Abstract
Restoration of the Little Qualicum River Estuary has focused on re-establishing the Carex lyngbyei channel edge vegetation lost to grubbing by the overabundant resident Canada goose population. Short-term sediment deposition rates were measured using weekly deployments of sediment traps between June and July 2019 to investigate how restoration is facilitating sediment retention to rebuild the marsh platform. Deposition rates varied between 6.82-107.88 g/m2/week with traps deployed on the denuded mud flat areas collecting more sediments than inside the older exclosures. It had been expected that the exclosures with a greater density of sedges would retain more sediment. Spatial variation may be attributed to differences in sampling elevations. Restoring C. lyngbyei may not increase localized sediment deposition directly but does protect the continued supply of organic input from the seasonal senescence of C. lyngbyei. The organic input from aboveground biomass may have a larger contribution to marsh accretion than allochthonous sediments.