The rates of bicarbonate-dependent uptake and efflux of 22Na+ in Vero cells were studied and compared with the uptake and efflux of 36Cl-. Both processes were strongly inhibited by DIDS. Whereas the transport of chloride increased approximately ten-fold when the internal pH was increased over a narrow range around neutrality, the uptake of Na+ was much less affected by changes in pH. The bicarbonate-linked uptake of 22Na+ was dependent on internal Cl- but not on internal Na+. At a constant external concentration of HCO3-, the amount of 22Na+ associated with the cells increased when the internal concentration of HCO3- decreased and vice versa, which is compatible with the possibility that the ion pair NaCO3- is the transported species and that the transport is symmetric across the membrane. Bicarbonate inhibited the uptake of 36Cl- both in the absence and presence of Na+. At alkaline internal pH, HCO3- stimulated the efflux of 36Cl- from preloaded cells, while at acidic internal pH both Na+ and HCO3- were required to induce 36Cl- efflux. We propose a model for how bicarbonate-dependent regulation of the internal pH may occur. This model implies the existence of two bicarbonate transport mechanisms that, under physiological conditions, transport OH(-)-equivalents in opposite directions across the plasma membrane.
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