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Дата последнего поиска статьи во внешних источниках: 18 июля 2013 г.
Аннотация:The facies structure and depositional environments of upper Meotian (Maeotin in European literature) sediments in the Taman Trough are considered. Eight facies of a shallow basin are defined and described in detail in the examined sections. It is established that depositional environments in the basin in the initial late Meotian were determined to a significant extent by the dominant influx of fresh (river) waters from the northeast. Diatomaceous sediments, which became later widespread, reflect cyclic ingressions of saline waters. Their enhanced inflow in the terminal late Meotian is evident from the taxonomic composition of diatom and molluscan assemblages.