Paper No. 12
Presentation Time: 4:05 PM


DOEBBERT, Amalia C., BP America, 1015 Aurora Street, Houston, TX 77009, JOHNSON, Clark M., Department of Geoscience, University of Wisconsin-Madison, NASA Astrobiology Institute, 1215 W. Dayton St, Madison, WI 53706, CARROLL, Alan R., Department of Geoscience, University of Wisconsin, Madison, 1215 West Dayton St, Madison, WI 53706, BEARD, Brian L., Department of Geoscience, University of Wisconsin-Madison, 1215 W. Dayton St, Madison, WI 53706, PIETRAS, Jeffrey T., Department of Geological Sciences, Binghamton University, Binghamton, NY 13902, RHODES-CARSON, Meredith, Geofuels, LLC, Madison, WI 53706, NORSTED, Brooke, Department of Geoscience, University of Wisconsin, Madison, Madison, WI 53706 and THROCKMORTON, Lauren A., Houston, TX 77079,

Many large modern lakes integrate drainage from across a geographically extensive watershed, and their character is often strongly influenced by climatic, geologic, and geomorphic processes occurring far from the lake itself. However, the depositional records of ancient lakes are nearly always interpreted solely in terms of local tectonic and climatic factors. Strontium isotopic ratios preserved in lacustrine carbonate offer a unique tool for deducing lakewater provenance, and therefore can facilitate reconstruction of the relationship between ancient lakes to their associated watershed. However, the 87Sr/86Sr ratios incorporated into lacustrine carbonates reflect not only the 87Sr/86Sr ratios of surrounding rocks, but the concentrations of Sr in the source terranes and their susceptibility to both physical and chemical weathering. Sr behavior should not be expected to be the same in every lake due to varying hydrology, geologic settings, and climate in lacustrine systems. In particular, the magnitude and rate of change expected in 87Sr/86Sr ratios and Sr concentrations of lacustrine waters needs to be considered in evaluation of 87Sr/86Sr records from lacustrine carbonates. In order to test controls on driving mechanisms associated with strontium isotope variability in lacustrine systems, we use a variable-volume reservoir model to investigate lacustrine evolution in response to changing concentration, composition, and size of influx in a variable-size Sr reservoir (lake), a model that best applies to lacustrine basins with closed hydrology.

Application of this model to the Green River Formation of Wyoming shows that rates of Sr sequestration can exert a strong influence on lacustrine Sr concentration, and consequently on rates of 87Sr/86Sr evolution in lacustrine systems. Overall, however, modeling suggests a short residence time for Sr (~103-104 years) in the Green River Formation lacustrine system. This in turn suggests that Sr isotopes from lacustrine carbonates can provide high-resolution (~102 years) records of water provenance in lacustrine systems if a sufficient range of 87Sr/86Sr ratios are present in the lacustrine catchment area.