Abstract
Mg2+ is essential for RNA folding and catalysis. However, for the first 1.5 billion years of life on Earth RNA inhabited an anoxic Earth with abundant and benign Fe2+. We hypothesize that Fe2+ was an RNA cofactor when iron was abundant, and was substantially replaced by Mg2+ during a period known as the ‘great oxidation’, brought on by photosynthesis. Here, we demonstrate that reversing this putative metal substitution in an anoxic environment, by removing Mg2+ and replacing it with Fe2+, expands the catalytic repertoire of RNA. Fe2+ can confer on some RNAs a previously uncharacterized ability to catalyse single-electron transfer. We propose that RNA function, in analogy with protein function, can be understood fully only in the context of association with a range of possible metals. The catalysis of electron transfer, requisite for metabolic activity, may have been attenuated in RNA by photosynthesis and the rise of O2.
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Acknowledgements
The authors thank J. Bada, R. Hazen, K. Barefield, J. Sadighi and D. Jenson for helpful discussions. This work was supported by the National Aeronautics and Space Administration Astrobiology Institute (NNA09DA78A).
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C.H., N.V.H, R.M.W., S.C.H. and L.D.W. conceived and designed the experiments and co-wrote the manuscript. C.H., C.D.O. and I-C.C. performed the experiments and analysed the data. J.C.B., E.B.O'N, S.S.A. and A.P. contributed materials and analysis tools. All the authors discussed the results and contributed to writing and editing the manuscript.
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Hsiao, C., Chou, IC., Okafor, C. et al. RNA with iron(II) as a cofactor catalyses electron transfer. Nature Chem 5, 525–528 (2013). https://doi.org/10.1038/nchem.1649
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DOI: https://doi.org/10.1038/nchem.1649
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