Hostname: page-component-848d4c4894-wg55d Total loading time: 0 Render date: 2024-05-21T12:15:16.879Z Has data issue: false hasContentIssue false

Trilobites from the Cedarina dakotaensis Zone, lowermost part of the Deadwood Formation (Marjuman Stage, Upper Cambrian), Black Hills, South Dakota

Published online by Cambridge University Press:  14 July 2015

James H. Stitt*
Affiliation:
Department of Geological Sciences, University of Missouri–Columbia, Columbia 65211

Abstract

Trilobites assigned to 14 genera and 14 species are reported from basal part of the Deadwood Formation in the Black Hills of South Dakota. Six additional taxa are left in open nomenclature. One new species, Cedarina dakotaensis, is described. These trilobites are assigned to a new zone, the Cedarina dakotaensis Zone, named after the most abundant trilobite species.

Species of Cedarina and Modocia are the most abundant in the Cedarina dakotaensis Zone, accompanied by less common specimens of species of Arapahoia, Menomonia, Hardyoides, Welleraspis, Kormagnostus, and Kingstonia. Cedarina dakotaensis and Modocia centralis are the most abundant species in the nearshore sandstone lithofacies, whereas Arapahoia spatulata is the predominate taxon in the offshore limestone lithofacies.

The fauna of the Cedarina dakotaensis Zone (which lacks species of Cedaria) occupies the biostratigraphic interval of the traditional Cedaria Zone of the Marjuman Stage. Trilobites from the Cedarina dakotaensis Zone can be used to correlate the basal part of the Deadwood with coeval strata elsewhere in 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

