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Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Priusaulax wilsoni
Taxonomy
Priusaulax wilsoni was named by Korth (2017). Its type specimen is KU 10173, a partial skull (partial cranium with right side of rostrum, max- illa and orbital wall containing right P4–M3), and it is a 3D body fossil. Its type locality is Martin Canyon Quarry A, which is in a Hemingfordian channel horizon in the Pawnee Creek Formation of Colorado.
Synonymy list
Year | Name and author |
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2017 | Priusaulax wilsoni Korth p. 251 figs. Figs. 1-3; Table 1 |
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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.
†Priusaulax wilsoni Korth 2017
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Diagnosis
Reference | Diagnosis | |
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W. W. Korth 2017 | Slightly larger than Priusaulax browni and smaller than P. senrudi; no anterior re-entrant valley or accessory cuspule (anterostylid) on p4 as in P. browni. |
Measurements
No measurements are available
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Source: f = family, subc = subclass, c = class, subp = subphylum | |||||
References: Ji et al. 2002, Lillegraven 1979, Carroll 1988, Nowak 1991, Hendy et al. 2009 |
Age range: Hemingfordian or 18.50000 to 16.30000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
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Hemingfordian | USA (Colorado) | Priusaulax wilsoni (type locality: 17965) |