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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Parablastomeryx gregorii
Taxonomy
Parablastomeryx gregorii was named by Frick (1937) [genotype]. Its type locality is Xmas Quarry, which is in a Clarendonian terrestrial horizon in the Ash Hollow Formation of Nebraska.
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.
†Parablastomeryx gregorii Frick 1937
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Diagnosis
| Reference | Diagnosis | |
|---|---|---|
| D. R. Prothero 2008 | Larger Parablastomeryx with no stylid on the paraconid of p4, relatively unreduced premolars relative to molar row length. |
Measurements
No measurements are available
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| Source: f = family, o = order, subc = subclass, c = class, subp = subphylum | |||||
| References: Nowak 1999, Lillegraven 1979, Nowak 1991, Hendy et al. 2009, Carroll 1988 | |||||
Age range: base of the Late/Upper Hemingfordian to the top of the Clarendonian or 18.50000 to 9.40000 Ma
Collections (5 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Late/Upper Hemingfordian | USA (Florida) | Blastomeryx sp. (18512) | |
| Barstovian | USA (Nebraska) | Parablastomeryx sp. (18412) | |
| Clarendonian | USA (Nebraska) | Parablastomeryx gregorii (18245 type locality: 18496) | |
| Clarendonian | USA (South Dakota) | Parablastomeryx sp. (18481) |