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The following mammal assemblage was identified among the materials collected in 2020 from the Pleistocene of the Lang Trang cave (northern Vietnam): the primates Pongo sp., Trachypithecus sp., Macaca cf. nemestrina (Linnaeus, 1766), and Macaca sp.; the carnivorans Arctonyx collaris rostratus Matthew et Granger, 1923 and Panthera sp.; the chiropteran Ia io Thomas, 1902; the rodent Hystrix kiangsenensis Wang, 1931; the proboscidean Elephas sp.; the perissodactyls Tapirus indicus (Desmarest, 1819) and Dicerorhinus sumatrensis (Fischer, 1814); the artiodactyls Sus scrofa Linnaeus, 1758, S. barbatus Müller, 1838, Tragulus kanchil (Raffles, 1821), Hydropotes inermis Swinhoe, 1870, Muntiacus muntjak (Zimmermann, 1780), Axis porcinus (Zimmermann, 1780), Rusa unicolor (Kerr, 1792), and Capricornis sumatraensis (Bechstein, 1799). I. io, S. barbatus, T. kanchil, H. inermis, and A. porcinus were detected in the Lang Trang fauna for the first time. The mammal assemblage is dominated by inhabitants of tropical forests (from lowlands to mountains), subtropical forms are also present.

The skull of a buffalo from the Upper Pleistocene deposits in the Lukerino village near the city of Kolomna (Moscow Region) was found to belong to Bubalus murrensis (Berckhemer, 1927). In Western Europe, this species occurred in the Middle and Late Pleistocene during interglacials. In the Pleistocene of the East European Plain, the fossil Bubalus is discovered for the first time. According to the radiocarbon ( 14 C) analysis of the collagen, the fossil dates to the Allerød interstadial (the age is ca. 12 800 years).

The giant deer Arvernocerosverestchagini David, 1992, authochtonous species of the Early Pleistocene biota of North Black Sea coastal area, is discovered in Crimea. The giant deer was a member of fossil fauna of vertebrates from the Pleistocene deposits of Taurida karst cave. According to biochronological data, this fauna is dated to 1.8-1.5 Ma.

We describe a vertebrate assemblage from the Pleistocene deposits of the Taurida karst cave discovered in 2018 in central Crimea (Zuya village, Belogorsk raion). The assemblage is correlated with Late Villafranchian faunas of the Eastern Mediterranean and has an approximate age of 1.8-1.5 Ma.