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Radiocarbon Dating in the Vernadsky Institute IV∗

Published online by Cambridge University Press:  18 July 2016

A. P. Vinogradov ,
A. L. Devirts ,
E. I. Dobkina  and
N. G. Markova
A. P. Vinogradov
Affiliation:
V. I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Academy of Sciences, USSR, Moscow
A. L. Devirts
Affiliation:
V. I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Academy of Sciences, USSR, Moscow
E. I. Dobkina
Affiliation:
V. I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Academy of Sciences, USSR, Moscow
N. G. Markova
Affiliation:
V. I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Academy of Sciences, USSR, Moscow
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Peat, at depth 3.5 m, from upper of 2 layers, at village of Timoshkovichi [53° 35′ N Lat, 26° 05° E Long], Korelichi Raion, Grodno Oblast, Belorussian SSR. Timoshkovichi is located on Novogrudok upland, beyond limits of region of Valday [Wurm] Glaciation. Cross section synchronous with ancient ravine of Neman R. basin where 2 horizons of peat can be detected: the lower, according to pollen data, accumulated at time of Mikulino [Eem] Interglacial; the upper believed accumulated at time of 2nd climatic optimum of Mikulino Interglacial, or at time of early Interstadial of Valday [Wurm] Glaciation (Tsapenko and Makhnach, 1959). Coll. 1962 by N. S. Chebotareva, Geog. Inst., Acad. of Sci., USSR.

Type
Research Article
Information
Radiocarbon , Volume 10 , Issue 2 , 1968 , pp. 451 - 453
Copyright
Copyright © The American Journal of Science 

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