“…Over the late Quaternary, the channel-levee-lobe systems has undergone lateral architectural changes of increasing/decreasing channel lengths and basinward/landward migration of avulsion points, corresponding to prograding/retrograding architectural fan cycles (Marsset et al, 2009;Picot et al, 2016). Studies of the Axial Fan show that climatic factors controlled by the West African monsoon are the primary control of architecture and timing of avulsions of the channel-levee-lobe systems (Laurent et al, 2020;Marsset et al, 2009;Picot et al 2016Picot et al , 2019. During the humid period, the progradation system occurs with high fluvial discharge and chemical erosion, elevating the transport capacity of the turbidity currents (Marsset et al, 2009;Picot et al 2016Picot et al , 2019.…”