Abstract
The Karoo basin of South Africa exposes a succession of Upper Permian to Lower Triassic terrestrial strata containing abundant terrestrial vertebrate fossils. Paleomagnetic/magnetostratigraphic and carbon-isotope data allow sections to be correlated across the basin. With this stratigraphy, the vertebrate fossil data show a gradual extinction in the Upper Permian punctuated by an enhanced extinction pulse at the Permian-Triassic boundary interval, particularly among the dicynodont therapsids, coinciding with negative carbon-isotope anomalies.
Original language | English |
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Pages (from-to) | 709-714 |
Number of pages | 6 |
Journal | Science |
Volume | 307 |
Issue number | 5710 |
DOIs | |
Publication status | Published - 4 Feb 2005 |
ASJC Scopus subject areas
- Multidisciplinary