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Jujuyaspis and associated trilobites from the Mungok Formation (Lower Ordovician), Yongwol, Korea

Published online by Cambridge University Press:  20 May 2016

Dong Hee Kim
Affiliation:
Department of Geological Sciences, Seoul National University, Seoul 151-742, Korea, <([email protected])>
Duck K. Choi
Affiliation:
Department of Geological Sciences, Seoul National University, Seoul 151-742, Korea, <([email protected])>

Abstract

The trilobite genus Jujuyaspis Kobayashi, 1936, an index fossil of earliest Ordovician age, is recorded from the Yosimuraspis Zone of the Mungok Formation (Lower Ordovician) for the first time in Korea. The Yosimuraspis Zone comprises Yosimuraspis vulgaris Kobayashi, 1960; Jujuyaspis sinensis Zhou in Chen et al., 1980; Elkanaspis jilinensis Qian in Chen et al 1985; and pilekid genus and species indeterminate. Closely comparable faunas to the Yosimuraspis Zone are well represented in North China. The occurrence of Jujuyaspis allows the correlation of the Yosimuraspis Zone with the earliest Ordovician faunas of North America, South America, and Scandinavia, and suggests that the Cambrian-Ordovician boundary in Korea be placed at the base of the Yosimuraspis Zone.

Type
Research Article
Copyright
Copyright © The Paleontological Society

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References

Aceñolaza, F. G., and Aceñolaza, G. F. 1992. The genus Jujuyaspis as a world reference fossil for the Cambrian-Ordovician boundary, p. 8192. In Webby, B. D. and Laurie, J. R. (eds.), Global Perspectives on Ordovician Geology. Balkema, Rotterdam.Google Scholar
Balashova, E. A. 1961. Some Tremadoc trilobites of the Aktyubinsk region. Akademiya Nauk SSSR, Trudy Geologicheskogo Instituta, 18:102145. (In Russian)Google Scholar
Baldis, B. A., Gonzalez, S., and Perez, V. 1984. Trilobites tremadocianos de la Formación Negritos (Perforación La Heliera), Llanos de Colombia. III Congreso Latinoamericano de Paleontología Memorias, Mexico, 2841.Google Scholar
Bruton, D. L., Erdtmann, B. D., and Koch, L. 1982. The Naersnes section, Oslo region, Norway: a candidate for the Cambrian-Ordovician boundary stratotype at the base of the Tremadoc Series, p. 6170. In Bassett, M. G. and Dean, W. T. (eds.), The Cambrian-Ordovician Boundary: Sections, Fossil Distributions, and Correlations. National Museum of Wales, Geology Series no. 3, Cardiff, Wales.Google Scholar
Bruton, D. L., Koch, L., and Repetski, J. E. 1988. The Naersnes section, Oslo Region, Norway: trilobites, graptolite and conodont fossils reviewed. Geological Magazine, 125:451455.CrossRefGoogle Scholar
Burmeister, H. 1843. Die Organisation der Trilobiten. Berlin, 147 p.Google Scholar
Chen, J., Teichert, C., Zhou, Z., Lin, Y., Wang, Z., and Xu, J. 1983. Faunal sequences across the Cambrian-Ordovician boundary in northern China and its international correlation. Geologica et Palaeontologica, 17:115.Google Scholar
Chen, J., Qian, Y., Lin, Y., Zhang, J., Wang, Z., Yin, L., and Erdtmann, B.-D. 1985. Study on Cambrian-Ordovician Boundary Strata and its Biotas in Dayangcha, Hunjiang, Jilin, China. China Prospect Publishing House, Beijing, 138 p.Google Scholar
Chen, J., Zhang, J., Lin, Y., Yin, L., Wang, Z., Wang, Z., Yang, J., and Wang, Y. 1988. The recommended Cambrian-Ordovician global boundary stratotype of the Xiaoyangqiao section (Dayangcha, Jilin Province), China. Geological Magazine, 125:415444.Google Scholar
