Mustelus, Linck, 1790
publication ID |
https://doi.org/10.4202/app.2008.0306 |
persistent identifier |
https://treatment.plazi.org/id/03DBAF0C-FFB5-EE49-FCD8-FC59D1B5FB3C |
treatment provided by |
Felipe (2024-08-08 19:16:40, last updated 2024-08-08 21:02:38) |
scientific name |
Mustelus |
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Mustelus View in CoL aff. M. vanderhoefti Herman, 1982
Fig. 6A View Fig .
2006 Mustelus sp. ; Adnet 2006: 76–78: pl. 26: 1–3.
Material.—Two teeth.
Description.—The species of this genus are characterised by a crushing−type dentition. The lateral tooth figured here ( Fig. 6A View Fig ) is slightly asymmetrical and transversely elongated, with a reduced, distally directed cusp. The enamel of the crown is strongly wrinkled, especially on the labial and lingual faces. The crown is as high as the root. Its occlusal face is flat and relatively smooth except on its labial edge, where it bears deep folds. The labial face of the crown broadly overhangs the root in profile ( Fig. 6A View Fig 2) and the lingual face bears a salient uvula located under the cusp ( Fig. 6A View Fig 1 View Fig , A 3 View Fig ). The root is thick with a flat basal face. The lingual protuberance of the root is well−developed under the uvula and several marginal foramina open on both sides. The nutritive groove is broad, straight and the principal nutritive foramen opens on it lingual edge.
Comments.—The fossil record of the genus Mustelus is poorly documented. The oldest record seems to be from the Thanetian of the Paris Basin ( Bault and Genault 1995) but this genus remains scarce in deposits until the Neogene, during which it becomes more abundant ( Herman 1982: 191; Bault and Genault 1995: 207). Mustelus is currently one of the most diverse triakid genera, including 22 living species, and inhabits mainly the neritic zone (up to 200 m depth) of the cold to tropical areas of most of the seas and oceans (e.g., Compagno 1984; Compagno et al. 2005). The tooth morphology of Mustelus species is very homogeneous and species are hardly differentiable on the basis of dental characters ( Herman et al. 1988, 1990), which partly explains why paleontologists hesitate to refer fossil Mustelus teeth to precise species ( Cappetta and Cavallo 2006). As a result, only three fossil species of Mustelus have been described and considered as valid (Cappetta 2006): Mustelus biddlei Bault and Genault, 1995 (Thanetian of Ressons−sur−Matz, northern France); Mustelus whitei Cappetta, 1976 (lower Ypresian of Burnham−on Crouch, London Clay, England) and Mustelus vanderhoefti Herman, 1982 (Ypresian of Egem, Belgium). The teeth of Premontré, like those from the middle Lutetian of southwestern France ( Adnet 2006), are closely similar to those of Mustelus vanderhoefti , known until the middle Eocene of England ( Kemp 1994).
Adnet, S. 2006. Nouvelles faunes de Selaciens (Elasmobranchii, Neoselachii) de l'Eocene moyen des Landes (Sud-Ouest, France). Implication dans la connaissance des communautes de selaciens d'eaux profondes. Palaeo Ichthyologica 10: 5 - 128.
Bault, J. - P. and Genault, B. 1995. Contribution a l'etude des elasmobranches du Thanetien (Paleocene) du Bassin de Paris. 1. Decouverte d'une faune d'elasmobranches dans la partie superieure des Sables de Bracheux (Thanetien, Paleocene) des regions de Compiegne (Oise) et de Montdidier (Somme). In: J. Herman and H. Van Waes (eds.), Selaciens et Stratigraphie. Belgian Geological Survey, Professional Papers 278: 185 - 259.
Cappetta, H. and Cavallo, O. 2006. Les selaciens du Pliocene de la region d'Alba (Piemont, Italie Nord-Ouest). Rivista Piemontese di Storia naturale 27: 33 - 76.
Compagno, L. J. V. 1984. FAO Species catalogue. Vol. 4 Sharks of the world. In: An annoted and illustrated catalogue of shark species known to date. Part. 2 Carcharhiniformes. FAO Fisheries Synopsis 125: 251 - 655.
Compagno, L. J. V., Dando, M., and Fowler, S. 2005. A Field Gguide to the Sharks of the World. 368 pp. Harper and Collins Publishers Ltd., London.
Herman, J. 1982. Additions to the Eocene fish-fauna of Belgium. 5. The discovery of Mustelus teeth in Ypresian, Paniselian and Wemmelian strata. Tertiary Research 3 (4): 189 - 193.
Herman, J., Hovestadt-Euler, M., and Hovestadt, D. C. 1988. Part A: Selachii. N ° 2 a. Order: Carcharhiniformes. Family: Triakidae. In: M. Stehmann (ed.), Contributions to the Study of the Comparative Morphology of Teeth and Other Relevant Ichthyodorulites in Living Supraspecific Taxa of Chondrichthyan Fishes. Bulletin de l'Institut royal des Sciences naturelles de Belgique 58: 99 - 126.
Herman, J., Hovestadt-Euler, M., and Hovestadt, D. C. 1990. Part A: Selachii. N ° 2 b. Order: Carcharhiniformes. Family: Scyliorhinidae. In: M. Stehmann (ed.), Contributions to the Study of the Comparative Morphology of Teeth and Other Relevant Ichthyodorulites in Living Supraspecific Taxa of Chondrichthyan Fishes. Bulletin de l'Institut royal des Sciences naturelles de Belgique 60: 181 - 230.
Kemp, D. 1994. Fossil Chondrichthyes from the Lower Barton and Bracklesham Groups of the Hampshire Basin: Their Taxonomy, Stratigraphic Distribution and Palaeobiology. 262 pp. Unpublished Ph. D. thesis. University of Portsmouth, Portsmouth.
Fig. 6. Triakid shark Mustelus aff. M. vanderhoefti Herman, 1982. Prémontré Abbey, late Ypresian.UM−PRE 18, lateral tooth, lingual face (A), profile view (B), occlusal face (C), and basal face (D).
Fig. 1. A. Location of the Prémontré Abbey (Aisne, northern France). B. Simplified stratigraphic column of Prémontré with fossiliferous (2–3) and non−fossiliferous (4–12) levels (from Dégrémont et al. 1985: 12).
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Mustelus
Adnet, Sylvain & Cappetta, Henri 2008 |
Mustelus sp.
Adnet, S. 2006: 76 |