Hughes H.J., Sondag Francis, Cocquyt C., Laraque Alain, Pandi A., André L., Cardinal D. (2011). Effect of seasonal biogenic silica variations on dissolved silicon fluxes and isotopic signatures in the Congo River. Limnology and Oceanography, 56 (2), p. 551-561. ISSN 0024-3590.
Titre du document
Effect of seasonal biogenic silica variations on dissolved silicon fluxes and isotopic signatures in the Congo River
Hughes H.J., Sondag Francis, Cocquyt C., Laraque Alain, Pandi A., André L., Cardinal D.
Source
Limnology and Oceanography, 2011,
56 (2), p. 551-561 ISSN 0024-3590
We report 2 yr of monthly data from the Congo River (the second largest river in the world) on dissolved silicon concentrations, biogenic silica particle concentrations, isotopic signatures of dissolved silicon, and biogenic siliceous particle counts. Diatoms predominated in the biogenic silica fraction, especially during low flow; phytoliths and sponge spicules were more abundant than diatoms only during the rainy season, when biogenic silica fluxes are low. Biological processes dominated the seasonal variations of the dissolved delta Si-30 ratio that are superimposed on a constant abiotic delta Si-30 value of +0.70 parts per thousand +/- 0.05 parts per thousand throughout the year. The measured biogenic silica concentration is less than the amount required to explain the monthly variations of dissolved delta Si-30 signatures. We use these signatures and a Rayleigh isotopic fractionation model to calculate that 82% +/- 7% of the diatoms produced each month would be exported out of the water column, probably through settling in the Malebo Pool or further upstream. The uptake of dissolved silicon by diatoms during low water flow periods could explain the absence of the dilution effect observed for the other major elements. Annual Si export to the estuary is 1.17 x 10(10) mol yr(-1) in the form of biogenic silica and 2.23 x 10(11) mol yr(-1) in dissolved Si form, with a mean dissolved delta Si-30 of +0.96 parts per thousand +/- 0.27 parts per thousand. Phytoliths make only a minor contribution to the annual biogenic silica flux, and dissolved Si fluxes predominate over biogenic Si fluxes.
