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Groundwater and associated nutrients discharge from the beachface to the Delaware Estuary at Cape Henlopen, Delaware, and appear to contribute significantly to the ecological structure of the adjacent intertidal and subtidal benthic communities. The cross-sectional distributions of salinity and nutrient concentrations at one seepage site indicate that there are two distinct groundwater masses that mix with seawater in the sandy beachface during discharge. The dissolved nutrient concentrations in the beachface at this site are substantially higher than those found in the adjacent estuarine surface water. Nutrient concentrations and distribution in the beachface water reflect: (1) the discharge of nutrient-rich upland water; (2) mixing between nutrient-rich groundwater and estuarine water; and (3) diagenetic recycling of estuarine organic material in the beachface mixing zone. Simple mixing and hydrological models are used to determine the relative magnitude of upland and diagenetic contributions and to estimate absolute nutrient discharges across the beachface. Nutrient fluxes during the summer at this site are sufficient to support carbon fixation rates of 4–17 mol C/m/year along the beachface. These nutrient fluxes are substantially higher than can be supported by the upland discharge alone. This suggests that beachfaces serve as traps and reservoirs of estuarine particulate matter and associated nutrient elements. During the summer, when samples were collected at the Cape Henlopen site, nutrient concentrations in the estuary are low and the remineralization of particles in the beachface may contribute significantly to the productivity of the dense plant and animal communities found adjacent to the beachface. [Copyright &y& Elsevier]