Foraminiferal and radiolarian biostratigraphy of the youngest (Late Albian through Late Cenomanian) sediments of the Tatra massif, Central Western Carpathians

Bąk, K.; Bąk, M.

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Foraminiferal and radiolarian biostratigraphy of the youngest (Late Albian through Late Cenomanian) sediments of the Tatra massif, Central Western Carpathians

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Bąk K. , Bąk M.

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Abstrakty

The foraminiferal and radiolarian biostratigraphy of selected sections of the Zabijak Formation, the youngest sediments of the Tatra massif (Central Western Carpathians), have been studied. Benthic foraminifers, mainly agglutinated species, occur abundantly and continuously throughout the studied succession, while planktic foraminifers are generally sparse. Five planktic and two benthic foraminiferal zones have been recognized. The marly part of the Zabijak Formation comprises the Pseudothalmanninella ticinensis (Upper Albian) through the Rotalipora cushmani (Upper Cenomanian) planktic foraminiferal zones, and the Haplophragmoides nonioninoides and Bulbobaculites problematicus benthic foraminiferal zones. The radiolarians were recognized exclusively in the Lower Cenomanian part of the formation.

Słowa kluczowe

Albian–Cenomanian Tatra massif biostratigraphy foraminifera radiolaria

alb cenoman Tatry masyw biostratygrafia otwornice promienice

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2013

Tom

Vol. 63, no. 2

Strony

223--237

Opis fizyczny

Bibliogr. 69 poz., il., tabl. 3

Twórcy

autor

Bąk K.

sgbak@cyf-kr.edu.pl

Institute of Geography, Pedagogical University of Cracow, Podchor¹¿ych St. 2, PL-30-084 Krakow, Poland

autor

Bąk M.

martabak@agh.edu.pl

Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, 30 Mickiewicza Av., PL-30-059 Krakow, Poland.

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