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Infralittoral molluscs, whose normal living depths are less than 25m, were recovered off the Nile delta between the coast and outer continental shelf and on the uppermost slope. At depths exceeding 25m, these 13 species are interpreted as relict markers of former low sea-level stands of latest Pleistocene-to-Holocene age. Their concentration in coast-parallel belts also records the role of seafloor erosion by Holocene to modern bottom-current activity, and also displacement by bioturbation. Widespread distribution of reworked molluscan faunas and low rates (to

Relict and Palimpsest Depositional Patterns on the Nile Shelf Recorded by Molluscan Faunas