中央研究院 生物化學研究所
The emergence of molecular oxygen on early Earth is conventionally attributed to the evolution of oxygenic photosynthesis. A persistent challenge for early life, however, was the management of reactive oxygen species such as hydrogen peroxide (H2O2), which could arise through a variety of abiotic processes. Here we report that some RNA molecules, when coordinated with ferrous iron (Fe2+), catalyze the oxidation of H2O2 into O2 and H2O under anoxic conditions that mimic the early Earth environment. This previously unrecognized RNA-based redox activity suggests that ancient RNA-metal complexes may have contributed to the detoxification of H2O2 and the management of oxidative stress prior to the evolution of protein enzymes. Such RNA-Fe complexes provide a plausible molecular mechanism linking early geochemical oxidants to primitive biological redox chemistry.
