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Check out D'Hondt et al in Geology 22:983-986 (Nov. 1994) for a good analysis of acid rain. Unlikely it did it. Signor-Lipps could certainly account for the last meter of missing verts. The record in all environments is generally poor enough that paleontologists should not rely on such details. Two factors enter: sampling error=we just missed finding the stuff; and bias=the animals simply did not live at a site throughout the entire time of their existance. In other words they emmigrated or migrated out of the site of deposition. True, not only for verts, but for the microplankton too. That's largely why they show a Sig-Lipps. Dave Lindberg and I have a paper in the works doing a complete reanalysis of Sig-Lipps and it cannot be avoided. What paleontologists can do best at these extinction events is to say something about conditions before and after, not during, the event, and how the faunas/floras changed systematically. There was certainly an extinction of dinosaurs (even if some are hiding out in the jungles today) based simply on what we've known for years about the generalities of their distribution. If we develop models for the changes we see and ask that the non-paleo types reconcile those bio-based models with their own, we might see some progress on this. As long as geophysicists keep telling us how dinosaurs +others went out and we keep telling them our stories, we'll never get at this problem. The K/T extinction event evidence comes not from paleo so much, but from geochem, mineralogy, and geology. At least in detail. Jere Jere H. Lipps Professor, Department of Integrative Biology Director, Museum of Paleontology University of California at Berkeley Berkeley, CA 94720 510-642-9006 fax 642-1822 jlipps@ucmp1.berkeley.edu
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