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The Sinian (Terminal Proterozoic) and Early Cambrian shallow to deep water sequences of the Yangtze Platform were investigated. Based on integrated lithostratigraphic, biostratigraphic, and other approaches, the shallow water sequence from the base of the Sinian (base of the Doushantuo Formation) to the top of the Qiongzhusian (top of the Yu’anshan Formation) was subdivided into 12 stratigraphic intervals. These 12 intervals were applied in turn to the subdivision and correlation of the sequences present in various facies of the Yangtze Platform. The high resolution stratigraphic framework here developed can serve as a time frame for ongoing multidisciplinary analyses of the “Cambrian explosion”.
Based on integrated lithostratigraphic, biostratigraphic, and other approaches, the shallow water sequence from the base of the base of the Sinian (base of the Doushantuo Formation) to the top of the Qiongzhusian (top of the Yu’anshan Formation) was subdivided into 12 stratigraphic intervals. These 12 intervals were applied in turn to the subdivision and correlation of the sequences present in various facies of the Yangtze Platform. The high resolution stratigraphic framework here developed can serve as a time frame for ongoing multidisciplinary analyzes of the “Cambrian explosion”.