Confirmation of the Floian-Darriwilian (Lower to Middle Ordovician) hiatus in the Taebaek Group, Korea: integration of conodont biostratigraphy and sedimentology

Author:

Lee Byung-Su,Cho Se Hyun,Choh Suk-Joo,Wang Xunlian

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference96 articles.

1. Àlvaro, J.J., Vennin, E., Moreno-Eiris, E., Perejón, A., and Bechstädt, T., 2000, Sedimentary patterns across the Lower-Middle Cambrian transition in the Esla nappe (Cantabrian Mountains, northern Spain). Sedimentary Geology, 137, 43–61.

2. An, T.X., Du, G.Q., Gao, Q.Q., Chen, X.B., and Li, W.T., 1981, Ordovician conodont biostratigraphy of the Huanghuachang area of Yichang, Hubei. Selected Papers of the 1st Convention of Micropalaeontological Society of China, Science Press, Beijing, p. 105–113. (in Chinese)

3. An, T.X., Zhang, F., Xiang, W.D., Zhang, Y.Q., Xu, W.H., Zhang, H.J., Jiang, D.B., Yang, C.S., Lin, L.D., Cui, Z.T., and Yang, X.C., 1983, The Conodonts of North China and the Adjacent Regions. Science Press, Beijing, 233 p. (in Chinese with English abstract)

4. Bergström, S.M., 1970, Conodont biostratigraphy of the Middle and Upper Ordovician of Europe and eastern North America. In: Sweet, W.C. and Bergström, S.M. (eds.), Symposium on Conodont Biostratigraphy. Geological Society of America Memoirs, 127, p. 83–162.

5. Branson, E.B. and Mehl, M.G., 1933, Conodonts from the Jefferson City (Lower Ordovician) of Missouri. University of Missouri Studies, 8, 53–64.

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