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 11/2024
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