Abstract
As a result of examining a large amount of information on stratotype sections of Neogene-Quaternary deposits of the south of Western Siberia, we have compiled a sequence through these deposits in which boundaries between geomagnetic subdivisions are linked with Pliocene-Quaternary biozones. The Brunhes zone Includes deposits with mammal remains of the Upper Paleolithic, Khazara, and Tiraspol' assemblages. The Gauss-Matuyama inversion has been identified in the upper Pliocene deposits with a Khapry mammal assemblage. The lower boundary of the Gauss zone apparently passes below strata with a Moldavian faunal complex. The data on the biologic linking of the magnetic zones demonstrate the synchronous development of the faunal assemblages of Pliocene-Quaternary time in Western Siberia and in the southwest of European USSR. —Authors.
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