Parotodus mangyshlakensis
Kozlov in Zhelezko & Kozlov, 1999
Classification: Elasmobranchii Lamniformes Otodontidae
Reference of the original description
Elasmobranhii i biostratigraphia paleogena Zauralia i Srednei Asii. (Elasmobranchii and Palaeogene biostratigraphy of Transural and Central Asia). Materialy po Stratigrafii i Paleontologii Urala, 3, 324 pp, Ekaterinburg, UrO RAN
Elasmobranhii i biostratigraphia paleogena Zauralia i Srednei Asii. (Elasmobranchii and Palaeogene biostratigraphy of Transural and Central Asia). Materialy po Stratigrafii i Paleontologii Urala, 3, 324 pp, Ekaterinburg, UrO RAN
Types
Parotodus mangyshlakensis
Holotype: Darwin Museum: GIK No. 15478/1; Paratype: Darwin Museum: GIK No. 15478/2, 5, 8-10;
Parotodus mangyshlakensis
Holotype: Darwin Museum: GIK No. 15478/1; Paratype: Darwin Museum: GIK No. 15478/2, 5, 8-10;
Description:
Citation: Parotodus mangyshlakensis Kozlov in Zhelezko & Kozlov, 1999: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 11/2024
Please send your images of "Parotodus mangyshlakensis" to info@shark-references.com
Parotodus mangyshlakensis Kozlov in Zhelezko & Kozlov, 1999, lingual view, Holotype GIK No. 15478/1 © State Darwin Museum, Moscow
Parotodus mangyshlakensis Kozlov in Zhelezko & Kozlov, 1999, lingual view, Holotype GIK No. 15478/1 © State Darwin Museum, Moscow
Remarks
shark-references Species-ID=4749;
shark-references Species-ID=4749;
References
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
Shark and ray faunas in the Middle and Late Eocene of the Fayum Area, Egypt. Proceedings of the Geologists' Association, 122(1), 47–66
DOI: 10.1016/j.pgeola.2010.09.004
Paleo-environments of the exposed Eocene Sediments between Wadi El-Hitan and east Siwa in the Egyptian Western Desert based on their faunal content especially the vertebrates. Thesis, Zagazig University, Faculty of Science, Geology Department
Descripción de asociaciones faunísticas de elasmobranquios fósiles del eoceno superior (Priaboniano) de las formaciones Tepetate y Bateque de Baja California Sur, México. unpublished Thesis, La Paz, Centro Interdisciplinario de Ciencias Marinas. XIII, 226 p.
Elasmobranhii i biostratigraphia paleogena Zauralia i Srednei Asii. (Elasmobranchii and Palaeogene biostratigraphy of Transural and Central Asia). Materialy po Stratigrafii i Paleontologii Urala, 3, 324 pp, Ekaterinburg, UrO RAN
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
Shark and ray faunas in the Middle and Late Eocene of the Fayum Area, Egypt. Proceedings of the Geologists' Association, 122(1), 47–66
DOI: 10.1016/j.pgeola.2010.09.004
Paleo-environments of the exposed Eocene Sediments between Wadi El-Hitan and east Siwa in the Egyptian Western Desert based on their faunal content especially the vertebrates. Thesis, Zagazig University, Faculty of Science, Geology Department
Descripción de asociaciones faunísticas de elasmobranquios fósiles del eoceno superior (Priaboniano) de las formaciones Tepetate y Bateque de Baja California Sur, México. unpublished Thesis, La Paz, Centro Interdisciplinario de Ciencias Marinas. XIII, 226 p.
Elasmobranhii i biostratigraphia paleogena Zauralia i Srednei Asii. (Elasmobranchii and Palaeogene biostratigraphy of Transural and Central Asia). Materialy po Stratigrafii i Paleontologii Urala, 3, 324 pp, Ekaterinburg, UrO RAN
