Net uptake of chloride across the posterior gills of the Chinese crab (Eriocheir sinensis)

Two methods are commonly used for the determination of transbranchial net fluxes of Na+ and Cl-: direct analysis of changes in ion concentrations in the external medium using flame spectrophotometry or titration (net flux method), and measurement of unidirectional ion fluxes by means of radioactive tracers (tracer method). When we applied both methods in the same preparation, the isolated perfused posterior gill of freshwater-acclimated Eriocheir sinensis, to determine net fluxes of Cl-, the results differed substantially. In artificial fresh water (AFW) containing NaCl, the net flux method yielded a net uptake, but the tracer method showed a net efflux of Cl-. The net uptake of Cl- was abolished in Na(+)-free AFW indicating that Cl- uptake is coupled with the uptake of Na+. Applying the tracer method, net efflux of Cl- remained almost unchanged in Na(+)-free AFW. This suggests the opposite mechanism, i.e. uncoupled uptake of Na+ and Cl-. The discrepancy in the results obviously depends on the method employed. Since the data obtained with the net flux method explain the osmoregulatory performance of crabs living in fresh water, we consider this method as appropriate for determining net transbranchial ion fluxes.