Late Miocene to Pleistocene sedimentation and sediment transport on the Cocos Ridge, eastern tropical Pacific Ocean

We use digital seismic reflection profiles within a 1°×1° survey area on the Cocos Ridge (COCOS6N) to study the extent and timing of sedimentation and sediment redistribution on the Cocos Ridge. The survey was performed to understand how sediment focusing might affect paleoceanographic flux measurements in a region known for significant downslope transport. COCOS6N contains ODP Site 1241 to ground truth the seismic stratigraphy, and there is a seamount ridge along the base of the ridge that forms a basin (North Flank Basin) to trap sediments transported downslope. Using the Site 1241 seismic stratigraphy and densities extrapolated from wireline logging, we document mass accumulation rates (MARs) since 11.2Ma. The average sediment thickness at COCOS6N is 196m, ranging from outcropping basalt at the ridge crest to ~400m at North Flank Basin depocenters. Despite significant sediment transport, the average sedimentation over the entire area is well correlated to sediment fluxes at Site 1241. A low mass accumulation rate (MAR) interval is associated with the ‘Miocene carbonate crash’ interval even though COCOS6N was at the equator at that time and relatively shallow. Highest MAR occurs within the late Miocene–early Pliocene biogenic bloom interval. Lowest average MAR is in the Pleistocene, as plate tectonic motions caused COCOS6N to leave the equatorial productivity zone. The Pliocene and Pleistocene also exhibit higher loss of sediment from the ridge crest and transport to North Flank Basin. Higher tidal energy on the ridge caused by tectonic movement toward the margin increased sediment focusing in the younger section. •Ground truth of paleoceanographic assumption that one drill site documents regional fluxes.•Cocos Ridge sedimentation is driven by regional paleoceanographic sediment events.•Sediment transport from the Cocos Ridge crest increased from the Miocene to the Pleistocene.•Increased sediment transport is caused by higher tidal energy near Costa Rica margin.