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A new Permian waagenophyllid coral from the Klamath Mountains, California

Published online by Cambridge University Press:  14 July 2015

Calvin H. Stevens ,
M. Meghan Miller  and
Merlynd Nestell
Calvin H. Stevens
Affiliation:
San Jose State University, San Jose, California 95192
M. Meghan Miller
Affiliation:
Stanford University, Stanford, California 94305
Merlynd Nestell
Affiliation:
University of Texas, Arlington 76019
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Abstract

Specimens of a new species of the Permian waagenophyllid coral genus Waagenophyllum, W. klamathensis, have been recovered from limestone lenses near the top of the Upper Permian Dekkas Formation in the eastern Klamath Mountains, and similar specimens have been collected from an isolated limestone mass in the eastern Hayfork terrane of the southwestern Klamath Mountains, northern California. Another specimen of Waagenophyllum, which may represent another species, has been recovered from another limestone mass in the Hayfork terrane. These specimens of Waagenophyllum, a genus which otherwise is restricted to the Tethyan Province, provide the only tie between the Permian limestone masses of the eastern Hayfork terrane, which also contain typical Tethyan foraminifers, and the eastern Klamath Mountains terrane (McCloud belt), which contains many fossils with non-Tethyan affinities.

Type
Research Article
Information
Journal of Paleontology , Volume 61 , Issue 4 , July 1987 , pp. 690 - 699
Copyright
Copyright © The Paleontological Society 

