Isurolamna bajarunasi
(Glikman & Zhelezko, 1985)
Classification: Elasmobranchii Lamniformes Lamnidae
Reference of the original description
(Paleogene sharks of the Mangyschlak Plateau and the Eocene/Oligocene boundary). «in russian». Byull. Mosk. Obshvhest. Ispyt. Prir., Otd. Geol., 60(5): 86–99, 2 fig., 1 pl.
(Paleogene sharks of the Mangyschlak Plateau and the Eocene/Oligocene boundary). «in russian». Byull. Mosk. Obshvhest. Ispyt. Prir., Otd. Geol., 60(5): 86–99, 2 fig., 1 pl.
Synonyms / new combinations and misspellings
Lamiostoma bajarunasi
Lamiostoma bajarunasi
Types
Isurolamna bajarunasi
Isurolamna bajarunasi
Description:
Citation: Isurolamna bajarunasi (Glikman & Zhelezko, 1985): In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 12/2024
Remarks
shark-references Species-ID=3219;
shark-references Species-ID=3219;
References
Chondrichthyan fishes from the Middle Eocene Osinovaya Formation of Rostov Region, Russia. Historical Biology, in press
DOI: 10.1080/08912963.2023.2291774
Faszination Haie – Die Welt der fossilen und der lebenden Haie. Der Steinkern, 58, 1–116
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
Records of Elasmobranchian Teeth in the Bartonian of the Northern Caucasus (Russia) and Crimea (Ukraine). Paleonotological Journal, 47(1), 98–103
DOI: 10.1134/S0031030113010085
Oxygen isotope analysis of shark teeth phosphates from Bartonian (Eocene) deposits in Mangyshlak peninsula, Kazakhstan. Mineralogia, 42(1), 53–61
DOI: 10.2478/v10002-011-0006-7
(Elasmobranchs of the western margin of the West Siberian Paleogene basin.) «in russian». Ekaterinburg: IGG UB RAS, 2006, 224 p., ICC 5–94332–048–2
Late Eocene Elasmobranchii in the Pleistocene Fluvial Taphocenosis in the Мiddle Trans-Ural: Biostratigraphic and Paleogeographic Importans [in russian]. Lithosphere, 4, 84–90
(Paleogene sharks of the Mangyschlak Plateau and the Eocene/Oligocene boundary). «in russian». Byull. Mosk. Obshvhest. Ispyt. Prir., Otd. Geol., 60(5): 86–99, 2 fig., 1 pl.
Chondrichthyan fishes from the Middle Eocene Osinovaya Formation of Rostov Region, Russia. Historical Biology, in press
DOI: 10.1080/08912963.2023.2291774
Faszination Haie – Die Welt der fossilen und der lebenden Haie. Der Steinkern, 58, 1–116
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
Records of Elasmobranchian Teeth in the Bartonian of the Northern Caucasus (Russia) and Crimea (Ukraine). Paleonotological Journal, 47(1), 98–103
DOI: 10.1134/S0031030113010085
Oxygen isotope analysis of shark teeth phosphates from Bartonian (Eocene) deposits in Mangyshlak peninsula, Kazakhstan. Mineralogia, 42(1), 53–61
DOI: 10.2478/v10002-011-0006-7
(Elasmobranchs of the western margin of the West Siberian Paleogene basin.) «in russian». Ekaterinburg: IGG UB RAS, 2006, 224 p., ICC 5–94332–048–2
Late Eocene Elasmobranchii in the Pleistocene Fluvial Taphocenosis in the Мiddle Trans-Ural: Biostratigraphic and Paleogeographic Importans [in russian]. Lithosphere, 4, 84–90
(Paleogene sharks of the Mangyschlak Plateau and the Eocene/Oligocene boundary). «in russian». Byull. Mosk. Obshvhest. Ispyt. Prir., Otd. Geol., 60(5): 86–99, 2 fig., 1 pl.
