Colobomycter

The type species, Colobomycter pholeter, was first described from fossil remains in 1958, at which time it was believed to represent a synapsid, specifically, a pelycosaur. However, the discovery of new material and reexamination of the holotype led to its reclassification as a member of the Eureptilia. More recent studies indicate that Colobomycter is properly placed within the amniote clade Parareptilia, as part of the group Lanthanosuchoidea and closely related to the taxon Acleistorhinus. A second species of Colobomycter was described in 2016, Colobomycter vaughni. No postcranial material is known for Colobomycter, and the skull material referred to the genus has all been recovered from a single locality, the Richards Spur site at the Dolese Brothers Limestone Quarry, 11 kilometers north of Fort Sill, Comanche County, Oklahoma, dating to the early Artinskian stage. This site comprises a fissure-fill deposit yielding a unique upland fauna. Other taxa recovered from these strata preserves a wide array of tetrapods, including lepospondyl and temnospondyl amphibians, Seymouria, microsaurs, captorhinomorphs, and synapsids. == Description ==

The skull of Colobomycter is considered one of the most enigmatic found in any of the parareptiles primarily due to the presence of greatly enlarged caniniform teeth possessing serrated edges in the premaxilla and, to a lesser extent, the maxilla. Modesto & Reisz (2008) speculate that hard-shelled insects and other arthropods may have formed the bulk of its diet, but that Colobomycter could also have fed on vertebrates, including small amphibians and eureptiles. It is notable as the smallest predatory amniote from the Richard's Spur deposits, with a skull measuring a mere 70-80 millimeters in length. == References ==