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Archaeotragulus krabiensis

Mammalia - Tragulidae

Taxonomy
Archaeotragulus krabiensis was named by Metais et al. (2001). Its type specimen is TF 2997, a mandible (sin. with p2-m2), and it is not a trace fossil. Its type locality is Wai Lek pit, which is in an Eocene terrestrial lignite in the Krabi Basin B2 Formation of Thailand. It is the type species of Archaeotragulus.

Synonymy list
YearName and author
2001Archaeotragulus krabiensis Metais et al. p. 232

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RankNameAuthor
kingdomAnimalia()
Bilateria
EubilateriaAx 1987
Deuterostomia
phylumChordataHaeckel 1874
subphylumVertebrata
superclassGnathostomata
Osteichthyes()
subclassSarcopterygii()
subclassDipnotetrapodomorpha(Nelson 2006)
subclassTetrapodomorpha()
Tetrapoda
Reptiliomorpha
Anthracosauria
subclassAmphibiosauriaKuhn 1967
Cotylosauria()
Amniota
subclassSynapsida
Therapsida()
infraorderCynodontia()
Mammaliamorpha
RankNameAuthor
Mammaliaformes
classMammalia
Cladotheria
Zatheria
subclassTribosphenida()
subclassTheria
Eutheria()
Placentalia
Boreoeutheria
Laurasiatheria
Scrotifera
Euungulata
Artiodactylamorpha
Artiodactyla()
Ruminantiamorpha
Ruminantia(Scopoli 1777)
infraorderTragulina
superfamilyTraguloidea
familyTragulidaeMilnes-Edwards 1864
genusArchaeotragulus
specieskrabiensis

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.

Archaeotragulus krabiensis Metais et al. 2001
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Diagnosis
ReferenceDiagnosis
G. Metais et al. 2001Small primitive ruminant with lower molars resembling those of Dorcatherium by the presence of a typical tragulid M structure at the rear of the trigonid and the derived pattern of its lower premolars, including the lack of a metaconid and the presence of a longitudinal groove on the posterior half of p4. Differs from Dorcatherium by its smaller size, its cusps more labio-lingually compressed, the lack of an ectostylid, the presence of a well-marked ‘entoconidian groove’ opening forwards, the presence of a rudimentary hypoconulid on m2–3 and by the transversely compressed hypoconulid on m3. Differs from Iberomeryx by its larger size, its cristid obliqua more lingually orientated, a well-marked M structure on the posterior side of the trigonid, the absence of an ectostylid and by its transversely compressed and pinched hypoconulid on m3. Archaeotragulus further differs from Zhailimeryx by its M structure, the lack of rudimentary paraconid on the lower molar and by its p4 lacking both distinct metaconid and entoconid.
Measurements
No measurements are available
Composition: phosphaticsubp
Environment: terrestrialo
Locomotion: actively mobilec
Life habit: ground dwellingf
Diet: frugivoref
Diet 2: grazerf
Reproduction: viviparoussubc
Created: 2005-06-08 10:11:09
Modified: 2005-08-23 13:14:24
Source: f = family, o = order, subc = subclass, c = class, subp = subphylum
References: Nowak 1991, Lillegraven 1979, Carroll 1988, Nowak 1999, Hendy et al. 2009

Age range: Late/Upper Eocene or 37.20000 to 33.90000 Ma

Collections (2 total)


Time interval Ma Country or state Original ID and collection number
Late/Upper Eocene37.2 - 33.9Thailand Archaeotragulus krabiensis (13127 type locality: 49078)