Chen, J., Zhou, Z., Zou, X., Lin, Y., Yang, X., Wang, Q., Qi, J., Wang, Q., and Lu, X. 1980. Ordovician sediments and faunas in the Taihang Mountains, North China. Memoirs of Nanjing Institute of Geology and Palaeontology, Academia Sinica, 16:111148. (In Chinese with English abstract)Google Scholar
Choi, Y. S., Kim, J. C., and Lee, Y. I. 1993. Subtidal flat-pebble conglomerates from the early Ordovician Mungok Formation, Korea: origin and depositional process. Journal of the Geological Society of Korea, 29:1529.Google Scholar
Choi, D. K. 1998. The Yongwol Group (Cambrian-Ordovician) redefined: a proposal for the stratigraphic nomenclature of the Choson Supergroup. Geoscience Journal, 2:220234.CrossRefGoogle Scholar
Choi, D. K., Park, G. H., and Kim, D. H. 1994. Tremadocian trilobites from the Mungog Formation, Yeongweol area, Korea. Journal of the Paleontological Society of Korea, 10:209226.Google Scholar
Cooper, R. A., and Nowlan, G. S. 1999. Proposed global stratotype section and point for base of the Ordovician System. Acta Universitatis Carolinae Geologica, 43:6164.Google Scholar
Dean, W. T. 1989. Trilobites from the Survey Peak, Outram and Skoki Formations (Upper Cambrian-Lower Ordovician) at the Wilcox Pass, Jasper National Park, Alberta. Geological Survey of Canada, Bulletin 389, 141 p.Google Scholar
Duan, J., An, S., and Zhao, D. 1986. Cambrian-Ordovician boundary and its internal biotas, southern Jilin, northeast China. Journal of Changchun College of Geology, Special Issue of Stratigraphy and Palaeontology, 135 p.Google Scholar
Fortey, R. A., and Chatterton, B. D. E. 1988. Classification of the trilobite suborder Asaphina. Palaeontology, 31:165222.Google Scholar
Fortey, R. A., and Owens, R. M. 1987. The Arenig Series in South Wales: stratigraphy and palaeontology. I. The Arenig Series in South Wales. Bulletin of the British Museum (Natural History), Geology, 41:69307.Google Scholar
Harrington, H. J. 1938. Sobre las faunas del ordoviciano inferior del norte Argentino. Revista del Museo de la Plata, nueva serie, Sectión Paleontología, 1:109289.Google Scholar
Harrington, H. J., and Leanza, A. F. 1957. Ordovician trilobites of Argentina. Department of Geology, University of Kansas, Special Publication, 1:1276.Google Scholar
Hawle, I., and Corda, A. J. C. 1847. Prodrom einer Monographie der böhmischen Trilobiten. Abhandlungen Koeniglichen Boehmischen Gesellschaft der Wissenschaften. J. C. Calve, Prague, 176 p.Google Scholar
Henningsmoen, G. 1957. The trilobite family Olenidae with description of Norwegian material and remarks on the Olenid and Tremadocian Series. Skrifter Utgitt av det Norske Videnskaps-Akademi i Oslo, I, Matematisk-naturvidenskapelig Klasse 1957(1):1303.Google Scholar
Jell, P. A. 1985. Tremadocian trilobites from the Digger Island Formation, Waratah Bay, Victoria. Memoirs of the Museum of Victoria, 46:5388.CrossRefGoogle Scholar
Kim, B. K., Cheong, C. H., and Choi, D. K. 1990. Occurrences of Sphenothallus (“Vermes”) from the Mungog and Yobong formations, Yeongweol area, Korea. Journal of the Geological Society of Korea, 31:454460.Google Scholar
Kim, D. H., and Choi, D. K. 1995. Kainella (Trilobita, Early Ordovician) from the Mungog Formation of Yeongweol area and its stratigraphic significance. Journal of the Geological Society of Korea, 31:576582.Google Scholar
