181 Paleontology/Paleobotany VIII: Preservational Bias and Experimental Taphonomy
Wednesday, 25 October 2006
8:00 AM - 12:00 PM
TAPHONOMY ON THE CONTINENTAL SHELF AND SLOPE: EIGHT-YEAR TRENDS—GULF OF MEXICO AND BAHAMAS
Paper number: 181-12
Program: Technical Sessions
Time: 10:45 AM – 11:00 AM
Authors
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W. Russell CallenderNational Oceanic and Atmospheric Administration, Silver Spring, MD
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George M. StaffAustin Community College, Austin, TX
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Karla Parsons-HubbardOberlin College, Oberlin, OH
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Carlton BrettUniv of Cincinnati, Cincinnati, OH
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Sally WalkerUniversity of Georgia, Athens, GA
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Anne RaymondTexas A&M University Dept. of Geology & Geophysics, College Station, TX
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Kathryn A. Ashton-AlcoxRutgers Univ, Port Norris, NJ
Abstract
Discoloration dissembled into five distinct processes: fading without discoloration, and discoloration to brown-to-red, orange/orange-mottled, green/green-mottled, and gray-to-black. Taphonomic signature after 8 yr was nearly exclusively a function of deployment location but EOD-level characteristics were insufficiently discriminative to delineate environments of preservation (EOP); hence our use of the acronym EOP. Depth did not exert a single significant effect on any taphonomic factor, likely because burial has taken some shallow-water arrays out of the photic zone. Trends in taphonomic signature cannot be explained by any simple combination of sediment type and degree of exposure. The discrepancy between expectation gleaned from visual observation of sediment type and biotic regime and the reality of definitive dissimilarity in taphonomic signature suggests that EOPs and EODs are not synonymous concepts. Certainly, although the desire to relate taphofacies to EOD is understandably important, the details of this conflation are still illusory.