2004 Denver Annual Meeting (November 7–10, 2004)

Paper No. 9
Presentation Time: 10:00 AM


JIANG, Ganqing, Department of Geoscience, Univ of Nevada, Las Vegas, NV 89154, KENNEDY, Martin J., Department of Earth Sciences, Univ of California, Riverside, 900 University Avenue, Riverside, CA 92521, CHRISTIE-BLICK, Nicholas, Department of Earth and Environmental Sciences and Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10968, MROFKA, David, Department of Earth Sciences, Univ of California, Riverside, CA 92521, WU, Huaichun, School of Earth Sciences and Resources, China Univ of Geosciences, Beijing, 100083 and ZHANG, Shihong, School of Earth Sciences and Resources, China Univ of Geosciences, Beijing, 100083, China, ganqingj@yahoo.com

The Neoproterozoic Doushantuo Formation (~600 to ~580 Ma?) of south China has attracted considerable interest for well-preserved early animal fossils and large positive-negative d13C shifts. Detailed isotopic analysis of two platform to basin transects, however, reveals strong d13C variability and trends between sections both adjacent and across the shelf to basin transects. Such isotopic heterogeneity may reflect 1) strongly diachronous development of sedimentary facies and d13C values leading to incomplete stratigraphic record at corresponding sample localities, 2) large (up to 10 per mil, PDB) isotopic gradient or lateral d13C variation not representative of the whole ocean signal, and 3) pervasive diagenetic alteration that has modified the primary d13C values.

Physical stratigraphic study seems not to support large stratigraphic hiatus or truncation applicable for the inconsistent d13C trends. Strong spatial d13C variations of some intervals between closely spaced sections no more than a few kilometers apart are difficult to be interpreted as resulting from a greater Neoprotrozoic isotopic gradient. In contrast, the similar isotopic values between tectonic veins and their host rocks, and the identical d13C values between carbonate rocks and interbedded shaly layers in which carbonate components are apparently formed from later fluids favor an interpretation that the d13C values of the Doushantuo Formation have been substantially modified by diagenetic fluids, even in the dolomicrite that has been considered as least susceptible to diagenetic alteration. However, such diagenetic overprints cannot be eliminated by application of existing geochemical screens and compels a reevaluation of the Neoproterozoic carbon isotopic record.