Characteristic dermal scutes of an armadillo (Dasypus cf. D. bellus) collected from alluvial deposits of late Blancan age (about 2.5 million years old) in Antelope County, Nebraska, represent the northernmost known occurrence of the Dasypodidae. Except for two other Blancan records, in Florida, the Nebraska specimens are also the oldest North American evidence of the family. The Big Springs Local Fauna, in which Dasypus comprises a rare element, also contains other vertebrate taxa (Geochelone, Bassariscus, Tapirus) whose modern ranges lie far to the south of Nebraska. A warm paleoclimate is thus suggested; however, enthusiasm for armadillos as paleoecological indicators should be tempered by the recent discovery of D. bellus in the late Pleistocene species may have been more cold-tolerant than its probable Recent descendant, D. novemcinctus.