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Comments: Converted from OV/VM to RFC822 format by PUMP V2.2X Date: Tue, 16 Jan 96 17:58:57 EST From: Doug Erwin <MNHPB028@SIVM.SI.EDU> Subject: Time magazine article & metazoans (posted for A. Martin) To: <paleonet-owner@NHM.AC.UK> Status: O Actually, the point of the Time article, and the Grotzinger et al. paper in Science upon which it was based, is that the Ediacaran faunas DO NOT preceed the Burgess by 100 million years, or more. Rather, the Ediacaran faunas have now been tightly constrained by Grotzinger, Bowring, Saylor and Kaufman to 565-543 (the pC/C boundary) with the Burgess and about 520. The old gap between the Ediacaran and the onset of the Cambrian small shellies (now in the Earliest Cambrian Manykaian Stage - see Knoll et al in the Dec. 1995 GEology) has virtually vanished. The oldest metazoans remains a contentious issue, with no clear resolution. Mitch Sogin's molecular data would suggest the higher eukaryote radiation (which preceeded the origin of metazoa) occurred somewhere from 1200 mya to 800 mya, but the dates could be way off. Trace fossil evidence is unconvincing, so the earliest good metazoans are probably the Twichia disks from the MacKenzie Mtns of Canada at about 610 mya. As with the Ediacaran fauna and the early Cambrian, we are probably a long way from pinning down the earliest metazoans. And if Davidson et al are correct (Science 1995 v. 270, pp1319-1325) we wouldn't find the earliest metazoans anyway. There are substanitive difficulties with their arguments, however.
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