Abstract
Silicate depletion was observed during a bloom of netplankton diatoms. Netplankton chlorophyll a increased over the same salinity range and at the same rate that silicate decreased. Silicate depletion coincided with a decrease in the apparent Si:N uptake ratio as well as a change in the magnitude and diurnal phasing of light saturated photosynthesis (P Bm ) by netplankton diatoms. Nanoplankton P Bm was unaffected by silicate depletion and increased with temperature. Consequently, nanoplankton P Bm eventually exceeded netplankton P Bm while netplankton biomass was still increasing relative to nanoplankton biomass.
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Communicated by I. Morris, West Boothbay Harbor
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Malone, T.C., Garside, C. & Neale, P.J. Effects of silicate depletion on photosynthesis by diatoms in the plume of the Hudson River. Marine Biology 58, 197–204 (1980). https://doi.org/10.1007/BF00391876
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DOI: https://doi.org/10.1007/BF00391876