The study of atmospheric aerosols over oceans is one of the new priority fields in the investigation of sedimentation in the oceans. Atmospheric transport of sedimentary particles suspended in the air is a link between the sources of matter transport from land, the ocean surface (substance mobilization zone), and bottom sediments [1‐3 and others]. Aeolian transport is especially important as a source of sedimentary matter in arid zones, where river discharge is minimal, especially in the ocean regions located far from the continents. Deserts, semideserts, and savannas in Africa are the main sources of aerosols in the Atlantic. A large number of publications is dedicated to the study of the main regions of outflow and pathways of transport of the African dust to the ocean observed by means of satellite images, calculation of inverse trajectories, identification of minerals and tracer elements, and so on [1‐5 and others]. However, publications estimating the specific contribution of aerosols to the composition of suspended particulate matter (SPM) in the ocean are quite rare. Most such works are dedicated to comparison of aerosol and matter fluxes collected by sedimentation traps in the water column [5 and others]. However, we did not find any publications devoted to comparison of the atmospheric aerosol and oceanic SPM samples taken simultaneously and processed using the same methods.