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I defer to Doug Erwin and Sam Bowring on the marine P/T, but can tell you that the highest Dicynodon sp. in the Karoo occurs just beneath a laminated unit unique in the Karoo that coincides with a major C13 isotope anomaly. These results will appear in the next issue of Geology (Smith and Ward, 2001) based on three years of field collecting. So, at least in the sections I am familiar with, the mass extinction as marked by the vertebrate fossil record falls coincident with an event bed. However, the Triassic, once defined by the presence of the first Lystrosaurus sp, can no longer be based on that taxon, since Lystrosaurus is definitely a Permian taxon that survives the extinction. From my experience the taxon formerly known as Proterosuchus might best mark the base of the Triassic if vertebrate fossils are used in non marine sections. Plant microfossils will obviously be better. Professor Peter D Ward Dept of Geological Sciences 206-543-2962 ( Office ) 206-543-1190 ( Dept Office ) 206-543-3836 ( Shared Fax )
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