The results of petromagnetic and paleomagnetic studies of two sections of the Lower Syzran subformation (Paleocene) – Gremyachka and Klyuchi-2, located in the north of the Saratov Right Bank and represented by weakly magnetic silicites, are presented. Paleomagnetic data on sections, despite their low quality and fragmentation, are important for magnetostratigraphy, because they confirm the presence of a reverse polarity magnetozone (analogous to chron C27r and/or C26r) in the Lower Syzran subformation and its lateral stability.
