Abstract:Nearly all living organisms require iron, the fourth most abundant element in the earth's crust, for survival. However, despite its abundance, ferric ion has extremely low solubility in aerobic environments at physiological pH (10
−18
M), and the Fe
II
/Fe
III
redox couple leads the production of destructive oxygen radicals via Fenton chemistry. To solubilize and regulate iron in biological systems, many organisms rely on proteins and smal… Show more
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