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Vous êtes ici : Accueil / Bibliographie générale / Coastal upwelling in the Canary Island region: spatial variability reflected by the surface sediment diatom record

Sílvia Nave, Pedro Freitas, and Fátima Abrantes (2001)

Coastal upwelling in the Canary Island region: spatial variability reflected by the surface sediment diatom record

Marine Micropaleontology, 42(1-2):1-23.

Modern diatom and Corg distribution patterns were investigated in 39 surface sediment samples of the Canary region in order to quantitatively determine the influence of coastal upwelling and Saharan dust on the flux of these sedimentary components.br/High diatom abundance in surface sediments (2×106 valves g-1 dry sediment) as well as the dominance of the assemblages by spores of Chaetoceros, which is a genus related to upwelling conditions, reflect the stronger coastal upwelling conditions occurring at Cape Ghir off the NW African coast. Further offshore, total diatom abundance decreases one order of magnitude (±1×105 valves g-1 dry sediment) and the assemblages are dominated by oceanic species of the genus Nitzschia and fresh water diatoms, mainly the genera Aulacoseira, which is known to be a component of Saharan dust. This association suggest that offshore diatom concentrations may be generated by dust input from desert regions.br/Even though the sediments are expected to preserve only a mixed and averaged oceanographic signal, characteristic biogeographic patterns of a phytoplankton community occurring across a gradient of turbulence and nutrient availability, are recorded in surface sediments off Cape Ghir. This is seen in the subsequent maximum abundances of the genera Thalassiosira, Chaetoceros and Rhizosolenia.

diatoms, NW Africa, surface sediments, dust input, Upwelling, phytoplankton succession, Canary Islands

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