“…The faunal remains from these sediments consist either of Permian species (with the exception of a phyllopod fauna from the upper horizons of thVtuffogenic sequence) or of local forms, which make an objective dating of the rocks impossible (Sadovnikov, 1964). In addition, new palynological (Odintsova, 1969), geological (Kuznetsov and Naumov, 1971), and the first radiometric data ( Chukhrov et al, 1973;Dmitriyev, 1975) have been provided, which indicate a broader age range for the volcanogenic formations of this region. The absolute-age data for the volcanics of the central part of the Siberian Platform may turn out to be useful in controlling the stratigraphy of the volcanics themselves.…”