Diversification of ordovician chitinozoans from South China, and its relationships with environment changes

Keywords

Ordovician / Time Slice / Foreland Basin / Late Ordovician / Yangtze Platform

References

[1] Chen X. H., Zhang M., Wang C. S.. The Ordovician Chitinozoan from South China, 2009, Beijing: Geological Publishing House 218

[2] Hou J. P., Wang X. F.. Chitinozoan Biostratigraphy in China. Bulletin of Society of Geology and Mineralogy, Bretagne C, 1982, 14(2): 78-89.

[3] Paris F., Achab A., Asselin E., . Webby B. D., Paris F., Droser M., . Chitinozoa. The Great Ordovician Biodiversification Event, 2004, New York: Columbia University Press 289 311

[4] Schmitz, B., Harper, D. A. T., Peucker-Ehrenbrink, B., et al., 2007. Asteroid Breakup Linked to the Great Ordovician Biodiversification Event. Nature, doi: 10.1038/ngeo.2007.37

[5] Shaw A.. Time in Stratigraphy, 1964, New York: McGraw-Hill 365

[6] Stouge, S., Wang, X. F., Wang, C. S., et al., 2005. Graphic Correlation of High-Latitude Lower-Middle Ordovician Boundary Successions from South China and Northeast Europe: Comparison with Low-Latitude Sections from North America and Argentina. http://www.ordovician.cn

[7] Wang X. F., Chen X. H.. Ordovician Chitinozoan Diversification Events in China. Science in China (Series D), 2004, 47(10): 874-879.

[8] Webby B. D., Cooper R. A., Bergström S. M., . Webby B. D., Paris F., Droser M., . Stratigraphic Framework and Time Slices. The Great Ordovician Biodiversification Event, 2004, New York: Columbia University Press 41 47

[9] Xu X. S., Wan F., Yin F. G., . Environment Facies Ecological Facies and Diagenrtic Facies of Baota Formation of Late Ordovician. Journal of Mineralogy and Petrology, 2001, 21(3): 61-68.