2005 Salt Lake City Annual Meeting (October 16–19, 2005)

Paper No. 2
Presentation Time: 1:55 PM


MONTANEZ, Isabel, Department of Earth and Planetary Sciences, University of California, Davis, One Shields Dr., Davis, CA 95616, TABOR, Neil J., Department of Geological Sciences, Southern Methodist Univ, Dedman College, Dallas, TX 75275, FIELDING, Christopher R., Dept. of Geosciences, University of Nebraska, Lincoln, NE 68588-0340, FRANK, Tracy, Department of Geosciences, Univ of Nebraska, Lincoln, NE 68588-0340, ISBELL, John, Dept. of Geosciences, University of Wisconsin, Milwaukee, WI 53201 and NIEMEIER, Deb, Dept. of Civil and Environmental Engineering, Univ. of California, Davis, CA 95616-5270, ipmontanez@ucdavis.edu

An integration of estimated paleo-atmospheric pCO2, tropical marine and continental paleotemperatures, and glaciation history from southern Gondwana over a 40 m.y. period of Permo-Carboniferous time reveals a more dynamic transition from the Gondwanan Ice Age to a greenhouse world than previously recognized. An estimation of tropical sea-surface temperatures from a global compilation of δ18O values of calcitic brachiopods indicates the onset of rising temperatures in the early Sakmarian interrupted by significantly cooler intervals in the early Artinskian, Kungarian and Wordian. Quantitative estimates of paleo-atmospheric pCO2 were developed over this interval using the δ13C values of pedogenic carbonates and goethites and fossil plant material from the Eastern Shelf of the Midland Basin, and Paradox and Orogrande Basins and constrained by Monte Carlo simulations. Best estimates of Late Paleozoic pCO2 delineate a rise from present-day levels in the early Early Permian (2nd half of the Sakmarian) to values of up to 2500 to 3500 ppmv by end-Artinskian time. Atmospheric CO2 concentrations declined once again before the close of the Early Permian (Kungarian). Superimposed on this longer-term trend are shorter-term fluctuations in pCO2 during the early Artinskian and (possibly) end-Carboniferous. Parallel shifts in paleo-atmospheric CO2 and earth surface temperatures indicate a well-coupled, Late Paleozoic climate-pCO2 system. Distribution of glacigenic deposits in Antarctica and Australia indicate multiple discrete and short-lived (1 to 4 my) episodes of glaciation and colder modes that appear to coincide with short-lived but large magnitude drops in atmospheric pCO2, tropical marine temperatures and relative sea-level. Warmer periods separating glaciations appear to have been synchronous with rises in pCO2, surface temperatures, and relative sea-level. This apparent CO2-climate-glaciation link suggests that atmospheric CO2 levels may have been the primary driver for the repeated buildup and retreat of continental ice sheets during the Late Paleozoic.