Abstract
The results of a comprehensive study of the reference section of the Upper Maastrichtian of Mount Klementyev (South-Eastern Crimea), composed of a terrigeneous-carbonate strata. It was found that sedimentation occurred in relatively deep-water conditions. Biostratigraphic analysis of benthic and planktonic foraminifera assemblages made it possible to identify foraminiferal zones in the section and confirm the deep-water type of sedimentation in the basin at this interval.
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