An isotope-edited FTIR investigation of the role of Ser-L223 in binding quinone (QB) and semiquinone (QB-) in the reaction center from Rhodobacter sphaeroides
- PMID: 16262252
- DOI: 10.1021/bi051328d
An isotope-edited FTIR investigation of the role of Ser-L223 in binding quinone (QB) and semiquinone (QB-) in the reaction center from Rhodobacter sphaeroides
Abstract
In the photosynthetic reaction center (RC) from the purple bacterium Rhodobacter sphaeroides, proton-coupled electron-transfer reactions occur at the secondary quinone (Q(B)) site. Several nearby residues are important for both binding and redox chemistry involved in the light-induced conversion from Q(B) to quinol Q(B)H(2). Ser-L223 is one of the functionally important residues located near Q(B). To obtain information on the interaction between Ser-L223 and Q(B) and Q(B)(-), isotope-edited Q(B)(-)/Q(B) FTIR difference spectra were measured in a mutant RC in which Ser-L223 is replaced with Ala and compared to the native RC. The isotope-edited IR fingerprint spectra for the C=O [see text] and C=C [see text] modes of Q(B) (Q(B)(-)) in the mutant are essentially the same as those of the native RC. These findings indicate that highly equivalent interactions of Q(B) and Q(B)(-) with the protein occur in both native and mutant RCs. The simplest explanation of these results is that Ser-L223 is not hydrogen bonded to Q(B) or Q(B)(-) but presumably forms a hydrogen bond to a nearby acid group, preferentially Asp-L213. The rotation of the Ser OH proton from Asp-L213 to Q(B)(-) is expected to be an important step in the proton transfer to the reduced quinone. In addition, the reduced quinone remains firmly bound, indicating that other distinct hydrogen bonds are more important for stabilizing Q(B)(-). Implications on the design features of the Q(B) binding site are discussed.
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