Aitken, J. D., Fritz, W. H., and Norford, B. S. 1972. Cambrian and Ordovician biostratigraphy of the southern Canadian Rocky Mountains. 24th International Geological Congress, Guidebook for Excursion A-19, 57 p.Google Scholar
Berkey, C. P. 1898. Geology of the St. Croix Dalles. American Geologist 21:270294.Google Scholar
Bonem, R. M. 1971. Upper Cambrian (Dresbachian) faunas of the Pilgrim Formation in southwestern Montana. Unpublished , , 204 p.Google Scholar
Deland, C. R., and Shaw, A. B. 1956. Upper Cambrian trilobites from western Wyoming. Journal of Paleontology, 30:542562.Google Scholar
Derby, J. R. 1965. Paleontology and stratigraphy of the Nolichucky Formation in southwestern Virginia and northeastern Tennessee. Unpublished , , 468 p.Google Scholar
Eby, R. G. 1981. Early Late Cambrian trilobite faunas of the Big Horse Limestone and correlative units in central Utah and Nevada. Unpublished , , 611 p.Google Scholar
Gilluly, J. 1956. General geology of central Cochise County, Arizona. U.S. Geological Survey Professional Paper 281, 169 p.CrossRefGoogle Scholar
Greggs, R. G. 1962. Upper Cambrian biostratigraphy of the southern Rocky Mountains, Alberta. Unpublished , .Google Scholar
Howell, B. F., and Duncan, C. 1939. Middle-Upper Cambrian transition fauna of North America. Wagner Free Institute Science Bulletin, 14:111.Google Scholar
Hu, C. H. 1969. Ontogeny and sexual dimorphism of three Upper Cambrain trilobites. Journal of Nanyang University, 3:438462.Google Scholar
Hu, C. H. 1971. Ontogeny and sexual dimorphism of lower Paleozoic Trilobita. Palaeontographica Americana 7, 155 p.Google Scholar
Hu, C. H. 1978. Ontogenies of four Upper Cambrian trilobites from the Bonneterre Dolomite, Missouri. Transactions and Proceedings of the Paleontological Society of Japan, new series 111:348357.Google Scholar
Hu, C. H. 1981. Studies on the ontogenetic and phylogenetic development of two Upper Cambrian trilobites from South Dakota. Transactions of the Proceedings of the Paleontological Society of Japan, 123:139167.Google Scholar
Hu, C. H. 1983. The ontogenetic development of two upper Middle Cambrian trilobites from the Bonneterre Dolomite, Missouri (with a discussion on the morphologic varieties of Cedarina vale Lochman). Memoir of the Geological Society of China, 5:275280.Google Scholar
Hu, C. H., and Li, I. L. 1971. Ontogenies of four proparian trilobites from the Upper Cambrian, Montana, U.S., (with a description of Vernaculina lushihi n. sp.). Proceedings of the Geological Society of China, 14 Hughes, N. C., Gunderson, G. D., and Weedon, M. J. 1997. Circumocular suture and visual surface of “Cedariawoosteri (Trilobita, Late Cambrian) from the Eau Claire Formation, Wisconsin. Journal of Paleontology, 71:103107.Google Scholar
Kobayshi, T. 1935. The Cambro-Ordovician formations and faunas of South Chosen; Paleontology; part III, Cambrian faunas of South Chosen with a special study on the Cambrian trilobite genera and families. Toky. Imperial University, Journal of the Faculty of Science, Section 2, 4:49344.Google Scholar
Kobayshi, T. 1938. Upper Cambrian fossils from British Columbia with a discussion on the isolated occurrence of the so-called “Olenus“ beds of Mt. Jubilee. Japanese Journal of Geology and Geography, 15:149192.Google Scholar
Kulik, J. W. 1965. Stratigraphy of the Deadwood Formation, Black Hills, South Dakota and Wyoming. Unpublished , , 263 p.Google Scholar
Lochman, C. 1936. New trilobite genera from the Bonneterre Dolomite of Missouri. Journal of Paleontology, 10:3543.Google Scholar
Lochman, C. 1940. Fauna of the basal Bonneterre Dolomite (Upper Cambrian) of southeastern Missouri. Journal of Paleontology, 14:153.Google Scholar
Lochman, C. 1950. Upper Cambrian trilobites from the Little Rocky Mountains. Journal of Paleontology, 24:322349.Google Scholar
Lochman, C., and Duncan, . 1944. Early Upper Cambrian faunas of central Montana. Geological Society of America Special Paper 54, 181 p.CrossRefGoogle Scholar
Lochman, C., and Hu, C. H. 1960. Upper Cambrian faunas from the northwest Wind River Mountains, Wyoming, Part I. Journal of Paleontology, 34:793834.Google Scholar
Lochman, C., and Hu, C. H. 1961. Upper Cambrian faunas from the northwest Wind River Mountains, Wyoming, Pt. II. Journal of Paleontology, 35:125146.Google Scholar
Lochman, C., and Hu, C. H. 1962. Upper Cambrian faunas from the northwest Wind River Mountains, Wyoming, Pt. III. Journal of Paleontology, 36:128.Google Scholar
Lochman-Balk, C. 1956. The Cambrian of the Rocky Mountains and southwest deserts of the United States and adjoining Sonora Province, Mexico, p. 529661. In Rodgers, J. (ed.), Pt. 2: Australia, America, El sistema Cambrico, su paleogeografia y el problema de su base. 20th International Geological Congress, Mexico City.Google Scholar
