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《Journal of Stratigraphy》 1986-03
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The sequence of Devonian-Carboniferous boundary beds and the regressive event of South Guizhou

Wu Xiang-he  
South Guizhou is the type area of the Lower Carboniferous of China. Based on the depositional feature and characteristic fossil assemblages two main facies of the carbonate basin and the carbonate platform may be distinguished. Each consists of the type sequence of C/D boundary beds and fossils. The sequence of the basin facies is named D-sequence, and the carbonate platform named S-sequence. As a result of studying of the two facies the regressive event may be found near the C/D boundary. Based on the foraminifers of the Xiasi section the C/D boundary of the carbonate platform is drawn near the top of Cystophrentis zone.
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