A Time-Resolved Iron-Specific X-ray Absorption Experiment Yields No Evidence for an Fe2+ Fe3+ Transition durin
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文摘
Previous time-resolved FTIR measurements suggested the involvement of an intermediarycomponent in the electron transfer step QA- QB in the photosynthetic reaction center (RC) fromRhodobacter sphaeroides [Remy and Gerwert (2003) Nat. Struct. Biol. 10, 637]. By a kinetic X-rayabsorption experiment at the Fe K-edge we investigated whether oxidation occurs at the ferric non-hemeiron located between the two quinones. In isolated reaction centers with a high content of functional QB,at a time resolution of 30 s and at room temperature, no evidence for transient oxidation of Fe wasobtained. However, small X-ray transients occurred, in a similar micro- to millisecond time range as inthe IR experiments, which may point to changes in the Fe ligand environment due to the charges on QA-and QB-. In addition, VIS measurements agree with the IR data and do not exclude an intermediate in theQA- QB transition.

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