Iron uptake and transfer from ceruloplasmin to transferrin

Background

Dietary and recycled iron are in the Fe^2 + oxidation state. However, the metal is transported in serum by transferrin as Fe^3 +. The multi-copper ferroxidase ceruloplasmin is suspected to be the missing link between acquired Fe^2 + and transported Fe^3 +.

Methods

This study uses the techniques of chemical relaxation and spectrophotometric detection.

Results

Under anaerobic conditions, ceruloplasmin captures and oxidizes two Fe^2 +. The first uptake occurs in domain 6 (< 1 ms) at the divalent iron-binding site. It is accompanied by Fe^2 + oxidation by Cu^2 +_D6. Fe^3 + is then transferred from the binding site to the holding site. Cu⁺_D6 is then re-oxidized by a Cu^2 + of the trinuclear cluster in about 200 ms. The second Fe^2 + uptake and oxidation involve domain 4 and are under the kinetic control of a 200 s change in the protein conformation. With transferrin and in the formed ceruloplasmin–transferrin adduct, two Fe^3 + are transferred from their holding sites to two C-lobes of two transferrins. The first transfer (~ 100 s) is followed by conformation changes (500 s) leading to the release of monoferric transferrin. The second transfer occurs in two steps in the 1000–10,000 second range.

Conclusion

Fe^3 + is transferred after Fe^2 + uptake and oxidation by ceruloplasmin to the C-lobe of transferrin in a protein–protein adduct. This adduct is in a permanent state of equilibrium with all the metal-free or bounded ceruloplasmin and transferrin species present in the medium.

General significance

Ceruloplasmin is a go-between dietary or recycled Fe^2 + and transferrin transported Fe^3 +.