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<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/"><rdf:Description rdf:about="https://dirros.openscience.si/IzpisGradiva.php?id=24864"><dc:title>Revision of Xanthopsis bodracus Makarenko, 1956 (Crustacea: Decapoda) from the Palaeogene of Ukraine</dc:title><dc:creator>Dernov,	Vitaly	(Avtor)
	</dc:creator><dc:subject>decapod crustaceans</dc:subject><dc:subject>Harpactoxanthopsis</dc:subject><dc:subject>Xanthopsis</dc:subject><dc:subject>Lutetian</dc:subject><dc:subject>taxonomy</dc:subject><dc:description>The  present  article  constitutes  a  revision  of  the  decapod  crustacean  species  Xanthopsis bodracus  Makarenko,  1956  from the early Lutetian (Eocene, Palaeogene) of the Crimean Peninsula, southern Ukraine. The distinctive morphological characteristics  of  Xanthopsis bodracus  enable  its  classification  within  the  genus  Harpactoxanthopsis Via  Boada,  1959,  as the type series of Xanthopsis bodracus precisely aligns with the diagnostic criteria of this genus. Of the five species in the genus Harpactoxanthopsis, Xanthopsis bodracus is morphologically closest to Harpactoxanthopsis quadrilobatus(Desmarest,  1822).  However,  there  are  currently  insufficient  grounds  to  confidently  synonymise  Xanthopsis bodracuswith Harpactoxanthopsis quadrilobatus, as the poorly preserved type material, of which only a part has been preserved, does  not  allow  this.  In  view  of  this,  Xanthopsis bodracus  has  been  revised  as  Harpactoxanthopsis  sp.  The  Palaeogene  decapod  assemblages  of  Crimea  consist  of  five  genera  including  Coeloma A.  Milne-Edwards,  1865,  Protocallianassa Beurlen, 1930, Arcticocarcinus Shweitzer et al., 2016, Xanthopsis M’Coy, 1849, and Harpactoxanthopsis Via Boada, 1959.</dc:description><dc:publisher>Geološki zavod Slovenije</dc:publisher><dc:date>2025</dc:date><dc:date>2025-12-23 03:58:44</dc:date><dc:type>Neznano</dc:type><dc:identifier>24864</dc:identifier><dc:language>sl</dc:language></rdf:Description></rdf:RDF>
