Brachycarcharias cf. twiggsensis

(Case, 1981)


Classification: Elasmobranchii Lamniformes Odontaspididae

Reference of the original description
Case, G.R. (1981)
Late Eocene selachians from South-central Georgia. Palaeontographica, Abt. A, 176(1–3), 52–79

Types
Brachycarcharias cf. twiggsensis



Description:


Citation: Brachycarcharias cf. twiggsensis (Case, 1981): In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 04/2024

No image available.
Please send your images of "Brachycarcharias cf. twiggsensis" to
info@shark-references.com

Description
Diagnosis after Case 1981 [391]: Teeth ranging in size from 1.5 to 3 cms, and averaging 2.5 cms, a vestigial median furrow (groove) on the root area, teeth with from 1 to 2 lateral cusps on either side. Description: Lower jaw teeth erect. Anterior teeth with slender cuspidate lateral cusps. Lateral teeth wider, with from 1 to 2 lateral cusps, triangular in shape, and the larger of the cusps — flaring out in opposite directions from the tooth blade. No medial furrow (groove), but an imperfectly developed "furrow" on some specimens, with a definitive apical foramen positioned on the lingual boss of the tooth's root.

Remarks
shark-references Species-ID=10281;
synonym of Brachycarcharias twiggsensisi after Ebersole et al. (2019) p. 43 [27789];


References
Zalmout, I.S. & Antar, S.M. & Abd-El Shafy, E. & Metwally, M.H. & Hatab, E.-B.E. & Gingerich, P.D. (2012)
Priabonian sharks and rays (late Eocene: Neoselachii) from Minqar Tabaghbagh in the Western Qattara Depression, Egypt. Contributions from the Museum of Paleontology, University of Michigan, 32(6): 71–90
Underwood, C.J. & Ward, D.J. & King, C. & Antar, S.M. & Zalmout, I.S. & Gingerich, P.D. (2011)
Shark and ray faunas in the Middle and Late Eocene of the Fayum Area, Egypt. Proceedings of the Geologists' Association, 122(1), 47–66
DOI: 10.1016/j.pgeola.2010.09.004
Antar, M.S.M. (2011)
Paleo-environments of the exposed Eocene Sediments between Wadi El-Hitan and east Siwa in the Egyptian Western Desert based on their faunal content especially the vertebrates. Thesis, Zagazig University, Faculty of Science, Geology Department