| Cockerellites Temporal range: Early Eocene, ~ | |
|---|---|
| | |
| Specimen of C. liops from the 18 inch layer of the Green River Formation, Wyoming | |
| Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Actinopterygii |
| Order: | Acanthuriformes |
| Family: | Moronidae |
| Genus: | † Cockerellites Jordan & Hanibal, 1923 |
| Species: | †C. liops |
| Binomial name | |
| †Cockerellites liops (Cope, 1877) | |
| Synonyms | |
| |
Cockerellites is a genus of extinct temperate bass [1] described from early Eocene-aged fossils found in the Green River Formation of Wyoming. [2] [3] It is characterized by a sunfish-like body and its stout dorsal and anal spines. The type species, C. liops, was originally named as a species of Priscacara by Edward Drinker Cope upon creating the genus in 1877, [4] but P. liops was moved to the newly created genus Cockerellites by D. Jordan and H. Hanibal in 1923. [5] Some authors, such as Whitlock (2010), still consider Cockerellites liops as a species of Priscacara. [1]
C. liops is based on the holotype USNM 4044, [6] and it was placed in Priscacara as P. liops but is now considered a separate genus. [7] C. liops was originally seen as the most common species of Priscacara within the Green River lacustrine deposits, and at specific locations, it outnumbers P. serrata by over 3:1. The two species differ in the number of dorsal and anal fin rays, as well as possibly a coarser serrated rear edge of the preopercle in P. serrata. C. liops also has small conical teeth on the pharyngeal jaw, whereas P. serrata has large grinding tooth plates, suggesting a diet of snails and crustaceans. [8]
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