Water, Protons, and the Gating of Voltage-Gated Potassium Channels
Abstract
:1. Introduction
2. Evidence Pertaining to a Possible Role for Water and Protons in Gating Channels, Especially the Voltage-Gated Potassium Channels Shaker and KV1.2
- (1)
- The Hv1 channel as an analogue of the VSD: Another major consideration is that some types of channels are known to conduct protons. The best known example is the Hv1 channel, which has a structure that is, in many ways, similar to the VSD [28,29,30,31]; however, there exist significant differences (for one thing, Hv1 is a dimer, and the proton path would differ somewhat from that in the VSD of the mammalian Kv1 channel; however, the fundamental structure is similar, and the upper part of the channel strongly resembles that of the VSD of the Kv1.2 channel). Although it is not generally considered that this challenges the standard model, it is difficult to see why it does not; it provides a similar path that could be taken by protons [32]. Hv1 is the subject of multiple studies, and there is still no general agreement on the gating mechanism [29,33,34,35,36,37,38]. It appears that protons contribute to the gating current [39]. The wide variety of suggested conformations implies that there is a complex set of states or that the gating mechanism involves something other than a conformational transformation of the channel. A number of residues, when mutated, change the gating, transport, and other properties of the channel [28,29,40,41]. While the Hv1 channel is not identical with the VSD of a Kv channel, the general structure is similar enough that it is reasonable to conclude that the VSD of a Kv channel can conduct protons in response to an electric field. In other words, this structure strongly suggests that the VSD has proton transport as a core function. The Hv1 channel appears to have an upper section that is very similar to the VSD. In our earlier calculations, we found that the second arginine could be a source of protons from an arg-glu-tyr (REY) triplet of amino acids [42]. This is also where most of the electric field drops [43], reaching values close to 108 V m−1, so that there is almost no field across the remainder of the VSD (108 V m−1 × 7 Ả = 70 mV, leaving nothing for the rest of the VSD). At a field of 108 V m−1, non-linear effects on ionization become important [44] (thus, one must be very careful in evaluating molecular dynamics results that use such a high field for the entire VSD). Our calculations therefore accord with the known effects. The Hv1 channel path diverges from that of the VSD below this point, as the path of the proton would be different in the two cases, but the analogy of the Hv1 still strongly suggests that the upper section should be able to produce a proton and that the proton should push additional protons to the inward side of the membrane. The Hv1 channel voltage sensor is also regulated in part by pH [45], which makes sense if the proton current starts with a proton transfer. It must also be possible to close the channel, and this is usually attributed to a hydrophobic gasket [40]; mutations in this gasket, to less hydrophobic amino acids, allows some of the proton current through. The VSD to allow just three protons through in some tens of microseconds could easily be possible with a very limited driving force. Electrostatic control of the proton current is consistent with pH control in that the field is altered by the state of protonation [46]. MD simulations suggest that a water wire exists in Hv1 but not in the VSD of a voltage-gated channel [47]. Modeling based on a putative (and probably correct) closed state of Hv1 suggests the existence of a water wire in the open state but a hydrophobic plug in the closed state [48,49]. Much of the electrophysiology of Hv1 has been worked out by Thomas DeCoursey and colleagues. Although DeCoursey assumes protein motion in gating, his data are consistent with pH and electrostatic control that does not require motion [35]. While we cannot go through all the details of the gating and conduction of the Hv1 channel, there is also strong evidence for the importance of water as a bridge between energy minima for the proton [50] and, more interestingly, for fluctuations of water as a factor in proton transport [36]. At this point, there has not been a test of the effects of fluctuations with the presence of a voltage. Early—pre 1980s—noise measurements notwithstanding, the interpretation of these results is not transparent.
- (2)
- Other channels, not so closely related to the Kv1 VSD, also transport protons. These include bacteriorhodopsin [51], cytochrome c [52,53,54], and the M2 channel of the influenza virus [55,56,57,58]. Bacteriorhodopsin has water as a critical component in the proton path [59,60,61,62,63]. So does cytochrome c [64,65,66,67,68,69,70,71,72,73] and the M2 channel of the influenza virus [56,74,75,76,77,78]. Much of the work on the influenza M2 channel concerns a water network; water networks include hydrogen bonding that involves extensions of hydronium ions (Eigen ions, Zundel ions [79,80,81,82]). Enough channels are known to transport protons to make it clear that proton transport in channels is fairly common and can be part of water networks. Again, the arrangement of side chains is part of the transport mechanism, but in none of these is a significant rearrangement of the backbone of the protein required. We have completed a set of nine optimizations of the gate region of the channel and found that Eigen and Zundel ions both appear when the ion approaches the PVPV level of the gate. Figure 2A illustrates an Eigen ion, while Figure 2B shows a potassium ion with one Eigen and one Zundel ion in a configuration that actually formed in an optimization.
