Paper No. 5
Presentation Time: 2:00 PM


BEARD, J. Andrew, Center for Integrative Geosciences, University of Connecticut, 354 Mansfield Road U-1045, Storrs, CT 06269, IVANY, Linda, Department of Earth Sciences, Syracuse University, Department of Earth Sciences, Syracuse University, Syracuse, NY 13244 and RUNNEGAR, Bruce, Dept. of Earth and Space Sciences and Institute of Geophysics and Planetary Physics, University of California, Los Angeles, CA 90095-1567,

Constraining paleoclimate conditions over the transition from a glaciated world to an ice-free one during the Permian is a topic of great interest due to the many ways it mirrors the present. The method commonly employed for understanding ancient temperatures is the use of the oxygen isotope values of marine carbonate, but this approaches is complicated when used on specimens older than the Cretaceous, due to uncertainties surrounding the potential for diagenesis and the uncertain isotopic composition of seawater prior to the Cenozoic. Microsampled accretionary calcite from fossil bivalves in SE Australia record the seasonal cycle of water temperature variation, thus demonstrating the primary nature of the isotope signal and allowing for evaluation of Permian seawater isotope composition and water temperature. The presence of co-occurring dropstones, diamicts, and glendonites constrain winter temperatures to near-freezing and allow for calculations of water composition. These records recovered from the bivalve Eurydesma span roughly 11° of paleolatitude (North Sydney Basin, New South Wales to Hobart, Tasmania) and reveal cyclic seasonal fluctuations in δ18Ocarb­ that vary with latitude. δ13Ccarb values exhibit ~1‰ of seasonal variation and are in agreement with characteristically positive values for the early Permian of ~5.5‰. The δ18Ocarb values vary seasonally in single specimens by up to 3.3‰ around a mean that decreases poleward from -1.2‰ to -1.8‰; more enriched isotope values correspond to dark growth bands within the shells, suggesting slower growth in the winter months. A decrease in both mean δ18O and seasonal amplitude with increasing latitude is similar to that observed off the coast of Greenland today. The reduction in amplitude is a result of decreasing summer temperatures, but relatively stable winter minima because of freezing conditions. The decrease in δ18Ocarb with latitude reflects a regional decrease in δ18Owater associated with the input of isotopically depleted fresh water, similar to that observed over a similar span of latitude in Greenland today. The magnitude of depletion, ~3‰ more than that seen in Greenland today, suggests either much fresher water or, potentially, more negative global average seawater.