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Ass. Lect. Belal Shehta Fathy Rezk Salem :: Publications:

Title:
New marine reptile (plesiosaur and mosasaur) fossils from the Upper Campanian Duwi Formation of the Dakhla Oasis area, Western Desert of Egypt
Authors: Belal S. Salem, Patrick M. O’ Connor, Matthew C. Lamanna, Sanaa El-Sayed, Erik R. Seiffert, Joseph J. W. Sertich, Hesham M. Sallam
Year: 2022
Keywords: Not Available
Journal: The Society of Vertebrate Paleontology 82 Annual Meeting
Volume: Not Available
Issue: Not Available
Pages: 306-307
Publisher: Not Available
Local/International: International
Paper Link:
Full paper Not Available
Supplementary materials Not Available
Abstract:

Upper Cretaceous deposits exposed in southern Egypt, near the Dakhla Oasis in the Western Desert, preserve abundant vertebrate fossils from nearshore marine paleoenvironments. Fieldwork carried out by researchers from the Mansoura University Vertebrate Paleontology Center in this area during 2008, 2010, 2011, and 2013 resulted in the discovery of numerous new vertebrate fossil localities within the upper Campanian part of the Duwi Formation. Fossils recovered from this unit include those of sharks, sawfishs, actinopterygians, and marine reptiles (mosasaurs and plesiosaurs). Here we report on elasmosaurid (Sauropterygia: Plesiosauria: Elasmosauridae) and mosasaurid (Squamata: Mosasauridae) fossils from the Duwi Formation. Elasmosaurids are represented by numerous large posterior cervical and dorsal vertebrae that are referable to this plesiosaur clade based on their possession of centra with lateral ridges and dumbbellshaped articular facets. Mosasaurids are the most abundant and diverse marine reptiles recovered from the Duwi Formation, with many craniodental (e.g., dentaries and teeth with differing morphologies) remains and dozens of vertebrae having been identified as those of Mosasaurinae or Halisaurinae. Within Mosasaurinae, an isolated, robust, and globular tooth crown of Globidens and a complete tooth of Carinodens (identified on the basis of its lateral flattening and two relatively pronounced sulci) indicate the presence of Globidensini. Many fragmentary dentaries pertain to an indeterminate mosasaurine, with two of these preserving teeth in situ and another showing a replacement tooth developed within a resorption pit. One small, fragmentary dentary with two preserved teeth is referred to Halisaurinae based on the presence of small, striated, hooked, snake-like teeth. This fossil represents the first record of Halisaurinae from Egypt and the oldest occurrence of this group from northern Africa. Egyptian mosasaurids ranged in size from small-bodied (~3 to 4 m) Halisaurinae to medium-sized (~6 to 8 m) Mosasaurinae, and were similarly diverse in morphology. Tooth crowns range in shape from cones adapted to pierce and hold, to bulbous teeth adapted to crush, to cutting blades; jaw morphology is also diverse. The new elasmosaurid and mosasaurid remains from the Duwi Formation therefore reveal high taxonomic and functional diversity and elevated endemism in the uppermost Cretaceous marine reptile faunas of northeastern Africa.

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