The species Xyronomys swainae (J. K. Rigby, 1980) was found in Torrejonian (Paleocene)-age strata of Swain Quarry in Wyoming, United States. Represented by a couple of teeth, this genus was originally assigned to Eucosmodontidae. Kielan-Jaworowska and Hurum (2001, p. 406) refer it to Neoplagiaulacidae on the basis of its possession of microprismatic enamel, i.e. the tooth enamel is built up from small prisms.
A second species Xyronomys robinsoni was found in Puercan (Lower Paleocene)-age strata of Colorado, US and was named by Middleton and Dewar in 2004.
Material assigned to this genus has also been reported from Rav W-1 in Saskatchewan, Canada.
References
Kielan-Jaworowska, Z. and Hurum, J.H. (2001), "Phylogeny and Systematics of multituberculate mammals", Paleontology44:389-429.
Rigby, J.K. (1980), "Swain Quarry of the Fort Union Formation, Middle Paleocene (Torrejonian), Carbon County, Wyoming: geologic setting and mammalian fauna", Evolutionary Monographs3, vi +179pp.