Particle fluxes in the Almeria-Oran Front: control by coastal upwelling and sea surface circulation

• Published in: Journal of marine systems Vol. 52; no. 1; pp. 89 - 106
• Main Authors: Sanchez-Vidal, A., Calafat, A., Canals, M., Fabres, J.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.12.2004
• Subjects: Almeria-Oran Front; Marine; Mediterranean Sea; Organic carbon; Particle fluxes; Satellite imagery; Sediment traps; MED, Alboran Sea, Almeria-Oran Front; MED, Alboran Sea; MED, Western Mediterranean; Satellite imagery; Organic carbon; Particle fluxes; Sediment traps; Mediterranean Sea; Almeria-Oran Front
• ISSN: 0924-7963; 1879-1573
• DOI: 10.1016/j.jmarsys.2004.01.010

Particle flux data were obtained from one instrumented array moored under the direct influence of the Almeria-Oran Front (AOF) in the Eastern Alboran Sea, Western Mediterranean Sea, within the frame of the “Mediterranean Targeted Project II-MAss Transfer and Ecosystem Response” (MTPII-MATER) EU-funded research project. The mooring line was deployed from July 1997 to May 1998, and was equipped with three sequential sampling sediment trap-current meter pairs at 645, 1170 and 2210 m (30 m above the seafloor). The settling material was analysed to obtain total mass, organic carbon, opal, calcium carbonate and lithogenic fluxes. Qualitative analyses of SST and SeaWiFS images allowed monitoring the location and development of the Western and Eastern Alboran Sea gyres and associated frontal systems to determine their influence on particle fluxes. Particle flux time series obtained at the three depths showed a downward decrease of the time-weighed total mass flux annual means, thus illustrating the role of pelagic particle settling. The total mass flux was dominated by the lithogenic fraction followed by calcium carbonate, opal and organic carbon. The time series at the various depths were rather similar, with two strong synchronous biogenic peaks (up to 98 mg m −2 day −1 of organic carbon and 156 mg m −2 day −1 of opal) recorded in July 1997 and May 1998. Through comparing the fluctuations of the lithogenic and calcium carbonate-rich fluxes with the biogenic flux, we observed that the non-biogenic fluxes remained roughly constant, while the biogenic flux responded strongly to seasonal variations throughout the water column. Overall, the temporal variability of particle fluxes appeared to be linked to the evolution of several tens of kilometres in length sea surface hydrological structures and circulation of the Alboran Sea. Periodic southeastward advective displacements of waters from upwelling events off the southern Spanish coast were observed on SST and SeaWiFS images. In between these periods, widespread phytoplankton blooms were observed. The influence of the varying surface structures resulted in changes in the biogenic particle flux. For example, we observed an opal pulse in April 1998 that resulted from a diatom-rich highly productive frontal surface situation above the mooring line. Estimation of the annual organic carbon export and calculation of a seasonality index indicate that the overall dynamics of the carbon reservoir within the Eastern Alboran Sea appears to be strongly influenced by the sea surface hydrological structures.