Orectolobus ziegenhinei
Cappetta & Case, 2016
Classification: Elasmobranchii Orectolobiformes Orectolobidae
Reference of the original description
A Selachian Fauna from the Middle Eocene (Lutetian, Lisbon Formation) of Andalusia, Covington County, Alabama, USA. Palaeontographica, Abt. A, 307(1–6), 43–103
A Selachian Fauna from the Middle Eocene (Lutetian, Lisbon Formation) of Andalusia, Covington County, Alabama, USA. Palaeontographica, Abt. A, 307(1–6), 43–103
Synonyms / new combinations and misspellings
Squatiscyllium aff. nigeriensis
Squatiscyllium aff. nigeriensis
Types
Orectolobus ziegenhinei
Holotype: USTL: UM-THT 2; Paratype: USTL: UM-PAD 1; USTL: UM-THT 3; USTL: UM-PAD 2; USTL: UM-PAD 3;
Orectolobus ziegenhinei
Holotype: USTL: UM-THT 2; Paratype: USTL: UM-PAD 1; USTL: UM-THT 3; USTL: UM-PAD 2; USTL: UM-PAD 3;
Description:
Citation: Orectolobus ziegenhinei Cappetta & Case, 2016: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 04/2024
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Please send your images of "Orectolobus ziegenhinei" to
info@shark-references.com
Description
Original diagnose after Cappetta & Case (2016) p. 47 [24889]: Orectolobus species with a dentition close to that of the Recent species. However, compared to Recent species like O. ornatus (De Vis, 1883), or O. maculatus (Bonnaterre, 1788), O. ziegenhinei nov. sp. has a more massive cusp, heels less transversely developed and more perpendicular to the base of the cusp in labial view, a more salient and thicker rounded apron. he root shows a furrow oten completely open, with a large central foramen, that is not the case in recent species. In lateral teeth, vertical folds can differentiate at the base of the labial face of the cusp above the apron. Low marginal cusplets can be present in teeth corresponding to juvenile specimens.
Original diagnose after Cappetta & Case (2016) p. 47 [24889]: Orectolobus species with a dentition close to that of the Recent species. However, compared to Recent species like O. ornatus (De Vis, 1883), or O. maculatus (Bonnaterre, 1788), O. ziegenhinei nov. sp. has a more massive cusp, heels less transversely developed and more perpendicular to the base of the cusp in labial view, a more salient and thicker rounded apron. he root shows a furrow oten completely open, with a large central foramen, that is not the case in recent species. In lateral teeth, vertical folds can differentiate at the base of the labial face of the cusp above the apron. Low marginal cusplets can be present in teeth corresponding to juvenile specimens.
Remarks
shark-references Species-ID=14823;
valid after Cappetta & Case (2016) p. 46 [24889]; Ebersole et al. (2019) p. 17 [27789];
shark-references Species-ID=14823;
valid after Cappetta & Case (2016) p. 46 [24889]; Ebersole et al. (2019) p. 17 [27789];
References
Taxonomy and biostratigraphy of the elasmobranchs and bony fishes (Chondrichthyes and Osteichthyes) of the lower-to-middle Eocene (Ypresian to Bartonian) Claiborne Group in Alabama, USA, including an analysis of otoliths. European Journal of Taxonomy, 585, 1–274
DOI: 10.5852/ejt.2019.585
A Selachian Fauna from the Middle Eocene (Lutetian, Lisbon Formation) of Andalusia, Covington County, Alabama, USA. Palaeontographica, Abt. A, 307(1–6), 43–103
An inquiry into the stratigraphic occurrence of a Claibornian (Eocene) vertebrate fauna from Covington County, Alabama. Bulletin of the Alabama Museum of Natural History, 31(2), 60–73
Taxonomy and biostratigraphy of the elasmobranchs and bony fishes (Chondrichthyes and Osteichthyes) of the lower-to-middle Eocene (Ypresian to Bartonian) Claiborne Group in Alabama, USA, including an analysis of otoliths. European Journal of Taxonomy, 585, 1–274
DOI: 10.5852/ejt.2019.585
A Selachian Fauna from the Middle Eocene (Lutetian, Lisbon Formation) of Andalusia, Covington County, Alabama, USA. Palaeontographica, Abt. A, 307(1–6), 43–103
An inquiry into the stratigraphic occurrence of a Claibornian (Eocene) vertebrate fauna from Covington County, Alabama. Bulletin of the Alabama Museum of Natural History, 31(2), 60–73
