Direct measurements of net production rates and pore water profiles of solutes in the fine-grained sediments of Saginaw Bay, imply corresponding steady-state fluxes to the overlying water of 1.1-1.3(I), 450-1010 (NH4(1+)), 1250-2650 (Si(OH)4), 3000-3400 (Ca(2+)), 440-1330 (Mg(2+)), 1.5-728 (Fe(2+)), and 179-281 (Mn(2+)) micromoles/sq m/day and 11.0-11.8 (alkalinity) meq/sq m/day at 17.5 C. Silica production rates in sediments apparently follow first order kinetics with a rate coefficient of approximately 0.09/day and a steady-state silica concentration of 1.2 mM at 23.5 C. The remaining solutes follow kinetics approximately independent of solute concentration over the range of concentrations observed. Measured solute production rates are consistent with observed solute profiles only if lateral diffusion gradients are maintained in the sediments by the burrowing and irrigation activity of benthic organisms such as Chironomous, the dominant burrower in Saginaw Bay. Assuming that solute fluxes from Saginaw Bay are representative of all of the post-glacial sediments of Lake Huron, the iodine flux from sediments is comparable to the total fluvial input of iodine. The extrapolated silica fluxes from Lake Huron sediments balance the estimated biogenic silica flux to the sediments.