Weltonia ancistrodon

(Arambourg, 1952)


Classification: Elasmobranchii Hexanchiformes Hexanchidae

Reference of the original description
Arambourg, C. (1952)
Les vertébrés fossiles des gisements de phosphates (Maroc-Algérie-Tunisie). Notes et Mémoires du Service Géologique du Maroc, 92, 1–372

Image of the original description

Original image of the Syntypes of Notidanus (Heptranchias) ancistrodon nov. sp., Arambourg, 1952, Pl . I. figs 59-71, Thanetian, Late Paleocene, Descenderie D, Ouled Abdoun, Morocco; Pl . I. figs 72-82, Thanetian, Late Paleocene, Boujniba, Khouribga region, Morocco; Ypresian, early Eocene; Pl . I. figs 83, 84, Mohammed Chleuh, Ouled Abdoun Basin, Morocco; ?coll. Muséum National d'Histoire Naturelle, Paris, France

Synonyms / new combinations and misspellings
Heptranchias cf. ancistrodon, Notidanus (Heptranchias) ancistrodon

Types
Weltonia ancistrodon

Notidanus (Heptranchias) ancistrodon
Syntype: MNHN(fossil): uncat.;


Description:


Citation: Weltonia ancistrodon (Arambourg, 1952): In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 10/2026

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Weltonia ancistrodon (Arambourg, 1952); Thanetian, late Paleocene; Ouled Abdoun Basin, Morocco; coll. Pollerspöck, © T. Reinecke, Bochum

Description
Original diagnosis after (Arambourg, 1952) [90]: Notidanus a denture caracterisée par le grand développement, aux dents latérales de la machoire supérieure, de la première cuspide, comprimée et recourbée en forme d'S vers la commissure; denticules latéraux au nombre de 4 ou 5. Dents mandibulaires a 7 denticules au maximum, regulièrement décroissants. Bord antérieur de la première cuspide très finement denticulé à sa base.

Remarks
shark-references Species-ID=7511;

Remark of Welton (1979 [2517]): Prior to the recent collection of Heptranchias cf. "N." ancistrodon in the Lodo Formation of California, it was thought that this species was restricted to the Paleocene and Eocene of Morocco (Arambourg, 1952}. The only differences observed between the Lodo tooth (LACM 115912), and those figured by Arambourg (1952: Plate 1, Figures 65-67 and 78-79) are the presence of a small mesial serration and absence of a flared distal ledge at the apical end of the cusp in the Lodo specimen. It is not possible to evaluate characteristics of the mesial and distal cutting ridges from either Arambourg's description or illustrations. Arambourg referred teeth of the Lodo morphology (his Figures 65-67 and 78-79) to "dents des files plus reculees vers la commissure (Arambourg, 1952: 45)". It is my interpretation that Arambourg has incorrectly assigned the teeth to the upper dentition and that they actually represent a lower antero-lateral tooth group. All lower antero-lateral teeth in Hexanchus, Heptranchias, and Notorynchus possess a well developed mesial depression just below the crown foot but this character is absent in the upper symphyseal and antero-lateral tooth groups of all hexanchoids. This mesial depression houses the distal end of the root of the adjacent (mesial) row and functions to strengthen the dental series. All of the teeth figured by Arambourg (1952: Figures 65-67 and 80-82(*)) and all specimens of this same morphology in comparative collections at the LACM, show a well developed mesial depression. Moreover, in the case of all extant hexanchoids, the lower antero-lateral tooth positions average between 20 and 80 percent longer than the upper dentition. Following Arambourgs interpretation, his upper laterals are usually larger than the teeth he interprets to represent the lower antero-laterals of Notidanus (Heptranchias) ancistrodon. I consider Arambourgs Figures 65-67 and 78-79 to represent lower antero-laterals and his Figures 59-64 and 72-77 to represent upper antero-lateral and symphysial tooth positions. All of the above probably also include a mixture of Heptranchias "N." ancistrodon and Hexanchus microdon teeth. The teeth which Arambourg interprets to represent lower antero-laterals of H. "N." ancistrodon are all teeth of Hexanchus, probably H. microdon.
(*) should probably read: 78-79

valid after Ward (1979) p. 118 [2493]; Case (1996) p. 4 [397]


References
Meisner, H. (2024)
Faszination Haie – Die Welt der fossilen und der lebenden Haie. Der Steinkern, 58, 1–116
Boles, Z.M. & Ullmann, P.V. & Putnam, I. & Ford, M. & Deckhut, J.T. (2024)
New vertebrate microfossils expand the diversity of the chondrichthyan and actinopterygian fauna of the Maastrichtian–Danian Hornerstown Formation in New Jersey. Acta Palaeontologica Polonica, 69(2), 173–198
DOI: 10.4202/app.01117.2023
Guinot, G. & Condamine, F.L. (2023)
Global impact and selectivity of the Cretaceous-Paleogene mass extinction among sharks, skates, and rays. Science, 379, 802–806
DOI: 10.1126/science.abn2080
Cocke, J. (2002)
Fossil Shark Teeth of the World. Lamna Books, 170 p
Case, G.R. (1996)
A new selachian fauna from the Lower Hornestown Formation (Early Paleocene/Montian) of Monmouth County, New Jersey. Palaeontographica, Abt. A, 242(1–3), 1–14
Welton, B.J. (1979)
Late Cretaceous and Cenozoic Squalomorphii of the Northwest Pacific Ocean. PhD, Univ. of California Berkeley, 553 p., 71 fig.
Arambourg, C. (1952)
Les vertébrés fossiles des gisements de phosphates (Maroc-Algérie-Tunisie). Notes et Mémoires du Service Géologique du Maroc, 92, 1–372