Sodium gradient-dependent L-glutamate transport is localized to the canalicular domain of liver plasma membranes. Studies in rat liver sinusoidal and canalicular membrane vesicles.

The driving forces for L-glutamate transport were determined in purified canalicular (cLPM) and basolateral (i.e. sinusoidal and lateral; blLPM) rat liver plasma membrane vesicles. Initial rates of L-glutamate uptake in cLPM vesicles were stimulated by a Na+ gradient (Na+o greater than Na+i), but not by a K+ gradient. Stimulation of L-glutamate uptake was specific for Na+, temperature sensitive, and independent of nonspecific binding. Sodium-dependent L-glutamate uptake into cLPM vesicles exhibited saturation kinetics with an apparent Km of 24 microM, and a Vmax of 21 pmol/mg X min at an extravesicular sodium concentration of 100 mM. Specific anionic amino acids inhibited L-[3H]glutamate uptake and accelerated the exchange diffusion of L-[3H]glutamate. An outwardly directed K+ gradient (K+i greater than K+o) further increased the Na+ gradient (Na+o greater than Na+i)-dependent uptake of L-glutamate in cLPM vesicles, resulting in a transient accumulation of L-glutamate above equilibrium values (overshoot). The K+ effect had an absolute requirement for Na+. In contrast, in blLPM the initial rates of L-glutamate uptake were only minimally stimulated by a Na+ gradient, an effect that could be accounted for by contamination of the blLPM vesicles with cLPM vesicles. These results indicate that hepatic Na+ gradient-dependent transport of L-glutamate occurs at the canalicular domain of the plasma membrane, whereas transport of L-glutamate across sinusoidal membranes results mainly from passive diffusion. These findings provide an explanation for the apparent discrepancy between the ability of various in vitro liver preparations to transport glutamate and suggest that a canalicular glutamate transport system may serve to reabsorb this amino acid from bile.