Abstract
A detailed study of the calcareous nannofossil assemblages of latest Danian to early Selandian age from Wadi Qena (the Qreiya-1, Qreiya-2, and Araas sections) in the central Eastern Desert and the Gebel Duwi section at the Red Sea Coast has been carried out to understand the local phytoplankton paleocommunities. For the first time in Egypt four calcareous nannofossil zones (NTp6, NTp7, NTp8, NTp9) and five subzones (NTp7A, NTp7B, NTp8A, NTp8B and NTp8C) were distinguished subdividing the standard NP4 and NP5 zones. The calcareous nannofossil zones were correlated with nannofossil zonations from the Tethyan region (e.g. Tunisia and the Zumaia section, the GSSP for the Danian/Selandian boundary). The calcareous nannofossil assemblages are moderately to well preserved. The event beds are characterized by a dark-brown shaley-marl bed rich in organic carbon and coprolites. Three main assemblages are distinguished: a pre-event assemblage, a transitional assemblage and a post-event assemblage. The paleoenvironments vary from cool eutrophic water below and above the event to warm oligotrophic conditions during the event. The result of this study concludes that the "Latest Danian Event" (LDE) may represent an early Paleocene hyperthermal. Abstract Copyright (2009) Elsevier, B.V.