Terrigenous materials are transported to the ocean via various pathways, which can modify the weight contents of calcium carbonate (wt% CaCO₃) in marine sediment and mask CaCO₃ dissolution profiles, especially in ocean margins. Although the effect of terrigenous dilution on marine CaCO₃ has long been established, there is still a lack of quantitative assessment on how the terrigenous input shapes sedimentary CaCO₃ depth distribution features. In this study, we focus on the CaCO₃ depth distribution patterns on the seafloor in the Southeast Atlantic Ocean. Based on an up-to-date compilation of surficial sedimentary CaCO₃ content data and a simple conceptual model, the regional dilution effect of terrigenous supply from the African continent on the basinal sedimentary CaCO3 depth distribution is quantified. Our results show that the flux of non-carbonate materials needed to reproduce the carbonate distribution decreases with distance to the African continent. The non-carbonate flux to pelagic sediment in the Southeast Atlantic Ocean is of the same order of magnitude of the dust deposition rate, while the flux to marginal sediment is intensified as a consequence of the fluvial discharge. Moreover, enhanced dissolution of CaCO₃ is found in marginal regions, which is due to faster rates of deep (boundary) currents than those in the pelagic ocean. These new insights help to distinguish the dilution impact from carbonate dissolution patterns and will advance research on land-ocean interaction and paleo-climate/environment reconstructions in ocean margins.