Hostname: page-component-7479d7b7d-k7p5g Total loading time: 0 Render date: 2024-07-12T06:15:18.847Z Has data issue: false hasContentIssue false
  • English
  • Français

Fasciculate rugose corals from Gzhelian and Lower Permian strata, Pequop Mountains, northeast Nevada

Published online by Cambridge University Press:  14 July 2015

Calvin H. Stevens
Calvin H. Stevens*
Affiliation:
Department of Geology, San Jose State University, San Jose, California 95192-0102,
Get access Rights & Permissions [Opens in a new window]

Abstract

Upper Carboniferous and Lower Permian shallow marine rocks in the Pequop Mountains of northeastern Nevada contain an abundance of fossils, especially fusulinids and fasciculate corals. As the composite stratigraphic section in this area represents the most nearly complete sequence of this type of corals anywhere in the Cordilleran miogeocline, this study was undertaken to document their occurrence sequentially. This information should be useful for comparison with other sections in the miogeocline containing similar corals.

Only one species of Durhamina is present in the Gzhelian rocks. Durhamina, Heintzella, and Paraheritschioides occur in the Asselian rocks, and all of these genera plus Wilsonastraea are present in the Sakmarian part of the section. Corals in the Artinskian and Kungurian are represented by an advanced species of Durhamina and the very advanced durhaminid, Sandolasma.

Newly described species are: Durhamina primitiva, D. snyderi, Sandolasma perplexa, Heintzella davydovi, Paraheritschioides nevadaensis, and Wilsonastraea fraseri.

Type
Research Article
Information
Journal of Paleontology , Volume 82 , Issue 6 , November 2008 , pp. 1190 - 1200
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

Breuninger, R. H. 1976. Palaeoaplysina (Hydrozoan?) carbonate buildups from the upper Paleozoic of Idaho. American Association of Petroleum Geologists, 60:584–607.Google Scholar
Dobrolyubova, T. A. 1936. Rugose corals of the Middle and Upper Carboniferous and Lower Permian of the northern Urals. Trudy Polyarnoi Komissii, Akademiya Nauk SSSR, 28:77–158. (In Russian, English summary).Google Scholar
Easton, W. H. 1960. Permian corals from Nevada and California. Journal of Paleontology, 34:570–583.Google Scholar
Fedorowski, J. 1967. The Lower Permian Tetracoralla and Tabulata from Treskelodden, Vestspitsbergen. Norsk Polarinstitutt Skrifter, 142:5–44.Google Scholar
Fedorowski, J., Bamber, E. W., and Stevens, C. H. 2007. Lower Permian colonial rugose corals, western and northwestern Pangaea: Taxonomy and distribution. NRC Research Press, Ottawa, Ontario, Canada, 219 p.CrossRefGoogle Scholar
Fraser, G. D., Ketner, K. B., and Smith, M. C. 1986. Geologic map of the Spruce Mountain 4 quadrangle, Elko County, Nevada. U.S. Geological Survey Miscellaneous Field Studies Map MF-1846, scale 1:24,000.Google Scholar
Marcantel, J. B. 1973. Upper Pennsylvanian and Lower Permian sedimentation in northeast Nevada. Unpublished Ph.D. dissertation, The Ohio State University, 112 p.Google Scholar
Meek, F. G. 1864. Description of the Carboniferous fossils, p. 3–16. In Meek, F. G. and Gabb, W. M., Palaeontology of California. Geological Survey of California, v. 1. Caxton Press, Philadelphia.Google Scholar
Minato, M. and Kato, M. 1965. Durhaminidae (Tetracoral). Journal of the Faculty of Science, Hokkaido University, Series 4, Geology and Mineralogy, 13(1):11–86.Google Scholar
Robinson, G. B. Jr. 1961. Stratigraphy and Leonardian fusulinid paleontology in central Pequop Mountains, Elko County, Nevada. Brigham Young University Geology Studies, 8:93–145.Google Scholar
Rowett, C. L. 1969. Upper Paleozoic stratigraphy and corals from the east-central Alaska Range, Alaska. Arctic Institute of North America Technical Paper 23, 120 p.Google Scholar
Sando, W. J. 1985. Paraheritschioides, a new rugose coral genus from the Upper Pennsylvanian of Idaho. Journal of Paleontology, 59:979–985.Google Scholar
Steele, G. 1960. Pennsylvanian-Permian stratigraphy of east-central Nevada and adjacent Utah, p. 91–113. In Boettcher, J. W., and Sloan, W. W. Jr. (eds.), Geology of east-central Nevada. Intermountain Association of Petroleum Geologists, 11th Annual Field Conference Guidebook.Google Scholar
Stevens, C. H. 1979. Lower Permian of the central Cordilleran Miogeosyncline. Geological Society of America Bulletin, Pt. II, 90:381–455.Google Scholar
Stevens, C. H. and Rycerski, B. 1989. Early Permian colonial rugose corals from the Stikine River area, British Columbia, Canada. Journal of Paleontology, 63:158–181.CrossRefGoogle Scholar
Wagner, D. B. 1974. Lower Permian paleogeography and fusulinid paleontology, northeastern Nevada and western Utah. Unpublished M.S. thesis, San Jose, CA, San Jose State University, 254 p.Google Scholar
Wardlaw, B. R., Davydov, V., Shilong, Mei, and Henderson, C. 1998. New reference sections for the Upper Carboniferous and Lower Permian in northeast Nevada. Permophiles (Newsletter of the Subcommission of Permian Stratigraphy), 31:5–8.Google Scholar
Wilson, E. C. 1982. Wolfcampian rugose and tabulate corals (Coelenterata; Anthozoa) from the Lower Permian McCloud Limestone of northern California. Contributions in Science, Natural History Museum of Los Angeles County, 337:1–90.Google Scholar
Wilson, E. C. 1994. Early Permian corals from the Providence Mountains, San Bernardino County, California. Journal of Paleontology, 68:938–951.CrossRefGoogle Scholar
Wilson, E. C. and Langenheim, R. L. Jr. 1962. Rugose and tabulate corals from Permian rocks in the Ely quadrangle, White Pine County, Nevada. Journal of Paleontology, 36:495–520.Google Scholar
Wilson, E. C. and Langenheim, R. L. Jr. 1993. Early Permian corals from Arrow Canyon, Clark County, Nevada. Journal of Paleontology, 67:935–945.CrossRefGoogle Scholar