Dinosaurs and other fossil vertebrates from fluvial deposits in the Lower Cretaceous of southern Tunisia

Citation
Mj. Benton et al., Dinosaurs and other fossil vertebrates from fluvial deposits in the Lower Cretaceous of southern Tunisia, PALAEOGEO P, 157(3-4), 2000, pp. 227-246
Citations number
52
Categorie Soggetti
Earth Sciences
Journal title
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN journal
00310182 → ACNP
Volume
157
Issue
3-4
Year of publication
2000
Pages
227 - 246
Database
ISI
SICI code
0031-0182(200004)157:3-4<227:DAOFVF>2.0.ZU;2-M
Abstract
Remains of dinosaurs and other vertebrates (sharks, bony fishes, coelacanth s, turtles, crocodilians, pterosaurs) are reported from the Chenini Formati on of the Tataouine region in southern Tunisia. The Formation is part of th e 'continental intercalaire', a succession of continental deposits of Early to Late Cretaceous age distributed over the whole of North Africa and the Sahara. It consists of bar and channel deposits of broad rivers that flowed NNW from the mid-Sahara region towards the southern shore of Tethys. Dinos aur-bearing units in the 'continental intercalaire' have been dated to the Hauterivian to Cenomanian, and the Chenini Formation is possibly Albian in age. Dinosaur fossils include abundant teeth of the theropods Carcharodonto saurus and Spinosaurus. as well as postcranial elements of theropods and a medium-sized sauropod. A tooth of an ornithocheirid is the first report of a pterosaur from the region. The dinosaur bones and teeth were transported some distance and deposited in a channel lag, associated with less damaged locally derived material such as fern fronds, coprolites, fish teeth and sc ales, and crocodilian scutes. (C) 2000 Elsevier Science B.V. All rights res erved.