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Gilmoreteius chulsanensis

Osteichthyes - Polyglyphanodontidae

Taxonomy
Macrocephalosaurus chulsanensis was named by Sulimski (1975). Its type specimen is ZPal MgR-I/14, a partial skeleton (Complete skull with the postcranial skeleton. Distal end of tail, left humerus, a part of anterior autopodium and dorsal elements of the scapulae missing), and it is a 3D body fossil. Its type locality is Khulsan (general) [PMPE], which is in a Campanian/Campanian eolian sandstone/sandstone in the Baruungoyot Formation of Mongolia.

It was recombined as Gilmoreteius chulsanensis by Langer (1998); it was recombined as Macrocephaleon chulsanensis by Alifanov (2000).

Synonymy list
YearName and author
1975Macrocephalosaurus chulsanensis Sulimski p. 41 figs. 2. 5-11, 14
1991Macrocephalosaurus chulsanensis Gao and Fox
1998Gilmoreteius chulsanensis Langer
2000Macrocephaleon chulsanensis Alifanov
2000Macrocephalosaurus chulsanensis Alifanov p. 373
2000Macrocephalosaurus chulsanensis Gao and Norell p. 70

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RankNameAuthor
kingdomAnimalia()
Bilateria
EubilateriaAx 1987
Deuterostomia
phylumChordataHaeckel 1874
subphylumVertebrata
superclassGnathostomata
classOsteichthyes
subclassSarcopterygii()
subclassDipnotetrapodomorpha(Nelson 2006)
subclassTetrapodomorpha()
Tetrapoda
Reptiliomorpha
RankNameAuthor
Anthracosauria
subclassAmphibiosauriaKuhn 1967
Cotylosauria()
Amniota
Sauropsida
classReptilia
Squamata()
Scincomorpha()
PolyglyphanodontiaAlifanov 2000
familyPolyglyphanodontidaeGilmore 1942
genusGilmoreteius
specieschulsanensis()

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.

Gilmoreteius chulsanensis Sulimski 1975
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Diagnosis
ReferenceDiagnosis
A. Sulimski 1975Length of skulls about 40 mm in the case of young specimens and 70-80 mm for adult ones. Skull slender, with widened naso-prefrontal region. The ratio of occipital to maxillary segments is 1:3 and width to length of frontals - 0.5. Parietal foramen always on the fronto-parietal suture. Surface of naso-prefrontal region forms a plane, slightly inclined anteriorly in relation to the fronto-parietal surface. Sculpture of covering bones often well developed in [he form of regularly arranged cusps and rosettes. Parietal process of the post-frontal poorly developed, frontal long and slender. Jugal process wide, short and sharply pointed, slightly bent outwards. Suborbital fenestrae reduced to small perforated hollows. Anterior teeth of the maxilla, four-five in number, enlarged, canine-like, but not so well developed as in M. gilmorei. Anterior teeth of the lower jaw , five-six in number , are unicuspid and are equal in height to cheek teeth. Lower jaw slender and not so deep in the angular region, as in M . gilmorei. Teeth in both jaws numerous, about 27 or 28; 8 premaxillary teeth are present. Scapulo-coracoid of iguanid type with three fenestrae.
Measurements
No measurements are available
Composition: phosphaticsubp
Environment: terrestrialuc
Locomotion: actively mobilec
Diet: herbivoreg
Created: 2007-01-25 08:36:01
Modified: 2007-01-25 10:36:01
Source: g = genus, c = class, subp = subphylum, uc = unranked clade
References: Kiessling 2004, Hendy et al. 2009, Carroll 1988, Gao and Norell 2000

Age range: base of the Middle Campanian to the top of the Late/Upper Campanian or 83.60000 to 72.20000 Ma

Collections (3 total)


Time interval Ma Country or state Original ID and collection number
Middle Campanian - Late/Upper Campanian83.6 - 72.2Mongolia (Omnogov) Macrocephalosaurus chulsanensis (type locality: 13776 62913 189007)