Hostname: page-component-848d4c4894-pftt2 Total loading time: 0 Render date: 2024-06-02T18:24:48.428Z Has data issue: false hasContentIssue false
  • English
  • Français

Late middle Cambrian (Cambrian Series 3) trilobite faunas from the lowermost part of the Sesong Formation, Korea and their correlation with North China

Published online by Cambridge University Press:  14 July 2015

Tae-Yoon Park ,
Ji-Hoon Kihm  and
Duck K. Choi
Tae-Yoon Park
Affiliation:
Division of Polar-Earth System Sciences, Korea Polar Research Institute, Incheon 406-840, Korea, ;
Ji-Hoon Kihm
Affiliation:
Division of Polar-Earth System Sciences, Korea Polar Research Institute, Incheon 406-840, Korea, ;
Duck K. Choi
Affiliation:
School of Earth and Environmental Sciences, Seoul National University, Seoul 151-747, Korea,
Get access Rights & Permissions [Opens in a new window]

Abstract

The Sesong Formation is a member of the Taebaek Group, Korea, which extends from late Cambrian Series 3 to middle Furongian in age. Recent studies on the trilobites of the Sesong Formation have contributed significantly to the revision of the biostratigraphy. However, trilobites in the lower part of the formation, which may include the “Stephanocare Zone”, have remained essentially overlooked since the establishment of the biozone, making it difficult to correlate with the equivalent biozones of North China. Here we report trilobite faunas from the lower part of the Sesong Formation in two different sections, the Seokgaejae and the Jikdong sections, which yield two species of Jiulongshania among other species. Species of Jiulongshania have been known to occur successively in North China, so are useful for detailed correlation. Specimens of Stephanocare richthofeni are fragmentary and rarely occur in association with Jiulongshania regularis, while Jiulongshania species occur throughout the studied intervals. Accordingly, it is reasonable to extend the previously established Jiulongshania Zone of the uppermost part of the underlying Daegi Formation into the lower part of the Sesong Formation. By doing so, the Jiulongshania Zone is correlated with the Blackwelderia Zone of North China with confidence. The lowermost part of the Sesong Formation in the Jikdong section yields a fauna including J. regularis, which implies that the boundary between the Daegi and Sesong formations is diachronous within the Taebaeksan Basin. The Daegi/Sesong formation boundary in Korea is comparable to the Zhangxia/Gushan boundary in North China in that it displays an abrupt change from a carbonate-dominant facies to a shale-dominant facies. The correlation employing the Jiulongshania species indicates that the facies shift occurred significantly earlier in Shandong, North China than in the Taebaeksan Basin, Korea.

Type
Research Article
Information
Journal of Paleontology , Volume 87 , Issue 6 , November 2013 , pp. 991 - 1003
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

