Abstract

Many transport processes in biological membranes show a saturation of transport rate when the concentration of the transported ions or molecules is sufficiently increased. Saturation will result when at high concentrations a translocation step which does not directly depend on bulk concentration becomes rate limiting, and it is expected for all multi-step translocation mechanisms. However, a possible alternative explanation for saturation is a regulatory process which decreases the number of translocating channels in response to an increase in bulk concentration of the transported species. In the frog epidermis, Na+ uptake from the extracellular space into the epithelial cytosol occurs through Na+-selective, passively conducting channels located in the apical membrane of the cells directly below the cornified outer cell layer. Saturation of transport occurs with increasing outer Na+ activity ([Na]o): the net Na+ current1,2, membrane conductance2,3 and unidirectional Na+ influx4 increase only subproportionally with [Na]0. The apical Na+ current can transiently be larger than the saturation value, suggesting that a fixed upper single channel transport rate is not responsible for the saturation, and it has, therefore been suggested that in this case saturation occurs through a [Na]o-dependent decrease in channel density2. The Na+-translocation process can be investigated by a statistical evaluation of spontaneous transport fluctuations. The reversible transport blocker amiloride can be used to induce random fluctuations of the Na+ current at the apical membrane. The power density spectrum of these fluctuations is of the lorentzian type and permits an estimation of the Na+ current which passes through individual translocators in the time intervals between blocks5. We have recorded the current fluctuations at different [Na]o values and different amiloride concentrations in the [Na]o range in which saturation of total Na+ current is observed. We report here that the density of the conducting pores decreases with increasing [Na]o.

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