Summary
This chapter reviews some of the evidence and the postulated proposals for how oxygenic photosynthesis first emerged as a distinct form of photoautotrophic metabolism using water as an electron donor. This form of photosynthesis is the most successful photoautotrophic metabolism in the contemporary biosphere and is found in all higher plants, green and red algae and both cyano- and oxyphoto-bacteria. We summarize the timetable for emergence and the biogeochemical consequences of oxygenic photosynthesis. Particular attention is paid to evolution of the inorganic core of the enzyme that catalyzes water oxidation, chemical speciation of the inorganic cofactors and possible alterative substrates. We discuss possible mineral remnants of early oxygenic photosynthesis and the emerging role of bicarbonate in assembly of the inorganic core and as an hypothesized evolutionary cofactor.
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Dismukes, G.C., Blankenship, R.E. (2005). The Origin and Evolution of Photosynthetic Oxygen Production. In: Wydrzynski, T.J., Satoh, K., Freeman, J.A. (eds) Photosystem II. Advances in Photosynthesis and Respiration, vol 22. Springer, Dordrecht. https://doi.org/10.1007/1-4020-4254-X_31
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DOI: https://doi.org/10.1007/1-4020-4254-X_31
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