Paper No. 1
Presentation Time: 8:05 AM


CUI, Huan, Department of Geology, University of Maryland, College Park, MD 20742, KAUFMAN, Alan J., Geology Department, University of Maryland, College Park, MD 20742, XIAO, Shuhai, Department of Geosciences, Virginia Polytechnic Institute and State University, 4044 Derring Hall, Blacksburg, VA 24061, ZHOU, Chuanming, Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences, Nanjing, 210008, China and ZHU, Maoyan, LPS, Nanjing Institute of Geology and Palaeontology, 39 East Beijing Road, Nanjing, 210008, China,

A basin-wide analysis of the Ediacaran Doushantuo Formation in South China provides a unique geological framework for the study of the enigmatic Shuram carbon isotope anomaly. High resolution time-series C, S, and Sr isotope analyses in the inner shelf Jiulongwan section compared with outer shelf Zhongling and Yangjiaping sections document important contrasts that support the likelihood of strong geochemical gradients in both the abundance and isotopic composition of carbon and sulfur. New time-series data from the uppermost Doushantuo in the outer shelf section at Zhongling reveal that the Shuram anomaly is poorly developed in dolomicrites and associated calcite cements and nodules are remarkably depleted in 13C. Sulfur and carbon isotope compositions of pyrite and organic matter, respectively, in samples from Zhongling and Yangjiaping are enriched in both 34S and 13C relative to equivalent horizons in the inner shelf section at Jiulongwan. In contrast to the outer shelf sections, the Shuram carbon isotope anomaly is well expressed in carbonates at Jiulongwan. Combined these observations suggest that both alkalinity and sulfate abundance were higher in the proximal environment, which is the expected consequence of the oxidation of organic matter and pyrite on exposed continental shelves triggered by a dramatic rise of oxygen in the atmosphere. In this biogeochemical model, sulfate and fossil organic matter delivered to the near shore environment at Jiulongwan stimulated sulfate reducing bacteria within the anoxic water column, resulting in the formation of additional 13C depleted alkalinity and 34S depleted sulfide, which rained down and accumulated as carbonate and pyrite at the basin floor. In the outer shelf environment at Zhongling and Yangjiaping we consider the possibility that sulfate was more limited and that the anaerobic oxidation of methane by sulfate reducers in pore waters resulted in both the 34S enrichment of pyrite and the formation of authigenic calcite cements strongly depleted in 13C. This analysis suggests that the worldwide expression of the Shuram anomaly is strongly linked to enhanced terrestrial chemical weathering, which is further supported by a rise in 87Sr/86Sr during this interval, stimulated by a pulsed rise in atmospheric oxygen.