Bergeron, J. N. 1899. Étude de quelques trilobites de Chine. Bulletin de la Societé Géologique de France, 3rd Series, 27:499–519.Google Scholar
Chang, W. T. 1963. A classification of the lower and middle Cambrian trilobites from north and northeastern China, with description of new families and new genera. Acta Palaeontologica Sinica, 11:447–487. (In Chinese)Google Scholar
Choi, D. K. and Chough, S. K. 2005. The Cambrian–Ordovician stratigraphy of the Taebaeksan Basin, Korea: a review. Geosciences Journal, 9:187–214.CrossRefGoogle Scholar
Choi, D. K., Chough, S. K., Kwon, Y. K., Lee, S.-B., Woo, J., Kang, I., Lee, H. S., Lee, S. M., Sohn, J. W., Shinn, Y. J., and Lee, D.-J. 2004. Taebaek Group (Cambrian–Ordovician) in the Seokgaejae section, Taebaeksan Basin: a refined lower Paleozoic stratigraphy in Korea. Geosciences Journal, 8:125–151.CrossRefGoogle Scholar
Chu, C.-L. 1959. Trilobites from the Kushan Formation of North and Northeastern China. Memoirs of the Institute of Palaeontology, Academia Sinica, 2:44–128. (In Chinese and English)Google Scholar
Duan, J.-Y., An, S.-L., Liu, P.-J., Peng, X.-D., and Zhang, L.-Q. 2005. The Cambrian stratigraphy, faunas and palaeogeography in eastern part of North China Plate. Yayuan Publishing Company, Hong Kong, 255p. (In Chinese)Google Scholar
Endo, R. and Resser, C. E. 1937. The Sinian and Cambrian formations and fossils of southern Manchoukuo. Manchurian Science Museum Bulletin, 1:1–474.Google Scholar
Fortey, R. A. 2001. Trilobite systematics: the last 75 years. Journal of Paleontology, 75:1141–1151.2.0.CO;2>CrossRefGoogle Scholar
Guo, H.-J. and Duan, J.-Y. 1978. Cambrian and Early Ordovician trilobites from northeastern Hebei and Western Liaoning. Acta Palaeontologica Sinica, 17:439–460. (In Chinese)Google Scholar
Guo, H.-J., Zan, S.-Q., and Luo, K.-L. 1996. Cambrian stratigraphy and trilobites of eastern Liaoning, Jilin University Press, Changchun, 184p. (In Chinese)Google Scholar
Hong, J., Cho, S.-H., Choh, S.-J., Woo, J., and Lee, D.-J. 2012. Middle Cambrian siliceous sponge-calcimicrobe buildups (Daegi Formation, Korea): metazoan buildup constituents in the aftermath of the early Cambrian extinction event. Sedimentary Geology, 253–254:47–57.CrossRefGoogle Scholar
Kang, I. and Choi, D. K. 2007. Middle Cambrian trilobites and biostratigraphy of the Daegi Formation (Taebaek Group) in the Seokgaejae section, Taebaeksan Basin, Korea. Geosciences Journal, 11:279–296.CrossRefGoogle Scholar
Kobayashi, T. 1931. Studies on the stratigraphy and palaeontology of the Cambro–Ordovician formation of Hualienchai and Niuhsintai, south Manchuria. Japanese Journal of Geology and Geography, 8 (3):131–189.Google Scholar
Kobayashi, T. 1935. The Cambro–Ordovician formations and faunas of South Chosen, Palaeontology, Part III: Cambrian faunas of South Chosen with a special study on the Cambrian genera and families. Journal of the Faculty of Science, Imperial University of Tokyo, Section 2, 4:49–344.Google Scholar
Kobayashi, T. 1941. Studies on Cambrian trilobite genera and families (I). Japanese Journal of Geology and Geography, 18 (1, 2):25–40.Google Scholar
Kobayashi, T. 1942. Studies on Cambrian trilobite genera and families (IV). Japanese Journal of Geology and Geography, 18 (4):197–212.Google Scholar
Kobayashi, T. 1955. Notes on Cambrian fossils from Yentzuyai, Tawenkou, in Shantung. Transactions and Proceedings of the Palaeontological Society of Japan, new series, 20:89–98.Google Scholar
Kobayashi, T. 1960. The Cambro–Ordovician formations and faunas of South Korea, part VII, Paleontology VI. Journal of the Faculty of Science, University of Tokyo, Section II 12:329–420.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 and faunas of other areas, Section A, The Chosen Group of South Korea. Journal of the Faculty of Science, University of Tokyo, Section II, 16:1–84.Google Scholar
