For the five years a set of various data was obtained from the relatively deep-water Upper Miocene sediments exposed in the Zheleznyi Rog section (Taman Peninsula, Russia). The data includes measurements of magnetic susceptibility (MS) and its further time-series analysis. The aim of these studies is to recognize the astronomic cycles correspond to the obliquity and precession variations. The results of this study reflect the strong correlations to the Messinian Salinity Crisis (MSC) of the Mediterranean. The study was supported by the RFBR 17-05-01085 A.