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Science 21 November 2003: Vol. 302. no. 5649, pp. 1388 - 1392 DOI: 10.1126/science.1090852
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Reports
Chondritic Meteorite Fragments Associated with the Permian-Triassic Boundary in Antarctica
Asish R. Basu,1*
Michail I. Petaev,2,3
Robert J. Poreda,1
Stein B. Jacobsen,2
Luann Becker4
Multiple chondritic meteorite fragments have been found in two sedimentary rock samples from an end-Permian bed at Graphite Peak in Antarctica. The Ni/Fe, Co/Ni, and P/Fe ratios in metal grains; the Fe/Mg and Mn/Fe ratios in olivine and pyroxene; and the chemistry of Fe-, Ni-, P-, and S-bearing oxide in the meteorite fragments are typical of CM-type chondritic meteorites. In one sample, the meteoritic fragments are accompanied by more abundant discrete metal grains, which are also found in an end-Permian bed at Meishan, southern China. We discuss the implications of this finding for a suggested global impact event at the Permian-Triassic boundary.
1 Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA.
2 Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA.
3 Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, MA 02138, USA.
4 Institute of Crustal Studies, Department of Geology, University of California, Santa Barbara, CA 93106, USA.
* To whom correspondence should be addressed. E-mail: abasu{at}earth.rochester.edu
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