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Douvillei at the top (Gargasian). All along the section, planktonic foraminifera are very rare and represented only by H. similis ? at the bottom and some unknown species of Hedbergella towards the top. The studied interval belongs possibly to the Upper Bedoulian-Gargasian (Late Early Aptian - Middle Aptian). At the contact between two formations, a brecciated surface with iron oxide is present displaying a mantling epikarstic condition. This implies that before the drowning surface exposure conditions should have occurred.
To the stratigraphy of the Hauterivian of the North Caucasus. In: Fauna, stratigrafiya i litologiya mezozoiskikh I kainozoiskikh otlozhenii Krasnodarskogo kraya. 16, Leningrad, Nedra Press, 244-285 [in Russian]. A. G. 1977. New data on the stratigraphy of the Boreal Hauterivian. Geologiia i Geofizika, Siberian Branch, No. 7, Novosibirsk, 75-82 [in Russian]. A. & Kemper, E. 1988. Comparative paleontology and stratigraphy of Valanginian Polyptychitinae and Simbirskitinae in Sverdrup Basin (Arctic Canada) and Lower Saxony Basin (Northwest Germany).
In Russian]. J. 2007. Stratigraphy and Boreal-Tethyan correlation of marine Lower Hauterivian of Russia and CIS. M. (Ed), Selected papers of the Third All-Russia Meeting 42 'Cretaceous system of Russia and near Overseas: problems of stratigraphy and paleogeography. Saratov, Publishing house of Saratov State University, 21-35 [in Russian]. J. 2008. Stratigraphy and Boreal-Tethyan correlation of marine Upper Hauterivian of Russia and CIS. A. N. (eds), Cretaceous System of Russia and adjacent countries: problems of stratigraphy and paleogeography.