Anomotodon genaulti
Guinot, Underwood, Cappetta & Ward, 2013
Classification: Elasmobranchii Lamniformes Mitsukurinidae
Reference of the original description
Sharks (Elasmobranchii: Euselachii) from the Late Cretaceous of France and the UK. Journal of Systematic Palaeontology, 11(6), 589–671
Sharks (Elasmobranchii: Euselachii) from the Late Cretaceous of France and the UK. Journal of Systematic Palaeontology, 11(6), 589–671
Description:
Citation: Anomotodon genaulti Guinot, Underwood, Cappetta & Ward, 2013: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 11/2024
Description
Original diagnose after Guinot et al. (2013) p. 641 [24889]: Medium-sized teeth; lingual ornamentation of slight flexuous vertical folds on lower half of the cusp of preferentially lower teeth. Anterior teeth with erect cusp and arched root branches; well-developed cutting edges in continuity with very low and inclined heels; lateral extremities of the heels bent lingually; slight labial bulge and strong lingual protuberance cut by a narrow, occasionally partly closed, nutritive groove. Lateral teeth as high as broad to broader than high in lateroposteriors; labiolingually compressed and triangular cusp with high heels that overtake the root laterally. Straight marginal root edges with a shallow notch in lateroposterior teeth. Root laterally expanded with slightly convex lingual face and subrectilinear basal edges of the branches.
Original diagnose after Guinot et al. (2013) p. 641 [24889]: Medium-sized teeth; lingual ornamentation of slight flexuous vertical folds on lower half of the cusp of preferentially lower teeth. Anterior teeth with erect cusp and arched root branches; well-developed cutting edges in continuity with very low and inclined heels; lateral extremities of the heels bent lingually; slight labial bulge and strong lingual protuberance cut by a narrow, occasionally partly closed, nutritive groove. Lateral teeth as high as broad to broader than high in lateroposteriors; labiolingually compressed and triangular cusp with high heels that overtake the root laterally. Straight marginal root edges with a shallow notch in lateroposterior teeth. Root laterally expanded with slightly convex lingual face and subrectilinear basal edges of the branches.
References
Global impact and selectivity of the Cretaceous-Paleogene mass extinction among sharks, skates, and rays. Science, 379, 802–806
DOI: 10.1126/science.abn2080
Feeding ecology has shaped the evolution of modern sharks. Current Biology, 31(23), 5138–5148
DOI: 10.1016/j.cub.2021.09.028
Climate cooling and clade competition likely drove the decline of lamniform sharks. Proceedings of the National Academy of Sciences of the United States of America, 116(41), 20584–20590
DOI: 10.1073/pnas.1902693116
Sharks (Elasmobranchii: Euselachii) from the Late Cretaceous of France and the UK. Journal of Systematic Palaeontology, 11(6), 589–671
DOI: 10.1080/14772019.2013.767286
Late Cretaceous elasmobranch palaeoecology in NW Europe. Palaeogeography, Palaeoclimatology, Palaeoecology, 388, 23–41
DOI: 10.1016/j.palaeo.2013.07.027
Regional to global patterns in Late Cretaceous selachian (Chondrichthyes, Euselachii) diversity. Journal of Vertebrate Paleontology, 33(3), 521–531
DOI: 10.1080/02724634.2013.740116
Global impact and selectivity of the Cretaceous-Paleogene mass extinction among sharks, skates, and rays. Science, 379, 802–806
DOI: 10.1126/science.abn2080
Feeding ecology has shaped the evolution of modern sharks. Current Biology, 31(23), 5138–5148
DOI: 10.1016/j.cub.2021.09.028
Climate cooling and clade competition likely drove the decline of lamniform sharks. Proceedings of the National Academy of Sciences of the United States of America, 116(41), 20584–20590
DOI: 10.1073/pnas.1902693116
Sharks (Elasmobranchii: Euselachii) from the Late Cretaceous of France and the UK. Journal of Systematic Palaeontology, 11(6), 589–671
DOI: 10.1080/14772019.2013.767286
Late Cretaceous elasmobranch palaeoecology in NW Europe. Palaeogeography, Palaeoclimatology, Palaeoecology, 388, 23–41
DOI: 10.1016/j.palaeo.2013.07.027
Regional to global patterns in Late Cretaceous selachian (Chondrichthyes, Euselachii) diversity. Journal of Vertebrate Paleontology, 33(3), 521–531
DOI: 10.1080/02724634.2013.740116
