Hydroclimatic modulation of diatom/Phaeocystis blooms in nutrient-enriched Belgian coastal waters (North Sea)

Breton, E.; Rousseau, V.; Parent, J.-Y.; Ozer, J.; Lancelot, C.

doi:/10.4319/lo.2006.51.3.1401

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Hydroclimatic modulation of diatom/Phaeocystis blooms in nutrient-enriched Belgian coastal waters (North Sea)

Breton, E.; Rousseau, V.; Parent, J.-Y.; Ozer, J.; Lancelot, C. (2006). Hydroclimatic modulation of diatom/Phaeocystis blooms in nutrient-enriched Belgian coastal waters (North Sea). Limnol. Oceanogr. 51(3): 1401-1409. dx.doi.org/10.4319/lo.2006.51.3.1401

In: Limnology and Oceanography. American Society of Limnology and Oceanography: Waco, Tex., etc. ISSN 0024-3590; e-ISSN 1939-5590

Available in	Authors
VLIZ: Open Marine Archive 134084 [ download pdf ]

Keywords

Algae > Diatoms
Algal blooms
AN, North Atlantic
ANE, North Sea, Southern Bight
Aquatic communities > Plankton > Phytoplankton
Belgium, Schelde R.
Coastal zone
Nitrate cycle
Water bodies > Coastal waters
Bacillariophyceae [WoRMS]; Phaeocystis Lagerheim, 1893 [WoRMS]
Belgian Coast [Marine Regions]; North Atlantic Ocean [Marine Regions]; Schelde [Marine Regions]; Southern Bight [Marine Regions]
Marine/Coastal

Authors		Top
Breton, E. Rousseau, V. Parent, J.-Y.	Ozer, J. Lancelot, C.

Abstract

Statistical analysis of 14 yr (1988-2001) of intensive phytoplankton monitoring at Station 330 in the central Belgian Coastal Zone (BCZ, Southern Bight of the North Sea) indicates that the long-term diatom biomass trend and the spring dominance of Phaeocystis colonies over diatoms are determined by the combined effect of the North Atlantic Oscillation (NAO) and freshwater and continental nitrate carried by the Scheldt. The strong correlation between diatoms and the NAO index is largely explained by the modulating effect of the latter on the water budget at the monitoring station. The relationship between Phaeocystis spring blooms and winter NAO (NAO_w) is indirect, better expressed by springtime Phaeocystis dominance over diatoms because of the higher response of the latter to the NAO. The spring Phaeocystis : diatom bloom ratio is negatively (or positively) linked to positive (or negative) NAO_w values. A complex cascade of events links large-scale NAO index variations with those local meteorological conditions (wind strength and direction, rainfall) that drive the hydrography and water budget of the BCZ. Local meteorological conditions in turn modulate the geographical spread of Scheldt nutrient loads in the coastal zone and ultimately regulate the magnitude of Phaeocystis spring blooms by determining winter nitrate enrichment. Hence, the absence of a linear relationship between Phaeocystis spring blooms and NAO_w is explained by the nonlinear response of river-based nitrate pulses to NAO due to local wind-driven hydrodynamical forcing.

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