CO 2 entry into Synechococcus sp. PCC7942 cells was drastically inhibited by the water channel blocker pchloromercuriphenylsulfonic acid suggesting that CO 2 uptake is, for the most part, passive via aquaporins with subsequent energy-dependent conversion to HCO 3 ؊ . Dependence of CO 2 uptake on photosynthetic electron transport via photosystem I (PSI) was confirmed by experiments with electron transport inhibitors, electron donors and acceptors, and a mutant lacking PSI activity. CO 2 uptake was drastically inhibited by the uncouplers carbonyl cyanide m-chlorophenylhydrazone (CCCP) and ammonia but substantially less so by the inhibitors of ATP formation arsenate and N, N,-dicyclohexylcarbodiimide (DCCD). Thus a ⌬H ؉ generated by photosynthetic PSI electron transport apparently serves as the direct source of energy for CO 2 uptake. Under low light intensity, the rate of CO 2 uptake by a high-CO 2 -requiring mutant of Synechococcus sp. PCC7942, at a CO 2 concentration below its threshold for CO 2 fixation, was higher than that of the wild type. At saturating light intensity, net CO 2 uptake was similar in the wild type and in the mutant IL-3 suggesting common limitation by the rate of conversion of CO 2 to HCO 3 ؊ . These findings are consistent with a model postulating that electron transport-dependent formation of alkaline domains on the thylakoid membrane energizes intracellular conversion of CO 2 to HCO 3 ؊ .On illumination, many photosynthetic microorganisms maintain the concentration of dissolved CO 2 ([CO 2(dis) ]) in their surrounding medium below that expected at chemical equilibrium with HCO 3 Ϫ (1-5). This displacement of [CO 2(dis) ] from equilibrium can be observed in the absence of CO 2 fixation and is largely due to CO 2 uptake, intracellular conversion to HCO 3 Ϫ , and release of the latter into the medium (5, 6). The reverse phenomenon has been described in Synechococcus WH 7803 (7) and Nannochloropsis sp. (8, 9) where HCO 3 Ϫ uptake, internal conversion to CO 2 , and efflux of the latter result in elevated [CO 2(dis) ] in the medium. HCO 3 Ϫ transport systems, in Cyanobacteria, are probably located at the cytoplasmic membrane and are believed to be driven by ATP either directly (10) or possibly indirectly (11-13). CO 2 uptake has been observed to result in HCO 3 Ϫ accumulation in the cytoplasm where [CO 2(dis) ] is maintained below that expected at chemical equilibrium, and it has been inferred that a CA 1 -like activity is involved in its uptake and intracellular conversion to HCO 3 Ϫ (6, 14 -17). The location of the CAlike activity has not been identified and the mode of energization of the active HCO 3 Ϫ accumulation is not understood. Active transport of CO 2 across the plasmalemma has also been suggested (5, 18), but it is difficult to distinguish this from diffusion of CO 2 across the plasma membrane with subsequent energy-dependent conversion to HCO 3 Ϫ (6, 19). Passive entry of CO 2 across the membrane may occur via aquaporins (20), a possibility examined here by the application of a ...