Abdounia lapierrei
Cappetta & Nolf, 1981
Classification: Elasmobranchii Carcharhiniformes Carcharhinidae
Reference of the original description
Les sélaciens de l'Auversien de Ronquerolles (Eocène supérieur du Bassin de Paris). Mededelingen Van De Werkgroep Voor Tertiaire En Kwartaire Geologie, 18(3), 87–107
Les sélaciens de l'Auversien de Ronquerolles (Eocène supérieur du Bassin de Paris). Mededelingen Van De Werkgroep Voor Tertiaire En Kwartaire Geologie, 18(3), 87–107
Synonyms / new combinations and misspellings
Abdounia kashiensis
Abdounia kashiensis
Types
Abdounia lapierrei
Abdounia lapierrei
Description:
Citation: Abdounia lapierrei Cappetta & Nolf, 1981: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 11/2024
Remarks
shark-references Species-ID=12;
shark-references Species-ID=12;
References
Integrated palaeontological investigation of a new mid-late Bartonian fish fauna from Călata area, Transylvanian Basin, Romania. Historical Biology, 34(9), 1788–1816
DOI: 10.1080/08912963.2021.1980879
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
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
Feeding ecology has shaped the evolution of modern sharks. Current Biology, 31(23), 5138–5148
DOI: 10.1016/j.cub.2021.09.028
Morphometrische Analyse der Kieferbezahnung fossiler wie rezenter carcharhinider Selachier. PhD Thesis, University of Leipzig
Eocene Carcharinidae and Triakidae (Elasmobranchii) of Crimea and Kazakhstan. Leipziger Geowissenschaften, 20, 1–57
Elasmobranchs from the late Eocene Wadi Esh-Shallala Formation of Qa'Faydat ad Dahikiya, east Jordan. Tertiary Research, 21(1–4), 77–94
Elasmobranch fossils from the late Eocene of the Wadi Esh-Shallala Formation, Qa'Faydat ad Dahikiya, east Jordan [Abstract]. Journal of Vertebrate Paleontology, 19(Supplement to Number 3), 66A
Elasmobranchs from the Lower Tertiary of the western Tarim Basin, China, and their biostratigraphic significance. Palaeoworld, 7, 107–136
Elasmobranchs from the Lower Tertiary of the western Tarim Basin, China, and their biostratigraphic significance. Palaeoworld, 7, 107–136
A Middle Eocene selachian fauna from the White Mountain Formation of the Kizylkum Desert, Uzbekistan, C.I.S. Palaeontographica, Abt. A, 242(4–6), 99–126
Fossil Sharks of the Chesapeake Bay Region. Egan Rees and Boyer, Inc. Columbia. 146 pp.
A checklist of Neoselachii (Pisces, Chondrichthyes) from the Palaeogene of the Paris Basin, France. Tertiary Research, 13(1) , 27–36
Fossils from the Bracklesham Group exposed in the M27 Motorway excavations, Southampton, Hampshire. Tertiary Research, 12(3–4), 131–137
A checklist of Palaeocene and Eocene sharks and rays (Chondrichthyes) from the Pamunkey Group, Maryland and Virginia, USA. Tertiary Research, 12(2), 81–88
An Illustrated Guide to the British Middle Eocene Vertebrates. Privately published, London, 59 pp.
The shark teeth of the Paris Basin and the shark teeth of the Armorican Massif. Geologisches Jahrbuch, Reihe A, 100, 390–391
Les sélaciens de l'Auversien de Ronquerolles (Eocène supérieur du Bassin de Paris). Mededelingen Van De Werkgroep Voor Tertiaire En Kwartaire Geologie, 18(3), 87–107
Integrated palaeontological investigation of a new mid-late Bartonian fish fauna from Călata area, Transylvanian Basin, Romania. Historical Biology, 34(9), 1788–1816
DOI: 10.1080/08912963.2021.1980879
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
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
Feeding ecology has shaped the evolution of modern sharks. Current Biology, 31(23), 5138–5148
DOI: 10.1016/j.cub.2021.09.028
Morphometrische Analyse der Kieferbezahnung fossiler wie rezenter carcharhinider Selachier. PhD Thesis, University of Leipzig
Eocene Carcharinidae and Triakidae (Elasmobranchii) of Crimea and Kazakhstan. Leipziger Geowissenschaften, 20, 1–57
Elasmobranchs from the late Eocene Wadi Esh-Shallala Formation of Qa'Faydat ad Dahikiya, east Jordan. Tertiary Research, 21(1–4), 77–94
Elasmobranch fossils from the late Eocene of the Wadi Esh-Shallala Formation, Qa'Faydat ad Dahikiya, east Jordan [Abstract]. Journal of Vertebrate Paleontology, 19(Supplement to Number 3), 66A
Elasmobranchs from the Lower Tertiary of the western Tarim Basin, China, and their biostratigraphic significance. Palaeoworld, 7, 107–136
Elasmobranchs from the Lower Tertiary of the western Tarim Basin, China, and their biostratigraphic significance. Palaeoworld, 7, 107–136
A Middle Eocene selachian fauna from the White Mountain Formation of the Kizylkum Desert, Uzbekistan, C.I.S. Palaeontographica, Abt. A, 242(4–6), 99–126
Fossil Sharks of the Chesapeake Bay Region. Egan Rees and Boyer, Inc. Columbia. 146 pp.
A checklist of Neoselachii (Pisces, Chondrichthyes) from the Palaeogene of the Paris Basin, France. Tertiary Research, 13(1) , 27–36
Fossils from the Bracklesham Group exposed in the M27 Motorway excavations, Southampton, Hampshire. Tertiary Research, 12(3–4), 131–137
A checklist of Palaeocene and Eocene sharks and rays (Chondrichthyes) from the Pamunkey Group, Maryland and Virginia, USA. Tertiary Research, 12(2), 81–88
An Illustrated Guide to the British Middle Eocene Vertebrates. Privately published, London, 59 pp.
The shark teeth of the Paris Basin and the shark teeth of the Armorican Massif. Geologisches Jahrbuch, Reihe A, 100, 390–391
Les sélaciens de l'Auversien de Ronquerolles (Eocène supérieur du Bassin de Paris). Mededelingen Van De Werkgroep Voor Tertiaire En Kwartaire Geologie, 18(3), 87–107