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A high-valent Fe(IV) species is proposed to be generated from the decay of a peroxodiferric intermediate in the catalytic cycle at the di-iron cofactor center of dioxygen-activating enzymes such as methane monooxygenase. However, it is believed that this intermediate is not formed in the di-iron substrate site of ferritin, where oxidation of Fe(II) substrate to Fe(III) (the ferroxidase reaction) occurs also via a peroxodiferric intermediate. In opposition to this generally accepted view, here we present evidence for the occurrence of a high-valent Fe(IV) in the ferroxidase reaction of an archaeal ferritin, which is based on trapped intermediates obtained with the freeze-quench technique and combination of spectroscopic characterization. We hypothesize that a Fe(IV) intermediate catalyzes oxidation of excess Fe(II) nearby the ferroxidase center.

Viperin, a radical-SAM enzyme conserved from fungi to humans, can restrict replication of many viruses. Neither the molecular mechanism underlying the antiviral activity of Viperin, nor its exact physiological function, is understood: most importantly, no radical-SAM activity has been discovered for Viperin. Here, using electron paramagnetic resonance (EPR) spectroscopy, mass spectrometry, and NMR spectroscopy, we show that UDP-glucose is a substrate of a fungal Viperin (58% pairwise identity with human Viperin at the amino acid level) in vitro. Structural homology modelling and docking experiments reveal a highly conserved binding pocket in which the position of UDP-glucose is consistent with our experimental data regarding catalytic addition of a 5′-deoxyadenosyl radical and a hydrogen atom to UDP-glucose. This article is protected by copyright. All rights reserved.

The iron-storage protein, ferritin, is widely found in all Domains of life. A conserved diiron center in ferritin catalyzes oxidation of Fe(II) and regulates storage of the resultant Fe(III) oxidation product. When this center is filled with Fe(III), in bacterial or archaeal ferritin the presence of phosphate accelerates the rate of Fe(II) oxidation. The molecular mechanism underlying this stimulatory effect of phosphate is unknown. Using site directed mutagenesis of the residues in the diiron center of the archaeal ferritin from Pyrococcus furiosus we show that phosphate facilitates displacement of Fe(III) by Fe(II) from this site. Therefore, the rate of Fe(II) oxidation increases only when the ferroxidase center is filled with Fe(III).