Absence of a bicarbonate-depletion effect in electron transfer between quinones in chromatophores and reaction centers of Rhodobacter sphaeroides.

Higher plants, algae, and cyanobacteria are known to require bicarbonate ions for electron flow from the first stable electron acceptor quinone QA to the second electron acceptor quinone QB, and to the intersystem quinone pool. It has been suggested that in Photosystem II of oxygenic photosynthesis, bicarbonate ion functions to maintain the reaction center in a proper conformation and, perhaps, to provide the protons needed to stabilize the semiquinone (QB-). In this paper, we show that bicarbonate ions do not influence the electron flow, from the quinone QA to QB and beyond, in the photosynthetic bacterium Rhodobacter sphaeroides. No measurable effect of bicarbonate depletion, obtained by competition with formate, was observed on cytochrome b-561 reduction in chromatophores; on the flash-dependent oscillation of semiquinone formation in reaction centers; on electron transfer from QA- to QB; or on either the fast or slow recovery of the oxidized primary donor (P+) which reflects the P+QA- ----PQA or the P+QB- ----PQB reaction. The lack of an observed effect in Rhodobacter sphaeroides in contrast to the effect seen in Photosystem II is suggested to be due to the amino-acid sequence differences between the reaction centers of the two systems.