Ma. Erbajva et al., THE FIRST DISCOVERY OF THE LATE CENOZOIC SMALL MAMMALIAN FAUNAS IN THE SOUTH OF EASTERN TRANSBAIKALIA, Geologia i geofizika, 38(9), 1997, pp. 1453-1457
Late Cenozoic deposits, named <<belesaya>>, sands, are widely distribu
ted in Eastern Transbaikalia. They have comprehensively been studied f
or the last decades. Mollusk faunas, pollen and sporen were described
from these sands. There are also several absolute data on these sands.
Up to date, however, no fossil remains of small mammals were found in
this region. Our recent excavations permitted us for the first time t
o collect Late Pliocene and Pleistocene remains of lagomorphs and rode
nts from five localities. Studying these fossils we have found that at
least three faunas are similar to West-Transbaikalian ones: Chikoi, T
ologoi and Upper Paleolithic faunistic complexes. The ancient fauna fo
und in Eastern Transbaikalia is represented by the Late Pliocene Chiko
i faunistic complex with Villanyia and Prosiphneus. The next Early Ple
istocene fauna includes representatives of the Tologoi faunistic compl
ex such as Eolagurus simplicidens, Myospalax wongi and Lasiopodomus br
andti. Upper Pleistocene fauna of Eastern Transbaikalia consists of sp
ecies of Upper Paleolithic faunistic compex. The presence of the above
-mentioned species widely distributed in Northern China, Mongolia and
Western Transbaikalia, permits us to correlate Late Pliocene and Pleis
tocene faunas and deposits of these regions.