| Volumes and Issues Contents of Issue 1 Special Issue |
www.biogeosciences-discuss.net/6/575/2009/
doi:10.5194/bgd-6-575-2009
© Author(s) 2009. This work is distributed
under the Creative Commons Attribution 3.0 License.
Short-term changes in particulate fluxes measured by drifting sediment traps during end summer oligotrophic regime in the NW Mediterranean Sea
1CNRS/INSU, Laboratoire d'Océanographie de Villefranche (UMR 7093), 06230 Villefranche-sur-Mer, France
2Université Pierre et Marie Curie-Paris 6, Laboratoire d'Océanographie de Villefranche, BP 8, 06238 Villefranche-sur-Mer CEDEX, France
3Laboratoire de Microbiologie, Géochimie et Ecologie Marines, Université de la Méditerranée; Centre d'Océanologie de Marseille, CNRS (UMR 6117), Campus de Luminy, case 901, 13288 Marseille Cedex 09, France
Abstract. Short-term changes in the flux of particulate matter were determined in the central north western Mediterranean Sea (near DYFAMED site) using drifting sediment traps at 200 m depth in the course of the DYNAPROC 2 cruise (14 September–17 October, 2004). In this period of marked water column stratification, POC fluxes varied by an order of magnitude, in the range of 0.03–0.29 mg C m−2 h−1 over the month and showed very rapid and high variations. Particulate carbon export represented less than 5% of integrated primary production, suggesting that phytoplankton production was essentially sustained by internal recycling of organic matter and retained within the photic zone. While PON and POP fluxes paralleled one another, the elemental ratios POC/PON and POC/POP, varied widely over short-term periods. Values were always higher than the conventional Redfield ratio indicating that the settling material was in part degraded. This was confirmed by the very low chlorophyll-a flux recorded in the traps (mean 0.017 μg m−2 h−1), the high phaeopigment and free lipid concentrations of the settling material, which all together indicated that the organic matter reaching 200 m depth was reworked (by grazing, fecal pellets production, degradation, . . .) and that algal sinking made a small contribution to the downward flux. Over time, the relative abundance of individual lipid classes in organic matter (OM) changed from glycolipids-dominated to neutral (wax esters, triglycerides) and phospholipids-dominated, suggesting ecosystem maturation as well as rapid and continual exchanges between dissolved, suspended and sinking pools. Our most striking result was documenting the rapid change in fluxes of the various measured parameters. In the situation encountered here, with dominant regenerated production, the effect of wind events was a decrease of fluxes (probably through reduction of grazing). But fluxes increased as soon as calm conditions settle.
Discussion Paper (PDF, 1088 KB) Interactive Discussion (Closed, 3 Comments) Final Revised Paper (BG)
Citation: Marty, J. C., Goutx, M., Guigue, C., Leblond, N., and Raimbault, P.: Short-term changes in particulate fluxes measured by drifting sediment traps during end summer oligotrophic regime in the NW Mediterranean Sea, Biogeosciences Discuss., 6, 575-606, doi:10.5194/bgd-6-575-2009, 2009. Bibtex EndNote Reference Manager XML
