Abstract
The Permian in slope facies area of southern Guizhou consists of 16 third order sequences, which can be grouped as four sequence sets and further into two mesosequences. Most of them are delineated by conformable or submarine erosion surfaces, and well controlled by conodont and fusulinid zones. Four important sea-level falls are recognized in the area, which occur respectively at the basalSweetognathodus whitei zone, lowerS.aff.hanzhongensis zone, middleJinogondolella xuanhanensis zone and the basalClarkina yini zone. Among the recognized transgression events, three are regarded as the most significant. They occur respectively at the basalNeogondolella exculptus zone, basalJinogondolella nankingensis zone and the lowerClarkina postbitteri zone, and are all accompanied by faunal turnovers. The key surfaces in sequences can be used to fine-tune the boundaries of bio-chronozones, stages and series.
Similar content being viewed by others
References
Zhang, Z. H., Wang, Z. H., Li, C. Q., Permian Stratigraphy of Southern Guizhou (in Chinese), Guiyang: Guizhou Peoples’ Press, 1988, 1–113.
Xiong, J. F., Zhai, Z. Q., Chen, L. Z., Boudary of transitional bed of Carboniferous-Permian in Luodian (black area), Guizhou, in Special Papers for Carboniferous Symposium of China (in Chinese), Beijing: Geological Publishing House, 1987, 234–242.
Wang, Z. H., Early Permian conodonts from the Nashui Section, Luodian of Guizhou, Palaeoworld, 1994, 4: 203.
Zhu, Z. L., Zhang, L. X., On the Chihsian successions in South China, Palaeoworld, 1994, 4: 114.
Sheng, J. Z., Jin, Y. G., Correlation of Permian deposits in China, Palaeoworld, 1994, 4: 14.
Jin, Y. G., Glenister, B. F., Kotlyar, G. V. et al., An operational scheme of Permian chronostratigraphy, Paleoworld, 1994, 4: 1.
Geological Survey of Guizhou Province, The Geology of Guizhou Province (in Chinese), Beijing: Geological Publishing House, 1987, 1–698.
Feng, Z. Z., Jin, Z. K., Yang, Y. Q. et al., Permian Lithological Paleogeography of Yunnan-Guizhou-Guangxi Region (in Chinese), Beijing: Geological Publishing House, 1994, 1–247.
Sha, Q. A., Wu, W. S., Fu, J. M., A Comprehensive Study of the Permian in Guizhou and Guangxi Region—wiith Reference on the Oil-Gas Potentials (in Chinese), Beijing: Science Press, 1990, 1–207.
Wu, H. R., Kuang, G. D., Wang, Z. C., Apreliminary sutdy of Late Paleozoic tectonic-sedimentary background in Guangxi Province, Scientia Geologica Sinica (in Chinese), 1997, 32(1): 11.
Metcalfe, I., Late Palaeozoic-Early Mesozoic evolution and palaeogeography of eastern Tethys, in Proceedings of the International Conference on Pangea and the Paleozoic-Mesozoic Transition (in Chinese) ((eds. Yin, H. F., Tong, J. N.), Wuhan: China Univ. Geosci. Press, 1999, 131–133.
Yin, H. F., Wu, S. B., Du, Y. S. et al., South China defined as part of Tethyan archipelagic ocean system, Earth Science-Jour. China Univ. Geosci. (in Chinese), 1999, 24(1): 1.
Jin, Y. G., Wardlaw, B. R., Glenister, B. F. et al., Permian chronostratigraphic subdivisions, Episodes, 1997, 20(1/2): 10.
Remane, J., International Stratigraphic Chart (Preliminary Edition), IUGS, 1998.
Bowring, S. A., Erwin, D. H., Jin, Y. G. et al., U/Pb zircon geochronology and tempo of the End-Permian mass extinction, Science, 1998, 280: 1039.
Boardman, D. B., Nestell, M. K., Wardlaw, B. R., Uppermost Carboniferous and Lowermost Permian deposition and conodont biostratigraphy of Kansas, USA, Palaeoworld, 1998, 9: 19.
Snyder, W. S., Gallegos, D. M., Sequence stratigraphy along Aidaralash Creek and the Carboniferous/Permian GSSP, Permophiles, 1997, 30: 8.
Chernykh, V. V., Ritter, M., Conodont biostratigraphy of Nikolsky section (southern Urals): a progress report, Permophiles, 1996, 29: 37.
Mei, S. L., Shi, X. Y., Chen, X. F. et al., Permian Cisuralian and Guadalupian sequence stratigraphy in south Guizhou and central Guangxi and its relation to conodont evolution, Earth Science-Jour. China Univ. Geosci.(in Chinese), 1999, 24(1): 21.
Mei, S. L., Zhu, Z. L., Shi, X. Y. et al., Sequence stratigraphy of Permian Lopingian strata in central Guangxi, Geoscience (in Chinese), 1999, 13(1): 11.
Wang, C. Y., Wu, J. J., Zhu, T., Permian conodonts from the Penglaitan section, Laibin County, Guangxi and the base of the Wuchiapingian stage (Lopingian Series), Acta Micropalaeontologica Sinica (in Chinese), 1998, 15(3): 226.
Tong, J. N., Yin, H. F., The marine Triassic sequence stratigraphy, Science in China, Ser. D, 1998, 41(3): 255.
Wang, H. Z., Shi, X. Y., A scheme of the hierarchy for sequence stratigraphy, J. China Univ. Geosci. (in Chinese), 1996, 7(1): 1.
Ross, C. A., Ross, J. R. P., Permian sequence stratigraphy, in The Permian of Northern Pangea ((eds. Scholle, P. A., Peryt, T. M., Ulmer-Scholle, D. S.), Berlin: Springer-Verlag, 1995, 98–123.
Davydov, V. I., Fusulinid biostratigraphy and the correlation of Mescovian-Guadalupian North America, Tethyan and Boreal (Russian Platform/Uralian) standards, Permophiles, 1996, 29: 47.
Zhou, Z. R., Glenister, B. F., Furnish, W. M. et al., Muti-Episodal extinction and ecological differentation of Permian ammonoids, Permophiles, 1996, 29: 52.
Jin, Y. G., Zhang, J., Shang, Q. H., Two phases of the end-Permian mass extinction, Can. Soc. Petrol. Geol., 1994, 17: 813.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Shi, X., Mei, S. & Sun, Y. Permian sequence stratigraphy of slope facies in southern Guizhou and chronostratigraphic correlation. Sci. China Ser. D-Earth Sci. 43, 63–76 (2000). https://doi.org/10.1007/BF02877831
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF02877831