Temporal changes in the biochemical composition of particulate organic matter sedimentation in the Bay of Banyuls-sur-Mer

Citation
A. Gremare et al., Temporal changes in the biochemical composition of particulate organic matter sedimentation in the Bay of Banyuls-sur-Mer, OCEANOL ACT, 21(6), 1998, pp. 783-792
Citations number
31
Categorie Soggetti
Aquatic Sciences
Journal title
OCEANOLOGICA ACTA
ISSN journal
03991784 → ACNP
Volume
21
Issue
6
Year of publication
1998
Pages
783 - 792
Database
ISI
SICI code
0399-1784(199811/12)21:6<783:TCITBC>2.0.ZU;2-Z
Abstract
Gross sedimentation rates (GSRs) were monitored together with meteorologica l data and the main biochemical characteristics of the collected material ( i.e. organic content, C, N, total proteins, carbohydrates, lipids and avail able proteins) over a three year cycle at a shallow station (18 m) of the B ay of Banyuls, France. GSRs were between 0.26 (11/04/92) and 317.75 gDW m(- 2) d(-1) (18/02/94). They followed an annual cycle with low and relatively constant values during spring and summer and high, variable Values during f all and winter. During the study GSRs correlated poorly (state of the sea, precipitation) or even non-significantly (wind speed) with the main meteoro logical parameters. GSRs correlated negatively with the organic content of the material collected within the sediment traps suggesting the importance of resuspension in controlling GSRs. This hypothesis is consistent with the fact that, among all the measured biochemical parameters, available protei ns (i.e. enzymatically hydrolizable proteins) are the most negatively corre lated with GSRs. Available proteins showed important temporal changes that are only partly described by changes in carbon and nitrogen contents. These results are discussed in relation to the conceptualisation and the modelli ng of benthic trophic networks. The major objectives of our research group within the framework of the second phase of the French "Programme National d'Oceanographie Cotiere" are briefly discussed. (C) Elsevier, Paris.