Abstract

Water-filled hydrophobic cavities in channel proteins serve as gateways for transfer of ions across membranes, but their properties are largely unknown. We determined water distributions along the conduction pores in two tetrameric channels embedded in lipid bilayers using neutron diffraction: potassium channel KcsA and the transmembrane domain of M2 protein of influenza A virus. For the KcsA channel in the closed state, the distribution of water is peaked in the middle of the membrane, showing water in the central cavity adjacent to the selectivity filter. This water is displaced by the channel blocker tetrabutyl-ammonium. The amount of water associated with the channel was quantified, using neutron diffraction and solid state NMR. In contrast, the M2 proton channel shows a V-shaped water profile across the membrane, with a narrow constriction at the center, like the hourglass shape of its internal surface. These two types of water distribution are therefore very different in their connectivity to the bulk water. The water and protein profiles determined here provide important evidence concerning conformation and hydration of channels in membranes and the potential role of pore hydration in channel gating.

Highlights

  • Detecting functionally important wet spots in ion channels is an experimental challenge

  • It has been suggested that dewetting transitions in the central hydrophobic cavity play a key role in the function of some ion channels (8 –10)

  • For the mammalian channel Kv1.2, which has a similar cavity architecture and size as KcsA, predictions of molecular dynamics simulations probing gating transitions over hundreds of microseconds have suggested that, at reverse and even zero transmembrane voltages, a cavity collapse can be observed [9, 10]. This hydrophobic collapse is accompanied by a complete dewetting, driving the number of water molecules in the cavity to 0

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Summary

Background

Detecting functionally important wet spots in ion channels is an experimental challenge. For the KcsA channel in the closed state, the distribution of water is peaked in the middle of the membrane, showing water in the central cavity adjacent to the selectivity filter. This water is displaced by the channel blocker tetrabutylammonium. There is little experimental evidence or general consensus regarding the presence and dynamics of water in the nonpolar cavities found in channel proteins [1] These cavities serve as sites for uptake and transfer of both nonpolar and polar molecules, including ions, across membranes [2].

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