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Agglutinated benthic foraminifera and changes of paleoenvironment conditions across the Cretaceous- Paleogene boundary in the Glanderud section, Alborz basin, North of Iran
Year: 2012
Abstract:
The Glanderud section has been studied for quantitative changes in agglutinated benthic foraminifera.Twenty-five species were recognized in the uppermost Maastrichtian Marl and in the K-P boundary clay layer. Three types of assemblages are:
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