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Regarding the P/T: I attended recently a meeting where a Chinese coleague displayed a slide illustrating the P/T boundary at its "type-locality" somewhere in the Sichuan (?) basin. I was really surprized (I was not the only one) to see that it falls in the middle of a limestone bed thought some obvious sedimentary changes take place below (in addition, there were not much paleontological evidences to support such a choice). Obviously there is no event in this type-section. It looks like people selected the median part of the bed to make sure of the continuity of the sedimentary record (in accordance to a "certain" rule!)! Which is not the case at the K/T boundary for instance! There are geochimical, even paleontological, and obviously sedimentological evidences to define the boundary at a sedimentary break taking place below this bed (there is possibly a missing time-record but "nobody is perfect"). I welcome more information on this particular sub-topic ... Cheers, B.G. ----- Original Message ----- From: "Peter Ward" <argo@u.washington.edu> To: <paleonet@nhm.ac.uk> Cc: <PaleoNet@ucmp1.Berkeley.edu> Sent: Monday, September 24, 2001 7:49 PM Subject: Re: paleonet Fwd: NYTimes.com Article: A Stark Explanation for Mankind From an Unlikely Rebel > I worked on (and am in) this series. Episode 3 (tomorrow night) profiles > extinction. There are some wonderful images of the P/T boundary in the > Karoo desert of South Africa, as well as images of late Permian > dicynodont skeletons from the South African Museum in Cape Town. This > episode is rich in fossil content. > > 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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