Scyliorhinus muelleri
Guinot, Underwood, Cappetta & Ward, 2013
Classification: Elasmobranchii Carcharhiniformes Scyliorhinidae
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: Scyliorhinus muelleri Guinot, Underwood, Cappetta & Ward, 2013: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 04/2024
Description
Original diagnose after Guinot et al. (2013) p. 656 [24889]: Teeth small (up to 1 mm high), showing a moderate degree of gradient monognathic heterodonty. Anterior and lateral teeth higher than wide; main cusp erect and lingually oriented flanked by a pair of triangular lateral cusplets. Lingual ornament of slight irregular vertical ridges not reaching the apex nor the base of the crown; labial ornament varying with jaw position; anterior teeth with marked longitudinal ridges not reaching the apex of the upper edge of the crown; lateral teeth with very few faint ridges at the base of the cusplets; posterior teeth with numerous labial ridges reaching the apex. Labial basal edge of the crown concave in occlusal view. Bilobate hemiaulacorhize root with convex basal face and flared lateral and labial edges with lateral edges curved towards the cusplets. Well-developed median protuberance and concave marginolingual edges of the crown in profile view.
Original diagnose after Guinot et al. (2013) p. 656 [24889]: Teeth small (up to 1 mm high), showing a moderate degree of gradient monognathic heterodonty. Anterior and lateral teeth higher than wide; main cusp erect and lingually oriented flanked by a pair of triangular lateral cusplets. Lingual ornament of slight irregular vertical ridges not reaching the apex nor the base of the crown; labial ornament varying with jaw position; anterior teeth with marked longitudinal ridges not reaching the apex of the upper edge of the crown; lateral teeth with very few faint ridges at the base of the cusplets; posterior teeth with numerous labial ridges reaching the apex. Labial basal edge of the crown concave in occlusal view. Bilobate hemiaulacorhize root with convex basal face and flared lateral and labial edges with lateral edges curved towards the cusplets. Well-developed median protuberance and concave marginolingual edges of the crown in profile view.
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
A marine microvertebrate fauna from a temporary exposure of the Atherfield Clay Formation, Reigate, Surrey. Proceedings of the Geologists' Association, Volume 134(5–6), 599–618
DOI: 10.1016/j.pgeola.2023.08.001
Combining palaeontological and neontological data shows a delayed diversification burst of carcharhiniform sharks likely mediated by environmental change. Scientific Reports, 12, Article 21906
DOI: 10.1038/s41598-022-26010-7
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
A marine microvertebrate fauna from a temporary exposure of the Atherfield Clay Formation, Reigate, Surrey. Proceedings of the Geologists' Association, Volume 134(5–6), 599–618
DOI: 10.1016/j.pgeola.2023.08.001
Combining palaeontological and neontological data shows a delayed diversification burst of carcharhiniform sharks likely mediated by environmental change. Scientific Reports, 12, Article 21906
DOI: 10.1038/s41598-022-26010-7
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
