Cantioscyllium cf. meyeri
Case & Cappetta, 1997
Classification: Elasmobranchii Orectolobiformes Ginglymostomatidae
Reference of the original description
A new selachian fauna from the Late Maastrichtian of Texas (Upper Cretaceous/Navarro Group; Kemp Formation). Münchner Geowissenschaftliche Abhandlungen Reihe A, Geologie und Paläontologie, 34, 131–189, 10 fig., 15 pl.
A new selachian fauna from the Late Maastrichtian of Texas (Upper Cretaceous/Navarro Group; Kemp Formation). Münchner Geowissenschaftliche Abhandlungen Reihe A, Geologie und Paläontologie, 34, 131–189, 10 fig., 15 pl.
Types
Cantioscyllium cf. meyeri
Cantioscyllium cf. meyeri
Description:
Citation: Cantioscyllium cf. meyeri Case & Cappetta, 1997: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 07/2025
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Remarks
shark-references Species-ID=13183;
shark-references Species-ID=13183;
References
New sharks in a chondrichthyan fauna from the Upper Cretaceous Aguja Formation (lower Campanian) of West Texas support biogeographic segregation among chondrichthyans in the Western Interior. Cretaceous Research, 175, Article 106151
DOI: 10.1016/j.cretres.2025.106151
A late Maastrichtian selachian assemblage from the Peedee Formation of North Carolina, USA. Vertebrate Anatomy Morphology Palaeontology, 3, 63–80
Elasmobranch and osteichthyan diversity from two late cretaceous (late campanian) transgressive lag deposits along the Neuse River, Lenoir County, North Carolina [Abstract]. Journal of Vertebrate Paleontology, 32(Suppl. 1), 79
DOI: 10.1080/02724634.2012.10635175

New sharks in a chondrichthyan fauna from the Upper Cretaceous Aguja Formation (lower Campanian) of West Texas support biogeographic segregation among chondrichthyans in the Western Interior. Cretaceous Research, 175, Article 106151
DOI: 10.1016/j.cretres.2025.106151
A late Maastrichtian selachian assemblage from the Peedee Formation of North Carolina, USA. Vertebrate Anatomy Morphology Palaeontology, 3, 63–80

Elasmobranch and osteichthyan diversity from two late cretaceous (late campanian) transgressive lag deposits along the Neuse River, Lenoir County, North Carolina [Abstract]. Journal of Vertebrate Paleontology, 32(Suppl. 1), 79
DOI: 10.1080/02724634.2012.10635175