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The document discusses foraminiferal biostratigraphy and paleobathymetry of the Maastrichtian to Paleocene succession in the north Farafra Oasis, Western Desert, Egypt. The succession is divided into three formations from oldest to youngest: Khoman, Dakhla, and Tarawan formations. Based on planktonic foraminifera, nine biozones are identified including the Globotruncana aegyptiaca Zone and Gansserina gansseri Zone from the Maastrichtian. The Cretaceous/Paleogene boundary lies between the Khoman and Dakhla f

Author

Sai Naing Lin aung

Language

EN