- (3)
- Proton wires, coupled to water networks and proteins: All of the channels mentioned in Section 2 above include proton wires that may be part of a network that includes water and protein. For example, bacteriorhodopsin proton transport requires both water and a side chain flip [83,84]. Trofimov and coworkers have shown the existence of water pools in the temperature sensing TRPV1 channel [85]. A central question for the role for water wires in channels concerns the hydrophobic barriers that are often cited as interrupting the passage of protons through a channel; such a barrier, for example, seems to be an argument against a proton-gating mechanism in the VSD of a KV1.2 channel. However, an interesting modeling effort by Kratochvil and colleagues [86] shows that water fluctuations can bridge such gaps; the bridge may be short lived, but it would be adequate to allow a few protons, enough for the gating current, to pass through. A simulation study [47] found a water cluster in the center of the Hv1 pore but not in the VSD of a potassium channel. However, even putting aside questions about MD studies, fluctuations between the upper and lower water pools may make it possible to have transient proton passage. Considering that only about three protons would have to pass in perhaps tens of microseconds, this would not be a large enough current to be blocked (in macroscopic terms, it would correspond to a transient current on the order of tens of fA). In addition to possible fluctuations, side chain rotations may be required in some cases. The influenza channel just discussed seems to require a histidine side chain to move and to ionize to different charge states to allow proton passage [87,88]. Water wires are not limited to channels, but may appear wherever proton transfer along a protein is required for function; a paper by Shinobu and Agmon shows this in the green fluorescent protein [89]. A combination of fluctuations in water surrounding a protein, coupled to the fluctuations of the protein, especially side chains, has been calculated for human carbonic anhydrase II [90,91]. Proton transport may also be coupled to an anion, as in the Cl−/H+ exchanger [92]. In cyt c, the proton transport is coupled to electron transport [93], and specific side chains again act as a sort of gate, coupled to fluctuations. These examples suffice to show how there are proton transport wires in multiple proteins, and that these are coupled through water and the side chains of proteins. The proposed proton chain in the VSD of KV1.2 is not unusual and behaves like normal proton transfer chains; it is limited to only about three protons because no more are available. The existence of a proton current with a single mutation is just what would be expected when protons are available. Fluctuations near a protein surface, especially the hydrophobic sections, are difficult to sample, but a method has been proposed for sampling that is more efficient [94]. Even defining a hydrophobic section requires care, as the water lone pair electrons on the oxygen can interact favorably with aromatic π electrons [95], and so the orientation of water at the surface and the orientation of aromatic side chains should be taken into account in deciding what is hydrophobic. More generally, water networks may span a protein, including one with hydrophobic sections; certain hydrophobic interactions are key to some protein functions [96]. Networks percolate across a surface, for example of a protein, and it has been suggested that the biological function depends on a percolation phase transition [97]. Ions can also interact with each other, as mediated by water [98], and we will come to that in the next section.
- (4)
- Ion hydration in confined spaces, like channels: Ions must pass through the gate of the channel and then through the pore. The ion pathway in the channel can be considered in three major sections (this is not the only possible choice of ways to consider the path, but it is the simplest and most direct). (i) Start with selectivity: selectivity of the KV1.2, and other potassium channels for potassium over sodium, appears to largely depend on a selectivity filter (SF) that is conserved from viruses through both domains of protists and essentially all eukaryotes. The filter has a sequence of amino acids (T)TVGYG, where all but the first T are essentially absolutely conserved [99], and the first T nearly so. For channels for which the ion path is from the intracellular to the extracellular space (this includes delayed rectifier channels like KV1.2), this SF is the last section, with the ion leaving from the end of the filter to the extracellular space. There have been a myriad of papers, mostly theoretical, on the passage of the ion through the pore. There are four positions in the filter that can be occupied by the ion or else by water. Determining the number of spaces occupied by ions, as opposed to those occupied by water, has been a struggle for years. A potassium ion in bulk water will have, most of the time, around six water molecules in its hydration shell. The energy of the water interaction decreases as the number of water molecules bound to the ion increases; this is most easily seen for the gas phase, where it was measured by Kebarle and coworkers half a century ago (Table 1 [100]).
