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Bakonybatrachus fedori
Taxonomy
Bakonybatrachus fedori was named by Szentesi and Venczel (2012). Its type specimen is MTM V 2010.283.1., a limb element (Incomplete right ilium), and it is a 3D body fossil. Its type locality is Iharkút mine, Bakony mountains (Unit 1), which is in a Santonian crevasse splay claystone/sandstone in the Csehbánya Formation of Hungary. It is the type species of Bakonybatrachus.
Synonymy list
| Year | Name and author |
|---|---|
| 2012 | Bakonybatrachus fedori Szentesi and Venczel p. 328 |
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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.
†Bakonybatrachus fedori Szentesi and Venczel 2012
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Diagnosis
| Reference | Diagnosis | |
|---|---|---|
| Z. Szentesi and M. Venczel 2012 | A small anuran, with estimated snoutevent length of 25-30 mm. It differs from gobiatine, bombinatorine, alytine frogs and Callobatrachus, as well as from the incertae sedis anurans Hatzegobatrachus and Yizhoubatrachus by the presence of a well developed iliac crest. It differs from discoglossine frogs, with the exception of some members of Discoglossus, by its dorsal protuberance being lower than that of the iliac crest and provided with a thickened and flattened dorsolateral surface circumscribed by a shallow groove. It differs also from Discoglossus, Latonia, Paradiscoglossus and Paralatonia by its more robustly built dorsal acetabular expansion and by its smaller ventral acetabular expansion. |
Measurements
No measurements are available
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| Source: subo = suborder, c = class, subp = subphylum, uc = unranked clade | |||||
| References: Kiessling 2004, Hendy et al. 2009, Carroll 1988, Uhen 2004 | |||||