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Hoplictis grangerensis
Taxonomy
Beckia grangerensis was named by Bryant (1968) [genotype]. Its type specimen is LACM 10642, a mandible, and it is a 3D body fossil. Its type locality is Granger Clay Pit, which is in a Miocene terrestrial horizon in the Ellensburg Formation of Washington. It is the type species of Beckia.
It was recombined as Ischyrictis grangerensis by Tedford et al. (1987); it was recombined as Hoplictis grangerensis by Baskin (1998).
It was recombined as Ischyrictis grangerensis by Tedford et al. (1987); it was recombined as Hoplictis grangerensis by Baskin (1998).
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1968 | Beckia grangerensis Bryant |
| 1976 | Beckia grangerensis Edwards p. 2 |
| 1987 | Ischyrictis grangerensis Tedford et al. |
| 1998 | Hoplictis grangerensis Baskin |
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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.
†Hoplictis grangerensis Bryant 1968
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: f = family, subc = subclass, c = class, subp = subphylum | |||||
| References: Carroll 1988, Lillegraven 1979, Nowak 1991, Hendy et al. 2009, Ji et al. 2002 | |||||
Age range: Clarendonian or 12.50000 to 9.40000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Miocene | USA (Washington) | Beckia grangerensis (type locality: 18903) | |
| Clarendonian | USA (California) | Beckia grangerensis (19391) |