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Middle-Upper Miocene stratigraphy of the Taman Peninsula, Eastern Paratethys
Authors:Eleonora P Radionova  Larisa A Golovina  Natalia Yu Filippova  Valery M Trubikhin  Sergey V Popov  Irina A Goncharova  Yulia V Vernigorova  Tatiana N Pinchuk
Institution:1. Geological Institute RAS, Pyzhevskii 7, Moscow, Russia
2. Paleontological Institute RAS, Profsoyuznaya 123, Moscow, Russia
3. Institute of Geological Sciences NAS, O. Gonchara 55, Kiev, Ukraine
4. Kuban University, Krasnodar, Russia
Abstract:The stratigraphy of the Taman Peninsula is defined using the sections at Zelensky Hill ?? Panagia, Popov Kamen, Taman and Zheleznyi Rog. The stratigraphy is constructed from distribution of mollusks, foraminifers, nannofossils, diatoms, and organic-walled phytoplankton, as well as incorporating paleomagnetic data. The occurrence of oceanic diatom species in the Middle-Upper Sarmatian, Maeotian and Lower Pontian makes a direct correlation possible between the sections studied, the Mediterranean basin and oceanic zonation. The new data on planktonic and benthic biotic groups suggests a pulsating connection of the Eastern Paratethys with the open marine basins, especially during transitional intervals within constant environments. Comprehensive studies of the Chokrakian-Kimmerian microbiota provide evidence for several levels of marine microbiotic associations that are related to short-term marine invasions. The biotic and paleomagnetic data of the Taman Peninsula sections give a more comprehensive, but sometimes a controversial picture on the Eastern Paratethys history and the nature of its relationship with the adjacent marine basins.
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