Estuarine soft sediments support a diverse group of eukaryotic and prokaryotic organisms though the role of the sediment per se for the functioning of these organisms remains largely unknown. The present study aimed to test the eVect of sediment grain size on the grazing activities of harpacticoid copepods. In controlled experiments, two common intertidal harpacticoid species (Paramphiascella fulvofasciata and Nitokra spinipes) were each oVered a mix of two benthic diatom species (Navicula phyllepta and Seminavis robusta) in diVerent sedimentary conditions. Several microcosms were created using a variety of sediment types, including Wne silt (<63 m), coarser grained sands (125-250, 250-450, 100-300 m), artiWcial 'sediments' of glass beads (250-500, 2000 m) and even the absence of sediment was tested. The diatoms were enriched in the stable carbon 13 C to facilitate tracing in the harpacticoids. Both copepod species were able to graze on the diatoms with highest uptake when sediment was absent. In contrast, both harpacticoid species showed no uptake in silty conditions. In general, grazing was favoured when mean sediment grain size increased. The strong negative eVect of Wne grains on the grazer's eYciency can be explained by the resulting diVerences in the structure (and accessibility) of the diatom bioWlm on the one hand and the mobility of the grazer on the other hand. In view of the subtle equilibrium between primary producers and grazers, these results might have important implications for the eVect of siltation of tidal Xats due to, e.g., human activities.