Kruse, P. D., Jago, J. B., and Laurie, J. R. 2009. Recent developments in Australian Cambrian biostratigraphy. Journal of Stratigraphy, 33:32–47.Google Scholar
Kuo, Z. M. 1965. New material of late Cambrian trilobite fauna from the Yehli area, Kaiping Basin, Hopei. Acta Palaeontologica Sinica, 13:629–637.Google Scholar
Kwon, Y. K., Chough, S. K., Choi, D. K., and Lee, D. J. 2006. Sequence stratigraphy of the Taebaek Group (Cambrian–Ordovician), mideast Korea. Sedimentary Geology, 192:19–55.CrossRefGoogle Scholar
Lu, Y.-H. 1957. Trilobita, p. 249–294. InNanjing Institute of Geology and Palaeontology (ed.), Index Fossils of China, Invertebrates, Part 3, Geological Publishing House, Beijing. (In Chinese)Google Scholar
Lu, Y.-H., Chang, W.-T., Chu, C.-L., Chien, Y.-Y., and Hsiang, L.-W. 1965. Chinese fossils of all groups, Trilobita. Science Press, Beijing, 766p. (In Chinese)Google Scholar
Luo, H.-L., Hu, S.-X., Hou, S.-G., Gao, H.-G., Zhan, D.-Q., and Li, W. C. 2009. Cambrian stratigraphy and trilobites from Southeastern Yunnan, China. Yunnan Science and Technology Press, Kunming. (In Chinese)Google Scholar
Mansuy, H. 1915. Faunes cambriennes du Haut-Tonkin. Mémoires du Service Géologique de L'Indochine, 4:1–29.Google Scholar
Mansuy, H. 1916. Faunes Cambriennes de l'Extrême Orient méridional. Mémoires du Service Géologique de l'Indochine, 5:1–44.Google Scholar
Meng, X., Ge, M., and Tucker, M. E. 1997. Sequence Stratigraphy, sea-level changes and depositional systems in the Cambro–Ordovician of the North China carbonate platform. Sedimentary Geology, 114:189–222.CrossRefGoogle Scholar
Meyerhoff, A. A., Kamen-Kaye, M., Chen, C., and Taner, I. 1991. China—Stratigraphy, Paleogeography, and Tectonics. Kluwer Academic Publishers, Dordrecht, The Netherlands, 188p.CrossRefGoogle Scholar
Monke, H. 1903. Beiträge zur Geologie von Schantung. Part 1: Obercambrische Trilobiten von Yen-tsy-yai. Jahrbuch der Königliche Preussische Geologische Landesanstalt, Berlin, 23:103–151.Google Scholar
Nan, R. 1976. Trilobites, p. 333–351. InShenyang Institute of Geology and Mineral Resources (ed.), Palaeontological Atlas of North China, Part 1, Inner Mongolia. Geological Publishing House, Beijing.Google Scholar
Öpik, A. A. 1967. The Mindyallan fauna of north-western Queensland. Bureau of Mineral Resources, Geology and Geophysics (Australia), Bulletin 74, 404 p. and 166 p. (2 vols.).Google Scholar
Özdikmen, H. 2006. Nomenclatural changes for fourteen trilobites genera. Munis Entomology and Zoology, 1:179–190.Google Scholar
Park, T.-Y. and Choi, D. K. 2010. Two middle Cambrian diceratocephalid trilobites, Cyclolorenzella convexa and Diceratocephalus cornutus, from Korea: development and functional morphology. Lethaia, 43:73–87.CrossRefGoogle Scholar
Park, T.-Y. and Choi, D. K. 2011. Trilobite faunal successions across the base of the Furongian Series in the Taebaek Group, Taebaeksan Basin, Korea. Geobios, 44:481–498.CrossRefGoogle Scholar
Park, T.-Y., Moon, S. J., Han, Z., and Choi, D. K. 2008a. Ontogeny of the middle Cambrian trilobite Shantungia spinifera Walcott, 1905 from North China and its taxonomic significance. Journal of Paleontology, 82:851–855.CrossRefGoogle Scholar
Park, T.-Y., Han, Z., Bai, Z., and Choi, D. K. 2008b. Two middle Cambrian trilobite genera, Cyclolorenzella Kobayashi, 1960 and Jiulongshania gen. nov., from Korea and China. Alcheringa, 32:247–269.CrossRefGoogle Scholar
Park, T.-Y., Kim, J.-H., and Choi, D. K. 2009. A middle Cambrian trilobite fauna from the lowermost part of the Sesong Formation at Gadeoksan, northern part of Taebaek. Journal of Paleontological Society of Korea, 25:119–128. (In Korean)Google Scholar
