Adnetoscyllium angloparisensis
Guinot, Underwood, Cappetta & Ward, 2013
Classification: Elasmobranchii Orectolobiformes Hemiscylliidae
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: Adnetoscyllium angloparisensis Guinot, Underwood, Cappetta & Ward, 2013: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 12/2024
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Description
Original diagnose after Guinot et al. (2013) p. 609 [24889]: Small teeth (less than 1mmwide) and moderate degree of gradient monognathic heterodonty. Crown with erect cusp and oval lower part of the labial face. Cutting edges in continuity with convex and inclined heels. Flat labial face of the lower part of the crown. Wide, convex (bifid in lateral teeth) and semicircular apron with a weak ridge following the outline of the apron from one marginal angle to the other; additional discontinuous ridge on the lower region of the labial face; apron not reaching the baseline of the tooth. Robust and trapezoidal lingual protuberance not reaching the lingual root edge. Concave profile of marginolingual faces with slightly flared basal region. Basal edge of the lingual face bearing a thin but sharp and continuous bulge, tapering near the marginal angles. Triangular root with well-marked lingual protuberance, concave marginolingual faces and rounded extremities. Main cusp directed to the posterior and displaced distally in lateroposterior teeth.
Original diagnose after Guinot et al. (2013) p. 609 [24889]: Small teeth (less than 1mmwide) and moderate degree of gradient monognathic heterodonty. Crown with erect cusp and oval lower part of the labial face. Cutting edges in continuity with convex and inclined heels. Flat labial face of the lower part of the crown. Wide, convex (bifid in lateral teeth) and semicircular apron with a weak ridge following the outline of the apron from one marginal angle to the other; additional discontinuous ridge on the lower region of the labial face; apron not reaching the baseline of the tooth. Robust and trapezoidal lingual protuberance not reaching the lingual root edge. Concave profile of marginolingual faces with slightly flared basal region. Basal edge of the lingual face bearing a thin but sharp and continuous bulge, tapering near the marginal angles. Triangular root with well-marked lingual protuberance, concave marginolingual faces and rounded extremities. Main cusp directed to the posterior and displaced distally in lateroposterior teeth.
Remarks
shark-references Species-ID=13542;
type species of Adnetoscyllium Guinot et al., 2016 p. 609 [24889] by original designation (Art. 68.2 ICZN);
valid after Guinot et al. (2013) p. 609 [24889];
shark-references Species-ID=13542;
type species of Adnetoscyllium Guinot et al., 2016 p. 609 [24889] by original designation (Art. 68.2 ICZN);
valid after Guinot et al. (2013) p. 609 [24889];
References
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
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
Late Cretaceous elasmobranch palaeoecology in NW Europe. Palaeogeography, Palaeoclimatology, Palaeoecology, 388, 23–41
DOI: 10.1016/j.palaeo.2013.07.027
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
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
Late Cretaceous elasmobranch palaeoecology in NW Europe. Palaeogeography, Palaeoclimatology, Palaeoecology, 388, 23–41
DOI: 10.1016/j.palaeo.2013.07.027