| Literature DB >> 8474848 |
Abstract
The present patch-clamp study shows that external Mg2+, Ca2+ and Sr2+ decrease the unit amplitude of inward current through the inward-rectifier K+ channel in a concentration-dependent manner. Sr2+ produces a voltage-dependent flickering block as well, and the fractional electrical distance between the external orifice and the Sr2+ binding site (delta) is 0.73. The decrease of unit amplitude is reversible and voltage independent while it does not increase the noise level on the open-channel current. Unit current decreased by Mg2+ or Ca2+ has a longer mean open time, which is inversely proportional to the unit amplitude. External Mg2+ does not decrease the amplitude of unit outward current. A surface potential shift, measured using voltage-dependent Cs+ block (delta = 1.60), failed to explain the current decrease. Therefore, we conclude that (1) the external divalent cations cause an extremely fast channel block, which appears as a decreased amplitude of the unit current on the recording system; (2) the blocking site (fast site) is present near the external orifice of the channel, and it is separate from the blocking site (slow site) to which Cs+ and Sr2+ bind.Entities:
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Year: 1993 PMID: 8474848 DOI: 10.1007/bf00375067
Source DB: PubMed Journal: Pflugers Arch ISSN: 0031-6768 Impact factor: 3.657