Park, T.-Y., Woo, J., and Choi, D. K. 2010. A trilobite fauna from the breccias of the Daegi Formation at the Dongjeom section, Taebaek, Korea and its geological implication. Journal of Paleontological Society of Korea, 26:173–181. (In Korean)Google Scholar
Park, T.-Y., Sohn, J. W., and Choi, D. K. 2012. Middle Furongian (late Cambrian) polymerid trilobites from the upper part of the Sesong Formation, Taebaeksan Basin, Korea. Geosciences Journal, 16:381–398.CrossRefGoogle Scholar
Peng, S.-C. 2007. Historical review of trilobite research in China, p. 171–191. InMikulic, D. G. and Landing, E.(eds.), Fabulous Fossils—300 years of Worldwide Research on Trilobites. N.Y. State Museum Bulletin, New York State Museum, Albany, New York.Google Scholar
Peng, S.-C., Babcock, L. E., and Lin, H.-L. 2004. Polymerid trilobites from the Cambrian of northwestern Hunan, China. Science Press, Beijing, Volume 1, 333 p. and Volume 2, 355 p.Google Scholar
Qiu, H.-A., Lu, Y.-H., Zhu, Z.-L., Bi, D.-C., Lin, T.-R., Zhang, Q.-Z., Qian, Y.-Y., Ju, T.-Y., Han, N.-R., and Wei, X.-Z. 1983. Trilobita, p. 28–254. InPalaeontological Atlas of East China, 1: Volume of Early Palaeozoic, Geological Publishing House, Beijing. (In Chinese)Google Scholar
Raymond, P. E. 1937. Upper Cambrian and Lower Ordovician Trilobita and Ostracoda from Vermont. Bulletin of the Geological Society of America, 48:1079–1146.CrossRefGoogle Scholar
Sun, Y.-C. 1924. Contributions to the Cambrian faunas of North China. Palaeontologia Sinica, Series B, 1:1–109.Google Scholar
Walcott, C. D. 1884. Paleontology of the Eureka district. United States Geological Survey, Monograph 8, p. 1–298.CrossRefGoogle Scholar
Walcott, C. D. 1905. Cambrian faunas of China. Proceedings of the U.S. National Museum, 29:1–106.CrossRefGoogle Scholar
Walcott, C. D. 1906. Cambrian faunas of China. Proceedings of the U.S. National Museum, 30:563–595.CrossRefGoogle Scholar
Walcott, C. D. 1911. Cambrian faunas of China. Smithsonian Miscellaneous Collections, 57:69–109.Google Scholar
Walcott, C. D. 1913. The Cambrian faunas of China, p. 3–276. InResearch in China, Volume 3. Carnegie Institution of Washington, Publication 54.Google Scholar
Whittington, H. B. and Kelly, S. R. A. 1997. Morphological terms applied to Trilobita, p. 313–329. InKaesler, R. L.(ed.), Treatise on Invertebrate Paleontology, Part O, Trilobita (Revised), Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Woo, J. and Chough, S. K. 2010. Growth patterns of the Cambrian microbialite: phototropism and speciation of Epiphyton. Sedimentary Geology, 229:1–8.CrossRefGoogle Scholar
Woo, J., Chough, S. K., and Han, Z. 2008. Chambers of Epiphyton thalli in microbial buildups, Zhangxia Formation (middle Cambrian), Shandong Province, China. Palaios, 23:55–64.CrossRefGoogle Scholar
Woodward, H. 1905. On a collection of trilobites from the upper Cambrian of Shantung, N. China. Geological Press, Beijing, 560p.Google Scholar
Zhang, W.-T. 1957. Preliminary note on the lower and middle Cambrian stratigraphy of Poshan, Central Shantung. Acta Palaeontologica Sinica, 5:13–32.Google Scholar
Zhang, W.-T. and Jell, P. A. 1987. Cambrian Trilobites of North China, Chinese Cambrian Trilobites Housed in the Smithsonian Institution. Science Press, Beijing, 459p.Google Scholar
Zhang, W.-T., Xiang, L.-W., Liu, Y.-H., and Meng, X.-S. 1995. Cambrian stratigraphy and trilobites from Henan. Palaeontologia Cathayana, 6:1–166.Google Scholar
Zhu, Z.-L. 1959. Trilobites from the Kushan Formation of north and northeastern China. Memoirs of the Institute of Palaeontology, Academia Sinica, 2:1–128.Google Scholar
Zhu, Z.-L. and Wittke, H. W. 1989. Upper Cambrian trilobites from Tangshan, Hebei Province, North China. Palaeontologica Cathayana, 4:199–259.Google Scholar