisbane, Queensland, Australia, 25-29 July 1988. Association of Australasian Palaeontologists, Memoir 8.Google Scholar
Elias, R. J., and Potter, A. W. 1984. Late Ordovician solitary rugose corals of the eastern Klamath Mountains, northern California. Journal of Paleontology, 58:1203–1214.Google Scholar
Hannah, J. L., and Moores, E. M. 1986. Age relationships and depositional environments of Paleozoic strata, northern Sierra Nevada, California. Geological Society of America Bulletin, 97:787–797.Google Scholar
McMath, V. E. 1958. The geology of the Taylorsville area, Plumas County, California. Unpubl. Ph.D. dissertation, University of California, Los Angeles, 199 p.Google Scholar
Merriam, C. W. 1972. Silurian rugose corals of the Klamath Mountains region, California. U.S. Geological Survey, Professional Paper 738, 50 p.Google Scholar
Neuman, R. B. 1980a. Paleogeographic implications of Upper Ordovician rocks in Maine. Geological Society of America, Abstracts with Programs, 12:75.Google Scholar
Neuman, R. B. 1980b. Trip B-4, itinerary: the core of the Weeksboro-Lunksoos Lake Anticline, and the Ordovician, Silurian, and Devonian rocks on its northwest flank, p. 114–126. In Roy, D. C. and Naylor, R. S. (eds.), A Guidebook to the Geology of Northeastern Maine and Neighboring New Brunswick. 72nd Annual Meeting, New England Intercollegiate Geological Conference.Google Scholar
Neuman, R. B. 1984. Geology and paleobiology of islands in the Ordovician Iapetus Ocean: review and implications. Geological Society of America Bulletin, 95:1188–1201.Google Scholar
Potter, A. W. 1990. Middle and Late Ordovician brachiopods from the eastern Klamath Mountains, northern California; Part 1. Palaeontographica, Abteilung A, 212:31–158.Google Scholar
Potter, A. W., Boucot, A. J., Bergström, S. M., Blodgett, R. B., Dean, W. T., Flory, R. A., Ormiston, A. R., Pedder, A. E. H., Rigby, J. K., Rohr, D. M., and Savage, N. M. 1990a. Early Paleozoic stratigraphic, paleogeographic, and biogeographic relations of the eastern Klamath belt, northern California, p. 57–74. In Harwood, D. S. and Miller, M. M. (eds.), Paleozoic and Early Mesozoic Paleogeographic Relations; Sierra Nevada, Klamath Mountains, and Related Terranes. Geological Society of America, Special Paper 255.Google Scholar
Potter, A. W., Watkins, R., Boucot, A. J., Elias, R. J., Flory, R. A., and Rigby, J. K. 1990b. Biogeography of the Upper Ordovician Montgomery Limestone, Shoo Fly Complex, northern Sierra Nevada, California, and comparisons of the Shoo Fly Complex and the Yreka terrane, p. 33–41. In Harwood, D. S. and Miller, M. M. (eds.), Paleozoic and Early Mesozoic Paleogeographic Relations; Sierra Nevada, Klamath Mountains, and Related Terranes. Geological Society of America, Special Paper 255.Google Scholar