biological diversity and tropical forests in tunisia - PART
biological diversity and tropical forests in tunisia - PART
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 />
. ..