Changing conditions during Quaternary glacial and interglacial stages have had a great influence on the location and amount of sedimentation, and on the grain size of deposits. In this modelling study, the volume and grain-size distribution in passive continental margin strata are investigated. A principal aspect of the basin-scale grain-size sorting process is the formation of a subaerial erosional unconformity. During forced regression, deltaic coarsening-up sequences are deposited on the shelf. The relatively coarse-grained topsets of these successions have a lower preservation potential than the finer prodelta deposits. Therefore, erosion on the exposed shelf results in enrichment of river-transported sediments with coarse material during sea-level lowstand. Thus, shelfal strata are depleted of coarse material, increasing the coarse content of deposits on the upper continental slope. In contrast, in the absence of an erosional unconformity, the composition of sediments on the shelf is relatively coarse. The extent to which sediment within a stratigraphic column has been separated into coarse strata, as opposed to mixed compositions, is expressed as a 'differentiation ratio'. Interconnectedness of coarse-grained sediment bodies in the stratigraphy of the continental shelf and slope is closely related to the palaeogeographical evolution, and is consequently a highly variable property.