The primary photochemistry of Fe-depleted and Zn-reconstituted reaction centers from Rhodopseudomonas sphaeroides R-26.1 was studied by transient absorption spectroscopy and compared with native, Fe2+-containing reaction centers. Excitation of metal-free reaction centers with 30-ps flashes produced the initial charge-separated state P+I-(P+BPh-, where P is the primary donor and BPh is bacteriopheophytin) with a yield and visible/near-infrared absorption difference spectrum indistinguishable from that observed in native reaction centers. However, the lifetime of P+I-was found to increase approximately 20-fold to 4.2 ± 0.3 ns (compared to 205 ps in native reaction centers), and the yield of formation of the subsequent state P+Q-(QA is the primary quinone acceptor) was reduced to 47 ± 5% (compared to essentially 100% in native reaction centers). The remaining 53% of the metal-free reaction centers were found to undergo charge recombination during the P+I-lifetime to yield both the ground state (28 ± 5%) and the triplet state PR (25 ± 5%). Reconstitution of Fe-depleted reaction centers with Zn2+ restored the "native" photochemistry. Possible mechanisms responsible for the reduced decay rate of P'l-in metal-free reaction centers are discussed.The reaction center (RC) from the photosynthetic bacterium Rhodopseudomonas sphaeroides is a membrane-spanning protein complex consisting of three polypeptides containing four bacteriochlorophyll molecules, two bacteriopheophytin (BPh) molecules, two ubiquinone molecules (QA and QB), and one high-spin Fe2" atom (1). Of the six tetrapyrrole pigments present, only three have been definitively shown to play a role in the photochemistry of the RC. Two bacteriochlorophyll molecules form a dimer (2-4), P (the primary donor), which is rapidly oxidized after absorption of a photon to produce P+ with an electron appearing on a BPh within about 4 ps (5, 6), thus forming the transient state P+BPh-(often denoted P+I-) (7-9). An electron is transferred from BPh-to the primary ubiquinone (QA) with a time constant of about 200 ps at 295 K, yielding the long-lived state P+QA (7)(8)(9)(10) "150-,us electron-transfer kinetics from QA to QB. They further reported that the yield of P+Q-formation after a saturating 400-ns flash was significantly reduced [from 102 ± 4% in native RCs (14)], with a concomitant formation of the triplet state, pR. The 100% yield of P+Q-was also restored by incorporation of any of the above-mentioned divalent metals.In this work we address the question of the role ofthe metal ion in the primary photochemistry, in particular in the formation and decay of state P+I-after a single turnover light flash. Transient optical spectra and kinetics were obtained with picosecond time resolution on native, Fe-depleted, and Zn-reconstituted RCs. From these and additional kinetic measurements made on a longer time scale, the yields of the different decay pathways of P+I-(to pR, to the ground state, and to P+Q-) were determined. A preliminary account of this work has been given (...