Abstract
L-type Ca2+ channels select for Ca2+ over sodium Na+ by an affinity-based mechanism. The prevailing model of Ca2+ channel permeation describes a multi-ion pore that requires pore occupancy by at least two Ca2+ ions to generate a Ca2+ current. At [Ca2+] < 1 microM, Ca2+ channels conduct Na+. Due to the high affinity of the intrapore binding sites for Ca2+ relative to Na+, addition of microM concentrations of Ca2+ block Na+ conductance through the channel. There is little information, however, about the potential for interaction between Na+ and Ca2+ for the second binding site in a Ca2+ channel already occupied by one Ca2+. The two simplest possibilities, (a) that Na+ and Ca2+ compete for the second binding site or (b) that full time occupancy by one Ca2+ excludes Na+ from the pore altogether, would imply considerably different mechanisms of channel permeation. We are studying permeation mechanisms in N-type Ca2+ channels. Similar to L-type Ca2+ channels, N-type channels conduct Na+ well in the absence of external Ca2+. Addition of 10 microM Ca2+ inhibited Na+ conductance by 95%; and addition of 1 mM Mg2+ inhibited Na+ conductance by 80%. At divalent ion concentrations of 2 mM, 120 mM Na+ blocked both Ca2+ and Ba2+ currents. With 2 mM Ba2+, the IC50 for block of Ba2+ currents by Na+ was 119 mM. External Li+ also blocked Ba2+ currents in a concentration-dependent manner, with an IC50 of 97 mM. Na+ block of Ba2+ currents was dependent on [Ba2+]; increasing [Ba2+] progressively reduced block with an IC50 of 2 mM. External Na+ had no effect on voltage-dependent activation or inactivation of the channel. These data suggest that at physiological concentrations, Na+ and Ca2+ compete for occupancy in a pore already occupied by a single Ca2+. Occupancy of the pore by Na+ reduced Ca2+ channel conductance, such that in physiological solutions, Ca2+ channel currents are between 50 and 70% of maximal.
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