The evolution of gateways determines variations in palaeo-environmental (ecological and depositional) conditions affecting trace maker communities, hence biogenic structures. With respect to palaeo-gateways, bottom currents and associated deposits (i.e., contourites) may be approached through trace fossil studies. Ichnological analysis -individual ichnotaxa and changes in ichnofacies- of Late Miocene contourites and associated facies from the Rifian Corridor palaeo-gateway (Morocco) reveals a major impact of food supply, flow velocity, seafloor heterogeneity, and hydrodynamic energy. The fact that Eocene to middle Miocene deep-marine deposits -mainly contourites- from the nearby Indian palaeo-gateway (Cyprus) show ichnofacies replacement is evidence of increased bottom-current flow velocity associated with sea level variations. Moreover, ichnofabric changes reflect pelagic, gravitational, and bottom-current processes that simultaneously influence sedimentation. Changes in the trace fossil composition of both areas
,
and in the shape of burrows, reflect intermittent bottom current processes that governed contourite deposition. Neoichnological studies complement and validate the trace fossil record of high-energy deep-sea environments that can occur in palaeo-gateways. Modern traces (
lebensspuren
) observed on the seafloor show variable features (e.g., diversity, density, morphology) depending on the type of disturbance that high-energy conditions exert on the trace-making benthic fauna. Parameters such as substrate consistency, nutrient availability/distribution, and the duration and intensity of energetic events play a major role in determining
lebensspuren
features. We conclude that an integrative palaeo- and neoichnological approach is a powerful tool when used to improve our knowledge of benthic ecosystems in high-energy deep-sea environments such as gateways.