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A slick, slack pathway through the pore
Author(s) -
Rothberg Brad S.
Publication year - 2017
Publication title -
the journal of physiology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.802
H-Index - 240
eISSN - 1469-7793
pISSN - 0022-3751
DOI - 10.1113/jp273497
Subject(s) - gating , cytosol , steric effects , biophysics , chemistry , ion channel , channel (broadcasting) , potassium channel , crystallography , physics , topology (electrical circuits) , computer science , biology , stereochemistry , biochemistry , mathematics , combinatorics , computer network , receptor , enzyme
Slo2.1 and Slo2.2 K+ channels (also called ‘Slick’ and ‘Slack’, respectively) are members of an extended gene family of K+ channels defined by the presence of ‘regulator of K+ conduction’ (RCK) domains at their carboxy termini (Yuan et al. 2000, 2003; Santi et al. 2006). RCK domains serve as cytosolic ligand sensors, and are activated by Na+ ions in the case of Slo2 channels. Other members of this gene family include BK (Slo1) channels, which are activated by cytosolic Ca2+ instead of Na+, as well as a host of orthologues found in prokaryotes, such as MthK (Rothberg & Magleby, 2000; Jiang et al. 2002; Latorre & Brauchi, 2006; Smith et al. 2013). These channels have been models for understanding biophysical mechanisms of channel gating, and as recent crystallographic and cryo-EM experiments provide information on channel structure, it becomes even more interesting to incorporate these structural details into our thinking. For example, as the RCK domains are tethered to the cytosolic face of the channel, it might seem quite reasonable to think that gating of Slo2 channels involves movement of the RCK domains to relieve steric hindrance of K+ ions by a molecular ‘gate’ at the cytosolic end of the pore. A combination of structural and functional evidence has supported the idea that the K+ channel gate is located near the cytosolic threshold of the pore and is formed by a ‘bundle-crossing’ of the four pore-lining helices of the channel. Support for this model can trace its origins to classical ‘blocker-trapping’ experiments in the squid axon K+ channel, which illustrated that a quaternary ammonium blocker molecule could access its binding site from the cytosolic side of the pore only after the K+ channel gate has been opened, and it can be subsequently ‘trapped’ following entry if the K+ channel’s activation gate is closed behind it (Armstrong, 1971; Armstrong & Hille, 1972). The molecular basis of the gate as a bundle-crossing was supported by elegant cysteine-modification experiments in the Shaker Kv channel and related channels, and finally by the crystal structure of the apparently closed KcsA channel (Holmgren et al. 1997; Liu et al. 1997; Doyle et al. 1998; del Camino & Yellen, 2001; Shin et al. 2001; Rothberg et al. 2002). However, more recent evidence has suggested that not all K+ channels may conform to this mechanism, and that the gate may instead lie deeper within the pore (Wilkens & Aldrich, 2006). In this issue of The Journal of Physiology, Giese et al. (2017) challenge whether the bundle-crossing hypothesis applies to Slo2 channels with a series of electrophysiological experiments. The authors first target two leucine residues, L267 and L270, using mutagenesis guided by recent structural data, to test their role in gating. These residues line the central axis of the pore not near the bundle-crossing, but instead near the channel’s selectivity filter (Hite et al. 2015). The authors find, interestingly, that substitution of these residues individually or together can render Slo2.1 channels constitutively open, consistent with the idea that these side chains impact movement of the gate. Such a key role for these deep-pore residues in modulating gating energetics is at odds with a model in which gating consists only of localized movements of the bundle-crossing at the cytosolic end of the pore. The authors then interrogate residues positioned near a potential bundle-crossing, focusing on M282 in Slo2.1 and its analogue M354 in Slo2.2. These methionine side chains appear to face the central axis of the pore, and would be the most likely to come together to form a hydrophobic gate in the closed conformation. If this idea were true, then one might predict that substituting these methionines with glutamate side chains might result in electrostatic repulsion at the bundle-crossing, to render the channel constitutively active. Interestingly, M282E and M354E channels did not show enhanced activation, again arguing against the idea that bundlecrossing gates the flow of K+ in these channels. The work of Giese et al. adds to an emerging picture of diversity among K+ channels in terms of their structural mechanisms to gate K+ conduction. In voltage-gated K+ channels (like Shaker), there is robust evidence that side chains near the bundle-crossing form a gate that is strongly controlled by the channel’s voltage sensor, and can impede the flow of large blocking molecules as well as small ions, such as Cd2+ or Ag+ (del Camino & Yellen, 2001). On the other hand, it now seems the K+ channels in the RCK family exhibit relatively weak (or ‘slack’?) steric hindrance at the bundle-crossing, which may impede the access of large blocking molecules, but not smaller ions (Li & Aldrich, 2004, 2006). These new results provide a rationale to probe deeper into the pore, in search of the elusive gate.

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