Manganese and the limits of high potential phototrophy

Photosynthetic reaction centers create high-energy electrons using light, harnessing the charge separation to simultaneously provide the cell with a strong oxidant and strong reductant. Many substrates can be used as electron donors for phototrophy, however there appears to be important energetic limits. In oxygenic photosynthesis photosystem II (PSII) provides a very strong oxidant that is capable of oxidizing water (ca. +830 mV) to molecular oxygen at the water-oxidizing complex, a redox-active tetra-manganese cluster. Anoxygenic photosystems however appear to only be able to oxidize lower potential electron donors (Fe2+, H2, S0, HS, S2O32-, NO2-, AsO33-).. Several transitional photosystems have been proposed as evolutionary intermediates between anoxygenic and oxygenic photosynthesis, with electron donors of higher redox potentials such as nitrite (ca. +431 mV) or Mn2+ (ca. +780 mV) bridging the redox gap to water. While a range of observations from the geological record support a Mn2+-based transitional photosystem (Johnson et al. 2013), this proposed photochemical scheme is distinct from that observed in anoxygenic photosynthetic organisms. Mechanistically all anoxygenic reaction centers receive their electrons indirectly via soluble electron carriers such as cytochrome c, high potential iron sulfur proteins or cupredoxins. Conversely Mn2+ oxidation is only known to occur today via direct oxidation, such as during photoassembly of the water-oxidizing complex of PSII, or by two distinct, non-energy-conserving mechanisms using molecular oxygen. No natural photosystem is known to solely perform Mn2+-oxidation. The highest redox-potential accessed by known anoxygenic phototrophs oxidizes nitrite (Schott et al. 2010), but it has been unclear until now whether the reaction center is specially adapted to produce high potential oxidants, similar to that of PSII to oxidize Mn2+ and water. To constrain this we sequenced the genome of the nitrite-oxidizing phototroph Thiocapsa sp. KS1. The data reveal that a type II reaction center that looks identical to other closely related strains that lack such a high potential metabolism. Unlike the direct Mn2+ oxidation, nitrite oxidation appears to require no special mutations, implying that nitrite oxidation occurs via cytochromes or cupredoxins, in family with other anoxygenic electron donations. These results define a broad limit for high potential electron donors for anoxygenic photosynthesis, and indicate that only Mn2+--oxidizing photosynthesis (prior to water oxidation by oxygenic phototrophs) likely requires a direct interaction with the reaction center. Johnson JE, Webb SM, Thomas K, Ono S, Kirschvink JL, Fischer WW (2013) Manganese-oxidizing photosynthesis before the rise of cyanobacteria, PNAS, Schott J, Griffin BM, Schink B (2010) Anaerobic phototrophic nitrite oxidation by Thiocapsa sp. strain KS1 and Rhodopseudomonas sp. strain LQ17, Microbiology, 156, 2428-2437.