During the 1960s to 1980s a human mandible, together with fossils of other animals and a lithic industry, were recovered from Units I to VI of Azokh Cave. After the year 2002, new excavations in Units I to V were undertaken. The new large mammal fossils are described and the fauna is revised, using part of the older collections. The only clear break in the sequence is the appearance of domestic mammals in Unit I. The following taxa recovered from Pleistocenic sediments were identified: Ursus spelaeus (the most abundant), Ursus sp. (U. aff. arctos/thibetanus), Vulpes vulpes, Canis aureus, Canis lupus, Meles meles, Martes cf. foina, Crocuta crocuta, Felis chaus, Panthera pardus, Equus hydruntinus, Equus ferus, Stephanorhinus hemitoechus, Stephanorhinus kirchbergensis, Sus scrofa, Capreolus pygargus, Dama aff. peleponesiaca, Dama sp., Megaloceros solilhacus, Cervus elaphus, Bison schoetensacki, Ovis ammon, Capra aegagrus and Saiga. Most species present are common in western Eurasia. All fossiliferous Units have taxa that in mid-latitude Europe are considered to be “interglacial” elements, while there are no clear “glacial” elements, which suggests temperate conditions despite the altitude of the cave. The evolutionary levels of various species suggest ages of about 300 ka for Units VI–IV, while Units III–II are slightly younger. Domestic mammals indicate a Holocene age for Unit I. Most sediments represent a normal transition between units. Processes of erosion, however, affected the top of the Pleistocene sediments recorded in the cave. Therefore, Unit I (Holocene sediments containing domestic animals) lies disconformably over Unit II (Late Pleistocene).