ПАЧКА ВІЛЛАМАНІН СВІТИ САН ЕМІЛІАНО (КАРБОН, ПІВНІЧНА ІСПАНІЯ): ЇЇ ВІК ТА ФУЗУЛІНОЇДНІ ФОРАМІНІФЕРИ

Автор(и)

  • A.C. van Ginkel

DOI:

https://doi.org/10.30836/igs.1025-6814.2014.2.139144

Ключові слова:

форамініферы, фузуліноідеї, світа Сан Еміліано, карбон, зона Profusulinella, Кантабрійські гори, Іспанія

Анотація

Світа Сан Еміліано (карбон, пенсільваній, північна Іспанія) представлена чергуванням морських і континентальних товщ, що містять рештки морських та континентальних викопних організмів. Фузуліноїдні форамініфери з покрівлі цієї світи (пачка Вілламанін) визначають вік верхньої частини зони Profusulinella. Форамініфери вищезалягаючої зони Fusulinella, зокрема види роду Fusulinella, відсутні. Тут часто трапляються види родів Profusulinella, Eoschubertella та Pseudostaffella. Представники роду Aljutovella в деяких місцях численні. Незважаючи на те, що подекуди трапляютьсяформи Profusulinella з муральними порами в стінці, що може свідчити про каширський вік порід, фузуліноїдний комплекс в цілому датується як пізньоверейський. Загалом дана фауна фузуліноїдей разом з іншими викопними рештками, такими як брахіоподи та рештки рослин, дозволяють корелювати верхню частину верейського горизонту Східної Європи із вестфалом Б Західної Європи.

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2014-07-16

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