Kim, D. H., and Choi, D. K. 1999. Occurrence of Leiostegium (Trilobita, Early ordovician) from the Mungok Formation, Yongwol, Korea. Journal of the Paleontological Society of Korea, 15:5458.Google Scholar
Kobayashi, T. 1934. Cambro-Ordovician formations and faunas of South Chosen, Palaeontology, Part I, Middle Ordovician faunas. Journal of the Faculty of Science, Imperial University of Tokyo, Section II, 3:329519.Google Scholar
Kobayashi, T. 1935. On the Kainella fauna of the basal Ordovician age found in Argentina. Japanese Journal of Geology and Geography, 12:5967.Google Scholar
Kobayashi, T. 1936. On the Parabolinella fauna from Province Jujuy, Argentina with a note on the Olenidae. Japanese Journal of Geology and Geography, 12:85102.Google Scholar
Kobayashi, T. 1953. On the Kainellidae. Japanese Journal of Geology and Geography, 23:3761.Google Scholar
Kobayashi, T. 1955. The Ordovician fossils from the McKay Group in British Columbia, western Canada, with a note on the Early Ordovician palaeogeography. Journal of the Faculty of Science, University of Tokyo, Section II, 9:355493.Google Scholar
Kobayashi, T. 1960. Cambro-Ordovician formations and faunas of South Korea, Part VI, Paleontology V. Journal of the Faculty of Science, University of Tokyo, Section II, 12:217275.Google Scholar
Kobayashi, T. 1966. The Cambro-Ordovician formations and faunas of South Korea, Part X, Stratigraphy of the Chosen Group in Korea and South Manchuria and its relation to the Cambro-Ordovician formations of other areas, Section A, The Chosen Group of South Korea. Journal of the Faculty of Science, University of Tokyo, Section II, 16:184.Google Scholar
Kuo, H., Duan, J., and An, S. 1982. Cambrian-Ordovician boundary in the North China platform with descriptions of trilobites. Journal of Changchun College of Geology, 3:928. (In Chinese)Google Scholar
Laurie, J. R., and Shergold, J. H. 1996. Early Ordovician trilobite taxonomy and biostratigraphy of the Emanuel Formation, Canning Basin, Western Australia (Part 1 and 2). Palaeontographica Abt. A, 240:65144.Google Scholar
Loch, J. D., Stitt, J. H., and Derby, J. R. 1993. Cambrian-Ordovician boundary interval extinctions: implications of revised trilobite and brachiopod data from Mount Wilson, Alberta, Canada. Journal of Paleontology, 67:497517.CrossRefGoogle Scholar
Loch, J. D., Stitt, J. H., and Miller, J. F. 1999. Trilobite biostratigraphy through the Cambrian-Ordovician boundary interval at Lawson Cove, Ibex, western Utah, U.S.A. Acta Universitatis Carolinae Geologica, 43:1316.Google Scholar
Lu, Y. H., 1975. Ordovician trilobite faunas of central and southwestern China. Palaeontologica Sinica, 11, 463 p. (In Chinese with English summary)Google Scholar
Ludvigsen, R. 1982. Upper Cambrian and Lower Ordovician trilobite biostratigraphy of the Rabbitkettle Formation, western District of Mackenzie. Life Sciences Contributions, Royal Ontario Museum, 134, 188 p.Google Scholar
Ludvigsen, R., Westrop, S. R., and Kindle, C. H. 1989. Sunwaptan (Upper Cambrian) trilobites of the Cow Head Group, western Newfoundland, Canada. Palaeontographica Canadiana, 6, 175 p.Google Scholar