Lochman-Balk, C. 1964. Paleo-ecologic studies of the Deadwood Formation (Cambro-Ordovician), p. 2538. In Sundaram, R. K. (ed.), Paleontology and Stratigraphy. Proceedings of Section 8 of the 22nd International Geological Congress, India.Google Scholar
Lochman-Balk, C. 1971. The Cambrian of the craton of the United States, p. 79168. In Holland, C. H. (ed.), Cambrian of the New World, Wiley-Interscience, New York.Google Scholar
Lochman-Balk, C., and Wilson, J. L. 1958. Cambrian biostratigraphy in North America. Journal of Paleontology, 36:312350.Google Scholar
Ludvigsen, R., and Westrop, S. R. 1985. Three new Upper Cambrian stages for North America. Geology, 13:139143.2.0.CO;2>CrossRefGoogle Scholar
McCubbin, D. G. 1982. Barrier island and strand-plain facies, p. 247279. In Scholle, P. A. and Spearing, D. R. (eds.), Sandstone Depositional Environments, American Association of Petroleum Geologists Memoir 31, 410 p.Google Scholar
M'Coy, F. 1849. On the classification of some British Crustacea, with notices of new forms in the University collection at Cambridge. Annual Magazine Natural History (London), Series 2, 4:161179; 392-414.CrossRefGoogle Scholar
Meek, F. B., and Hayden, F. V. 1862. Description of new Lower Silurian (Primordial), Jurassic, Cretaceous, and Tertiary fossils collected in Nebraska territory by the exploring expedition under the command of Captain W. F. Reynolds, U.S. Topographical Engineers; with remarks on the rocks from which they were obtained. Proceedings of the Academy of Natural Sciences for 1861, Philadelphia, 13:415447.Google Scholar
Melzak, A., and Westrop, S. R. 1994. Mid-Cambrian (Marjuman) trilobites from the Pika Formation, southern Canadian Rocky Mountains, Alberta. Canadian Journal of the Earth Sciences, 31:969985.CrossRefGoogle Scholar
Meyerhoff, H. A., and Lochman, C. 1934. Faunal zones in the Deadwood Formation of South Dakota. Proceedings of the Geological Society of America for 1934:352353.Google Scholar
Meyerhoff, H. A., and Lochman, C. 1935. Deadwood faunas in South Dakota and eastern Wyoming. Proceedings of the Geological Society of America for 1935, p. 386387.Google Scholar
Miller, B. M. 1936. Cambrian trilobites from northwestern Wyoming. Journal of Paleontology, 10:2334.Google Scholar
Nelson, C. A. 1951. Cambrian trilobites from the St. Croix valley. Journal of Paleontology, 25:765784.Google Scholar
Palmer, A. R. 1954. The faunas of the Riley Formation in central Texas. Journal of Paleontology, 28:709786: reprinted as University of Texas at Austin Report of Investigations no. 24.Google Scholar
Palmer, A. R. 1962. Glyptagnostus and associated trilobites in the United States. U.S. Geological Survey Professional Paper 374-F, 49 p.CrossRefGoogle Scholar
Palmer, A. R. 1965. Trilobites of the Late Cambrian Pterocephaliid Biomere in the Great Basin, United States. U.S. Geological Survey Professional Paper 374-F, 105 p.CrossRefGoogle Scholar
Palmer, A. R. 1998. A proposed nomenclature for stages and series of the Cambrian of Laurentia. Canadian Journal of Earth Sciences, 35:323328.CrossRefGoogle Scholar
Palmer, A. R., and Peel, J. S. 1981. Dresbachian trilobites and stratigraphy of the Cass Fjord Formation, western North Greenland. Gronlands Geologiske Undersogelse Bulletin 141, 46 p.Google Scholar
Pratt, B. R. 1992. Trilobites of the Marjuman and Steptoean stages (Upper Cambrian), Rabbitkettle Formation, southern Mackenzie Mountains, northwest Canada. Palaeontographica Canadiana 9, 179 p.Google Scholar
Rasetti, F. 1965. Upper Cambrian trilobite faunas of northeastern Tennessee. Smithsonian Miscellaneous Collections, 148, 127 p.Google Scholar
Raymond, P. E. 1937. Upper Cambrian and Lower Ordovician Trilobita and Ostracoda from Vermont. Geological Society of America Bulletin, 48:10791145.CrossRefGoogle Scholar
Raymond, P. E. 1938. Fourth contribution to nomenclature of Cambrian fossils. SmithsonianMiscellaneous Collections, 95:143.Google Scholar
Resser, C. E. 1935. Nomenclature of some Cambrian trilobites. Smithsonian Miscellaneous Collections, 93:146.Google Scholar
Resser, C. E. 1937. Third contribution to nomenclaure of Cambrian trilobites. Smithsonian Miscellaneous Collections, 95:129.Google Scholar
Resser, C. E. 1938. Cambrian system (restricted) of the southern Appalachians. Geological Society of America Special Paper 15, 140 p.Google Scholar
Resser, C. E. 1942. Fifth contribution to nomenclaure of Cambrian trilobites. Smithsonian Miscellaneous Collections, 101:158.Google Scholar
Richter, R. 1933. Crustacea. Handworterbuch der Naturwissenschsften, 2nd edition. v. 2. Jena, p. 840864.Google Scholar
