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biological diversity and tropical forests in tunisia - PART

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center <strong>and</strong> the lake edge is highly developed. There is a salt process<strong>in</strong>g .<br />

area near Tunis where a sizable area has been sectioned off, but it is<br />

still used by waders <strong>and</strong> waterfowl.<br />

The most serious <strong>in</strong>fluence on the lake is a development project that<br />

has already filled 900 ha <strong>and</strong> is projected to fill at least 1,500 ha for a<br />

new section of the city of Tunis. The project will reduce the area<br />

available to waterfowl<strong>and</strong> <strong>in</strong>crease disturbance <strong>in</strong> the unfilled portion of<br />

the lake. This development is occur<strong>in</strong>g <strong>in</strong> spite of the fact that Lake<br />

Tunis was designated a Protected Wetl<strong>and</strong> <strong>in</strong> 1980 (see Section 5.4).<br />

3.3.1.4. Lake Monastir<br />

On the coast just south of Monastir <strong>and</strong> 160 km south of Tunis is Lake<br />

Monastir. More properly called a coastal lagoon, Lake Monastir is the<br />

site of the former Monastir salt ponds; ab<strong>and</strong>onned ic 1952 ort tier 1977).<br />

The lagoon is formed by a s<strong>and</strong>y barrier spit that extends for 2.5 km along<br />

the coast <strong>and</strong> a f<strong>in</strong>al 0.5 km artificial rock bank that has been<br />

constructed at the south end to complete the barrier acd close off a 175<br />

ha water body. Canals at the north <strong>and</strong> south ends providi communication<br />

with the sea. Most of the lagoon is less thac 2 m deep, b~t the Office<br />

National des Peches (~ational Fisheries office) has dragged channels 2.5 -<br />

3.5 m deep to improve fssh production. The channels allow water to<br />

circulate betweec the 2 canals to the sea, <strong>and</strong> <strong>in</strong> good weather a current<br />

provides partial water replacement every 6 hours.<br />

A. Vegetation<br />

Mortier (1977) described 5 zones <strong>in</strong> the lagoon:<br />

1. Cymodocea zone.<br />

stagnant waters.<br />

Dense Cymodocea nodosa dom<strong>in</strong>ates the shallow non-<br />

2. Caulerpa zone. In the deeper, more turbid <strong>and</strong> less frequently<br />

recewed waters <strong>and</strong> <strong>in</strong> parts of the canals the more tolerant<br />

Caulerpa prolifera grows.<br />

3. Greec filamentous algae - zone. Some parts atta<strong>in</strong> extreme levels of<br />

temperature <strong>and</strong> sal<strong>in</strong>ity dur<strong>in</strong>g periods, restrict<strong>in</strong>g growth of<br />

Cymodocea <strong>and</strong> result<strong>in</strong>g <strong>in</strong> the formation of algae mats.<br />

4.<br />

5.<br />

Shallow muddy-s<strong>and</strong> zone. Unvegetated.<br />

Deep stagnant zone. Turbid <strong>and</strong> unvegetated canals.<br />

B. Fauna<br />

Little <strong>in</strong>formation is published regard<strong>in</strong>g the vertebrate fauna of the<br />

lagoon, but it is probably similar to the rest of the coastl<strong>in</strong>e of the<br />

Gulf of Hammamet. Terns, grebes <strong>and</strong> other fish eat<strong>in</strong>g birds are attracted<br />

by the fish be<strong>in</strong>g raised <strong>in</strong> the lagoon.<br />

Marice Fauna. The mar<strong>in</strong>e fauna o or tier 1977) is composed of:<br />

Nereis sp. (~olychete) Cmstaceacs<br />

Ceriithium vulgatum (~astero~od) Isopods<br />

Clibacarias misanthropus " Amphi pods<br />

Lucicia lactea (pelecypod) Kaldacid Polychetes<br />

. ..

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