Carcharocles sokolowi
(Jaekel, 1895)
Classification: Elasmobranchii Lamniformes Otodontidae
	Reference of the original description
	
	
Unter-tertiäre Selachier aus Südrussland. Mémoirs du Comité geologique de St. Petersburg, 9(4), 19–35
Unter-tertiäre Selachier aus Südrussland. Mémoirs du Comité geologique de St. Petersburg, 9(4), 19–35
	Types
Carcharocles sokolowi
	
	
	
Carcharocles sokolowi
Description:
Citation: Carcharocles sokolowi (Jaekel, 1895): In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 11/2025
		Remarks
shark-references Species-ID=8089;
		
		shark-references Species-ID=8089;
		References
		
	
		
		
			
Feeding ecology has shaped the evolution of modern sharks. Current Biology, 31(23), 5138–5148
DOI: 10.1016/j.cub.2021.09.028
	
	
		
		
			
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
	
	
		
		
			
Review of the Middle Eocene (Lutetian) selachian fauna of Jebal eth Thuleithuwat, east Jordan. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen, 237(3), 399–422
	
	
		
		
			
Middle Eocene selachian fauna from Wadi Al-Rijla Al-Bayda, Eastern Desert of Jordan. Abhath Al–Yamouk Basic Sciences and Engineering, 12(2b), 619–631
	
	
		
		
			
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 unpublished Thesis, La Paz, Centro Interdisciplinario de Ciencias Marinas.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.
	
	
		
		
			
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
	
	
		
		
			
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
	
	
Feeding ecology has shaped the evolution of modern sharks. Current Biology, 31(23), 5138–5148
DOI: 10.1016/j.cub.2021.09.028

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

Review of the Middle Eocene (Lutetian) selachian fauna of Jebal eth Thuleithuwat, east Jordan. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen, 237(3), 399–422

Middle Eocene selachian fauna from Wadi Al-Rijla Al-Bayda, Eastern Desert of Jordan. Abhath Al–Yamouk Basic Sciences and Engineering, 12(2b), 619–631
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.

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

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
				
				
    					
    					
    					
    					
                        
    					








