Origin, evolution and significance of giant buried sediment mounds near the Sahara Slide Complex, North-west African margin

Mixed turbidite–contourite depositional systems result from interactions between down-slope turbidity currents and along-slope bottom currents, comprising excellent records of past oceanographic currents. Modern and ancient systems have been widely documented along the continental margins of the Atlantic Ocean. Yet, few examples have so far been identified on the North-west African continental margin, limiting understanding of the sedimentary and palaeoceanographic evolution in this area. This work uses two-dimensional seismic reflection profiles to report, for the first time, the presence of three giant sediment mounds beneath the headwall region of the Sahara Slide Complex. The sediment mounds are elongated and separated by two broad canyons, showing a north-west/south-east orientation that is roughly perpendicular to the continental margin. These mounds are 24 to 37 km long and 12 to 17 km wide, reaching a maximum height of ca 1000 m. Numerous slide scarps are observed within and al...