2008 Joint Meeting of The Geological Society of America, Soil Science Society of America, American Society of Agronomy, Crop Science Society of America, Gulf Coast Association of Geological Societies with the Gulf Coast Section of SEPM

Paper No. 10
Presentation Time: 3:45 PM

A Calcium Isotope Record across the Permian-Triassic Boundary from An Isolated Carbonate Platform in South China

PAYNE, Jonathan L., Department of Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Bldg 320, Stanford, CA 94305, TURCHYN, Alexandra, Department of Earth Sciences, Cambridge University, Downing Street, Cambridge, CB2 3EQ, United Kingdom, PAYTAN, Adina, Institute of Marine Sciences, University of California Santa Cruz, Santa Cruz, CA 95064, DEPAOLO, Donald J., Univ California - Berkeley, 301 McCone Hall, Berkeley, CA 94720-4767, LEHRMANN, Daniel J., Department of Geology, Univ of Wisconsin-Oshkosh, 800 Algoma Blvd, Oshkosh, WI 54901, WEI, Jiayong, Guizhou Regional Mapping Team, Guizhou Geological Survey, Bagongli, Guiyang, 550005, China and YU, Meiyi, College of Resource and Environment Engineering, Guizhou University, Guiyang, 550025, China, jlpayne@stanford.edu

We measured the calcium isotope composition (δ44Ca) of marine carbonate sediments spanning the Permian-Triassic boundary on an isolated carbonate platform in the Nanpanjiang Basin of southern China. The calcium isotope composition (δ44Ca) of the sediments exhibits a transient negative excursion of 0.2‰ to 0.3‰ across the end-Permian extinction horizon. Isotopically light values persist through the basal Triassic Hindeodus parvus conodont zone. Strata within the overlying Isarcicella isarcica zone exhibit heavier values, similar to those observed in pre-extinction strata. The excursion could reflect either a change in the local fractionation between seawater Ca and carbonate minerals or a shift in the δ44Ca composition of seawater. Because the dominant mode of carbonate deposition shifted from skeletal to microbial across the boundary, a local change in fractionation is difficult to rule out. However, δ44Ca values return to pre-extinction values within strata still lacking any significant skeletal contribution, suggesting that the isotope excursion may instead record a global shift in δ44Ca of seawater. If the values measured do reflect an excursion in the isotope composition of calcium in the oceans, they imply an increase of approximately 20% in the marine calcium concentration over a few hundred thousand years or less. Such an increase could result from ocean acidification via the addition of CO2 (and possibly SO2) to the ocean and atmosphere. Such a scenario could also account for the coeval negative excursion in δ13C and the preferential extinction of heavily calcified marine invertebrates.