1. High-frequency fluxes of labile compounds in the central Ligurian Sea, northwestern Mediterranean
- Author
-
Goutx, M., Momzikoff, A., Striby, L., Andersen, V., Marty, J.C, and Vescovali, I.
- Subjects
Proteins ,Lipids ,Sedimentation ,Earth sciences - Abstract
To link to full-text access for this article, visit this link: http://dx.doi.org/10.1016/S0967-0637(99)00101-6 Byline: M Goutx, A Momzikoff, L Striby, V Andersen, J.C Marty, I Vescovali Keywords: Particle fluxes; High-frequency sampling; Particulate organic carbon; Proteins; Lipid classes; Northwestern Mediterranean Abstract: Sinking particles were collected every 4h with drifting sediment traps deployed at 200m depth in May 1995 in a 1-D vertical system during the DYNAPROC observations in the northwestern Mediterranean sea. POC, proteins, glucosamine and lipid classes were used as indicators of the intensity and quality of the particle flux. The roles of day/night cycle and wind on the particle flux were examined. The transient regime of production from late spring bloom to pre-oligotrophy determined the flux intensity and quality. POC fluxes decreased from, on average, 34 to 11 mg m.sup.-2 d.sup.-1, representing 6-14% of the primary production under late spring bloom conditions to 1-2% under pre-oligotrophic conditions. Total protein and chloroplast lipid fluxes correlated with POC and reflected the input of algal biomass into the traps. As the season proceeded, changes in the biochemical composition of the exported material were observed. The C/N ratio rose from 7.8 to 12. Increases of serine (10-28% of total proteins), total lipids (7-9 to 14-28% of POC) and reserve lipids (1-5 to 5-22% of total lipids) were noticeable, whereas total protein content in POC decreased (20-27 to 18-7%). N-acetyl glucosamine, a tracer of fecal pellet flux, showed that zooplankton grazing was a major vector of downward export during the decaying bloom. Against this background pattern, episodic events specifically increased the flux, modifying the quality and the settling velocity of particles. Day/night signals in biotracers (POC, N-acetyl glucosamine, protein and chloroplast lipids) showed that zooplankton migrations were responsible for sedimentation of fresh material through fast sinking particles (V=170-180md.sup.-1) at night. Periodic signatures of re-processed material (high lipolysis and bacterial biomass indices) suggested that other zooplankton fecal pellets or small aggregates, probably of lower settling velocities (V Article History: Received 6 October 1997; Revised 3 March 1999; Accepted 25 June 1999
- Published
- 2000