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Functional evaluation of chemically modified human erythrocytes has led to the proposal that amino acid residue E681 of the band 3 anion exchanger AE1 lies on the anion translocation pathway and is a proton carrier required for H+/SO2−4 cotransport. We have tested in Xenopus oocytes the functional consequences of mutations in the corresponding residue E699 of mouse AE1. Most mutations tested abolished AE1-mediated Cl influx and efflux. Only the E699Q mutation increased stilbene disulfonate-sensitive efflux and influx of SO2−4. E699Q-mediated Cl influx was activated by elevation of intracellular SO2−4, but E699Q-mediated Cl efflux was undetectable. The DNDS (4,4′-dinitrostilbene-2,2′-disulfonic acid) sensitivity of E699Q-mediated SO2−4 efflux was indistinguishable from that of wt AE1-mediated Cl efflux. The extracellular anion selectivity of E699Q-mediated SO2−4 efflux was similar to that of wt AE1-mediated Cl efflux. The stoichiometry of E699Q-mediated exchange of extracellular Cl with intracellular SO2−4 was 1:1. Whereas SO2−4 injection into oocytes expressing wt AE1 produced little change in membrane potential or resistance, injection of SO2−4, but not of Cl or gluconate, into oocytes expressing E699Q depolarized the membrane by 17 mV and decreased membrane resistance by 66%. Replacement of bath Cl with isethionate caused a 28-mV hyperpolarization in SO2−4-loaded oocytes expressing E699Q, but had no effect on oocytes expressing wt AE1. Extracellular Cl-dependent depolarization of SO2−4-preloaded oocytes was blocked by DNDS. AE1 E699Q-mediated inward current measured in the presence of extracellular Cl was of magnitude sufficient to account for measured 35SO2−4 efflux. Thus, AE1 E699Q-mediated SO2−4/ Cl exchange operated largely, if not exclusively, as an electrogenic, asymmetric, 1:1 anion exchange. The data confirm the proposal that E699 resides on or contributes to the integrity of the anion translocation pathway of AE1. A single amino acid change in the sequence of AE1 converted electroneutral to electrogenic anion exchange without alteration of SO2−4/Cl exchange stoichiometry.

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