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Proceedings of the Second Mediterranean Symposium on Marine

Proceedings of the Second Mediterranean Symposium on Marine

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PROCEEDINGS OF THE SECOND MEDITERRANEAN SYMPOSIUM ON MARINE VEGETATION (ATHENS, 12-13 DECEMBER 2003)<br />

148<br />

Lithophyllum byssoides – formati<strong>on</strong> (“trottoir”): Present in places with high<br />

hydrodynamism and steep slope. The growth <str<strong>on</strong>g>of</str<strong>on</strong>g> Lithophyllum byssoides s<br />

creates an overhang in <str<strong>on</strong>g>the</str<strong>on</strong>g> upper infralittoral level that prevents <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

growth <str<strong>on</strong>g>of</str<strong>on</strong>g> Cystoseira.<br />

Cystoseira spp. (sheltered envir<strong>on</strong>ments): Mainly characterized by Cystoseira crinita,<br />

C. brachycarpa, C. elegans but also by o<str<strong>on</strong>g>the</str<strong>on</strong>g>r species <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> same genus.<br />

The same categories used for C. mediterranea can be used.<br />

Cystoseira compressa: Belt <str<strong>on</strong>g>of</str<strong>on</strong>g> Cystoseira compressa, it can also be distinguished in <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

5 categories we have used for C. mediterranea / C. amentocea var. stricta.<br />

Posid<strong>on</strong>ia oceanica: Barrier reefs <str<strong>on</strong>g>of</str<strong>on</strong>g> Posid<strong>on</strong>ia oceanica, whose leaves attain <str<strong>on</strong>g>the</str<strong>on</strong>g> water<br />

surface can be observed in sheltered envir<strong>on</strong>ments, usually toge<str<strong>on</strong>g>the</str<strong>on</strong>g>r with<br />

Cystoseira spp.<br />

Cymodocea nodosa: Meadows dominated by this species in very sheltered<br />

envir<strong>on</strong>ments, over sand, mud or gravel.<br />

Zostera noltii: Meadows dominated by this species in extremely sheltered envir<strong>on</strong>ments,<br />

usually over muddy and silty bottoms.<br />

Corallina el<strong>on</strong>gata: This unit is characterized by <str<strong>on</strong>g>the</str<strong>on</strong>g> dominance <str<strong>on</strong>g>of</str<strong>on</strong>g> this species, which is<br />

widespread in <str<strong>on</strong>g>the</str<strong>on</strong>g> Northwestern <str<strong>on</strong>g>Mediterranean</str<strong>on</strong>g>, but always with <str<strong>on</strong>g>the</str<strong>on</strong>g> absence<br />

<str<strong>on</strong>g>of</str<strong>on</strong>g> Cystoseira. In fact, <str<strong>on</strong>g>the</str<strong>on</strong>g> categories 1 and 2 <str<strong>on</strong>g>of</str<strong>on</strong>g> Cystoseira should be usually<br />

attributed to this or o<str<strong>on</strong>g>the</str<strong>on</strong>g>r communities with <str<strong>on</strong>g>the</str<strong>on</strong>g> presence <str<strong>on</strong>g>of</str<strong>on</strong>g> some Cystoseira<br />

individuals.<br />

Haliptil<strong>on</strong> virgatum: Community dominated by this species, sometimes with Dictyota<br />

fasciola and Laurencia microcladia. Absence <str<strong>on</strong>g>of</str<strong>on</strong>g> Cystoseira plants.<br />

Mytilus galloprovincialis: Mussel beds, without Cystoseira.<br />

Green algae: Green littoral belts dominated by Ulva, Cladophora without Cystoseira.<br />

Encrusting corallines : Belts dominated by <str<strong>on</strong>g>the</str<strong>on</strong>g> encrusting corallines Lithophyllum<br />

incrustans, Neog<strong>on</strong>iolith<strong>on</strong> brassica-florida, and, even, crusts <str<strong>on</strong>g>of</str<strong>on</strong>g> Corallina<br />

el<strong>on</strong>gata.<br />

Blue green algae: The dominant species are blue green algae, perhaps with some<br />

ulvacean algae and Derbesia tenuissima.<br />

The presence/absence and abundance <str<strong>on</strong>g>of</str<strong>on</strong>g> every community is determined not <strong>on</strong>ly by<br />

polluti<strong>on</strong> or o<str<strong>on</strong>g>the</str<strong>on</strong>g>r antrhopogenic disturbances but also by <str<strong>on</strong>g>the</str<strong>on</strong>g> natural envir<strong>on</strong>ment.<br />

Therefore, different geomorphological parameters that most probably are involved in <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

establishment and/or development <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> communities have to be evaluated in order to<br />

account for this natural variability. The geomorphological factors that we have c<strong>on</strong>sidered<br />

are <str<strong>on</strong>g>the</str<strong>on</strong>g> following:<br />

- Coastline morphology: c<strong>on</strong>tinuous rock, blocks, st<strong>on</strong>es…<br />

- Substrate c<strong>on</strong>stituti<strong>on</strong>: calcareous, basaltic, granitic…<br />

- Coastline slope<br />

- Coastline orientati<strong>on</strong><br />

- Natural\Artificial<br />

- Degree <str<strong>on</strong>g>of</str<strong>on</strong>g> wave exposure<br />

- Height <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> sea-cliffs

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