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Baraguatherium takumara

Osteichthyes - Mylodontidae

Taxonomy
Baraguatherium takumara was named by Rincón et al. (2016). It is considered to be a form taxon. It is a 3D body fossil. Its type locality is Cerro La Cruz, which is in a Burdigalian lagoonal mudstone in the Castillo Formation of Venezuela. It is the type species of Baraguatherium.

Synonymy list
YearName and author
2016Baraguatherium takumara Rincón et al.

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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
Americatheria
Xenarthra()
infraorderPilosaFlower 1883
Folivora
classEufolivoraDelsuc et al. 2001
familyMylodontidaeAmeghino 1889
subfamilyOrophodontinaeHoffstetter 1954
genusBaraguatherium
speciestakumara

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.

Baraguatherium takumara Rincón et al. 2016
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Diagnosis
ReferenceDiagnosis
A. D. Rincón et al. 2016Baraguatherium differs from other sloths in thefollowing character combination: toothrows parallel in occlu-sal view; long axis of molariforms parallel to the long axis ofthe toothrow; mandibular symphysis extends to the middle ofthe second lower tooth (mf1); diastema absent; tooth with avery thin layer of cementum; mf1-mf3 series of similar sizeand bilobate, with mf3 conspicuously piriform (anterior lobemuch wider than the posterior lobe); occlusal surface of toothbeveled. Femur diaphysis straight; third trochanter positioned atthe middle of the diaphysis and projects posteriorly;ectepicondyle and entepicondyle robust and project prominently.Baraguatherium differs from members of Megatheroideaand several Miocene mylodontoids (except Brievabradys,Orophodon,Octodontotherium,andOctodontobradys)inhaving a piriform last lower molariform (mf3). Differs fromParoctodontotherium,Octodontotherium,andOrophodon inhaving molariforms with a thin layer of cementum. Differsfrom Bolivartherium,Orophodon,andPseudoprepotheriumconfusum by the presence of three bilobate lower molariforms.Differs from Brievabradys by its larger size, the presence ofthree bilobate lower molariforms, and the parallel lowertoothrow. Differs from Octodontotherium by the absence ofa marked asymmetric step between the anterior and posteriorlobes in the last lower molariform. Differs fromOctodontobradys by molariforms more quadrangular (in oc-clusal view) and mf3 piriform. Differs from Pseudoglyptodonspp. by the presence of bilobed (not trilobed) lowermolariforms
Measurements
No measurements are available
Composition: phosphaticsubp
Environment: terrestrialsubc
Locomotion: actively mobilec
Life habit: ground dwellingf
Diet: herbivoref
Reproduction: viviparoussubc
Created: 2005-08-22 16:27:29
Modified: 2005-08-22 18:30:22
Source: f = family, subc = subclass, c = class, subp = subphylum
References: Lillegraven 1979, Carroll 1988, Ji et al. 2002, Nowak 1999, Hendy et al. 2009

Age range: Burdigalian or 20.45000 to 15.98000 Ma

Collections: one only


Time interval Ma Country or state Original ID and collection number
Burdigalian20.45 - 15.98Venezuela (Lara) Baraguatherium takumara (type locality: 175185)