Abstract

Net proton secretion and unidirectional chloride fluxes were measured in isolated skin of toads ( Bufo bufo) and frogs ( Rana esculenta) mounted in an Ussing chamber and exposed to a Ringer's solution on the serosal side and a freshwater-like solution (1-3 mM Cl(-)) on the external side. Active proton secretion was 34.2+/-2.0 pmol.cm(-2).s(-1) ( n=18) in frog skin, and 16.7+/-1.7 pmol.cm(-2).s(-1) ( n=10) in toad skin. Proton secretion by toad skin was dependent on the transepithelial potential ( V(T)), and an amiloride-insensitive short-circuit current was stimulated by exogenous CO(2)/HCO(3)(-), indicating the presence of a rheogenic proton pump. Cl(-) influx was 37.4+/-7.5 pmol.cm(-2).s(-1) ( n=14) in frog skin and 19.5+/-3.5 pmol.cm(-2).s(-1) ( n=11) in toad skin. In toad skin, the mean Cl(-) flux ratio was larger than expected for simple electro-diffusion. In 8 of 11 sets of paired skins, influx was greater than the efflux indicating active uptake of Cl(-). Cl(-) influx in toad skin was unaffected by large perturbations (100-150 mV) of V(T), which was accomplished by adding amiloride to the outer bath under open circuit conditions. A component of the Cl(-) efflux seemed to be dependent on V(T). 4,4'-Diisothiocyanato-stilbene-2,2'-disulfonic acid (DIDS; 0.3 mM or 1.3 mM) inhibited Cl(-) influx and, surprisingly, increased Cl(-) efflux in toad skin. Influx and efflux of Cl(-) in toad skin were highly dependent on the external [Cl(-)] in the freshwater range (0.1-4 mM). (36)Cl(-) influx decreased whereas the total Cl(-) efflux increased as a function of external [Cl(-)]. These data indicate the presence of a DIDS-sensitive, electroneutral carrier mechanism with an external binding site for Cl(-). Ethoxzolamide (100 micro M), an inhibitor of carbonic anhydrase, reduced proton secretion and Cl(-) influx in frog skin. Concanamycin A (0.1-10 micro M), a specific vacuolar-type proton pump (V-ATPase) inhibitor, significantly reduced proton secretion in frog skin. In addition, concanamycin A (1 micro M) significantly reduced Cl(-) influx in frog skin. We suggest that the active proton secretion and Cl(-) influx are coupled. We hypothesise that an apical V-ATPase is capable of energising active Cl(-) uptake in fresh water by creating a favourable gradient for an apical HCO(3)(-) exit in exchange for external Cl(-). The data also suggest that a carbonic anhydrase activity provides H(+) and HCO(3)(-) for apically co-expressed proton pumps and Cl(-)/HCO(3)(-) exchangers.

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