An inside-alkaline pH gradient (pH 7.7 inside, 5.5 outside) stimulated Cl uptake in brush-border vesicles from rabbit ileum. The addition of HCO3 without changing the pH gradient further stimulated Cl uptake to a level fourfold greater than equilibrated Cl uptake. Although a K diffusion potential stimulated Cl uptake, this was insensitive to inhibition by 4,4-diisothiocyanostilbene-2,2'-disulfonate (DIDS), whereas pH and HCO3 gradient-stimulated Cl uptake was inhibited by DIDS. pH and HCO3 gradient-stimulated Cl uptake was found to be a saturable function of the Cl concentration with a Km of 3.5 mM and a Vmax of 49 nmol X mg prot-1 X min-1. To distinguish between coupling of Na and Cl transport by cotransport or dual exchange (Na-H and Cl-HCO3 exchange), we determined uptake with high (134 mM Tris-HEPES-MES) internal buffer and low (1.34 mM Tris-HEPES-MES) internal buffer concentrations. Inwardly directed gradients of 50 mM Na, 50 mM K, or 50 mM Na and K did not stimulate Cl uptake, and 50 mM Cl, 50 mM K, or 50 mM KCl did not stimulate Na uptake, with high internal buffer, excluding cotransport. In contrast, 50 mM Na stimulated Cl uptake (inhibited by 1 mM DIDS) and 50 mM Cl stimulated Na uptake (inhibited by 1 mM amiloride) in low buffer media. To determine a role for carbonic anhydrase, Na-stimulated Cl uptake was determined in low buffer media, equilibrated with either 100% N2 or 95% N2-5% CO2. Na stimulated Cl uptake 80% (compared with trimethylammonium control) with CO2 but only 30% with N2 (P less than 0.05). Acetazolamide partially inhibited (P less than 0.025) the stimulation of Cl uptake with CO2 but not with N2. Carbonic anhydrase activity was measured in homogenate and brush-border membrane and was enriched 7.9 +/- 0.4-fold, whereas sucrase was enriched 14.0 +/- 1.1-fold. We conclude that coupled Na and Cl transport occurs by dual exchange (Na-H and Cl-HCO3) and carbonic anhydrase, apparently located on the brush-border membrane, facilitates dual exchange by providing HCO3.