Abstract
Apical Na+ entry into frog skin epithelium is widely presumed to be electrodiffusive in nature, as for other tight epithelia. However, in contrast to rabbit descending colon and Necturus urinary bladder, the constant field equation has been reported to fit the apical sodium current (INa)-membrane potential (psi mc) relationship over only a narrow range of apical membrane potentials or to be inapplicable altogether. We have re-examined this issue by impaling split frog skins across the basolateral membrane and examining the current-voltage relationships at extremely early endpoints in time after initiating pulses of constant transepithelial voltage. In this study, the rapid transient responses in psi mc were completed within 0.5 to 3.5 msec. Using endpoints to 1 to 25 msec, the Goldman equation provided excellent fits of the data over large ranges in apical potential of 300 to 420 mV, from approximately -200 to about +145 mV (cell relative to mucosa). Split skins were also studied when superfused with high serosal K+ in order to determine whether the INapsi mc relationship could be generated purely by transepithelial measurements. Under these conditions, the basolateral membrane potential was found to be -10 +/- 3 mV (cell relative to serosa, mean +/- SE), the basolateral fractional resistance was greater than zero, and the transepithelial current was markedly and reversibly reduced. For these reasons, use of high serosal K+ is considered inadvisable for determining the INa-psi mc relationship, at least in those tissues (such as frog skin) where more direct measurements are technically feasible. Analysis of the INa-psi mc relationships under baseline conditions provided estimates of intracellular Na+ concentration and of apical Na+ permeability of 9 to 14 mM and of approximately 3 X 10(-7) cm X sec-1, respectively, in reasonable agreement with estimates obtained by different techniques.
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