24 Paleontology (Posters)
Friday, 14 March 2003
1:00 PM - 5:00 PM
CHONDRICHTHYAN AND REPTILIAN FOSSILS FROM THE UPPER CRETACEOUS PEEDEE FORMATION AT ELIZABETHTOWN, SOUTHEASTERN NORTH CAROLINA, AND COMPARISON TO NEW JERSEY FAUNAS
Paper number: 24-2
Program: Technical Sessions
Time: 1:00 PM – 5:00 PM
Authors
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Roger J. CuffeyPenn State Univ, University Park, PA
Abstract
At Elizabethtown, isolated shark teeth are the most common vertebrate fossils. Species identified include Scapanorhynchus texanus (the most numerous), Anomotodon angustidens (*),Cretodus borodini, Cretolamna appendiculata, Odontaspis samhammeri (or macrorhiza), Squalicorax kaupi, and Synodontaspis holmdelensis. A few ray teeth are mixed in (Brachyrhizodus wichitaensis, Ptchyotrygon vermiculata). All but one (*) of these species also occur at Ellisdale or Sewell. Occasional circular shark vertebrae, ovoid ray vertebrae, spiral-striated shark coprolites, possible ray dermal denticles, and very fragmentary teleost remains were also recovered.
In addition to these Cretaceous species, rare teeth (one shark, Mitsukurina lineata; two rays, Aetobatus arcuatus, Hypopholodon sylvestris) at Elizabethtown were previously known only from Tertiary strata. These fossils may represent artificial mixing by construction equipment working the dump, or possibly a range extension earlier in time.
Much less abundant at Elizabethtown than fish fossils are reptile fragments. Most are broken shell and limb bones of the robust toxocheliid turtle Osteopygis emarginatus, a few the soft-shelled turtle Trionyx (or Aspideretes? ) sp. Several teeth belong to an indeterminate crocodilian and a small pliosaur (Trinacromerum sp.). A single tooth represents a hadrosaur (dinosaur) not further identifiable.
The dominance of marine or aquatic reptiles, along with the numerous fishes, supports previous workers' inference that the Peedee here was nearshore marine paleoenvironmentally.