Aclistomycter is an extinct genus of oreodont from the late Eocene of Texas and Mexico. It is the oldest known member of Merycoidodontidae (the family containing most oreodonts), and its distinctive qualities allow it to occupy its own monotypicsubfamily, Aclistomycterinae. Aclistomycter was a small herbivorousartiodactyl with a short face and small, tusk-like canine teeth. Though small by the standards of Oligocene-Miocene oreodonts, it was somewhat larger than other late Eocene oreodonts.
The type speciesAclistomycter middletoni was first reported from the Porvenir local fauna in the Chambers Tuff Formation, near Adobe Springs in Presidio County, Texas. This site is late Duchesnean in age (about 38 Ma). It has also been reported from the Rancho Gaitan site in Chihuahua, Mexico. A second potential species, Aclistomycter? dunagani, occurs in the nearby Little Egypt local fauna, which is slightly younger (earliest Chadronian, about 37 Ma).
Posterior base of zygomatic processes wide, making the skull broad posteriorly.
Bullae thought to be inflated (though the bullae are not exposed in the figures of the type specimen illustrated by Wilson).
References
12Lander, B. (1998). "Oreodontoidea". In Janis, C.M.; Scott, K.M.; Jacobs, L.L. (eds.). Evolution of Tertiary mammals of North America. Cambridge: Cambridge University Press. pp.402–425. ISBN0-521-35519-2.