Abstract
An astrochronological (cyclostratigraphic) binding of the lithological and geochemical characteristics of the Jurassic deposits of the Mountainous Crimea and the Caucasus to the cycles of eccentricity of the Earth’s orbit is carried out, an analysis of the relationship between the established variations of climate and paleotemperature with the moments of coincidence of different-order cycles of eccentricity and their paleoclimatic characteristics is given. New data on paleotemperatures of the Southern Demerdzhi mountain section are presented.
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