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Biophys J, June 2000, p. 2900-2917, Vol. 78, No. 6
*Membrane Transport Research Group, Departments of Physics and
Chemistry, Université de Montréal, Montréal, Quebec
H3C 3J7, Canada, and
Department of Biochemistry and
Structural Biology, Weill Medical College of Cornell University,
New York, New York 10021 USA
Molecular dynamics (MD) simulations of an atomic model of
the KcsA K+ channel embedded in an explicit
dipalmitoylphosphatidylcholine (DPPC) phospholipid bilayer solvated by
a 150 mM KCl aqueous salt solution are performed and analyzed. The
model includes the KcsA K+ channel, based on the recent
crystallographic structure of Doyle et al. (1998,
Science. 280:69-77), 112 DPPC, K+ and
Cl
ions, as well as over 6500 water molecules for a total
of more than 40,000 atoms. Three K+ ions are explicitly
included in the pore. Two are positioned in the selectivity filter on
the extracellular side and one in the large water-filled cavity.
Different starting configurations of the ions and water molecules in
the selectivity filter are considered, and MD trajectories are
generated for more than 4 ns. The conformation of KcsA is very stable
in all of the trajectories, with a global backbone root mean square
(RMS) deviation of less than 1.9 Å with respect to the
crystallographic structure. The RMS atomic fluctuations of the residues
surrounding the selectivity filter on the extracellular side of the
channel are significantly lower than those on the intracellular side.
The motion of the residues with aromatic side chains surrounding the
selectivity filter (Trp67, Trp68,
Tyr78, and Tyr82) is anisotropic with the
smallest RMS fluctuations in the direction parallel to the membrane
plane. A concerted dynamic transition of the three K+ ions
in the pore is observed, during which the K+ ion located
initially in the cavity moves into the narrow part of the selectivity
filter, while the other two K+ ions move toward the
extracellular side. A single water molecule is stabilized between each
pair of ions during the transition, suggesting that each K+
cation translocating through the narrow pore is accompanied by exactly
one water molecule, in accord with streaming potential measurements
(Alcayaga et al., 1989, Biophys. J. 55:367-371). The
displacement of the ions is coupled with the structural fluctuations of
Val76 and Gly77, in the selectivity filter, as
well as the side chains of Glu71, Asp80, and
Arg89, near the extracellular side. Thus the mechanical
response of the channel structure at distances as large as 10-20 Å from the ions in the selectivity filter appears to play an important
role in the concerted transition.
Biophys J, June 2000, p. 2900-2917, Vol. 78, No. 6
© 2000 by the Biophysical Society 0006-3495/00/06/2900/18 $2.00
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