Impacts of high-nitrate freshwater inputs on macrotidal ecosystems. II. Specific role of the silicic acid pump in the year-round dominance of diatoms in the Bay of Brest (France)

Abstract

To assess the consequences of very-high-nitrate freshwater ~n p u t s on phytoplankton cornmunity structure a complete 1993-1994 annual c ~c l e is descnbed for the Bay of Brest (France). In contrast to other nitrate-enriched coastal ecosystcnis where small and non-siliceous species dominate in summer. In this well-mixed macrotidal ecosyst6:m diatoms > l 0 pm dominated bloom successions in surface waters from March to September 1993. Follov ing a small bloom of Skeletonema costaturn in March, an intensive spring bloom (biogenic sillca, BSi = 1.8 to 2 pm01 Si I-') observed in April-May (first dominated by Thalassiosira spp. and then by Rhliosolenja spp. by late May) collapsed due to Si Ilm~tation. Although dinoflagellates developed during the decline of this spring bloom and remained abundant until late September, a new diatom-dominated population (Chaetoceros spp.) developed from the end of May untll late September (BSI decreased from about 1 to 0.5 pm01 Si I-'). Finally, at the end of the productive per~od (September), a bloom dominated, by the c10 pm size class, essentially due to cryptophyceans, occurred. On an annual basis, the > l 0 pm size class accounted for 73 to 74 O/o of the time-weighted averages of chlorophyll a, of primary production, and of biogenic silica in surface waters. Finally, there is no evidence that the phytoplankton community structure of the Bay of Brest was dramatically affected by nitrate enrichment, either in terms of size structure or of diatom abundance relat~ve to dinoflagellates (although the emergence of some undesirable species among the dinoflagellates was observed). A silicic acid (i.e. silicate) pump, specific to well-mixed coastal ecosystems, is inferred to explain the dominance of diatoms during the periods following the spring bloom. It provldes a mechanism that prevents silicon loss out of the system by trapping it at the shallow watersediment interface at the end of thv spring bloom The tidally induced vertical mixing allows silicic acid from biogenic silica dissolution to become readily available for new diatom developments in surface waters.