“…These gradients drive microbially mediated chemical transformations that modify solute concentrations in groundwater prior to discharge. Chemical transformations in coastal aquifers include dissolved organic carbon (DOC) degradation (Kroeger & Charette, ), aerobic respiration (Slomp & Van Cappellen, ), denitrification (Meile et al, ; Santos et al, ), nitrification (Ullman et al, ), anaerobic ammonium oxidation (Slomp & Van Cappellen, ), dissimilatory reduction to ammonium (Santoro, ), sulfate reduction (McAllister et al, ), and iron oxidation (Charette & Sholkovitz, ). Iron oxidation leads to precipitation of iron oxides onto sediment surfaces that adsorb and sequester solutes including phosphate and arsenic along groundwater flow paths (Charette & Sholkovitz, ; Jung et al, ).…”