“…The core M77/2-005-3 off Callao receives a Ti flux primarily from the discharge of the rivers Chancay, Chillón, Rimac, and Lurín, while the G14 core off Pisco is influenced by the Pisco and Ica rivers. Under the current climate, the flow of coastal rivers is usually low and increases during austral summer because of the monsoon rainfall in the High Andes 3,27,28 . During El Niño events, especially those with high sea surface temperature (SST) anomalies in the Eastern Pacific (EP), strong thunderstorms and precipitation occur on the coast 5,29,30,31,32 .…”