2006
DOI: 10.1016/j.envres.2006.03.001
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The present environmental scenario of the Nador Lagoon (Morocco)

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Cited by 103 publications
(44 citation statements)
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“…The spatial variation in sediment contaminant content seems to be driven also by variation in grain size distribution, which in the Stagnone follows a concentric pattern, with silt and clay more concentrated in the Centre of the basin (Vizzini 2000). As an example, in South, As content showed averaged values lower than the ranges reported for other Mediterranean lagoons (e.g., Nador lagoon-Morocco, Ruiz et al 2006), whereas in Centre, values were similar to those for contaminated lagoons (e.g., central part of Venice lagoon-Italy, Bellucci et al 2002). Moreover, As, Cd, and THg showed values approaching or exceeding the Italian regulatory limits (Gazzetta Ufficiale della Repubblica Italiana D.M.…”
Section: Trace Elementsmentioning
confidence: 72%
“…The spatial variation in sediment contaminant content seems to be driven also by variation in grain size distribution, which in the Stagnone follows a concentric pattern, with silt and clay more concentrated in the Centre of the basin (Vizzini 2000). As an example, in South, As content showed averaged values lower than the ranges reported for other Mediterranean lagoons (e.g., Nador lagoon-Morocco, Ruiz et al 2006), whereas in Centre, values were similar to those for contaminated lagoons (e.g., central part of Venice lagoon-Italy, Bellucci et al 2002). Moreover, As, Cd, and THg showed values approaching or exceeding the Italian regulatory limits (Gazzetta Ufficiale della Repubblica Italiana D.M.…”
Section: Trace Elementsmentioning
confidence: 72%
“…This implies a lack or depletion of meiofauna (Bodergat et al 2002;Ruiz et al 2006) because only a few ostracod species can adapt to such conditions (Ruiz et al 2005).…”
Section: Discussionmentioning
confidence: 99%
“…• The marine waters passing through the artifi cial inlet, which are always dominant; • The hydrogeological contributions from two aquifersGareb, located in southern Selouane, and Bou Areg, situated near the southern margin of the lagoon; and • The surface water inputs, with periodic fl ows of 10 small streams (''oueds'') (Ruiz et al 2006). In the lagoon, these individual infl ows are managed by internal currents, which have a clockwise direction from the artifi cial inlet toward the NW coast, moving about the internal face of the sandy spit and the internal lagoon margin (Guelorget et al 1987).…”
Section: Methodsmentioning
confidence: 99%