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* Istituto di Chimica del Riconoscimento Molecolare, CNR, 20131 Milan, Italy; and
Groningen Biomolecular Sciences and Biotechnology Institute (GBB), Department of Biophysical Chemistry, University of Groningen, 9747 AG Groningen, The Netherlands
Correspondence: Address reprint requests to Giorgio Colombo, Istituto di Chimica del Riconoscimento Molecolare, CNR, via Mario Bianco 9, 20131 Milan, Italy. Tel.: +39-02-28500031; Fax: +39-02-28500036; E-mail: colombo{at}icrm.cnr.it or Alan E. Mark, Groningen Biomolecular Sciences and Biotechnology Institute (GBB), Department of Biophysical Chemistry, University of Groningen, Nijenborgh 4, 9747 AG Groningen, The Netherlands. Tel.: +31-50-3634457; Fax: +31-50-3634800; E-mail: mark{at}chem.rug.nl.
| ABSTRACT |
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| INTRODUCTION |
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The best characterized member of this family is the prokaryotic large conductance mechanosensitive channel (MscL), which was originally isolated from Escherichia coli by Kung and co-workers (Sukharev et al., 1997
). MscL is a nonselective ion channel of
2.5 nS conductance that is activated in vitro by the application of membrane tension (Blount et al., 1999
; Sukharev et al., 1994
). The channel is localized in the inner cell membrane and, at least in the case of Mycobacterium tuberculosis (Tb-MscL) for which the x-ray crystal structure has been solved, is a homopentamer (Chang et al., 1998
). The protein is predominantly
-helical and can be subdivided into transmembrane and cytoplasmatic domains, as illustrated in Fig. 1. Each of the five subunits consists of two transmembrane helices, labeled TM1 (green in Fig. 2) and TM2 (blue in Fig. 2), which are tilted by 30 degrees with respect to the membrane normal (Chang et al., 1998
). The TM1-helix, residues 1543, crosses the membrane and defines the pore. A large loop (residues 4468), which is resolved in the crystal structure, connects TM1 to TM2 (residues 6989). TM2 again crosses the membrane and returns to the cytoplasm. Each of the TM1-helices makes contact with four other helices: two TM1-helices from the adjacent subunits and two TM2-helices, one from the same subunit and one from an adjacent subunit. Moreover, TM1 is lined with several polar and charged residues (Thr-25, Thr-28, Thr-32, Thr-35, Lys-33, and Asp-36) forming a possible pathway for solutes or even small proteins through the membrane (Fig. 2). The channel is constricted at the cytoplasmatic side by an array of hydrophobic residues (Ile-14 and Val-21), which probably act to gate passing ions and water molecules. MscL is believed to play a primary role in protecting cells exposed to osmotic downshock from lysis. Placing cells in a hypoosmotic environment leads to the influx of water into the cell. This in turn leads to an increase in turgor pressure within the cell and an increase in the tension within the membrane. MscL is believed to open in response to high levels of tension within the membrane, allowing ions and other solutes to be released from the cell and thus preventing rupture of the cell membrane.
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In this paper we attempt to directly model the gating mechanism of MscL by applying physically appropriate forces on the protein within a realistic environment. Using essentially an all-atom representation of the protein, the membrane (POPC), and water, we follow the time evolution of the system under different stress conditions during a series of MD simulations. Our aim is to evaluate the effect of tension and compression within the membrane on the structure of the pore to shed light on the initial stages of the gating process.
| MATERIALS AND METHODS |
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The structure obtained with this procedure was refined using the WHATIF (Vriend, 1990
) package to place atoms in residues which were not observed in the x-ray structure. The starting configuration for the simulations was generated as follows. In a preequilibrated POPC bilayer containing 128 lipid molecules, a cylindrical hole large enough to accommodate the protein was created in the bilayer by displacing from their starting positions all molecules whose phosphate atoms fell within 2.5 nm of the central axis of the cylinder. A short MD simulation which included an additional repulsive force that acted radially from the central axis of the cylinder was then used to drive any remaining atoms out of the region of the cylinder. The x-ray structure of the MscL protein was subsequently inserted into the cavity that had been created. The system was then solvated with simple point charge (SPC) water molecules (Berendsen et al., 1981
). Fifteen chloride ions were added to neutralize the system by replacing water molecules at the positions of lowest coulomb potential. The final system consisted of 1 Tb-MscL molecule, 128 lipid molecules, 4956 water molecules, and 15 chloride ions, giving in total 24730 atoms in a rectangular box (Fig. 2). Before initiating the simulations the system was first energy minimized to relax bad contacts within the protein and between the protein and POPC molecules. The system was then simulated for 50 ps with the protein and the POPC molecules positionally restrained to allow the water molecules to relax. This was followed by two more 50-ps simulations without position restraints during which time the temperature of the system was slowly brought to 300 K and the pressure equilibrated to P0 = 1 bar.
All simulations were performed using the GROMACS software package (van der Spoel et al., 1994
). The GROMOS96 forcefield (43al) (van Gunsteren et al., 1996
; 1998
) was used for the protein. POPC lipid parameters were taken from the work of Berger et al. (Berger et al., 1997
). These lipid parameters have been used extensively with the GROMOS96 forcefield for proteins (Tieleman and Berendsen, 1998
; Shrivastava et al., 2002
).
