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The Cenomanian–Turonian succession exposed in the Wadi Feiran, Sinai, Egypt, is composed of siliciclastic and carbonate sediments belonging to the Raha (at the base), Abu Qada and Wata formations. Biostratigraphically, the succession has been subdivided into five ammonite zones, which are coeval with five planktic foraminiferal zones. The foraminiferal zones are the Late Cenomanian Hedbergella planispira...
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