Ferrosomes are recently discovered lipid-bound bacterial organelles that store iron as iron-phosphate biominerals, yet the chemical nature and physiological consequences of ferrosome-stored iron remain poorly understood. Here, we combined X-ray absorption spectroscopy (XAS), electron microscopy, inductively coupled plasma mass spectrometry (ICP-MS), and physiological analyses to characterize ferrosome iron in Clostridioides difficile. XAS analysis of isolated ferrosomes revealed an amorphous iron-phosphate biomineral containing mixed Fe(II)/Fe(III), consistent with partial oxidation during aerobic isolation. In contrast, whole-cell XAS of intact anaerobically maintained cells demonstrated that ferrosomes predominantly contain a structurally disordered ferrous phosphate biomineral with local Fe-O-P coordination features similar to those of vivianite. Upon air exposure, this ferrous biomineral rapidly oxidized to a ferric phosphate-like state, revealing a highly oxygen-sensitive iron-storage phase. Despite containing abundant redox-active Fe(II), ferrosome-stored iron contributed minimally to the cytosolic labile iron pool. Consistent with this observation, isolated ferrosomes exhibited little ROS-generating activity, and ferrosome-overproducing cells displayed no substantial increase in sensitivity to oxygen, peroxide, or paraquat stress relative to ferrosome-deficient controls. Together, these results establish ferrosomes as iron-storage organelles that sequester redox-active Fe(II) in a mineralized ferrous phosphate phase, limiting its participation in cytosolic ROS chemistry and providing a mechanism for the safe storage of reactive iron.
Pi, H., Zhao, K., Ferrara, K., Liu, Y., Abernathy, M., Sarangi, R.
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