The system was studied in the NPT ensemble. The temperature and pressure were maintained by weak coupling to external temperature and pressure baths with coupling times of
T = 0.1 and
P = 1.0 ps, respectively (Berendsen et al., 1984
). The protein, lipids, and water were each coupled to separate temperature baths at 300 K in all simulations. A twin-range cutoff was used in which Lennard-Jones and short-range coulombic interactions within 1.0 nm were determined every step while interactions within 1.8 nm were evaluated every 10 steps together with the pair-list update. Although this is not as accurate as a full treatment of the coulomb forces using a lattice-sum method, it is much cheaper and has been tested with the forcefield and algorithms used in these simulations (Tieleman and Berendsen, 1998
).
The LINCS algorithm was used to constrain all bond lengths within the protein and lipids. High-frequency motions associated with the explicit treatment of polar and aromatic hydrogens were eliminated by reconstructing the positions of the hydrogens based on the positions of the heavy atoms to which they are attached as described by Feenstra et al. (Feenstra et al., 1999
). This allows a time step of 4 fs to be used without significantly affecting the thermodynamic properties of the system or the conformations sampled in extended simulations (Feenstra et al., 2002
).
In total, four simulations were performed using different pressure coupling conditions. The lateral pressure Pxy and normal pressure Pz in these simulations are coupled independently (semiisotropic coupling). The difference between the lateral and normal pressure gives rise to a membrane tension
= L(Pz - Pxy) with L denoting the membrane thickness. In the first simulation, labeled Normal Pressure (NP), a pressure of 1 bar was applied in both the lateral and normal directions, corresponding to a tensionless state of the membrane. In the second simulation labeled Press 100 (P100), a constant pressure of 1 bar was applied in the z-direction, while a pressure of 100 bar was applied in the xy-plane. Taking L = 5 nm as a typical membrane thickness,
= -50 mN/m for the P100 simulation. This mimics hyperosmotic conditions. In the simulations Stretch 100 (S100) and Stretch 1000 (S1000), a pressure of 1 bar was again applied in the z-direction, while a negative pressure of -100 bar and -1000 bar was applied in the xy-plane of S100 and S1000, respectively. The corresponding surface tensions are
= 50 mN/m (S100) and
= 500 mN/m (S1000). The negative lateral pressure mimics the lateral stretching of the membrane under hypoosmotic conditions for which MscL gating is observed.
The systems labeled NP, P100, and S100 were equilibrated at their respective pressures for l00 ps with position restraints on the protein and for another 100 ps without position restraints before sampling commenced. S1000 was started from the last conformation obtained after the 30-ns-long accumulation run S100. The three systems NP, P100, and S100 were simulated for 30 ns, while S1000 (started from the last conformation obtained from S100) was terminated after 22 ns.
All simulations were performed in parallel on a Linux PC-cluster consisting of 600 MHz Pentium III dual processor machines, at a rate of 0.5 ns/24 CPU hours per machine. The analysis of the trajectories from the simulations was performed using the routines present in the GROMACS package (van der Spoel et al., 1994
). The principal radii of the protein were obtained from its moments of inertia, assuming an ellipsoidal shape (Lide, 1992
). Visualization of the individual structures was performed using the programs RasMol (Figs. 2 and 6) and VMD (Figs. 1 and 5) (Humphrey et al., 1996
).
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| RESULTS AND DISCUSSION |
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The conformational change that the system undergoes at high negative lateral pressure is also evident in changes in the principal radii of the protein. Fig. 3 shows the principal radii as a function of simulation time for each of the four pressure conditions simulated. In the S1000 simulation there is an abrupt decrease in the principal radius along the z-axis as evident in Fig. 3 d. In contrast, the two lateral dimensions expand. This redistribution around the z-axis (pore axis) is consistent with pore opening. No equivalent change in the principal radii was evident in the other simulations (Fig. 3, ac). Except for some fraying involving residues at the cytoplasmatic end of the TM1 and TM2 helices and the region around Ile-14 and Val-21 in S1000, the loss of secondary structure during the simulations is minimal. Thus, from the simulations the gating mechanism would appear to involve primarily a spatial rearrangement of the helices in response to the applied tension in the membrane as opposed to an unfolding-refolding transition. This seems to be accompanied by a structural variation in the region around Ile-14 and Val-21, a point that will be discussed further below. Based on their mechanistic analysis, Oakley et al. had proposed that the formation of ordered secondary ß-type structure involving the external (periplasmic) loop might be associated with the conformational transition leading to the open conformation of the pore (Oakley et al., 1999
). In the current simulations the external loops remain unstructured under all conditions examined. In particular, no formation of regular or ordered secondary structure was apparent in the S1000 simulation associated with the conformational changes observed.
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0.2 nm, makes it likely that this structure represents the closed, or a nearly closed, state. In the simulations NP and P100, where the channel should remain in a closed state, the hydrophobic patch formed by residues Ile-14 and Val-21 remains stable throughout. In fact, in the P100 simulation, where a positive lateral pressure was applied, the pore becomes even more constricted (radius of the hole
0.18 nm). In contrast, in simulations S100 and S1000, in which a negative lateral pressure is applied mimicking the stretching of the membrane, the diameter of this region increases. