Downward particle fluxes within different productivity regimes off the Mauritanian upwelling zone (EUMELI program) |
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| Institution: | 1. Université de Bordeaux, UMR CNRS 5805 EPOC, Bat 18, Allée Geoffroy Saint-Hilaire, 33615 Pessac, France;2. Laboratoire de Recherche sur les Transferts dans l''Environnement, Institut de Radioprotection et de Sûreté Nucléaire (IRSN), PRP-ENV/SERIS/LRTE, Centre de Cadarache, bat 159, 13115 St Paul lez durance, France;1. Dipartimento di Scienze Biologiche, Geologiche e Ambientali (BiGeA), University of Bologna, Piazza di Porta San Donato 1, Bologna, Italy;2. General and Analytical Chemistry, Montanuniversität Leoben, Franz-Josef-Str. 18, Leoben, Austria |
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| Abstract: | A 2-yr record of downward particle flux was obtained with moored sediment traps at several depths of the water column in two regions characterized by different primary production levels (mesotrophic and oligotrophic) of the eastern subtropical North Atlantic Ocean. Particle fluxes, of ～71–78% biogenic origin (i.e. consisting of CaCO3, organic matter and opal) on average, decrease about six-fold from the mesotrophic site (highest fluxes in the North Atlantic) nearer the Mauritanian margin (18°30′N, 21°00′W) to the remote, open-ocean, oligotrophic site (21°00′N, 31°00′W). This decrease largely reflects the difference in total primary production between the two sites, from ～260 to ～110 g organic C m?2 yr?1. At both sites, temporal variability of the downward particle flux seems to be linked to westward surface currents, which are likely to transport seaward biomass-rich water masses from regions nearer the coast. The influence of coastal upwelling is marked at the mesotrophic site. The large differences between the 1991 and 1992 records at that site, where carbon export is large, underscore the interest of long-term studies for export budget estimates. The different productivity regimes at the two sites seem to induce contrasting downward modes of transport of the particulate matter, as shown in particular by the faster settling rates and the higher E ratio (particulate organic carbon export versus total primary production) estimated at the mesotrophic site. |
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