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Detailed Reference Information |
Shen, Y. and Schidlowski, M. (2000). New C isotope stratigraphy from southwest China: Implications for the placement of the Precambrian-Cambrian boundary on the Yangtze Platform and global correlations. Geology 28(7): 623-626. |
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A high-resolution C isotope profile from a fossiliferous section spanning the Precambrian-Cambrian (PC-C) boundary on the Yangtze Platform, southwest China, is used to constrain C isotope chemostratigraphy and its global correlation. The discovery of a strong negative C isotopic anomaly just below the China marker A indicates that this negative anomaly can be correlated globally, and demonstrates that the PC-C boundary of the Chinese successions should be close to marker A. On the basis of C isotope chemostratigraphic constraints and biostratigraphic data, we rind that C isotopic peak S2, also first reported here from the Chinese successions, can be correlated with C isotopic peak I in northern Siberia and C isotope feature D in southwest Mongolia. By integrating the data from archaeocyaeothan fauna, the C isotopic peak S3 in the middle Dahai carbonates may be correlative with feature G in the Mongolian section. |
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BACKGROUND DATA FILES |
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Abstract |
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Table 1A |
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Table 1B |
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Experimental Methods |
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Keywords
c-13/c-12, chemostratigraphy, precambrian-cambrian boundary, yangtze platform, early animal evolution, carbon-isotope, proterozoic stratigraphy, earth history, siberia, chemostratigraphy, record, region |
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Publisher
The Geological Society of America P.O. Box 9140 Boulder, CO 80301 1-303-447-2020 1-303-357-1071 member@geosociety.org |
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