The mechanism of inorganic carbon (C i ) acquisition by the economic brown macroalga, Hizikia fusiforme (Harv.) Okamura (Sargassaceae), was investigated to characterize its photosynthetic physiology. Both intracellular and extracellular carbonic anhydrase (CA) were detected, with the external CA activity accounting for about 5% of the total. Hizikia fusiforme showed higher rates of photosynthetic oxygen evolution at alkaline pH than those theoretically derived from the rates of uncatalyzed CO 2 production from bicarbonate and exhibited a high pH compensation point (pH 9.66). The external CA inhibitor, acetazolamide, significantly depressed the photosynthetic oxygen evolution, whereas the anion-exchanger inhibitor 4,4 0 -diisothiocyano-stilbene-2,2 0 -disulfonate had no inhibitory effect on it, implying the alga was capable of using HCO 3 À as a source of C i for its photosynthesis via the mediation of the external CA. CO 2 concentrations in the culture media affected its photosynthetic properties. A high level of CO 2 (10,000 ppmv) resulted in a decrease in the external CA activity; however, a low CO 2 level (20 ppmv) led to no changes in the external CA activity but raised the intracellular CA activity. Parallel to the reduction in the external CA activity at the high CO 2 was a reduction in the photosynthetic CO 2 affinity. Decreased activity of the external CA in the high CO 2 grown samples led to reduced sensitiveness of photosynthesis to the addition of acetazolamide at alkaline pH. It was clearly indicated that H. fusiforme, which showed CO 2 -limited photosynthesis with the half-saturating concentration of C i exceeding that of seawater, did not operate active HCO 3 À uptake but used it via the extracellular CA for its photosynthetic carbon fixation.Key index words: brown alga; carbonic anhydrase; CO 2 ; inorganic carbon; Hizikia fusiforme; marine macroalgae; photosynthesis Abbreviations: AZ, acetazolamide; CA, carbonic anhydrase; C i , inorganic carbon; DIDS, 4,4 0 -diisothiocyano-stilbene-2,2 0 -disulfonate; FW, fresh weightThe dissolved gaseous CO 2 , [CO 2 ] aq , is only about 12 mM, being less than 1% of HCO 3 À in the airequilibrated seawater (201 C, pH 8.2, salinity 35 psu). Photosynthesis of marine algae might be CO 2 -limited because it diffuses slowly in water, being about 7000 times slower than in air. The photosynthetic oxygen evolution rates of many marine macroalgae, however, have been found to be faster than the theoretical maximum rates of CO 2 supply from the uncatalyzed spontaneous dehydration of HCO 3