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Prolibytherium fusus

Osteichthyes - Climacoceratidae

Taxonomy
Prolibytherium fusus was named by Danowitz et al. (2016). Its type specimen is PMNH Z 162, a partial skull (caudoventral portion of braincase), and it is a 3D body fossil. Its type locality is Z124, which is in a Burdigalian/Serravallian terrestrial horizon in the Vihowa Formation of Pakistan.

Synonymy list
YearName and author
2016Prolibytherium fusus Danowitz et al. p. 203

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RankNameAuthor
kingdomAnimalia()
Bilateria
EubilateriaAx 1987
Deuterostomia
phylumChordataHaeckel 1874
subphylumVertebrata
superclassGnathostomata
classOsteichthyes
subclassSarcopterygii()
subclassDipnotetrapodomorpha(Nelson 2006)
subclassTetrapodomorpha()
Tetrapoda
Reptiliomorpha
Anthracosauria
subclassAmphibiosauriaKuhn 1967
Cotylosauria()
Amniota
subclassSynapsida
Therapsida()
RankNameAuthor
infraorderCynodontia()
Mammaliamorpha
Mammaliaformes
classMammalia
Cladotheria
Zatheria
subclassTribosphenida()
subclassTheria
Eutheria()
Placentalia
Boreoeutheria
Laurasiatheria
Scrotifera
Euungulata
Artiodactylamorpha
Artiodactyla()
familyClimacoceratidae()
genusProlibytheriumArambourg 1961
speciesfusus

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.

Prolibytherium fusus Danowitz et al. 2016
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Diagnosis
ReferenceDiagnosis
M. Danowitz et al. 2016Prolibytherium fusus differs from P. magnieri in the following characters: the anterior basioccipital tuberosities are less distinct, and their surface contains longitudinal ridges instead of small bumps seen on P. magnieri. The elongated fossa between the posterior and anterior basioccipital tuberosities is one unified surface in P. magnieri, and is separated into two plates by a midline longitudinal groove in P. fusus. In P. fusus, the posterior basioccipital tuberosities are more approximated with the ar- ticular surface of the occipital condyles, and are thicker and shorter. The posterior basioccipital tuberosities are also ap- proximated across the midline in P. fusus, separated only by a narrow, deep groove, and the caudal surface contains several bony growths concentrated medially. In P. magnieri, the pos- terior basioccipital tuberosities are separated at the midline, also by a deep groove, and the surface contains a distinct elevated transverse ridge, and no bony growths. The U- shaped ventral margin on the occipital condyles is more shal- low in P. fusus, and the condyles are oriented laterally, where- as the condyles are oriented dorso-laterally and have a deeper U-shaped ventral margin in P. magnieri. The notch between the paraoccipital process and the lateral occipital condyles is thicker and lower in P. fusus (Fig. 4: character 5).
Measurements
No measurements are available
Composition: phosphaticsubp
Environment: terrestrialo
Locomotion: actively mobilec
Life habit: ground dwellingo
Diet: grazero
Diet 2: browsero
Reproduction: viviparoussubc
Created: 2005-08-26 14:03:05
Modified: 2005-09-19 12:23:23
Source: o = order, subc = subclass, c = class, subp = subphylum
References: Carroll 1988, Hendy et al. 2009, Nowak 1999, Lillegraven 1979

Age range: base of the Burdigalian to the top of the Serravallian or 20.45000 to 11.63000 Ma

Collections: one only


Time interval Ma Country or state Original ID and collection number
Burdigalian - Serravallian20.45 - 11.63Pakistan (Baluchistan) Prolibytherium fusus (type locality: 180613)