Abstract
Resuspension of bottom sediments accounted for 69–92% of mean deposition rates (11·6–69·3 gm −2 day −1) measured at 5 sites in the Peel-Harvey Estuarine System, Western Australia. Deposition rates at all but one of the sites were found to be correlated ( P<0·05) with a function of wind combining a fetch factor with the number of hours of winds greater than 5 ms −1 weighted by the third power of wind velocity. The exception was the only site with a cover of benthic algae ( Cladophora) during the study. Wind-related resuspension greatly affects the forms and amounts of productivity in this system.
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