Iron is a vital mineral for almost all living organisms and has a pivotal role in central metabolism. Despite its great abundance on earth, the accessibility for microorganisms is often limited, because poorly soluble ferric iron (Fe³⁺) is the predominant oxidation state in an aerobic environment. Hence, the reduction of Fe³⁺ is of essential importance to meet the cellular demand of ferrous iron (Fe²⁺) but might become detrimental as excessive amounts of intracellular Fe²⁺ tend to undergo the cytotoxic Fenton reaction in the presence of hydrogen peroxide. We demonstrate that the complex formation rate of Fe³⁺ and phenolic compounds like protocatechuic acid was increased by 46% in the presence of HCO₃^- and thus accelerated the subsequent redox reaction, yielding reduced Fe²⁺ Consequently, elevated CO₂/HCO₃^- levels increased the intracellular Fe²⁺ availability, which resulted in at least 50% higher biomass-specific fluorescence of a DtxR-based Corynebacterium glutamicum reporter strain, and stimulated growth. Since the increased Fe²⁺ availability was attributed to the interaction of HCO₃^- and chemical iron reduction, the abiotic effect postulated in this study is of general relevance in geochemical and biological environments.IMPORTANCE In an oxygenic environment, poorly soluble Fe³⁺ must be reduced to meet the cellular Fe²⁺ demand. This study demonstrates that elevated CO₂/HCO₃^- levels accelerate chemical Fe³⁺ reduction through phenolic compounds, thus increasing intracellular Fe²⁺ availability. A number of biological environments are characterized by the presence of phenolic compounds and elevated HCO₃^- levels and include soil habitats and the human body. Fe²⁺ availability is of particular interest in the latter, as it controls the infectiousness of pathogens. Since the effect postulated here is abiotic, it generally affects the Fe²⁺ distribution in nature.

Anna-Lena Hacker

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