Palynological, palynofacies and organic geochemical results of 46 samples retrieved from the Upper Cretaceous – Eocene Matulla, Brown Limestone and Thebes formations, Belayim oilfields, central Gulf of Suez, Egypt are presented. The two latter formations are not dated palynologically as their lithology is not promising for palynological yield. However the Matulla Formation is dated as Turonian–Santonian age, based on the combined evidence of pollen and dinocysts. Palynofacies analysis carried out under both transmitted and fluorescent microscopy indicated that both the Thebes and Brown Limestone formations are deposited under a distal suboxic–anoxic environment. On the other hand, the Turonian–Santonian Matulla Formation supported the existence of a marginal marine deposition under dysoxic–anoxic basin to proximal suboxic–anoxic shelf environments. Rock-Eval pyrolysis and TOC results indicated that most of the studied formations are thermally immature to marginally mature and have...
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