Suspension feeding bivalves have the potential to mitigate estuarine and coastal marine eutrophication by permanently removing nitrogen (N) from the system. We conducted an integrated field and laboratory examination of the effect of eastern oyster biodeposition on sediment denitrification (DNF) and anammox (AMX) rates to quantify the N removal potential of oyster aquaculture using 2 commercial-scale sites in Chesapeake Bay, USA. Sediment N 2 production rates were measured using 2 techniques, 15 N isotope tracer (n = 51) and N 2 :Ar (n = 30). Oyster biodeposit N-load rates explained 21% of variation in sediment N 2 production (DNF and AMX). Oyster sediment N 2 production rates ranged from 0.00 to 1.56 mmol N m −2 d −1 and were almost always lower than reference sediments. From laboratory-based biodeposit addition and fieldbased forced biodeposit accumulation experiments, we found ~2.50 mmol N m −2 d −1 to be the maximum sediment N 2 production capacity of these sediments, regardless of increasing organic N or labile organic carbon delivery rates. We found no evidence to support the contention that biodeposition associated with oyster aquaculture significantly impacts annual N removal via sediment N 2 production, i.e. stimulation or inhibition, above reference rates, but there was evidence that sediment NH 4 + efflux rates were increased. We estimate the N removal rate via sediment N 2 production at similar oyster cultivation sites (1750 m 2 ) with 5 × 10 5 oysters ranges from 0.49 to 12.60 kg N yr −1 , compared to 2.27 to 16.72 kg N yr −1 at reference sites. Thus, aqua cultured oyster biodeposition did not have a ubiquitously enhancing effect on N removal rates via N 2 production and is therefore unlikely to be effective as a policy initiative for eutrophication mitigation.