Robison, R. A. 1960. Some Dresbachian and Franconian trilobites of western Utah. Brigham Young University Research Studies, 7, 59 p.Google Scholar
Robison, R. A. 1964. Late Middle Cambrian faunas from western Utah. Journal of Paleontology, 38:510566.Google Scholar
Robison, R. A. 1988. Trilobites of the Holm Dal Formation (late Middle Cambrian), central North Greenland. Meddelelser om Gronland, Geoscience 20:23103.CrossRefGoogle Scholar
Sepkoski, J. J. 1982. Flat pebble conglomerates, storm deposits, and the Cambrian bottom fauna, p. 371385. In Einsele, G. and Seilacher, A. (eds.), Cyclic and Event Stratification, Springer-Verlag, Berlin.CrossRefGoogle Scholar
Shaw, A. B. 1952. Paleontology of northwestern Vermont. II. Fauna of the Upper Cambrian Rockledge Conglomerate near St. Albans. Journal of Paleontology, 26:458483.Google Scholar
Shaw, A. B. 1956a. A Cambrian Aphelaspis fauna from Steel Butte, near Boulder, Wyoming. Journal of Paleontology, 30:4852.Google Scholar
Shaw, A. B. 1956b. Notes on Modocia and Middle Cambrian trilobites from Wyoming. Journal of Paleontology, 30:141145.Google Scholar
Shaw, A. B. 1966. Paleontology of northwestern Vermont. Fossils from the (Cambrian) Skeels Corners Formation. Journal of Paleontology, 40:269295.Google Scholar
Shumard, B. F. 1861. The Primordial zone of Texas, with descriptions of new fossils. American Journal of Science, 2nd series, 32:213221.CrossRefGoogle Scholar
Swinnerton, H. H. 1915. Suggestions for a revised classification of trilobites. Geological Magazine, new series, 2:407496, 538-545.Google Scholar
Syoyanow, A. A. 1936. Correlation of Arizona Paleozoic formations. Geological Society of America Bulletin, 47:459540.CrossRefGoogle Scholar
Tasch, P. 1951. Fauna and paleontology of the Upper Cambrian Warrior Formation of central Pennsylvania. Journal of Paleontology, 25:275300.Google Scholar
Tortello, M. F., and Bordonaro, O. L. 1997. Cambrian agnostid trilobites from Mendoza, Argentina: a systematic revision and biostratigraphic implications. Journal of Paleontology, 71:7486.CrossRefGoogle Scholar
Walch, J. E. I. 1771. Die Naturgeschichte der versteinerungen zur erlauterung der Knorrischen Sammlung von Merkwurdigkeiten der Natur. Nurnberg. Volume 3 of Knorr, G. W. and Walch, J. E. I., 17681774.Google Scholar
Walcott, C. D. 1884. Paleontology of the Eureka district. U.S. Geological Survey Monograph 8, 298 p.Google Scholar
Walcott, C. D. 1890. Description of new forms of Upper Cambrian fossils. U.S. National Museum Proceedings, 13(280):267279. (Published 1891).Google Scholar
Walcott, C. D. 1916. Cambrian trilobites: Smithsonian Miscellaneous Collections, 64:157258.Google Scholar
Walcott, C. D. 1924. Cambrian and lower Ozarkian trilobites, no. 2 of Cambrian geology and Paleontology, v. Smithsonian Miscellaneous Collections, 75:5360.Google Scholar
Walcott, C. D. 1925. Cambrian and Ozarkian trilobites, no. 3 of Cambrian geology and Paleontology, v. Smithsonian Miscellaneous Collections, 75:61146.Google Scholar
Weller, S. 1899. Descriptions of Cambrian trilobites from New York, with notes on the age of the Magnesian Limestone. Annual report of the Geological Survey of New Jersey, 1899:4753.Google Scholar
Westrop, S. R. 1989. Facies anatomy of an Upper Cambrian grand cycle: Bison Creek and Mistaya formations, southern Alberta. Canadian Journal of Earth Sciences, 26:2,292-2,304.CrossRefGoogle Scholar
Westrop, S. R. 1992. Upper Cambrian (Marjuman-Steptoen) trilobites from the Port au Port Group, western Newfoundland. Journal of Paleontology, 66:228255.CrossRefGoogle Scholar
Westrop, S. R., Ludvigsen, R., and Kindle, C. H. 1996. Marjuman (Cambrian) agnostid trilobites of the Cow Head Group, western Newfoundland. Journal of Paleontology, 70:804829.CrossRefGoogle Scholar
Whitfield, R. P. 1877. Preliminary report on the paleontology of the Black Hills, containing descriptions of new species of fossils from the Potsdam, Jurassic, and Cretaceous formations of the Black Hills of Dakota. U.S. Geographic and Geologic Survey of Rocky Mountain Region, (Powell), 49 p.CrossRefGoogle Scholar
Whitfield, R. P. 1880. Report on the geology and resources of the Black Hills of Dakota, p. 325468. In Newton, H., and Jenney, W. P., U.S. Geographic and Geologic Survey, Rocky Mountain Region, 566 p.Google Scholar
Whittington, H. B., and Kelly, S. R. A. 1997. Morphological terms applied to Trilobita, p. 313329. In Kaesler, R. L. (ed.), Treatise on Invertebrate Paleontology, Pt. O, Revised. ARTHROPODA 1, TRILOBITA 1. Geological Society of America and the University of Kansas Press, Lawrence, Kansas. 530 p.Google Scholar
Wilson, J. L. 1954. Late Cambrian and Early Ordovician trilobites from the Marathon uplift, Texas. Journal of Paleontology, 28:249285.Google Scholar