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J. Biol. Chem., Vol. 262, Issue 9, 3964-3968, 03, 1987
PH Hsyu and KM Giacomini
Recent studies have suggested that there is an organic cation-proton
exchange mechanism in the renal brush border membrane which may be
responsible for the active secretion of organic cations by the kidney. In
all of these studies, the movement of organic cations was specifically
monitored in the presence of a proton gradient. In this study, the organic
cation-proton exchange mechanism in renal brush border membrane vesicles
was examined by studying the movement of protons in the presence of
favorable gradients of the organic cation, tetraethylammonium (TEA). Using
acridine orange, a pH-sensitive fluorescent probe, we demonstrated that in
isolated brush border membrane vesicles prepared from rabbit renal cortex,
the rate of proton efflux increased with increasing inwardly directed
gradients of TEA, although the efflux was saturable. An outwardly directed
TEA gradient could also accelerate the influx of protons. The rate of
exchange of protons for TEA was slower than that for Na+. This slower rate
appears to be due to a lower Vmax of the exchange of organic cations with
protons. These data provide more direct evidence for an exchange of organic
cations with protons or a cotransport of organic cations and hydroxyl ions
in the renal brush border membrane.
The pH gradient-dependent transport of organic cations in the renal brush border membrane. Studies with acridine orange
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