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MAP Technical Reports Series No. 106 UNEP

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- 73 -<br />

Tyrrhenian Sea. One area repeatedly affected by high trophic conditions and significant<br />

dystrophic processes is the Lagoon of Orbetello (Grosseto - southern Tuscany). The large<br />

amounts of nutrients of urban origin which have been discharged into the lagoon for 15 years<br />

promote periodic algae blooms which, particularly during the summer and autumn, cause<br />

frequent crisis of anoxic. Still, once normal conditions have been restored the ecosystem<br />

generally recovers rapidly (Lenzi and Salvatori, 1986). The resulting damage to the fish<br />

population of this lagoon ecosystem have led to short-term measures including the collection<br />

of the macroalgal biomass and the forced exchange of waters (Lenzi, 1992).<br />

Dystrophies caused by eutrophication phenomena are not reported in the coastal<br />

discharge area of the River Tiber (Pettine et al., 1983). In spite of the high trophic levels normally<br />

found at the two mouths of the river, as a result of the very active hydrodynamics of the site, the<br />

natural conditions of oligotrophy of the Tyrrhenian Sea and/or the presence of toxic substances<br />

capable of inhibiting the growth of autotrophic biomass, no microalgal blooms are reported<br />

(Zoppini et al., 1989).<br />

After the conspicuous increase in the human population of the adjacent areas, which<br />

started in the '30s, the coastal Lake of Sabaudia (7 km 2 in area, in southern Latium) gradually<br />

passed into a state of eutrophy; sewage inputs from the town of Sabaudia (5,000 residents +<br />

15,000 tourists during the summer season) and from a pig farm of 1,500 head led to recurrent<br />

anoxic crises. The most serious one occurred in July 1979, when all the fish stocks were<br />

destroyed (Perdicaro et al., 1980). From 1980 the treatment of the sewage and the closure of<br />

the pig-farm led to a gradual improvement of the basin (Perdicaro, 1985).<br />

Other reports of eutrophic environments come from the Lagoons of Miseno, Fusaro and<br />

Patria (Naples), where the discharge of untreated sewage and industrial effluents have seriously<br />

reduced water quality. For the Fusaro lagoon, Carrada et al. (1988) also reports a bloom of<br />

Gymnodinium catenatum (dinoflagellate capable of synthesizing PSP group toxins) with<br />

concentrations of 6,000,000 cells/l.<br />

Gulf of Naples. Two subsystems can be recognized in the Gulf of Naples: one is of<br />

"open sea water" with oligotrophic characteristics essentially determined by waters originating<br />

offshore; the other, nearshore system presents pronounced eutrophication phenomena triggered<br />

by the inputs along the coast (Genovese, 1979). However, there are significant variations in the<br />

coastal area; because of the poor circulation of the waters particularly in the<br />

summer months, plumes of dark waters caused by sewage outfalls may often be identified.<br />

Carrada et al. (1979) recorded high algal biomass values to the East of Naples in the areas with<br />

the highest nutrient input during the summer of 1977. Zingone et al. (1985) report a bloom<br />

caused by Chaetoceros simplex in the summer of 1983 that reached 120,000,000 cells/l in the<br />

areas most affected by the effluents from the city of Naples. Ribera D'Alcalà et al. (1989)<br />

encountered algal blooms in the same area in May 1987 which, although not widespread,<br />

reached peak concentrations of chlorophyll-a of 176 mg/m 3 . Modigh et al. (1985) emphasize the<br />

inverse correlation between salinity and chlorophyll-a values that further underlines the role of<br />

nutrient-rich waters and biostimulants from the sewage system.<br />

Carrada et al. (1982) found in the Gulf of Salerno in <strong>No</strong>vember 1981 the coast-offshore<br />

gradients of the autotrophic biomass to be low with concentration between 0.1 - 0.8 mg/m 3 of<br />

chlorophyll-a.<br />

<strong>No</strong> further episodes of eutrophication are reported from other areas of the Tyrrhenian,<br />

including southern Campania and the Calabrian coast which seems to be unaffected by<br />

eutrophication (De Domenico, 1979).

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