- (5)
- A few mutations: There have been far more mutation experiments reported than could be reviewed here. Only a limited number are directly relevant. The entire standard model began with the finding that substituting cysteine for arginine made it possible to determine the side of the membrane from which the substituted residue was accessible. The interpretation ignored the size difference between the tiny cysteine side chains and the large arginine and the fact that water could penetrate the VSD, so that cysteine could ionize in situ without moving to the surface, as was necessary for the standard model. Given these assumptions, accessibility required S4 motion. If the penetration of water, and the size difference of cysteine and arginine side chains, are taken into account, the interpretation of accessibility in terms of motion ceases to be obvious. Here, we will be concerned with certain mutations of residues that are conserved and ionizable, so that they are possibly relevant to the presence and transmission of protons. These include the finding of Lee et al. [120] that a glutamate in the S4–S5 linker is required for the channel to function. Lee and coworkers found that in addition to E327, a histidine, H418 (in the 3Lut numbering from the pdb), played a key role in the pH gating of the Kv1.2 channel, both near the junction of the S4–S5 linker (i.e., the linker between the VSD and the gate) where the linker joins the pore below the gate. Results on the C-terminus of the Kv1.2 channel [121] help to confirm this interpretation. Given their positions, it is easy to see how they must be part of the path through the linker for protons, as they enter the gate section. If protonatable residues were not present at the location where the linker joins the gate, it would be difficult to see how to have a proton path. The fact that these are absolutely necessary and well conserved suggests that there is in fact a proton path, as these residues have no special mechanical properties that would make it difficult to replace them with other residues of a similar size. Without these residues, the channel does not function. It is not obvious why in the standard models, in the absence of a proton path, these would be critical. Second, in a pair of papers from Swartz and coworkers [122,123], it was shown that a substitution of aspartate for proline (P→D mutation) made the channel constitutively open at all physiological voltages (other similar mutations produced a lesser effect in this direction). They concluded that the channel underwent some sort of transformation that opened the channel even without a gating current. On the model we are proposing, the aspartates (there are four, one per domain) absorbed up to four protons, neutralizing the gate, with the consequence that the channel was open—the protons no longer formed a barrier to the progress of the positively charged K+ ion. The pore diameter distances in the open channel are still about the same in the open channel X-ray structure when aspartate is present as when the original, highly conserved proline, is.
- (6)
- If the hydration of ions and the activity of water are important, then it must be the case that osmotic effects are significant. If the osmotic strength on one side of the membrane increases, so that the activity of water that is accessible to that side of the membrane changes, several processes change. Osmotic effects are well known. For one thing, the osmotic pressure can do mechanical work, and there is a large class of channels that are mechanically sensitive; we have not discussed these here, although there is evidence that their gating amounts to breaking a water column in the pore [124,125,126,127] (this list is not at all comprehensive but just offers a few examples). There are a number of channels, of types other than the type we are emphasizing here, on which similar experiments have been conducted [128]. Diaz-Franulic et al. combined osmotic pressure, streaming current, and viscosity experiments to suggest that water displacement during gating of the KV1.2 channel was comparable to that in slow inactivation, as well as to suggest that water displacement was important in both [129].
- (7)
- Aquaporin channels—water channels: There is another class of channels that can deal with osmotic stress, the aquaporin (aqp) channels. These transmit water in response to osmotic gradients. The 2003 Nobel Prize was shared (with Roderick MacKinnon) by Peter Agre, who discovered them. Hundreds of specific aqp channels are known in multiple families. The aquaporins are close to being ubiquitous in plants and are found in all domains of life. They are critical in the lens of the eye [130]. These channels have an interesting property in that they transmit water without transmitting protons, a trick that has led to a fair amount of puzzlement. One guess is that these channels have proton-transmitting water chains that double back, so that protons cannot be transmitted to the other side of the membrane, but return to the side from which they began. Other suggestions for the mechanism of action of these channels involve the electric field and free energy of the ions [131]. A more recent work has made different suggestions [132]. Overall, this class of channels has been the subject of a huge number of studies concerning their location as well as their mechanism of transmitting water while not allowing the transport of H+ [130,131,133,134,135,136]. There are several suggestions for detailed mechanisms that involve lipids and phosphorylation, among other factors. The existence of these channels is to be expected, given the central role that water, and the activity of water, plays in maintaining the conditions that allow cells to function.
3. Conclusions
Author Contributions
Funding
Institutional Review Board Statement
Data Availability Statement
Acknowledgments
Conflicts of Interest
Appendix A
References
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N(H2O) ** | H+ | Na+ | K+ | Cl− | Br− |
---|---|---|---|---|---|
0→1 | ** | 100.8 | 75.2 | 55.0 | 52.9 |
1→2 | 151 | 83.2 | 67.6 | 53.5 | 51.6 |
2→3 | 93.5 | 66.2 | 55.4 | 49.1 | 48.2 |
3→4 | 71.4 | 56 | 49.6 | 46.6 | 45.7 |
4→5 | 64.3 | 51.7 | 44.9 | ||
5→6 | 54.6 | 44.9 | 42.0 |
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Kariev, A.M.; Green, M.E. Water, Protons, and the Gating of Voltage-Gated Potassium Channels. Membranes 2024, 14, 37. https://doi.org/10.3390/membranes14020037
Kariev AM, Green ME. Water, Protons, and the Gating of Voltage-Gated Potassium Channels. Membranes. 2024; 14(2):37. https://doi.org/10.3390/membranes14020037
Chicago/Turabian StyleKariev, Alisher M., and Michael E. Green. 2024. "Water, Protons, and the Gating of Voltage-Gated Potassium Channels" Membranes 14, no. 2: 37. https://doi.org/10.3390/membranes14020037
APA StyleKariev, A. M., & Green, M. E. (2024). Water, Protons, and the Gating of Voltage-Gated Potassium Channels. Membranes, 14(2), 37. https://doi.org/10.3390/membranes14020037