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Proceedings of the Second Mediterranean Symposium on Marine

Proceedings of the Second Mediterranean Symposium on Marine

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At <str<strong>on</strong>g>the</str<strong>on</strong>g> end <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> summer 1999, an unprecedented mass mortality <str<strong>on</strong>g>of</str<strong>on</strong>g> benthic<br />

invertebrates (mainly gorg<strong>on</strong>ians, sp<strong>on</strong>ges, ascidians and bryozoans) occurred al<strong>on</strong>g <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

coasts <str<strong>on</strong>g>of</str<strong>on</strong>g> Provence (France), French Riviera and Ligury (Italy). Excepti<strong>on</strong>ally high<br />

temperatures throughout <str<strong>on</strong>g>the</str<strong>on</strong>g> water column (23-24°C) for over <strong>on</strong>e m<strong>on</strong>th, down to<br />

40 m depth, could have created an envir<strong>on</strong>mental c<strong>on</strong>text favourable to <str<strong>on</strong>g>the</str<strong>on</strong>g> mass<br />

mortality event (Cerrano et al., 2000; Coma et al., 2000; Pérez et al., 2000; Romano et<br />

al., 2000). This episode is <str<strong>on</strong>g>of</str<strong>on</strong>g> particular interest since, should <str<strong>on</strong>g>the</str<strong>on</strong>g> present day warming<br />

trend c<strong>on</strong>tinue, it could be <str<strong>on</strong>g>the</str<strong>on</strong>g> harbinger <str<strong>on</strong>g>of</str<strong>on</strong>g> even more drastic events.<br />

Unfortunately, as far as macrophytes are c<strong>on</strong>cerned, very little informati<strong>on</strong> is available<br />

about <str<strong>on</strong>g>the</str<strong>on</strong>g> possible effect <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> warming up <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> <str<strong>on</strong>g>Mediterranean</str<strong>on</strong>g> water: (i) Some<br />

encrusting corallines (Rhodobi<strong>on</strong>ta, Plantae) were said to have been affected by <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

1999 summer warm episode (Cerrano et al., 2000), but nothing is known about <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

extent <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> phenomen<strong>on</strong> and <str<strong>on</strong>g>the</str<strong>on</strong>g> subsequent recovery. (ii) The native Caulerpa<br />

prolifera (Chlorobi<strong>on</strong>ta, Plantae) is extending its range area northwards, from Corsica, <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

Tyrrhenian Sea and <str<strong>on</strong>g>the</str<strong>on</strong>g> French Riviera to Ligury and Provence (Bianchi and Morri, 1994<br />

and unpublished data). Outside <str<strong>on</strong>g>the</str<strong>on</strong>g> <str<strong>on</strong>g>Mediterranean</str<strong>on</strong>g>, in <str<strong>on</strong>g>the</str<strong>on</strong>g> Gulf <str<strong>on</strong>g>of</str<strong>on</strong>g> Maine (USA), a<br />

synergy between climate change and introduced species has been observed (Harris and<br />

Tyrrell, 2001).<br />

A CASE STUDY: THE DECLINE OF CYSTOSEIRA FORESTS<br />

More than 50 taxa bel<strong>on</strong>ging to <str<strong>on</strong>g>the</str<strong>on</strong>g> genus Cystoseira (Fucophyceae, Chromobi<strong>on</strong>ta,<br />

Stramenopiles) thrive in <str<strong>on</strong>g>the</str<strong>on</strong>g> <str<strong>on</strong>g>Mediterranean</str<strong>on</strong>g> Sea (Ribera et al., 1992). Most <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g>m are keyspecies<br />

in a variety <str<strong>on</strong>g>of</str<strong>on</strong>g> forest communities which are encountered <strong>on</strong> subtidal and<br />

circalittoral hard bott-oms (Giacc<strong>on</strong>e and Bruni, 1972-1973). In additi<strong>on</strong>, <str<strong>on</strong>g>the</str<strong>on</strong>g>y are usually K<br />

strategists and l<strong>on</strong>g-lived (at least 45 years for C. spinosa; Ballesteros et al., 1995, 1998).<br />

Since <str<strong>on</strong>g>the</str<strong>on</strong>g> 1960s, Cystoseira forests have underg<strong>on</strong>e a severe decline in extensive areas<br />

<str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> <str<strong>on</strong>g>Mediterranean</str<strong>on</strong>g>. Several species <str<strong>on</strong>g>of</str<strong>on</strong>g> Cystoseira and <str<strong>on</strong>g>the</str<strong>on</strong>g> communities <str<strong>on</strong>g>the</str<strong>on</strong>g>y dominate<br />

are c<strong>on</strong>sidered as threatened (Boudouresque et al., 1990). The decline <str<strong>on</strong>g>of</str<strong>on</strong>g> C.<br />

amentacea, which thrives in <str<strong>on</strong>g>the</str<strong>on</strong>g> subtidal fringe under str<strong>on</strong>g surf exposure, has been<br />

related to polluti<strong>on</strong> (Bellan-Santini, 1966). The regressi<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> deeper Cystoseira forests<br />

(e.g. C. brachycarpa, C. spinosa and C. zosteroides) may be due to a cascade effect<br />

(sensu Steneck, 1998), though o<str<strong>on</strong>g>the</str<strong>on</strong>g>r causes may be involved (Sala et al., 1998): overfishing<br />

<str<strong>on</strong>g>of</str<strong>on</strong>g> sea-urchin predator fish (e.g. Sparus aurata) leads to a surge in numbers <str<strong>on</strong>g>of</str<strong>on</strong>g><br />

<str<strong>on</strong>g>the</str<strong>on</strong>g> browser Paracentrotus lividus, which in turn overgrazes benthic macrophytes,<br />

especially palatable and str<strong>on</strong>gly preferred (Verlaque and Nédélec, 1983; Lemée et al.,<br />

1996) Cystoseira species, which results in "barren grounds" with <strong>on</strong>ly encrusting<br />

corallines, ephemeral macrophytes and sea-urchins (Verlaque, 1987a; Sala et al., 1998;<br />

Boudouresque and Verlaque, 2001). O<str<strong>on</strong>g>the</str<strong>on</strong>g>r causes <str<strong>on</strong>g>of</str<strong>on</strong>g> more local significance can be put<br />

forward to explain <str<strong>on</strong>g>the</str<strong>on</strong>g> Cystoseira forest's decline, e.g. turbidity (which diminishes<br />

irradiance and <str<strong>on</strong>g>the</str<strong>on</strong>g>refore <str<strong>on</strong>g>the</str<strong>on</strong>g> compensati<strong>on</strong> depth), silting, gill nets and trawling.<br />

ACTES DU DEUXIEME SYMPOSIUM MEDITERRANEEN SUR LA VEGETATION MARINE (ATHENES, 12-13 DECEMBRE 2003)<br />

47

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