Mobile hydrogen carbonate acts as proton acceptor in photosynthetic water oxidation

Cyanobacteria, algae, and plants oxidize water to the O₂ we breathe, and consume CO₂ during the synthesis of biomass. Although these vital processes are functionally and structurally well separated in photosynthetic organisms, there is a long-debated role for CO₂/ in water oxidation. Using membrane-inlet mass spectrometry we demonstrate that acts as a mobile proton acceptor that helps to transport the protons produced inside of photosystem II by water oxidation out into the chloroplast’s lumen, resulting in a light-driven production of O₂ and CO₂. Depletion of from the media leads, in the absence of added buffers, to a reversible down-regulation of O₂ production by about 20%. These findings add a previously unidentified component to the regulatory network of oxygenic photosynthesis and conclude the more than 50-y-long quest for the function of CO₂/ in photosynthetic water oxidation.Oxygenic photosynthesis in cyanobacteria, algae, and higher plants leads to the reduction of atmospheric CO₂ to energy-rich carbohydrates. The electrons needed for this process are extracted in a cyclic, light-driven process from water that is split into dioxygen (O₂) and protons. This reaction is catalyzed by a penta-µ-oxo bridged tetra-manganese calcium cluster (Mn₄CaO₅) within the oxygen-evolving complex (OEC) of photosystem II (PSII) (1–4). The possible roles of inorganic carbon, , in this process have been a controversial issue ever since Otto Warburg and Günter Krippahl (5) reported in 1958 that oxygen evolution by PSII strictly depends on CO₂ and therefore has to be based on the photolysis of H₂CO₃ (“Kohlensäure”) and not of water. These first experiments were indirect and, as became apparent later, were wrongly interpreted (6–8). Several research groups followed up on these initial results and identified two possible sites of C_i interaction within PSII (reviewed in refs. 9–12). Functional and spectroscopic studies showed that facilitates the reduction of the secondary plastoquinone electron acceptor (Q_B) of PSII by participating in the protonation of . Binding of (or ) to the nonheme Fe between the quinones Q_A and Q_B was recently confirmed by X-ray crystallography (3, 13, 14). Despite this functional role at the acceptor side, the very tight binding of to this site makes it impossible for the activity of PSII to be affected by changing the C_i level of the medium; instead inhibitors such as formate need to be added to induce the acceptor-side effect (15). Consequently, the water-splitting electron-donor side of PSII has also been studied intensively (for recent reviews, see refs. 11 and 12). Although a tight binding of C_i near the Mn₄CaO₅ cluster is excluded on the basis of X-ray crystallography (3, 14), FTIR spectroscopy (16), and mass spectrometry (17, 18), the possibility that a weakly bound affects the activity of PSII at the donor side remains a viable option (reviewed in refs. 10 and 19).In the present study using higher plant PSII membranes, we specifically evaluate a recently suggested role of weakly bound , namely, that it acts as an acceptor for, and transporter of, protons produced by water splitting in the OEC (20–22).