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Assemblages of foraminiferids from the Upper Cretaceous section of the Subsilesian unit (Polish Outer Carpathians) have been analyzed. The age of the studied samples bas been estimated as Turonian-Campanian, based on agglutinated as well as planktonic foraminiferids. Morphogroup analysis of the studied foraminiferids showed an increase of the organic flux on the basin floor.
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Tom
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99--107
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Bibliogr. 22 poz.
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- Institute of Geological Sciences, Jagiellonian University, Kraków, Poland
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Bibliografia
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bwmeta1.element.baztech-article-BSL8-0003-0008