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Ogilbia luzanensis

Actinopteri - Ophidiiformes - Bythitidae

Taxonomy
Ogilbia luzanensis was named by Schwarzhans and Bratischko (2011). Its type specimen is ULUZ 2/139, an otolith, and it is a 3D body fossil. Its type locality is Luzanivka [Tashlik Fm], which is in a Selandian/Thanetian shallow subtidal sandstone in the Tashlik Formation of Ukraine.

Synonymy list
YearName and author
2011Ogilbia luzanensis Schwarzhans and Bratischko pp. 94-95 figs. figs. 9A-F, 15H

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RankNameAuthor
kingdomAnimalia()
—Bilateria
—EubilateriaAx 1987
—Deuterostomia
phylumChordataHaeckel 1874
subphylumVertebrata
superclassGnathostomata
—Osteichthyes()
superclassActinopterygii()
classActinopteri()
subclassNeopterygii(Regan 1923)
—Teleosteomorpha
—Teleostei(Müller 1846)
—Osteoglossocephalai
—ClupeocephalaPatterson and Rosen 1977
RankNameAuthor
—Euteleosteomorpha
—NeoteleosteiRosen 1973
—Eurypterygia(Rosen 1973)
—Ctenosquamata
—Acanthomorphata(Rosen 1973)
—Euacanthomorphacea
—Percomorphaceae
—Ophidiimorpharia
orderOphidiiformesBerg 1937
suborderBythitoidei
familyBythitidaeGill 1861
subfamilyDinematichthyinaeWhitley 1928
genusOgilbiaJordan and Evermann 1898
speciesluzanensis

If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.

†Ogilbia luzanensis Schwarzhans and Bratischko 2011
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Diagnosis
ReferenceDiagnosis
W. Schwarzhans and A. Bratischko 2011Elongate, thin otoliths; OL:OH = 1.9-2.2; OH:OT = 2.0-2.5. Dorsal rim with concavity behind post- dorsal angle. Inner face slightly convex; outer face flat. Sul- cus clearly divided into longer ostium and shorter, deepened cauda.