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U/Pb Zircon Geochronology and Tempo of the End-Permian Mass Extinction
S. A. Bowring,*
D. H. Erwin,
Y. G. Jin,
M. W. Martin,
K. Davidek,
W. Wang
The mass extinction at the end of the Permian was the most profound
in the history of life. Fundamental to understanding itscause is
determining the tempo and duration of the extinction.Uranium/lead
zircon data from Late Permian and Early Triassicrocks from south China
place the Permian-Triassic boundary at251.4 ± 0.3 million years
ago. Biostratigraphic controls fromstrata intercalated with ash beds
below the boundary indicatethat the Changhsingian pulse of the
end-Permian extinction, correspondingto the disappearance of about 85 percent of marine species, lastedless than 1 million years. At
Meishan, a negative excursion in13C at the boundary had
a duration of 165,000 years or less, suggestinga catastrophic addition
of light carbon.
S. A. Bowring, M. W. Martin, and K. Davidek are in the
Department of Earth, Atmospheric and Planetary Sciences, Massachusetts
Institute of Technology, Cambridge, MA 02319, USA. D. H. Erwin is in the Department of Paleobiology, National Museum of Natural
History, Washington, DC 20560, USA. Y. G. Jin and W. Wang are
at the Laboratory of Paleobiology and Stratigraphy, Nanjing Institute
of Geology and Paleontology, Academia Sinica, Nanjing, 210008, People's Republic of China.
*
To whom correspondence should be addressed.
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Paul Wignall, Bruce Thomas, Robbert Willink, John Watling;, Becker, R. J. Poreda, and K. O. Pope (22 October 2004) Science306 (5696), 609d.
[DOI: 10.1126/science.306.5696.609d] |Full Text »|PDF »
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