<p>The deep basin and continental shelf of the Gulf of Lion (North Western Mediterranean) are known for the formation of dense water in wintertime by the action of N-NW continental winds. This dense water is formed both offshore and at the coast. The area of Cap de Creus and its adjacent canyon is the main zone where dense coastal water is exported. Dense water dynamics on the continental shelf are also influenced by E-SE storms. Transfers of organic, inorganic, particulate and dissolved matter from the surface to the deep basin and from the shelf towards the slope by these physical processes can influence the redistribution of chemical elements in sediments, as well as the structure and functioning of benthic and pelagic ecosystems. The CASCADE cruise aimed to determine the characteristics of these two physical mechanisms and their numerous impacts, as well as monitoring changes in the hydrology, dynamics, sedimentology and biogeochemistry of water bodies. We propose a qualitative and quantitative estimate of particulate and dissolved, organic and inorganic matter fluxes exported towards the slope and the deep basin by these mechanisms.</p>
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The objective is to achieve a significant improvement in markers of palaeoclimate, athorough study of the ecology of these ecosystems in ogan current Gulf of Biscay, in combination with modeling
Comprehensive analysis of the marine ecosystem of the Strait of Gibraltar: physical forcing and trophic levels.
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Fate of the northwestern Mediterranean open sea spring bloom
Biodiversity and ecosystem functioning in contrasting southern European deep-sea environments: from virases to megafauna
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Weather Ocean Report
Benthopelagic ecosystem structure in the western Mediterranean: a multidisciplinary approach and different time scales in the Balearic Islands.