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SHORT-TERM VARIATIONS OF SESTON CHARACTERISTICS EFFECT OF WIND-INDUCED RESUSPENSION IN A SHALLOW TROPICAL LAGOON:

Marcel L. Bouvy, Daniel Guiral

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Abstract

In January 1993, a 24 hour survey based on an hourly sampling was conducted in a station (1 m depth) located in the Ebrie lagoon, Cote d'Ivoire, in order to determine short-term changes in seston quality and quantity and relate them to physical conditions. Water samples were collected just below the surface and at 0.9 m depth to assess the seston distribution in the water column. Located in an estuarine environment, the study site was submitted to periodic effect of tides with low currents. Under certain conditions, sediment resuspension by wind-induced waves was observed in the shallow parts of this ecosystem. From the analysis of hydrodynamic processes (tide, wind and sedimentation rates), four basic situations were distinguished in the course of the study: a period with no wind and high sedimentation rates, a period characterized by wind-induced resuspension, followed by a period of sedimentation and finally, a period without wind during the second flood tide. The particle size spectra were similar throughout the study, the distributions being unimodal (mode of 4 pm diameter). The finer particles (40 um) were resuspended over the whple water column at the beginning of the resuspension period, whereas the larger particles were resuspended if . the wind speed exceeded 3 m s-1. Phytoplankton species were found to provide information on the physical factors controlling the pelagic system: small cells, such as those of cyanobacteria (Synechococcus sp.), were always present over the whole tidal cycles, whereas large motile cells were predominant in the water column during the resuspension period. The seston characteristics of this part of Ebrie lagoon are mainly controlled by tidal currents, but wind-induced resuspension can modify the structure of the pelagic food web.

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What this paper is about

In January 1993, a 24 hour survey based on an hourly sampling was conducted in a station (1 m depth) located in the Ebrie lagoon, Cote d'Ivoire, in order to determine short-term changes in seston quality and quantity and relate them to physical conditions. Water samples were collected just below the surface and at 0.9 m depth to assess the seston distribution in the water column. Located in an estuarine environment, the study site was submitted to periodic effect of tides with low currents. Under certain conditions, sediment resuspension by wind-induced waves was observed in the shallow parts of this ecosystem. From the analysis of hydrodynamic processes (tide, wind and sedimentation rates), four basic situations were distinguished in the course of the study: a period with no wind and high sedimentation rates, a period characterized by wind-induced resuspension, followed by a period of sedimentation and finally, a period without wind during the second flood tide. The particle size spectra were similar throughout the study, the distributions being unimodal (mode of 4 pm diameter). The finer particles (40 um) were resuspended over the whple water column at the beginning of the resuspension period, whereas the larger particles were resuspended if . the wind speed exceeded 3 m s-1. Phytoplankton species were found to provide information on the physical factors controlling the pelagic system: small cells, such as those of cyanobacteria (Synechococcus sp.), were always present over the whole tidal cycles, whereas large motile cells were predominant in the water column during the resuspension period. The seston characteristics of this part of Ebrie lagoon are mainly controlled by tidal currents, but wind-induced resuspension can modify the structure of the pelagic food web.

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Available abstract

In January 1993, a 24 hour survey based on an hourly sampling was conducted in a station (1 m depth) located in the Ebrie lagoon, Cote d'Ivoire, in order to determine short-term changes in seston quality and quantity and relate them to physical conditions. Water samples were collected just below the surface and at 0.9 m depth to assess the seston distribution in the water column. Located in an estuarine environment, the study site was submitted to periodic effect of tides with low currents. Under certain conditions, sediment resuspension by wind-induced waves was observed in the shallow parts of this ecosystem. From the analysis of hydrodynamic processes (tide, wind and sedimentation rates), four basic situations were distinguished in the course of the study: a period with no wind and high sedimentation rates, a period characterized by wind-induced resuspension, followed by a period of sedimentation and finally, a period without wind during the second flood tide. The particle size spectra were similar throughout the study, the distributions being unimodal (mode of 4 pm diameter). The finer particles (40 um) were resuspended over the whple water column at the beginning of the resuspension period, whereas the larger particles were resuspended if . the wind speed exceeded 3 m s-1. Phytoplankton species were found to provide information on the physical factors controlling the pelagic system: small cells, such as those of cyanobacteria (Synechococcus sp.), were always present over the whole tidal cycles, whereas large motile cells were predominant in the water column during the resuspension period. The seston characteristics of this part of Ebrie lagoon are mainly controlled by tidal currents, but wind-induced resuspension can modify the structure of the pelagic food web.

Key concepts: Seston, Water column, Environmental science, Phytoplankton, Sedimentation, Oceanography, Pelagic zone, Sediment

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