Southeastern Section - 67th Annual Meeting - 2018

Paper No. 36-14
Presentation Time: 1:30 PM-5:30 PM


SNYDER, Keith1, MCLAIN, Matthew A.2, SNYDER, Ivan1 and CHADWICK, Arthur V.3, (1)Biology Department, Southern Adventist University, Collegedale, TN 37315, (2)Department of Biological and Physical Sciences, The Master’s University, 21726 Placerita Canyon Road, Santa Clarita, CA 91321, (3)Geology, Southwestern Adventist University, 100 Magnolia, Keene, TX 76059

In the Upper Cretaceous deposits of western North America, monodominant hadrosaurid and ceratopsid and multitaxic microvertebrate bonebeds are commonly encountered, but multitaxic macrovertebrate bonebeds are uncommon. Long bones in these bonebeds often shows no strongly supported to weakly supported orientation trends. Between 2014 and 2017, we excavated an area approximately 150 m2, discovering a peculiar multitaxic macrovertebrate assemblage in the Lance Formation of eastern Wyoming. Parts of three ornithischians, a Triceratops, a Thescelosaurus, and an Edmontosaurus, along with a caenagnathid theropod Anzu were uncovered. The partial remains of these four individuals are slightly disarticulated to disarticulated but associated. Other taxa are represented in the bonebed only by isolated elements. Compounding the uniqueness of this assemblage is the distribution of elements across the quarry. The majority of the approximately 115 bones of the Thescelosaurus are localized to a within a 3-meter circle. The skull, pubis, femur, tibia, metatarsals, and phalanges of the Triceratops are immediately adjacent to the Thescelosaurus, but are distributed in a northwest trend. Likewise the 70 articulated caudal vertebrae and disarticulated hip and limb elements from the Edmontosaurus exhibit a northwest orientation. Confoundingly, the associated tibia, fibula, astragalus, metatarsals, and caudal vertebrae of the Anzu point to the southwest. The remains of all four individuals are in close proximity, overlapping, or partially overlapping, yet appear to be laid down in three different orientations. These specimens seem to have been hydrodynamically transported here, but we don’t fully understand how flowing water could generate this particular pattern of deposition. We will continue to excavate the site and study it’s sedimentology to gain a better understanding of the assemblage’s mysterious taphonomic history.
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