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Neal Evenhuis wrote: >Obviously, despite the lacustrine environment consistencies of the various >localities requested, the taphonomy of each area could be widely different >and might contain useful information to stimulate other discussions as >well. I am particularly interested in the Oeningen fossil beds in >Switzerland and how they compare in degree of insect diversity with the >Florissant beds of Colorado. Though the fossil beds of Oeningen (to my >knowledge) have not been worked for a very long time, the hypothesis had >been put forward by T.D.A. Cockerell in the early part of this century >(and also possibly by others?) that continued research might show the >Oeningen beds to be as diverse or more than the Florisssant beds. Was the >taphonomy of the organisms preserved in each of those localities the same? >or different? Both are associated with volcanic ash deposits. For Oeningen see: Wollanke, g. & Zimmerle, W. (1990) Petrographic and geographic aspects of fossil embrdding in exceptionally well preserved fossil deposits. Mitteilugen Geologisch-Palaontologischen Institut der Universitat Hamburg, 69: 77-97. For Florrisant see: McLeroy, C.A. & Anderson, R.Y. (1966) Laminations in the Oligocene Florissant Lake deposits. Geological Society of America, Bulletin, 77: 605-618. Chris cnedin@geology.adelaide.edu.au nedin@ediacara.org ------------------------------------------------------------------- Many say it was a mistake to come down from the trees, some say the move out of the oceans was a bad idea. Me, I say the stiffening of the notochord in the Cambrian was where it all went wrong, it was all downhill from there.
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