Thermodynamic and Kinetic Studies of the Interaction of Nuclear Receptor Coactivator-4 (NCOA4) with Human Ferritin.

Ferritinophagy is a ferritin autophagic degradation process mediated by the selective nuclear receptor coactivator-4 (NCOA4). NCOA4 binds to ferritin and delivers it to nascent autophagosomes, which then merge with the lysosomes for ferritin degradation and iron release. Earlier studies have demonstrated a specific association of NCOA4 with ferritin H-subunits, but not L-subunits. However, neither the thermodynamics of this interaction nor the effect of NCOA4 on iron oxidation, iron mineral core formation, or iron mobilization in ferritin has been explored. Using isothermal titration calorimetry, light absorption spectroscopy, and a soluble fragment (residues 383-522) of human NCOA4 expressed in Escherichia coli, we show that the NCOA4 fragment specifically binds H-rich ferritins with a binding stoichiometry of ∼8 NCOA4 molecules per ferritin shell, and Kd values of ∼0.4 and ∼2 µM for homopolymer H-chain ferritin and heteropolymer H-rich ferritin, respectively. The binding reaction was both enthalpically and entropically favored. Whereas the iron oxidation kinetics were not affected by the presence of NCOA4, iron mobilization from ferritin by two different reducing agents (FMN/NADH and sodium dithionite) showed a strong inhibitory effect that was dependent on the concentration of NCOA4 present in solution. Our results suggest that the binding of NCOA4 to ferritin may interfere in the electron transfer pathway through the ferritin shell and may have important biological implications on cellular iron homeostasis.

Ferritin exhibits Michaelis-Menten behavior with oxygen but not with iron during iron oxidation and core mineralization.

The excessively high and inconsistent literature values for Km,Fe and Km,O2 prompted us to examine the iron oxidation kinetics in ferritin, the major iron storage protein in mammals, and to determine whether a traditional Michaelis-Menten enzymatic behavior is obeyed. The kinetics of Fe(ii) oxidation and mineralization catalyzed by three different types of ferritins (recombinant human homopolymer 24H, HuHF, human heteropolymer ∼21H:3L, HL, and horse spleen heteropolymer ∼3.3H:20.7L, HosF) were therefore studied under physiologically relevant O2 concentrations, but also in the presence of excess Fe(ii) and O2 concentrations. The observed iron oxidation kinetics exhibited two distinct phases (phase I and phase II), neither of which obeyed Michaelis-Menten kinetics. While phase I was very rapid and corresponded to the oxidation of approximately 2 Fe(ii) ions per H-subunit, phase II was much slower and varied linearly with the concentration of iron(ii) cations in solution, independent of the size of the iron core. Under low oxygen concentration close to physiological, the iron uptake kinetics revealed a Michaelis-Menten behavior with Km,O2 values in the low µM range (i.e. ∼1-2 µM range). Our experimental Km,O2 values are significantly lower than typical cellular oxygen concentration, indicating that iron oxidation and mineralization in ferritin should not be affected by the oxygenation level of cells, and should proceed even under hypoxic events. A kinetic model is proposed in which the inhibition of the protein's activity is caused by bound iron(iii) cations at the ferroxidase center, with the rate limiting step corresponding to an exchange or a displacement reaction between incoming Fe(ii) cations and bound Fe(iii) cations.