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MAP Technical Reports Series No. 106 UNEP

MAP Technical Reports Series No. 106 UNEP

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Bay of Thessaloniki (north-west of the Gulf of Thermaikos). A eutrophic situation similar<br />

to that in the Bay of Elefsis and the Gulf of Amvrakikos (Balopoulos and Friligos, 1986;<br />

Samanidou et al., 1986). Huge amounts of nutrients are carried into this Gulf by industrial<br />

effluents and the sewage outfalls of the city of Thessaloniki (population 1,300,000) and the<br />

waters of four rivers. The Axios river is held responsible for transferring large quantities of<br />

nitrates of agricultural origin into the Gulf. In this zone, the increase in the phytoplankton biomass<br />

is directly correlated with the increases in nitrates and phosphates and with the reduction in<br />

salinity values. The blooms are generally caused by diatoms: Nitzschia closterium, Cerataulina<br />

bergonii, Leptocylindrus minimus, Chaetoceros socialis and Thalassiosira sp. are the dominant<br />

species in the majority of cases (Gotsis-Skretas and Friligos, 1988).<br />

Gulf of Kavala. Although the trophic levels are generally lower than in the other areas<br />

mentioned, it appears that a bloom of the dinoflagellate Gonyaulax polyedra with 10,000,000<br />

cells/l that occurred in August 1986 in the north-western part of the Gulf was caused by the<br />

wrecking of a ship transporting phosphate fertilizers (Panagiotides et al., 1989).<br />

Estuary of the Vistonis River. Yiannakopoulou (1992) reports an intense bloom in<br />

August 1984 with maximum chlorophyll-a values of 86.0 mg/m 3 , consisting mainly of<br />

cyanobacteria.<br />

Gulf of Alexandropoulis (to the <strong>No</strong>rth-East of the Aegean). A trophic situation similar to<br />

Kavala. Mainly because of the emissions of the Evros river, in 1981-1982 concentrations of<br />

silicates and nitrates were three times and six times respectively higher than normal (Pagou,<br />

1990).<br />

5.2.7 Malta: Central Mediterranean<br />

A three year monitoring program (1989-1991) was carried out in Malta in order to define<br />

the trophic state of two intensely urbanized port areas with heavy commercial traffic, the Grand<br />

Harbour and the Marsamxett Harbour. Axiak et al. (1992) found that the nutrient and chlorophyll<br />

levels were comparable to those measured in other areas of the Mediterranean where clear<br />

signs of eutrophication already exist. Increased levels of primary productivity has reduced the<br />

transparency of the waters, particularly in the innermost areas with the longest water residence<br />

times, showing a mean of 2.6 m. The same areas have the highest mean values of nutrients<br />

(26.4 and 1.6 mg-at/m 3 for nitrates and orthophosphate, respectively) and chlorophyll-a. Nutrient<br />

inputs come above all from sewage outfalls (population of 73,000 in the capital Valletta and its<br />

suburbs), although the contribution of shipping and tourism should also be mentioned.<br />

5.2.8 Turkey: <strong>No</strong>rth-eastern Mediterranean<br />

Open marine waters of Turkey generally present conditions of oligotrophy; only in<br />

limited costal areas affected by the inputs of rivers, sewage outfalls or industrial effluents<br />

conditions of eutrophy are reported.<br />

The Sea of Marmara is an exception because of both its size, hydrology and<br />

hydrodynamics. A semi-enclosed sea, with an area of 11,500 km 2 and a volume of 3,378 km 3 ,<br />

its dominant low-density surface current tends to flow from East to West, while the bottom<br />

current carries high-density Mediterranean water from the Dardanelles towards the Bosphorus.<br />

During an oceanographic cruise in the Sea of Marmara from 30 June to 8 July 1990, Aubert et<br />

al. (1990) measured particularly high orthophosphate and inorganic nitrogen

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