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References

Albers, J. P., and Robertson, J. F. 1961. Geology and ore deposits of East Shasta copper-zinc district, Shasta County, California. U.S. Geological Survey Professional Paper 338, 107 p.CrossRefGoogle Scholar
Blome, C. D., and Irwin, W. P. 1983. Tectonic significance of late Paleozoic to Jurassic radiolarians from the North Fork terrane, Klamath Mountains, California, p. 77–89. In Stevens, C. H. (ed.), Pre-Jurassic Rocks in Western North American Suspect Terranes. The Pacific Section, Society of Economic Paleontologists and Mineralogists, Los Angeles, California.Google Scholar
Burchfiel, B. C., and Davis, G. A. 1975. Nature and controls of Cordilleran orogenesis, western United States: extensions of an earlier synthesis. American Journal of Science, 275-A:363–396.Google Scholar
Choi, D. R. 1984. Late Permian-Early Triassic paleogeography of northern Japan: did Pacific microplates accrete to Japan? Geology, 12:728–731.Google Scholar
Coney, P. J., Jones, D. L., and Monger, J. W. H. 1980. Cordilleran suspect terranes. Nature, 288:329–333.Google Scholar
Coogan, A. H. 1960. Stratigraphy and Paleontology of the Permian Nosoni and Dekkas Formations (Bollibokka Group). University of California Publications in Geological Sciences, 36:243–316.Google Scholar
Danner, W. R. 1977. Paleozoic rocks of northwest Washington and adjacent parts of British Columbia, p. 481–502. In Stewart, J.H., Stevens, C. H., and Fritsche, A. E. (eds.), Pacific Coast Paleogeographic Symposium 1: Paleozoic Paleogeography of the Western United States. The Pacific Section, Society of Economic Paleontologists and Mineralogists, Los Angeles, California.Google Scholar
Davis, G. A., Monger, J. W. H., and Burchfiel, B. C. 1978. Mesozoic construction of the Cordilleran collage, central British Columbia to central California, p. 1–32. In Howell, D. G. and McDougall, K. A. (eds.), Pacific Coast Paleogeographic Symposium 2: Mesozoic Paleogeography of the Western United States. The Pacific Section, Society of Economic Paleontologists and Mineralogists, Los Angeles, California.Google Scholar
Fagin, S. W., and Gose, W. A. 1983. Paleomagnetic data from the Redding section of the eastern Klamath belt, northern California. Geology, 11:505–508.2.0.CO;2>CrossRefGoogle Scholar
Grabau, A.W. 1931. The Permian of Mongolia, a report on the Permian fauna of the Jisu Honguer Limestone of Mongolia and its relations to the Permian of other parts of the world. In Reeds, C. A. (ed.), Natural History of Central Asia. American Museum of Natural History, New York, Vol. 4, 665 p.Google Scholar
Harper, G.D., and Wright, J. E. 1984. Middle to Late Jurassic tectonic evolution of the Klamath Mountains, California-Oregon. Tectonics, 3:759–772.CrossRefGoogle Scholar
Irwin, W. P. 1972. Terranes of the western Paleozoic and Triassic belt in the southern Klamath Mountains, California. U.S. Geological Survey Professional Paper 800–C:C103–C111.Google Scholar
Irwin, W. P. 1985. Age and tectonics of plutonic belts in accreted terranes of the Klamath Mountains, California and Oregon, p. 187–199. In Howell, D. G. (ed.), Tectonostratigraphic terranes of the circum-Pacific region. Circum-Pacific Council for Energy and Mineral Resources, Earth Science Series 1.Google Scholar
Irwin, W. P., Wardlaw, B. R., and Kaplan, T. A. 1983. Conodonts of the western Paleozoic and Triassic belt, Klamath Mountains, California and Oregon. Journal of Paleontology, 57:1030–1039.Google Scholar
Luken, M. D. 1985. Petrography and origin of limestones in the western Paleozoic and Triassic belt, Klamath Mountains. Unpubl. M.S. thesis, San Jose State University, San Jose, California, 131 p.Google Scholar
Mankinen, E. A., Irwin, W. P., and Gromme, C. S. 1982. Tectonic rotation of the eastern Klamath Mountains terrane, California. Eos Transactions, American Geophysical Union, 63:914.Google Scholar
Miller, M. M. 1986. Tectonic evolution of late Paleozoic island-arc sequences in the western U.S. Cordillera; with detailed studies from the eastern Klamath Mountains, northern California. Unpubl. Ph.D. dissertation, Stanford University, Stanford, California, 201 p.Google Scholar
Minato, M., and Kato, M. 1965. Waagenophyllidae. Journal of the Faculty of Science, Hokkaido University, Series IV, Geology and Mineralogy, XII(3, 4), 241 p.Google Scholar
Mortimer, N. 1984. Petrology and structure of Permian to Jurassic rocks near Yreka, Klamath Mountains, California. Unpubl. Ph.D. dissertation, Stanford University, Stanford, California, 84 p.Google Scholar
Nelson, S. J., and Nelson, E. R. 1985. Allochthonous Permian micro- and macrofauna, Kamloops area, British Columbia. Canadian Journal of Earth Sciences, 22:442–451.CrossRefGoogle Scholar
Nestell, M. K., Irwin, W. P., and Albers, J. P. 1981. Late Permian (early Djulfian) Tethyan foraminifera from the southern Klamath Mountains, California. Geological Society of America, Abstracts with Programs, 13:519.Google Scholar
Sanborn, A. F. 1960. Geology and paleontology of the southwest quarter of the Big Bend quadrangle. California Division of Mines Special Report 63, 26 p.Google Scholar
Schultz, K. L., and Levi, S. 1983. Paleomagnetism of Middle Jurassic plutons of the north-central Klamath Mountains. Geological Society of America, Abstracts with Programs, 15:427.Google Scholar
Scott, G. R., et al. 1985. Paleomagnetism of a Permian Nosoni Formation ignimbrite and implications to accretionary models of eastern Klamath belt tectonics. Geological Society of America, Abstracts with Programs, 17:407.Google Scholar
Skinner, J. W., and Wilde, G. L. 1965. Permian biostratigraphy and fusulinid faunas of the Lake Shasta area, northern California. University of Kansas Paleontological Contributions, Protozoa 6, 98 p.Google Scholar
Speed, R. C. 1979. Collided Paleozoic micro-plate in the western United States. Journal of Geology, 87:279–292.CrossRefGoogle Scholar
Stevens, C. H. 1983. Corals from a dismembered late Paleozoic paleo-Pacific plateau. Geology, 11:603–606.2.0.CO;2>CrossRefGoogle Scholar
Stevens, C. H. 1985. Reconstruction of Permian paleogeography based upon distribution of Tethyan faunal elements. Compte Rendu, Ninth International Congress of Carboniferous Stratigraphy and Geology, 5:383–393.Google Scholar
Stevens, C. H., and Rycerski, B. A. 1983. Permian colonial rugose corals in the western Americas—aids in positioning of suspect terranes, p. 23–36. In Stevens, C. H. (ed.), Pre-Jurassic Rocks in Western North American Suspect Terranes. Pacific Section, Society of Economic Paleontologists and Mineralogists, Los Angeles, California.Google Scholar
Watkins, R. 1979. Carboniferous rocks of the eastern Klamath Mountains, California. U.S. Geological Survey Professional Paper 1110-CC: CC33–CC36.Google Scholar
Wilson, E. C. 1982. Wolfcampian rugose and tabulate corals (Coelenterata: Anthozoa) from the Lower Permian McCloud Limestone of northern California. Natural History Museum of Los Angeles County, Contributions in Science, 337, 90 p.Google Scholar
Wright, J. E. 1982. Permo-Triassic accretionary subduction complex, southwestern Klamath Mountains, northern California. Journal of Geophysical Research, 87:3805–3818.CrossRefGoogle Scholar