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This report describes the effect of aquaculture effluent on benthonic foraminiferal populations in Clam Bay, Nova Scotia. The study area is 45 miles east of Halifax (Fig. 1) and was first visited by the author in 1968. At that time, coastal geodynamic processes were monitored by marine geologists of the Bedford Institute and a definition of these conditions attempted. All geodynamic processes studied were in relation to sediment movement on the foreshore and regression of berm lines in the backshore area. Specifically three sets of energy indicators were monitored. These consisted of the measurement of current velocity within the bay, daily tidal fluctuation in the area and lastly the combined factors of wave frequency, height and intensity.

Effects of Aquaculture Outfall on Benthonic Foraminifera in Clam Bay, Nova Scotia