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New sedimentological, bio-, and magnetostratigraphic data on the Jurassic-Cretaceous boundary interval of Eastern Crimea (Feodosiya)
Authors:A Yu Guzhikov  V V Arkad’ev  E Yu Baraboshkin  M I Bagaeva  V K Piskunov  S V Rud’ko  V A Perminov  A G Manikin
Institution:1. Chernyshevsky Saratov State University, ul. Astrakhanskaya 83, Saratov, 410012, Russia
2. St. Petersburg State University, Universitetskaya nab. 7/9, St. Petersburg, 199034, Russia
3. Lomonosov Moscow State University, Leninskie Gory, Moscow, 119992, Russia
4. Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017, Russia
5. Center of Ecological-Naturalistic Creativity of Students “Intellekt”, Feodosiya, Ukraine
Abstract:The first compiled composite section comprises continuous succession of upper Tithonian-lower Berriasian strata (Jacobi Zone) from different isolated outcrops of the Feodosiya area. Based on new magnetostratigraphic and sedimentological data, the paleomagnetic section is correlated with succession of M20r, M19n, M19r, M18b chrons and M18n.1r Subchron (“Brodno”). The thorough complex bio- and magnetostratigraphic correlation of the upper Tithonian-lower Berriasian interval (Jacobi Zone) carried out through the Western Tethys and Eastern Paratethys provided grounds for first defining age analogs of the Durangites Zone in the Crimean Mountains and specifying location of the boundary between the Jurassic and Cretaceous systems, as well as for determining late Tithonian age of strata in the Dvuyakornaya Bay section barren of fossils.
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