The effect of endogenous phosphate on the H+/Mn2+ ratio and the state of Mn2+ in the mitochondrial matrix.

Abstract

1. Kinetics and stoichiometry of H+ extrusion and reuptake and of Mn2+ uptake and release have been measured in respiring liver mitochondria in the absence of external added Pi. H+ and Mn2+ fluxes are parallel during aerobic cation uptake but not during uncoupler induced cation release. The H+/Mn2+ is 1.24. Addition of SH reagents, in concentrations inhibiting the Pi carrier, modifies the kinetics of H+ extrusion and of Mn2+ uptake and release. The slow phase of uncoupler induced Mn2+ release is diminished. The H+/Mn2+ is increased to 1.72. Addition of SH reagents, after the phase of aerobic uptake is completed, results in a significant reduction of the extent of uncoupler-induced Mn2+ release. The extent of reuptake of endogenous Pi during aerobic uptake of Mn2+ is about 8 nmol x mg protein-1. 2. Aerobic uptake of Mn2+ in the absence of external Pi results in an electron spin resonance spectrum which is the sum of two components. One, denoted as S, corresponds to Mn(H2O)2+(6). Another denoted as E, reflects spin exchange narrowing. In contrast to previous claims the following evidence suggests that the spin exchange component is due to Mn3(PO4)2 precipitate: (a) the dimension of the spin exchange spectrum is markedly reduced by abolition of Pi transport; (b) the spin exchange spectrum is released very slowly by addition of uncouplers under conditions where uncouplers cause a rapid deenergization of mitochondria, reuptake of H+ and release of cations; (c) the free matrix Mn2+ is released slowly after addition of uncoupler if there is a large spin exchange signal; howeover the free matrix Mn2+ is abolished rapidly by uncoupler when formation of the spin exchange signal is prevented by pretreatment with Ca2+; (d) the band width of the spin exchange fraction is independent of the Mn2+/protein ratio either under kinetic or steady state conditions; (e) the experimental spectrum recalls closely that obtained by computer simulation by assuming it as a combination of Mn(H2O)2+(6) and Mn3(PO4)2. 3. It is concluded that endogenous Pi affects the process of aerobic divalent cation uptake. A part of Mn2+ uptake in the absence of externally added anions, consists of a Mn3(PO4)2 precipitate. This accounts for a H+/Mn2+ ratio lower than 2.