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Conodont fauna and biostratigraphy of the Outram, Skoki, and Owen Creek Formations (Lower to Middle Ordovician), Wilcox Pass, Alberta, Canada

Published online by Cambridge University Press:  20 May 2016

Leanne J. Pyle
Affiliation:
School of Earth and Ocean Sciences, University of Victoria, P.O. Box 3055, Victoria, B.C. V8W 3P6, Canada, , ,
Christopher R. Barnes
Affiliation:
School of Earth and Ocean Sciences, University of Victoria, P.O. Box 3055, Victoria, B.C. V8W 3P6, Canada, , ,
Zailiang Ji
Affiliation:
School of Earth and Ocean Sciences, University of Victoria, P.O. Box 3055, Victoria, B.C. V8W 3P6, Canada, , ,

Abstract

A collection of 60,886 conodonts was recovered from 141 samples of the Outram, Skoki and Owen Creek Formations (Lower to Middle Ordovician) that outcrop through the Wilcox Pass section, Jasper National Park, Alberta, Canada. This section representσ the standard reference section for the Lower-Middle Ordovician of the Southern Canadian Cordillera. The well preserved fauna is assigned to 75 species representing 48 genera. The species are representative of both the Midcontinent and Atlantic faunal realms, but dominantly the former. Nine Midcontinent Realm zones are recognized in the upwards shallowing carbonate platform succession including the Scolopodus subrex, Acodus kechikaensis, Oepikodus communis, Jumudontus gananda, Tripodus laevis, Histiodella altifrons, Histiodella sinuosa, Histiodella holodentata, and Phragmodus “pre-flexuosus” zones. Zones recognized that are characteristic of the Atlantic Realm include Paroistodus proteus, Paracordylodus gracilis, Oepikodus evae, Paroistodus originalis, and Microzarkodina flabellum. A new genus, Filodontus, is proposed for elements assigned previously to the form genus “Scolopodus” filosus. A new species, Leptochirognathus wilcoxi, is described and one new species, left in open nomenclature, is assigned to Rossodus?.

Type
Research Article
Copyright
Copyright © The Paleontological Society

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Footnotes

2

Present address: Department of Geological Sciences, Queen's University, Kingston, Ontario K7L 3N6, Canada

