Anotodus is an extinct genus of thresher sharks that lived during the Neogene. It contains one valid species, Anotodus retroflexus, which has been found in North America, South America, Europe, and Australia.[3][4]

Anotodus
Temporal range: Burdigalian-Zanclean
Tooth of Anotodus retroflexus
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Chondrichthyes
Subclass: Elasmobranchii
Order: Lamniformes
Family: Alopiidae
Genus: Anotodus
Le Hon, 1871[2]
Species:
A. retroflexus
Binomial name
Anotodus retroflexus
(Agassiz, 1838)[1]
Synonyms[citation needed]
  • Oxyrhina retroflexa Agassiz, 1838
  • Isurus retroflexus (Agassiz, 1838)
  • Anotodus agassizii Le Hon, 1871

Taxonomy

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Oxyrhina retroflexa was named by Louis Agassiz in an 1838 illustration,[1] which was followed by his text description in 1843.[5][a] Its holotype is a tooth of unknown provenance housed in the State Museum of Natural History, Karlsruhe.[1][5] In 1871, Henri Le Hon named Anotodus agassizii for teeth from the Pliocene of Belgium, while acknowledging that it could be the same as O. retroflexa.[2] The former species is now regarded as a junior synonym of the latter; while some authors consider it to belong to Isurus,[7] it is more widely accepted as a distinct genus of alopiid.[3][4][8]

Notes

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  1. ^ The publication dates are based on Brignon (2014).[6]

References

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  1. ^ a b c Agassiz, J.L.R. (1835–1843). Recherches sur les poissons fossiles. Atlas, Tome III. Neuchâtel, CH: H. Nicolet. p. tab. 33, fig. 10. doi:10.5962/bhl.title.4275.
  2. ^ a b Le Hon, H. (1871). Préliminaires d'un mémoire sur les poissons tertiaires de Belgique. Brussels, BE: C. Muquardt. pp. 8–9.
  3. ^ a b Cappetta, H. (2012). Handbook of Paleoichthyology. Volume 3E. Chondrichthyes. Mesozoic and Cenozoic Elasmobranchii: Teeth. Munich, DE: Verlag Dr. Friedrich Pfeil. pp. 242–243. ISBN 978-3-89937-148-2.
  4. ^ a b Carrillo-Briceño, J.D.; Luz, Z.; Hendy, A.; Kocsis, L.; Aguilera, O.; Vennemann, T. (2019). "Neogene Caribbean elasmobranchs: diversity, paleoecology and paleoenvironmental significance of the Cocinetas Basin assemblage (Guajira Peninsula, Colombia)". Biogeosciences. 16 (1): 33–56. Bibcode:2019BGeo...16...33D. doi:10.5194/bg-16-33-2019.
  5. ^ a b Agassiz, J.L.R. (1837–1843). Recherches sur les poissons fossiles. Tome III. Neuchâtel, CH & Soleure, CH: Petitpierre & Jent et Gassmann. p. 281. doi:10.5962/bhl.title.4275.
  6. ^ Brignon, A. (2014). "The paleoichthyological and geological researches on the Permian deposits of Muse near Autun (Saône-et-Loire, France) at the beginning of the XIXth century". Bulletin de la Société géologique de France. 185 (4): 233–252. doi:10.2113/gssgfbull.185.4.233.
  7. ^ Kent, B.W. (2018). "The cartilaginous fishes (chimaeras, sharks, and rays) of Calvert Cliffs, Maryland". In Godfrey, S.J. (ed.). The Geology and Vertebrate Paleontology of Calvert Cliffs, Maryland, USA. Smithsonian Contributions to Paleobiology. Number 100. Washington, DC: Smithsonian Institution Scholarly Press. pp. 45–157. doi:10.5479/SI.1943-6688.100.
  8. ^ Szabó, M.; Kocsis, L.; Bosnakoff, M.; Sebe, K. (2021). "A diverse Miocene fish assemblage (Chondrichthyes and Osteichthyes) from the Pécs-Danitzpuszta sand pit (Mecsek Mts, Hungary)". Földtani Közlöny. 151 (4): 363–410. doi:10.23928/foldt.kozl.2021.151.4.363.

Further reading

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  • J. Herman. 1977. Les sélaciens des terrains néocrétacés and paléocènes de Belgique and des contrées limitrophes. Eléments d'une biostratigraphie intercontinentale. Mémoires pour Servir a l'Explication des Cartes Géologiques et Minières de la Belgique 15:1-450