Biochemistry I   Spring & Fall Terms

Potassium Channel: Ion Conduction Mechanism

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  Membrane thickness (Å)

  K+ Selectivity Pore
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  K+ at sites 2 & 4
  K+ between sites
  K+ at sites 1 & 3

  K+ Efflux Mechanism
  Scripted Animation

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Structure of the KcsA K+ channel from Streptomyces lividans
The initial view of the potassium channel tetramer is from the plane of the membrane. Each subunit is colored separately and contains three a-helices. The long inner and outer helices span the bilayer membrane. The selectivity pore residues (Sticks, colored white) are in the turn that connects the short pore helices to the inner helices. Waters are shown as small red balls on the extracellular side (top) and in the cytosol (bottom). The K+ ions are shown spacefill, colored dark green.
The membrane thickness indicated is the apolar region of the membrane.
K+ Selectivity Pore
Close-up: Only three of the subunits are shown to provide a clearer view of the pore. All seven of the possible K+ locations are shown. However, only four, at most, are occupied at the same time; the other sites contain waters. Residues 75-79 comprise the selectivity pore and are shown as Sticks, colored CPK. The mainchain C=O's of these residues coordinate the K+ ions. The water-filled cavity is colored cyan. All of the waters shown here are highly-ordered and thus differ from the "bulk" water surrounding the channel.
K+ at sites 2 & 4: Each K+ ion is coordinated by eight oxygens with water between them. For example, K+ at site 4 is coordinated by the side chains and C=O's of Thr 75.
K+ between sites: The K+ ions are coordinated by only four of the mainchain C=O's. For example, the K+ between sites 2 and 3 is coordinated only by Val 76. A K+ is about to enter the pore from the cavity.
K+ at sites 1 & 3: The K+ ions are coordinated by eight mainchain C=O's. For example, K+ at site 1 is coordinated by Gly 77 and Tyr 78.
The pore is normally occupied by two K+ ions and two waters. Concerted movement of the two ions and their waters leads to K+ exit from, or entry into the cell. The scripted animation shows the sequence of steps in the exit pathway.
K+ Efflux Mechanism
The steps shown in the animation (See Morais-Cabral et al., Figs. 4 and 5.):
State I   Water-filled pore: The K+ that will soon exit is in the cavity.
State H   K+ at site 4: The K+ enters the pore and is replaced by another in the cavity.
State E   K+ at site 3: The K+ moves up one position (with the waters). Another K+ occupies the cavity from the cytosol.
State C   K+ at sites 2 & 4: The K+ moves up another position.
Intermediate between site 2 and the extracellular site: The K+ is coordinated by only four of the mainchain C=O's prior to dissociation, first by Tyr 78 and finally by Gly 79.
Dissociation from extracellular site: The K+ binds briefly at site 0 and at the fully hydrated extracellular site, then diffuses into the extracellular solution.
Script ends with K+ at sites 2 & 4. For multiple cycles of ion efflux, the pathway resumes at State C above. K+ entry follows the same pathway in reverse direction. A single cycle takes about 10 nanoseconds to complete!

The refined structure of the potassium channel is described by:
Zhou, Y. Morais-Cabral, J. H. Kaufman, A. & MacKinnon, R. (2001) "Chemistry of ion coordination and hydration revealed by a K+ channel-Fab complex at 2.0 Å resolution". Nature 414: 43     PubMed [1K4C.pdb]
(A "fake" coordinate file containing the K+ ions and water used for the animation was added to 1K4C.pdb as Model 2.)
The ion-conduction pathways are described by:
Morais-Cabral, J. H. Zhou, Y. & MacKinnon, R. (2001) "Energetic optimization of ion conduction rate by the K+ selectivity filter" Nature 414: 37     PubMed
References to Figs. above are to those of Morais-Cabral et al.)

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8.21.04