БІОСТРАТИГРАФІЯ ПАЛЕОЦЕНУ–ЕОЦЕНУ ПЛАТФОРМНОЇ УКРАЇНИ ЗА КРУПНИМИ ФОРАМІНІФЕРАМИ
DOI:
https://doi.org/10.30836/igs.2522-9753.2016.144248Ключові слова:
біостратиграфія, кореляція, палеоцен, еоцен, крупні форамініфери, УкраїнаАнотація
Наведено опис біостратиграфічної схеми палеогену Південної України за крупними форамініферами, яка являє собою подальший розвиток зональної стратиграфії еоценових відкладів за нумулітами Північної нумулітової провінції Г.І. Немкова (1967 р.). Качинський регіоярус верхнього палеоцену характеризують верстви Discocyclina seunesi. Бахчисарайський регіоярус нижнього еоцену – зони Operculina semiinvoluta, Nummulites crimensis і Assilina placentula в Криму та верстви з Ass. placentula у Північному Причорномор’ї. Сімферопольський регіоярус – зони N. distans, N. polygyratus, дрібних нумулітів і Ass. tenuimarginata у передгірському Криму і верстви з N. distans, Ass. exponens, N. atacicus у Північному Причорномор’ї. Верстви з N. variolarius характеризують новопавлівський регіоярус Північного Причорномор’я і південного схилу Українського щита. Їх аналогом є комплекс з N. variolarius, N. orbigny київського регіоярусу Північної України. Верстви з N. litoralis, N. concinnus, N. prestwichianus в альминському регіоярусі Північного Причорномор’я і обухівському регіоярусі Українського щита і Дніпровсько-Донецької западини. Нумулітові зони і верстви Криму і Північного Причорномор’я скорельовані із зональною шкалою за крупними форамініферами для мілководних зон палеоокеану Тетіс (Serra-Kiel et al., 1998). Границя іпрського і лютетського ярусів на півдні України проведена всередині сімферопольського регіоярусу по підошві зони N. polygyratus в Південно-Західному Криму. У Північному Причорномор’ї вона проходить в середині верств з N. distans, Ass. exponens, N. atacicus.Посилання
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