Miller, J. F., and Stitt, J. H. 1995. Stratigraphic position and significance of Jujuyaspis and Iapetognathus in the Wilberns Formation, Texas, p. 105108. In Cooper, J. D., Droser, M. L., and Finney, S. C. (eds.), Ordovician Odyssey: Short Papers for the Seventh International Symposium on the Ordovician System. The Pacific Section Society for Sedimentary Geology, Fullerton, California.Google Scholar
Miller, J. F., and Taylor, M. E. 1995. Biostratigraphic Significance of Iapetognathus (Conodonta) and Jujuyaspis (Trilobita) in the House Limestone, Ibex area, Utah, p. 109112. In Cooper, J. D., Droser, M. L., and Finney, S. C. (eds.), Ordovician Odyssey: Short Papers for the Seventh International Symposium on the Ordovician System. The Pacific Section Society for Sedimentary Geology, Fullerton, California.Google Scholar
Nicoll, R. S., Miller, J. F., Nowlan, G. S., Repetski, J. E., and Ethington, R. L. 1999. Iapetonudus (new genus) and Iapetognathus Landing, unusual earliest Ordovician multielement conodont taxa and their utility for biostratigraphy. Brigham Young University Geology Studies, 44:27101Google Scholar
Nikolaisen, F., and Henningsmoen, G. 1985. Upper Cambrian and lower Tremadoc olenid trilobites from the Digermul Peninsula, Finnmark, northern Norway. Norges Geologiske Unders⊘kelse, Bulletin 400:149.Google Scholar
Norford, B. S. 1969. The early Canadian (Tremadocian) trilobites Clelandia and Jujuyaspis from the Rocky Mountains of Canada. Geological Survey of Canada, Bulletin 182:115.Google Scholar
Paik, I. S., Woo, K. S., and Chung, G. S. 1991. Stratigraphic, sedimentologic and paleontologic investigation of the Paleozoic sedimentary rocks in Yeongweol and Gabsan areas: depositional environments of the Lower Ordovician Mungog Formation in the vicinity of Yeongweol. Journal of the Geological Society of Korea, 27:357370.Google Scholar
Palmer, A. R. 1968. Cambrian trilobites of east-central Alaska. Lower Paleozoic paleontology and stratigraphy of east-central Alaska. United States Geological Survey Professional Paper 559–B, 115 p.Google Scholar
Park, K. H., Choi, D. K., and Kim, J. H. 1994. The Mungog Formation (Lower Ordovician) in the northern part of Yeongweol area: lithostratigraphic subdivision and trilobite faunal assemblages. Journal of the Geological Society of Korea, 30:168181.Google Scholar
Peng, S. 1990a. Tremadocian stratigraphy and trilobite fauna of northwestern Hunan. 1. Trilobites from the Nantsinkwan Formation of the Yangtze Platform. Beringeria, 2:153.Google Scholar
Peng, S. 1990b. Tremadocian stratigraphy and trilobite fauna of northwestern Hunan. 2. Trilobites from the Panjiazui Formation and the Madaoyu Formation in the Jiangnan Slope Belt. Beringeria, 2:55171.Google Scholar
PŘibyl, A., and Vanēk, J. 1980. Ordovician trilobites of Bolivia. Rozpravy Českoslevenské Akademie Vēd, Řada Matematických a PŘírodnich Věd, 90(2):390Google Scholar
Qian, Y. 1986. Trilobites, p. 255313. In Chen, J. (ed.), Aspects in Cambrian-Ordovician Boundary in Dayangcha, China. China Prospect Publishing House, Beijing.Google Scholar
Rasetti, F. 1944. Upper Cambrian trilobites from the Levis Conglomerate. Journal of Paleontology, 18:229258.Google Scholar
Raymond, P. E. 1924. New Upper Cambrian and Lower Ordovician trilobites from Vermont. Proceedings of the Boston Society of Natural History, 37:389466.Google Scholar
Robison, R. A., and Pantoja-Alor, J. 1968. Tremadocian trilobites from the Nochixtlan Region, Oaxaca, Mexico. Journal of Paleontology, 42:767800.Google Scholar
