Heterodontus pineti
Case, 1981
Classification: Elasmobranchii Heterodontiformes Heterodontidae
Reference of the original description
Late Eocene selachians from South-central Georgia. Palaeontographica, Abt. A, 176(1–3), 52–79
Late Eocene selachians from South-central Georgia. Palaeontographica, Abt. A, 176(1–3), 52–79
Synonyms / new combinations and misspellings
Heterodontus cf. pineti
Heterodontus cf. pineti
Description:
Citation: Heterodontus pineti Case, 1981: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 11/2024
Description
Original diagnose after Case (1981) p. 55 [391]: Anterior tooth : of a juvenile, crown height approximately 1.5 mm, and width of the tooth across the three cusps approximately 1.5 mm, a partially fragmented tooth, missing portions of the root base, enameloid tooth surface is complete, although it is smooth-devoid of any plication or rugosity. Median-lateral tooth : of an adult, approximately 5 mm in its longest width, and approximately 2 mm in its greatest height (from the base of the root to the tip of the crown apex), and in its occlusal aspect, the median-lateral tooth of Heterodontus pineti n. sp., shows an overall "conchoidal" ornamentation on its enameloid surface (pi. 1, fig. 2d), root base slightly less than the length of the crown, and noticeable foramina and fenestration present.
Original diagnose after Case (1981) p. 55 [391]: Anterior tooth : of a juvenile, crown height approximately 1.5 mm, and width of the tooth across the three cusps approximately 1.5 mm, a partially fragmented tooth, missing portions of the root base, enameloid tooth surface is complete, although it is smooth-devoid of any plication or rugosity. Median-lateral tooth : of an adult, approximately 5 mm in its longest width, and approximately 2 mm in its greatest height (from the base of the root to the tip of the crown apex), and in its occlusal aspect, the median-lateral tooth of Heterodontus pineti n. sp., shows an overall "conchoidal" ornamentation on its enameloid surface (pi. 1, fig. 2d), root base slightly less than the length of the crown, and noticeable foramina and fenestration present.
References
An early Eocene fish assemblage associated with a barite deposit in the lower part of the Crescent Formation, Olympic Peninsula, Washington State, USA. Paläontologische Zeitschrift, 98(3), 443–467
DOI: 10.1007/s12542-024-00692-y
Reassessment and revision of the fossil Heterodontidae (Chondrichthyes: Neoselachii) based on tooth morphology of extant taxa. Palaeontos, 30, 1–73
Late Eocene selachians from Irwinton Sand Member of the Barnwell Formation (Jacksonian), WKA mines, Gordon, Wilkinson Country, Georgia. Münchner Geowissenschaftliche Abhandlungen Reihe A, Geologie und Paläontologie, 39, 5–16, 5 pl., 3 fig., 1 tabl.
Die Neoselachier der Paleokaribik (Pisces: Elasmobranchii). Courier Forschungsinstitut Senckenberg, 119, 1–102
Late Eocene selachians from South-central Georgia. Palaeontographica, Abt. A, 176(1–3), 52–79
An early Eocene fish assemblage associated with a barite deposit in the lower part of the Crescent Formation, Olympic Peninsula, Washington State, USA. Paläontologische Zeitschrift, 98(3), 443–467
DOI: 10.1007/s12542-024-00692-y
Reassessment and revision of the fossil Heterodontidae (Chondrichthyes: Neoselachii) based on tooth morphology of extant taxa. Palaeontos, 30, 1–73
Late Eocene selachians from Irwinton Sand Member of the Barnwell Formation (Jacksonian), WKA mines, Gordon, Wilkinson Country, Georgia. Münchner Geowissenschaftliche Abhandlungen Reihe A, Geologie und Paläontologie, 39, 5–16, 5 pl., 3 fig., 1 tabl.
Die Neoselachier der Paleokaribik (Pisces: Elasmobranchii). Courier Forschungsinstitut Senckenberg, 119, 1–102
Late Eocene selachians from South-central Georgia. Palaeontographica, Abt. A, 176(1–3), 52–79