References

Aitken, J. D., and Norford, B. S. 1967. Lower Ordovician Survey Peak and Outram formations, southern Rocky Mountains of Alberta. Bulletin of Canadian Petroleum Geology, 15:150207.Google Scholar
Albanesi, G. L. 1998. Taxonomia de conodontes de las Secuencias Ordovicicas Del Cerro Potrerillo, Precordillera Central De San Juan, R. Argentina, p. 101253. In Hünicken, M. A. (ed.), Bioestratigrafia, Biofacies y Taxonomia de Conodontes de las Secuencias Ordovicicas del Cerro Potrerillo, Precordillera Central De San Juan, R. Argentina. Academia Nacional de Ciencias, Cordoba.Google Scholar
Branson, E. B., and Mehl, M. G. 1943. Ordovician conodont faunas from Oklahoma. Journal of Paleontology, 17:374387.Google Scholar
Cooper, R. A., Nowlan, G. S., and Williams, S. H. 2001. Global stratotype section and point for base of the Ordovician System. Episodes, 24:1928.CrossRefGoogle Scholar
Dean, W. T. 1978. Preliminary report on the stratigraphy and trilobites of the Survey Peak and Outram formations at Wilcox Pass, Jasper National Park, Canada. Geological Survey of Canada Paper, 76-34, 10 p.Google Scholar
Dean, W. T. 1989. Trilobites from the Survey Peak, Outram and Skoki Formations (Upper Cambrian-Lower Ordovician) at Wilcox Pass, Jasper National Park, Alberta. Geological Survey of Canada Bulletin, 389, 141 p.Google Scholar
Dean, W. T., and Martin, F. 1982. The sequence of trilobite faunas and acritarch microfloras at the Cambrian-Ordovician boundary, Wilcox Pass, Alberta, Canada, p. 131140. In Bassett, M. G. and Dean, W. T. (eds.), The Cambrian-Ordovician Boundary: Sections, Fossil Distribution, and Correlations. National Museum of Wales, Cardiff, Geological Series 3.Google Scholar
Derby, J. R., Lane, H. R., and Norford, B. S. 1972. Uppermost Cambrian-Basal Ordovician faunal succession in Alberta and correlation with similar sequences in the western United States. 24 International Geological Congress, Proceedings, Section 7:503512.Google Scholar
Duan, J. 1990. Ordovician conodonts from northern Jiangsu and indices of their colour alteration. Acta Micropalaeontologica Sinica, 7:1941. (In Chinese)Google Scholar
Ethington, R. L., and Clark, D. L. 1964. Conodonts from the El Paso Formation (Ordovician) of Texas and Arizona. Journal of Paleontology, 38:685705.Google Scholar
Ethington, R. L., and Clark, D. L. 1965. Lower Ordovician conodonts and other microfossils from the Columbia Ice fields section, Alberta, Canada. Brigham Young University, Geological Studies, 12:185205.Google Scholar
Ethington, R. L., and Clark, D. L. 1982. Lower and Middle Ordovician conodonts from the Ibex area, western Millard County, Utah. Brigham Young University, Geologic Studies, 28:1160.Google Scholar
Ethington, R. L., Lehnert, O., and Repetski, J. E. 2000. Stiptognathus new genus (Conodonta: Ibexian, Lower Ordovician), and the apparatus of Stiptognathus borealis (Repetski, 1982). Journal of Paleontology, 74:92100.CrossRefGoogle Scholar
Fåhræus, L. E., and Nowlan, G. S. 1978. Franconian (Late Cambrian) to early Champlainian (Middle Ordovician) conodonts from the Cow Head Group, western Newfoundland. Journal of Paleontology, 52:444471.Google Scholar
Harris, A. G., Bergström, S. M., Ethington, R. L., and Ross, R. J. Jr. 1979. Aspects of Middle and Upper Ordovician conodont biostratigraphy of carbonate facies in Nevada and southeast California and comparison with some Appalachian successions, p. 733. In Sandberg, C. A. and Clark, D. L. (eds.), Conodont Biostratigraphy of the Great Basin and Rocky Mountains. Brigham Young University Geology Studies, 26.Google Scholar
Ji, Z., and Barnes, C. R. 1994. Lower Ordovician conodonts of the St. George Group, Port au Port Peninsula, western Newfoundland, Canada. Palaeontographica Canadiana, 11:1149.Google Scholar
Ji, Z., and Barnes, C. R. 1996. Uppermost Cambrian and Lower Ordovician conodont biostratigraphy of the Survey Peak Formation (Ibexian/Tremadoc), Wilcox Pass, Alberta, Canada. Journal of Paleontology, 70:871890.CrossRefGoogle Scholar
Johnston, D. I., and Barnes, C. R. 1999. Early and Middle Ordovician (Arenig) conodonts from St. Pauls Inlet and Martin Point, Cow Head Group, Western Newfoundland, Canada. Geologica et Palaeontologica, 33:2170.Google Scholar
Jones, P. J. 1971. Lower Ordovician conodonts from the Bonaparte Gulf Basin and the Daly River Basin, north-western Australia. Australia Bureau of Mineral Resources, Geology and Geophysics Bulletin, 117:180.Google Scholar
Landing, E. 1981. Upper Cambrian and Lower Ordoviican conodont biostratigraphy, Wilcox Peak, Jasper National Park, Alberta, p. 5152. In Taylor, M. E. (ed.), Field Guidebook of Second International Symposium on the Cambrian System.Google Scholar
Lindström, M. 1955. Conodonts from the lower-most Ordovician strata of south-central Sweden. Geologiska Föreningens i Stockholm Förhandlingar, 76:517604.CrossRefGoogle Scholar
