Photosynthetic acquisition of inorganic carbon was studied in the brown seaweed Endarachne binghamiae J. Agardh. Photosynthesis was saturated at 245 mmol photons m À2 s À1 and photoinhibition did not occur at an irradiance as high as 750 mmol photons m À2 s À1 . The dependence of O 2 evolution on inorganic carbon (Ci) concentration demonstrated that the normal Ci composition in natural seawater was not saturating for irradiance-saturated photosynthesis. Three lines of evidence demonstrated that E. binghamiae was able to acquire HCO À 3 as a source of Ci for photosynthesis: (i) the high value of photosynthetic conductance for CO 2 (220.6 mm s À1 ); (ii) the high pH compensation point of 9.7; and (iii) the measured photosynthetic rates being in excess of the theoretical maximum rates supported solely by the CO 2 supply from the spontaneous dehydration of HCO À 3 in the bulk seawater. In order to establish the mechanism of Ci acquisition, specific inhibitors and a proton buffer were applied to examine their inhibitory effects on photosynthesis. No inhibitory effects were found for the proton buffer tris(hydroxymethyl)aminomethane and the anion exchanger inhibitor, 4,4 0 -diisothiocyano-stilbene-2,2 0 -disulphonate. By contrast, photosynthetic O 2 evolution in natural seawater was significantly depressed by the extracellular carbonic anhydrase (CA) activity inhibitor, acetazolamide, and the plasma membrane P-type H þ -ATPase inhibitor, vanadate.These results suggested that carbon acquisition from the natural seawater was mostly through the external CA-mediated HCO À 3 dehydration mechanism, and that P-type H þ -ATPase (proton pump) in the plasma membrane simultaneously functioned in photosynthesis of E. binghamiae. Additional experiments on the O 2 exchange versus pH value relationship indicated that, in contrast to photosynthesis, dark respiration of E. binghamiae was insensitive to the change of pH in the seawater, which resulted in a decreasing instantaneous balance between net carbon gain and respiratory carbon loss at high pH values in seawater.