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Raul- Can you give some more information on the bed's geological context (i.e., is it unique in the formation,or part of a recognizable cycle? does it differ from the the underlying and overlying beds in any sedimentological aspects other than bioclastic concentration? Does it have evidence of a scoured base, graded bedding, or cross-bedding? Are the shells and bones current-aligned? A good place to start might be numerous papers on storm sedimentation in this volume: Cyclic and Event Stratification (Ed. by G. Einsele & A. Seilacher), pp. 161–174. Springer Verlag, New York. Another similar volume with the title "Cycles and Events in Stratigraphy" was published in 1991, and is also worth checking out. The papers on the Triassic Musselkalk might be especially interesting as they discuss both vertebrate and invertebrate remains in storm beds, I believe. They are both available at the UCR library, not far from you. Good luck, -Seth ---- Original message ---- >Date: Thu, 5 Jan 2006 09:56:13 -0800 >From: "Esperante, Raul \(LLU\)" <resperante@llu.edu> >Subject: paleonet storm shelly deposits >To: <paleonet@nhm.ac.uk> > > Happy New Year to all paleonetters: > > I am requesting some guidance in regard to a > possible storm deposit with marine vert and invert > material. The deposit consists of a 20-cm thick > layer of sst with shells and abundant marine > vertebrates, including sharks, fish and cetaceans. A > Georef search hasn't provided references that I use > to compare with. Could someone provide me with some > references of studies done in possible sotrm beds > with vert and invert material? Or can give a hint on > what the layer I'm studying could be? > > Raúl Esperante, PhD > Paleontologist > Geoscience Research Institute > Loma Linda, California 92350, USA > Tel. (909) 558 4548 > FAX (909) 558 4314 > email: resperante@llu.edu > Seth Finnegan Dept. of Earth Sciences -036 University of California Riverside, CA 92521 Phone:(951)452-2759 Fax: (951)787-4324
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