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Dee Ann I am sure there are several different rules of thumb. And it probably depends on what unit you're studying. For instance if you're studying deposits of an epeiric sea and you're distinguishing between some that are shallower and others that are deeper, then it depends on the depth of that sea and whether it has a consistent difference between the deeper parts and the shallower parts. If you're just looking at a marine shelf like the modern marine shelves, you might be separating peritidal deposits that would have been deposited in water no deeper than a few meters from inner shelf deposits that might represent meters to a few tens of meters of water or outer shelf deposits that might represent a couple of hundred meters. Just define your situation and explain why you've chosen the depths you have an I think you'll be fine. David David C. Kopaska-Merkel Geological Survey of Alabama P.O. Box 869999 Tuscaloosa AL 35486-6999 (205) 247-3695 (direct line/voice mail) (205) 349-2852 (switchboard) fax 349-2861 www.gsa.state.al.us To join sednet, an e-mail group for discussion of sedimentology, send a blank e-mail message to sednet-subscribe@yahoogroups.com. To join a new list about science education in Alabama, send a blank e-mail message to ALScienceEdNews-subscribe@yahoogroups.com. -----Original Message----- From: paleonet-owner@nhm.ac.uk [mailto:paleonet-owner@nhm.ac.uk] On Behalf Of Dee Ann Cooper Sent: Monday, December 12, 2005 8:37 AM To: paleonet Subject: paleonet "shallow marine environment" my husband and i are working on a paper concerning an extremely fossil-rich isochronous layer in a marine carbonate. the further into it we get, the more we debate how "shallow" shallow is. is there is an exact definition of "shallow" or a "rule-of-thumb" definition of "shallow". all of our "critters" seem to fall into the "shallow marine" category and i think we have some evidence of terrigenous input as well (i.e. kaolinite). Dee Ann Cooper, BS, MS, PG Phone: (409) 751-6907 Address: 17890 Nonie Lane, Lumberton, TX 77657
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