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Antilocapra pacifica

Mammalia - Antilocapridae

Taxonomy
Antilocapra pacifica was named by Richards and McCrossin (1991). Its type specimen is UCMP 131828, a partial skull, and it is a 3D body fossil. Its type locality is Big Break (UCMP V-87047), which is in a Pleistocene/Holocene terrestrial sandstone/sandstone in the Piper Series Sands Formation of California.

Synonymy list
YearName and author
1991Antilocapra pacifica Richards and McCrossin p. 628 figs. Figs. 3 - 6

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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)
Pecora()
familyAntilocapridae
genusAntilocapraOrd 1818
speciespacifica

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.

Antilocapra pacifica Richards and McCrossin 1991
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Diagnosis
ReferenceDiagnosis
G. D. Richards and M. L. McCrossin 1991Species exhibits single, tall-based, mediolaterally compressed, but highly inflated horn cores. Cranial size falls in the median range for A. americana whereas horn-core dimensions are greater than the modern range (Table 2). The horns are supraorbital, but differ from those of A. americana by arising from the whole supraorbital margin. The anterior origin of the horn core is placed superior to the frontolacrimal suture with the anterior border rising anterosuperiorly from this point. The bony prominence located at the posterior origin of the horn core in A. americana is incorporated into the posterior border of A. pacifica nov. sp. The core cross-section is more inflated throughout than in A. americana (Fig. 5). Compared to modern pronghorns, the outer wall of the postorbital process is rotated inferiorly. The portion of the temporal fossa located between the inferior border of the postorbital processand a line throughthe infratemporal crest is reduced (Figs. 4A, 4B). The posteornual fossa is oriented more posteriorly relative to the condition in A. americana.
Measurements
No measurements are available
Composition: phosphaticsubp
Environment: terrestrialo
Locomotion: actively mobilec
Life habit: ground dwellingf
Diet: browserf
Diet 2: grazerf
Reproduction: viviparoussubc
Created: 2005-06-08 10:11:09
Modified: 2005-08-31 16:51:41
Source: f = family, o = order, subc = subclass, c = class, subp = subphylum
References: Carroll 1988, Hendy et al. 2009, Nowak 1991, Lillegraven 1979, Nowak 1999

Age range: base of the Late/Upper Pleistocene to the top of the Holocene or 0.12900 to 0.00000 Ma

Collections: one only


Time interval Ma Country or state Original ID and collection number
Late/Upper Pleistocene - Holocene0.129 - 0.0USA (California) Antilocapra pacifica (type locality: 209581)