Lindström, M. 1971. Lower Ordovician conodonts of Europe, p. 2161. In Sweet, W. C. and Bergström, S. M. (eds.), Symposium on Conodont Biostratigraphy. Geological Society of America, Memoir 127.Google Scholar
Martin, F. 1992. Uppermost Cambrian and Lower Ordovician acritarchs and Lower Ordovician chitinozoans from Wilcox Pass, Alberta. Geological Survey of Canada Bulletin 420, 57 p.Google Scholar
Mound, M. C. 1968. Conodonts and biostratigraphy of the Iowa Arbuckle Group (Ordovician), Arbuckle Mountains, Oklahoma. Micropaleontology, 14:393434.CrossRefGoogle Scholar
Norford, B. S. 1969. Ordovician and Silurian stratigraphy of the southern Rocky Mountains. Geological Survey of Canada, Bulletin 176, 90 p.Google Scholar
Pei, F., and Cai, S. 1987. The discovery of Lower Ordovician conodonts from Linxian County of Henan Province and biostratigraphical correlation. Regional Geology of China = Zhongquo Quyu Dizhi, 2:123128.Google Scholar
Pyle, L. J., and Barnes, C. R. 2000. Upper Cambrian to Lower Silurian stratigraphic framework of platform-to-basin facies, northeastern British Columbia. Bulletin of Canadian Petroleum Geology, 48:123149.CrossRefGoogle Scholar
Pyle, L. J., and Barnes, C. R. 2001. Ordovician-Silurian stratigraphic framework, Macdonald Platform to Ospika Embayment transect, northeastern British Columbia. Bulletin of Canadian Petroleum Geology, 49:513535.CrossRefGoogle Scholar
Pyle, L. J., and Barnes, C. R. 2002. Taxonomy, evolution and biostratigraphy of conodonts from the Kechika Formation, Skoki Formation and Road River Group (Upper Cambrian to Lower Silurian), northeastern British Columbia. National Research Council of Canada Monograph Series, 44461, 227 p.Google Scholar
Pyle, L. J., and Barnes, C. R. 2003. Conodonts from a platform-to-basin transect, Lower Ordovician to Lower Silurian, Northeastern British Columbia, Canada. Journal of Paleontology, 77:146171.Google Scholar
Repetski, J. E. 1982. Conodonts from El Paso Group (Lower Ordovician) of westernmost Texas and southern New Mexico. New Mexico Bureau of Mines and Mineral Resources, Memoir 40, 121 p.Google Scholar
Repetski, J. E., and Ethington, R. L. 1983. Rossodus manitouensis (Conodonta), a new early Ordovician index fossil. Journal of Paleontology, 57:289301.Google Scholar
Rohr, D. M., Norford, B. S., and Yochelson, E. L. 1995. Stratigraphically significant Early and Middle Ordovician gastropod occurrences, western and northwestern Canada. Journal of Paleontology, 69:10471053.CrossRefGoogle Scholar
Ross, R. J. Jr., Hintze, L. F., Ethington, R. L., Miller, J. F., Taylor, M. E., and Repetski, J. E. 1997. The Ibexian, lowermost Series in the North American Ordovician, p. 150. In Taylor, M. E. (ed.), Early Paleozoic Biochronology of the Great Basin. U.S. Geological Survey Professional Paper 1579.Google Scholar
Seo, K., Lee, H., and Ethington, R. L. 1994. Early Ordovician conodonts from the Dumugol Formation in the Baegunsan Syncline, eastern Yeongweol and Samcheog areas, Kangweon-Do, Korea. Journal of Paleontology, 68:599616.CrossRefGoogle Scholar
Smith, M. P. 1991. Early Ordovician conodonts of East and North Greenland. Meddelelser om Gr⊘nland, Geoscience, 26:181.Google Scholar
Stait, K. A., and Druce, E. C. 1993. Conodonts from the Lower Ordovician Coolibah Formation, Georgina Basin, central Australia. AGSO Journal of Australian Geology and Geophysics, 13:293322.Google Scholar
Stouge, S., and Bagnoli, G. 1988. Early Ordovician conodonts from Cow Head Peninsula, western Newfoundland. Palaeontographia Italica, 75:89179.Google Scholar
Stouge, S., and Bagnoli, G. 1990. Lower Ordovician (Volkhovian-Kundan) conodonts from Hägudden, northern Öland, Sweden. Palaeontographia Italica, 77:154.Google Scholar
Sweet, W. C., and Schönlaub, H. P. 1975. Conodonts of the genus Oulodus Branson and Mehl, 1933. Geologica et Palaeontologica, 9:4159.Google Scholar
Sweet, W. C., Ethington, R. L., and Barnes, C. R. 1971. North American Middle and Upper Ordovician conodont faunas. Geological Society of America Memoir, 127:163193.CrossRefGoogle Scholar
Tipnis, R. S., Chatterton, B. D. E., and Ludvigsen, R. 1978. Ordovician conodont biostratigraphy of the southern district of Mackenzie, Canada, p. 3991. In Stelck, C. R. and Chatterton, B. D. E. (eds.), Western and Arctic Canadian Biostratigraphy. Geological Association of Canada Special Paper 18.Google Scholar
van Wamel, W. A. 1974. Conodont biostratigraphy of the Upper Cambrian and Lower Ordovician of north-western Öland, south-eastern Sweden. Utrecht Micropaleontology Bulletin, 10:1126.Google Scholar
Walcott, C. D. 1928. Pre-Devonian Paleozoic formations of the Cordilleran provinces of Canada. Smithsonian Miscellaneous Collections, 75(5):175368.Google Scholar