Ross, R. J. Jr. (ed.). 1982. The Ordovician System in the United States. International Union of Geological Sciences, Publication 12, 73 p.Google 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. U.S. Geological Survey Professional Paper, 1579:150.Google Scholar
Salter, J. W. 1864. A monograph of British trilobites. Part 1. Palaeontographical Society Monograph, 180.Google Scholar
Salter, J. W. 1866. On the fossils of North Wales. Memoir of the Geological Survey of Great Britain, 3:239381.Google Scholar
Stitt, J. H., and Miller, J. F. 1987. Jujuyaspis borelis and associated trilobites and conodonts from the Lower Ordovician of Texas and Utah. Journal of Paleontology, 61:112121.CrossRefGoogle Scholar
Swinnerton, H. H. 1915. Suggestions for a revised classification of trilobites. Geological Magazine (new series), 6(2):407496,538–545.Google Scholar
Taylor, J. F., and Repetski, J. E. 1995. High-Resolution trilobite and conodont biostratigraphy across the Cambrian-Ordovician boundary in south-central New Mexico, p. 133136. In Cooper, J. D., Droser, M. L., and Finney, S. C. (eds.), Ordovician Odyssey: Short Papers for the Seventh International Symposium on the Ordovician System. The Pacific Section Society for Sedimentary Geology, Fullerton, California.Google Scholar
Ulrich, E. O., and Resser, C. E. 1930. The Cambrian of the Upper Mississippi Valley. Part 1, Trilobita, Dokelocephalinae and Osceolinae. Public Museum of Milwaukee Bulletin, 12:1122.Google Scholar
Westrop, S. R. 1986. Trilobites of the Upper Cambrian Sunwaptan Stage, southern Rocky Mountains, Alberta. Palaeontographica Canadiana, 3, 179 p.Google Scholar
Westrop, S. R. 1995. Sunwaptan and Ibexian (Upper Cambrian-Lower Ordovician) trilobites of the Rabbitkettle Formation, Mountain River region, northern Mackenzie Mountains, northwest Canada. Palaeontographica Canadiana, 12, 75 p.Google Scholar
Whittington, H. B., and Kelly, S. R. A. 1997. Morphological terms applied to Trilobita, p. 313330. In Whittington, H. B., Chatterton, B. D. E., Speyer, S. E., Fortey, R. A., Owens, R. M., Chang, W. T., Dean, W. T., Jell, P. A., Laurie, J. R., Palmer, A. R., Repina, L. N., Rushton, A. W. A., Shergold, J. H., Clarkson, E. N. K., Wilmot, N. V., and Kelly, S. R. A. (eds.), Treatise on Invertebrate Paleontology, Part O, Revised, Arthropoda 1, Trilobita 1. Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Whitworth, P. H. 1969. The Tremadoc trilobite Pseudokainella impar (Salter). Palaeontology, 12:406413.Google Scholar
Winston, D., and Nicholls, H. 1967. Late Cambrian and Early Ordovician faunas from the Wilberns Formation of Central Texas. Journal of Paleontology, 41:6696.Google Scholar
Yosimura, I. 1940. Geology of the Neietsu District, Kogendo, Tyosen (Korea). Journal of the Geological Society of Japan, 47:112122. (in Japanese)CrossRefGoogle Scholar
Zhou, Z. Y., and Zhang, J. L. 1978. Cambrian-Ordovician boundary of the Tangshan area with descriptions of the related trilobite fauna. Acta Palaeontologica Sinica, 17:132. (In Chinese with English summary)Google Scholar
Zhou, Z. Y., and Zhang, J. L. 1985 (dated 1984). Uppermost Cambrian and lowest Ordovician trilobites of North and Northeast China, p. 63163. In Nanjing Institute of Geology and Palaeontology (ed.), Stratigraphy and Palaeontology of Systemic Boundaries in China, Cambrian-Ordovician Boundary (2). Anhui Science and Technology Publishing House, Hefei.Google Scholar