Basic info Taxonomic history Classification Included Taxa
Morphology Ecology and taphonomy External Literature Search Age range and collections

Patene campbelli

Mammalia - Sparassodonta

Discussion

HOLOTYPE. LACM 140628, isolated left M4. HYPODIGM. The holotype only.

Taxonomy
Patene campbelli was named by Goin and Candela (2004) [n. sp.]. It is a 3D body fossil. Its type locality is Santa Rosa (LACM Loc. 6289), which is in a Rupelian terrestrial mudstone/sandstone in the Yahuarango Formation of Peru.

Synonymy list
YearName and author
2004Patene campbelli Goin and Candela

Is something missing? Join the Paleobiology Database and enter the data

RankNameAuthor
kingdomAnimalia()
—Bilateria
—EubilateriaAx 1987
—Deuterostomia
phylumChordataHaeckel 1874
subphylumVertebrata
superclassGnathostomata
—Osteichthyes()
subclassSarcopterygii()
subclassDipnotetrapodomorpha(Nelson 2006)
subclassTetrapodomorpha()
—Tetrapoda
—Reptiliomorpha
—Anthracosauria
subclassAmphibiosauriaKuhn 1967
—Cotylosauria()
—Amniota
subclassSynapsida
RankNameAuthor
—Therapsida()
infraorderCynodontia()
—Mammaliamorpha
—Mammaliaformes
classMammalia
—Theriamorpha(Rowe 1993)
—Theriiformes()
—Trechnotheria
—Cladotheria
—Zatheria
subclassTribosphenida()
subclassTheria
subclassMetatheria()
—Marsupialiformes
orderSparassodonta()
subfamilyHathlyacininae()
genusPatene
speciescampbelli

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.

†Patene campbelli Goin and Candela 2004
show all | hide all
Diagnosis
ReferenceDiagnosis
F. J. Goin and A. M. Candela 2004DIAGNOSIS. Differs from Patene simpsoni Paula Couto, 1952b, in its smaller size and by the presence, in M4, of a more reduced metacone and less developed anterobasal cingulum. It differs from Patene colhuapiensis Simpson, 1935, by its smaller size and by having M4 with persistent anterobasal cingulum, paraconule and metacone more developed,and trigon basin wider.