THE PLIOCENE-PLEISTOCENE BOUNDARY IN PELAGIC OOZES OFF RÉUNION ISLAND, WESTERN INDIAN OCEAN

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dc.contributor.author Duczmal-Czernikiewicz A.
dc.contributor.author Jugowiec-Nazarkiewicz M.
dc.contributor.author Szydło A.
dc.date.accessioned 2024-09-14T06:08:23Z
dc.date.available 2024-09-14T06:08:23Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=29634435
dc.identifier.citation Acta Geologica Polonica, 2006, 56, 4, 407-419
dc.identifier.issn 0001-5709
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/45164
dc.description.abstract Nannoplankton and foraminifera from the pelagic oozes from a water depth of 3 684 meters, 150 km southeast of Réunion Island, Indian Ocean, prove the NN18 and NN19 nannoplankton zones, indicating the Pliocene-Pleistocene boundary. The Pliocene-Pleistocene boundary was established at 220-230 cm depth. The abundance of Globorotalia truncatulinoides increases from about 50 cm below the sea floor. The microfossil assemblages and clay mineral components of the sediments may be correlated with changes of climatic conditions influenced by glaciations.
dc.subject BIOSTRATIGRAPHY
dc.subject CALCAREOUS NANNOPLANKTON
dc.subject FORAMINIFERS
dc.subject INDIAN OCEAN
dc.subject PELAGIC OOZE
dc.subject RÉUNION ISLAND
dc.title THE PLIOCENE-PLEISTOCENE BOUNDARY IN PELAGIC OOZES OFF RÉUNION ISLAND, WESTERN INDIAN OCEAN
dc.type Статья
dc.subject.age Кайнозой::Четвертичная::Плейстоцен
dc.subject.age Кайнозой::Неоген::Плиоцен
dc.subject.age Cenozoic::Quaternary::Pleistocene
dc.subject.age Cenozoic::Neogene::Pliocene


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