Myliobatis cf. latidens
Woodward, 1888
Classification: Elasmobranchii Myliobatiformes Myliobatidae
	Reference of the original description
	
	
Notes on the determination of the fossil teeth of Myliobatis, with a revision of the English Eocene species. Annals and Magazine of Natural History, (Series 6), 1, 36–47
Notes on the determination of the fossil teeth of Myliobatis, with a revision of the English Eocene species. Annals and Magazine of Natural History, (Series 6), 1, 36–47
	Types
Myliobatis cf. latidens
	
	
	
Myliobatis cf. latidens
Description:
Citation: Myliobatis cf. latidens Woodward, 1888: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 11/2025
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		Remarks
shark-references Species-ID=13073;
		
		shark-references Species-ID=13073;
		References
		
	
		
		
			
Sharks and rays from the Mokattamian Stage (middle and late Eocene) of Egypt, including some species from the middle Eocene Midra Shale of Qatar. Egyptian Journal of Geology, 66(1), 105–153
DOI: 10.21608/EGJG.2022.173845.1028
	
	
		
		
			
Die Eocaenfaunen der bayrischen Alpen, I. Teil: die Faunen des Unter- und Mitteleocaen. II. Teil: Die Obereocaenfauna. Abhandlungen der Bayerischen Akademie der Wissenschaften, Mathematisch–Naturwissenschaftliche Abteilung, 30, 79–153
	
	
		
		
			
Myliobatiden aus dem Mitteleocän der bayerischen Alpen. Zeitschrift der Deutschen Geologischen Gesellschaft, 56(3), 249–267
	
	
Sharks and rays from the Mokattamian Stage (middle and late Eocene) of Egypt, including some species from the middle Eocene Midra Shale of Qatar. Egyptian Journal of Geology, 66(1), 105–153
DOI: 10.21608/EGJG.2022.173845.1028
Die Eocaenfaunen der bayrischen Alpen, I. Teil: die Faunen des Unter- und Mitteleocaen. II. Teil: Die Obereocaenfauna. Abhandlungen der Bayerischen Akademie der Wissenschaften, Mathematisch–Naturwissenschaftliche Abteilung, 30, 79–153

Myliobatiden aus dem Mitteleocän der bayerischen Alpen. Zeitschrift der Deutschen Geologischen Gesellschaft, 56(3), 249–267
				
				
    					
    					
    					
    					
                        
    					








