“…This situation is usually characterized by an increased level of nutrients (NH 4 , NO 3 , PO 4 ) and suspended particulate matter in the water column, by nitrogen and phosphorus enrichment of sediments, by dissolved oxygen depletion which can lead to anoxic crisis in summer, and the frequent occurrence of macroalgal blooms (Zaouali, 1977;De Casabianca, 1983;Comin, 1984;Sfriso et al, 1988;Viaroli et al, 1993;Lundin and Linden, 1993;De Casabianca et al, 1994). If water inputs and their high nutrient loads are generally used to explain eutrophication in coastal lagoons, primary productivity, sediments and occasionally secondary productivity, also play a key role in nutrient recycling, and thus play a great part in sustaining eutrophic conditions.…”