Carcharhinus cf. brachyurus-f
(Günther, 1870)
Classification: Elasmobranchii Carcharhiniformes Carcharhinidae
	Reference of the original description
	
	
Catalogue of the fishes in the British Museum. London, British Museum(Natural History). Vol. 8: 549 p.
Catalogue of the fishes in the British Museum. London, British Museum(Natural History). Vol. 8: 549 p.
	Types
Carcharhinus cf. brachyurus-f
	
	
	
Carcharhinus cf. brachyurus-f
Description:
Citation: Carcharhinus cf. brachyurus-f (Günther, 1870): 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=16908
		shark-references Species-ID=16908
		References
		
	
		
		
			
Sharks and rays (Chondrichthyes: Elasmobranchii) from the Peace River and Tamiami formations (Late Miocene–Early Pliocene) on the submerged continental shelf near Venice, Florida, USA. Palaeontologia Electronica, 28(3), Article a49
DOI: 10.26879/1529
	
	
		
		
			
Quaternary fossil shark (Neoselachii: Galeomorphii and Squalomorphii) diversity from southern Brazil. Journal of South American Earth Sciences, 122, Article 104176
DOI: 10.1016/j.jsames.2022.104176
	
	
		
		
			
Fossil chondrichthyans and other new paleontological resources at gulf islands national seashore. New Mexico Museum of Natural History and Science Bulletin, 94, 143–154
	
	
		
		
			
Fossiliensuche in den Mittelatlantikstaaten der USA: Potomac River und Chesapeake Bay in Virginia und Maryland. Der Steinkern, 41, 50–66
	
	
		
		
			
First report on a diverse Neogene cartilaginous fish fauna from Borneo (Ambug Hill, Brunei Darussalam). Journal of Systematic Palaeontology, 17(10), 791–819
DOI: 10.1080/14772019.2018.1468830
	
	
		
		
			
Neogene Caribbean elasmobranchs: diversity, paleoecology and paleoenvironmental significance of the Cocinetas Basin assemblage (Guajira Peninsula, Colombia). Biogeosciences, 16, 33–56
DOI: 10.5194/bg-16-33-2019
	
	
		
		
			
The Bahía Inglesa Formation Bonebed: Genesis and Palaeontology of a Neogene Konzentrat Lagerstätte from north-central Chile. Postgraduate Thesis, University of Portsmouth, 440 pp.
	
	
		
		
			
Chapter 15: Chondrichthyans in the Cretaceous and Tertiary of Australia. Vertebrate Palaeontology of Australasia: 497–568, 40 pl.
	
	
		
		
			
An Early Pliocene shark tooth assemblage in South Australia. South Australia Department of Mines and Energy, Special. Publication, 5: 287–299, 2 fig., pl. 1–19.
	
	
Sharks and rays (Chondrichthyes: Elasmobranchii) from the Peace River and Tamiami formations (Late Miocene–Early Pliocene) on the submerged continental shelf near Venice, Florida, USA. Palaeontologia Electronica, 28(3), Article a49
DOI: 10.26879/1529

Quaternary fossil shark (Neoselachii: Galeomorphii and Squalomorphii) diversity from southern Brazil. Journal of South American Earth Sciences, 122, Article 104176
DOI: 10.1016/j.jsames.2022.104176

Fossil chondrichthyans and other new paleontological resources at gulf islands national seashore. New Mexico Museum of Natural History and Science Bulletin, 94, 143–154

Fossiliensuche in den Mittelatlantikstaaten der USA: Potomac River und Chesapeake Bay in Virginia und Maryland. Der Steinkern, 41, 50–66

First report on a diverse Neogene cartilaginous fish fauna from Borneo (Ambug Hill, Brunei Darussalam). Journal of Systematic Palaeontology, 17(10), 791–819
DOI: 10.1080/14772019.2018.1468830
Neogene Caribbean elasmobranchs: diversity, paleoecology and paleoenvironmental significance of the Cocinetas Basin assemblage (Guajira Peninsula, Colombia). Biogeosciences, 16, 33–56
DOI: 10.5194/bg-16-33-2019

The Bahía Inglesa Formation Bonebed: Genesis and Palaeontology of a Neogene Konzentrat Lagerstätte from north-central Chile. Postgraduate Thesis, University of Portsmouth, 440 pp.


Chapter 15: Chondrichthyans in the Cretaceous and Tertiary of Australia. Vertebrate Palaeontology of Australasia: 497–568, 40 pl.

An Early Pliocene shark tooth assemblage in South Australia. South Australia Department of Mines and Energy, Special. Publication, 5: 287–299, 2 fig., pl. 1–19.
				
				
    					
    					
    					
    					
                        
    					








