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Plionictis gazini
Taxonomy
Martes (Tomictis) gazini was named by Hall (1931). Its type specimen is CIT 391, a mandible (left lower jaw bearing Ml, Ps, the alveolus of M2, and the alveoli of P4), and it is a 3D body fossil. Its type locality is Skull Spring, which is in a Barstovian terrestrial volcaniclastic in the Butte Creek Formation of Oregon.
It was recombined as Plionictis gazini by Baskin (1998).
It was recombined as Plionictis gazini by Baskin (1998).
Synonymy list
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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.
†Plionictis gazini Hall 1931
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Diagnosis
Reference | Diagnosis | |
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E. R. Hall 1931 | Size about as in Mustela nigripes Audubon and Bachman; M1: metaconid slightly better developed than in Martes a. americana and with posterior margin directly medial to posterior margin of protoconid; talonid trenchant without suggestion of basining even at medial margin; talonid one- third as long as trigonid; Ps without accessory cusp; mental foramen below middle of Ps; anterior margin of masseteric fossa below posterior margin of M2 |
Measurements
No measurements are available
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Source: f = family, subc = subclass, c = class, subp = subphylum | |||||
References: Carroll 1988, Ji et al. 2002, Nowak 1991, Hendy et al. 2009, Lillegraven 1979 |
Age range: Barstovian or 16.30000 to 12.50000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
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Barstovian | USA (Oregon) | Martes gazini (type locality: 19056) |