Parotodus pavlovi
(Menner, 1928)
Classification: Elasmobranchii Lamniformes Otodontidae
Reference of the original description
Les Sélaciens du Paléogène de Manghyschlak, d'Emba et du versant oriental d'Oural. «in russian». Bulletin de la Société Impériale des Naturalistes de Moscou, Section Géologique, 6(3–4), 292–338
Les Sélaciens du Paléogène de Manghyschlak, d'Emba et du versant oriental d'Oural. «in russian». Bulletin de la Société Impériale des Naturalistes de Moscou, Section Géologique, 6(3–4), 292–338
Image of the original description
Parotodus pavlovi (Menner, 1928), Eocene, Ypresian, Aksuat Well, Emba River, western Kazakhstan, central Asia, Plate 10 Fig. 32-35 Menner, 1928
Parotodus pavlovi (Menner, 1928), Eocene, Ypresian, Aksuat Well, Emba River, western Kazakhstan, central Asia, Plate 10 Fig. 32-35 Menner, 1928
Synonyms / new combinations and misspellings
Otodus pavlovi
Otodus pavlovi
Types
Parotodus pavlovi
Parotodus pavlovi
Description:
Citation: Parotodus pavlovi (Menner, 1928): In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 04/2024
Please send your images of "Parotodus pavlovi" to info@shark-references.com
Parotodus pavlovi (Menner, 1928), Eocene, Ypresian, France © Jean-Francois LHOMME, www.vertebres-fossiles.com
Parotodus pavlovi (Menner, 1928), Eocene, Ypresian, France © Jean-Francois LHOMME, www.vertebres-fossiles.com
Distribution Geographic
Aksuat Well, Emba River, western Kazakhstan, central Asia [1639]; Marke clay pit, western Belgium [15339]; France, Paris Basin
Aksuat Well, Emba River, western Kazakhstan, central Asia [1639]; Marke clay pit, western Belgium [15339]; France, Paris Basin
Distribution Strategraphy
Ypresian, Eocene
Ypresian, Eocene
Remarks
shark-references Species-ID=4752;
shark-references Species-ID=4752;
References
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
Des dents de requins fossiles! 9. Le genre Parotodus: le faux requin-mako. Fossiles – Revue Francaise de Paléontologie, 37, 39–50
The Aktulagay section, west Kazakhstan: a key site fornorthern mid-latitude Early Eocene stratigraphy. Stratigraphy, 10(3): 171–209
Quantitative analysis of Elasmobranch assemblages from two successive Ypresian (early Eocene) facies at Marke, western Belgium. Geologica Belgica, 15(3), 146–153
Les Sélaciens du Paléogène de Manghyschlak, d'Emba et du versant oriental d'Oural. «in russian». Bulletin de la Société Impériale des Naturalistes de Moscou, Section Géologique, 6(3–4), 292–338
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
Des dents de requins fossiles! 9. Le genre Parotodus: le faux requin-mako. Fossiles – Revue Francaise de Paléontologie, 37, 39–50
The Aktulagay section, west Kazakhstan: a key site fornorthern mid-latitude Early Eocene stratigraphy. Stratigraphy, 10(3): 171–209
Quantitative analysis of Elasmobranch assemblages from two successive Ypresian (early Eocene) facies at Marke, western Belgium. Geologica Belgica, 15(3), 146–153
Les Sélaciens du Paléogène de Manghyschlak, d'Emba et du versant oriental d'Oural. «in russian». Bulletin de la Société Impériale des Naturalistes de Moscou, Section Géologique, 6(3–4), 292–338
