Scyliorhinus alaformis
Feichtinger, Pollerspöck, Harzhauser, Auer, Ćorić, Kranner, Beaury & Guinot, 2024
Classification: Elasmobranchii Carcharhiniformes Scyliorhinidae
Reference of the original description
Earliest Danian outer neritic elasmobranch assemblages reveal an environmentally controlled faunal turnover at the Cretaceous–Palaeogene boundary in the northern Tethyan Realm (Austria). Papers in Palaeontology, 10(1), Article e1547
Earliest Danian outer neritic elasmobranch assemblages reveal an environmentally controlled faunal turnover at the Cretaceous–Palaeogene boundary in the northern Tethyan Realm (Austria). Papers in Palaeontology, 10(1), Article e1547
Types
Scyliorhinus alaformis
Holotype: NHMW: 2023/0141/0004; Paratype: NHMW: 2023/0141/0002; NHMW: 2023/0142/0002;
Scyliorhinus alaformis
Holotype: NHMW: 2023/0141/0004; Paratype: NHMW: 2023/0141/0002; NHMW: 2023/0142/0002;
Description:
Citation: Scyliorhinus alaformis Feichtinger, Pollerspöck, Harzhauser, Auer, Ćorić, Kranner, Beaury & Guinot, 2024: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 08/2026
No image available.
Please send your images of "Scyliorhinus alaformis" to
info@shark-references.com
Please send your images of "Scyliorhinus alaformis" to
info@shark-references.com
Description
Original diagnosis after Feichtinger, Pollerspöck, Harzhauser, Auer, Ćorić, Kranner, Beaury & Guinot, 2024 [32635]: Tiny teeth with pronounced heterodonty. Straight and strongly lingually projected main cusp flanked by one pair of lateral cusps in anterior teeth, distally inclined main cusp flanked by one or two distal cusplets; a variable number of fused mesial cusplets in lateral teeth. Lingual crown face convex with long enameloid folds, labial face concave with coarse, parallel and short enameloid folds at the crown base. Moderate mediolingual root protuberance, flat and flared basal root face protruding. Strongly concave margino-lingual root faces in basal view; concave labial root face. Medio-lingual foramen on lingual protuberance and one pair of margino-lingual foramina present. Medio-labial foramen accompanied by one pair of marginal foramina.
Original diagnosis after Feichtinger, Pollerspöck, Harzhauser, Auer, Ćorić, Kranner, Beaury & Guinot, 2024 [32635]: Tiny teeth with pronounced heterodonty. Straight and strongly lingually projected main cusp flanked by one pair of lateral cusps in anterior teeth, distally inclined main cusp flanked by one or two distal cusplets; a variable number of fused mesial cusplets in lateral teeth. Lingual crown face convex with long enameloid folds, labial face concave with coarse, parallel and short enameloid folds at the crown base. Moderate mediolingual root protuberance, flat and flared basal root face protruding. Strongly concave margino-lingual root faces in basal view; concave labial root face. Medio-lingual foramen on lingual protuberance and one pair of margino-lingual foramina present. Medio-labial foramen accompanied by one pair of marginal foramina.
Remarks
shark-references Species-ID=17009
shark-references Species-ID=17009
References
Ecological restructuring of North Tethyan marine vertebrate communities triggered by the end-Cretaceous extinction. Proceedings of the National Academy of Sciences of the United States of America, 122(22), Article e2409366122
DOI: 10.1073/pnas.2409366122
Earliest Danian outer neritic elasmobranch assemblages reveal an environmentally controlled faunal turnover at the Cretaceous–Palaeogene boundary in the northern Tethyan Realm (Austria). Papers in Palaeontology, 10(1), Article e1547
DOI: 10.1002/spp2.1547
Haie und Rochen an der Kreide-Paläogen-Grenze. Fossilien, 3/2024, 48–57

Ecological restructuring of North Tethyan marine vertebrate communities triggered by the end-Cretaceous extinction. Proceedings of the National Academy of Sciences of the United States of America, 122(22), Article e2409366122
DOI: 10.1073/pnas.2409366122
Earliest Danian outer neritic elasmobranch assemblages reveal an environmentally controlled faunal turnover at the Cretaceous–Palaeogene boundary in the northern Tethyan Realm (Austria). Papers in Palaeontology, 10(1), Article e1547
DOI: 10.1002/spp2.1547

Haie und Rochen an der Kreide-Paläogen-Grenze. Fossilien, 3/2024, 48–57








