Two lithological-stratigraphic intervals have been distinguished in the Morocco basin by a study of lithologic composition of bottom sediments as well as of planktic and bottom foraminifera present in them. Conditions, under which they developed, are discussed.
Supplement to: Trimonis, Egidius S; Lukashina, Nadezhda P (1985): Sediment accumulation in the Morocco Basin during the Late Quaternary. Oceanology, 25(3), 356-360