Plicatodus sp.
Classification: Elasmobranchii Xenacanthiformes Xenacanthidae
	Types
Plicatodus sp.
	
	
	
Plicatodus sp.
Description:
Citation: Plicatodus sp. : In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 11/2025
		Remarks
shark-references Species-ID=11996;
		
		shark-references Species-ID=11996;
		References
		
	
		
		
			
Pisces. In Piller, W.E. (ed.) Catalogus Fossilium Austriae, Band 3 - Verlag der Österreichischen Akademie der Wissenschaften, Wien, ISBN13: 978-3-7001-7238-3, 576 pp.
	
	
		
		
			
Climatic and biotic changes around the Carboniferous/Permian boundary recorded in the continental basins of the Czech Republic. International Journal of Coal Geology, 119, 114–151
DOI: 10.1016/j.coal.2013.07.014
	
	
		
		
			
Carboniferous and Permian faunas and their occurence in the limnic basins of the Czech Republic. Muzeum vychodních Cech v Hradci Králové, 2008
	
	
		
		
			
Biota of the Líně Formation (Stephanian C), mode of preservation and its palaeoecological interpretation [Abstract]. 11th Coal Geology Conference Prague 2004, Volume of Abstracts: 35–36
	
	
		
		
			
Vertebrate zonation of the non-marine Upper Carboniferous - Lower Permian basins of the Czech Republic. Courier Forschungsinstitut Senckenberg, 223, 563–575
	
	
	

Pisces. In Piller, W.E. (ed.) Catalogus Fossilium Austriae, Band 3 - Verlag der Österreichischen Akademie der Wissenschaften, Wien, ISBN13: 978-3-7001-7238-3, 576 pp.

Climatic and biotic changes around the Carboniferous/Permian boundary recorded in the continental basins of the Czech Republic. International Journal of Coal Geology, 119, 114–151
DOI: 10.1016/j.coal.2013.07.014

Carboniferous and Permian faunas and their occurence in the limnic basins of the Czech Republic. Muzeum vychodních Cech v Hradci Králové, 2008

Biota of the Líně Formation (Stephanian C), mode of preservation and its palaeoecological interpretation [Abstract]. 11th Coal Geology Conference Prague 2004, Volume of Abstracts: 35–36

Vertebrate zonation of the non-marine Upper Carboniferous - Lower Permian basins of the Czech Republic. Courier Forschungsinstitut Senckenberg, 223, 563–575
				
				
    					
    					
    					
    					
                        
    					








