А new species Ovis gracilis sp. nov. is described based on the study of fossil remains of Bovidae from the Lower Pleistocene of the Taurida Cave, the Crimea. This not very large sheep had the horn cores with homonymous torsion and short sinuses, and slender metapodia. The remains of Ovis from Taurida are among the oldest in Europe and the first evidence of the presence of Ovis in the Еarly Pleistocene of the Crimea. The species O. gracilis was a part of the fauna of the Taurida Cave, dated within 1.8–1.5 Ma. The appearance of this species in the south of Eastern Europe could be associated with one of the early waves of dispersal from Asia, along the Alpine-Himalayan belt just prior to the Olduvai paleomagnetic episode.