REGULATION OF ALGAL BLOOMS IN ANTARCTIC SHELF WATERS BY THE RELEASE OF IRON FROM MELTING SEA-ICE

During summer 1995-96, we measured iron in the water column and conduc ted iron-enrichment bottle-incubation experiments at a station in the central Ross Sea (76 degrees 30'S, 170 degrees 40'W), first, in the pr esence of melting sea ice, and 17 days later, in ice-free conditions. We observed a striking temporal change in mixed-layer dissolved iron c oncentrations at this station, from 0.72-2.3 nM with sea ice present, to 0.16-0.17 nM in ice-free conditions. These changes were accompanied by a significant drawdown in macronutrients and an approximate doubli ng of algal (diatom) biomass. Our incubation experiments suggest that conditions were iron-replete in the presence of sea ice, and iron-defi cient in the absence of sea ice. We surmise that bioavailable iron was released into seawater from the melting sea ice, stimulating phytopla nkton production and the biological removal of dissolved iron from the mixed layer, until iron-limited conditions developed. These observati ons suggest that the episodic release of bioavailable iron from meltin g sea ice is an important factor regulating phytoplankton production, particularly ice-edge blooms, in seasonally ice-covered Antarctic wate rs.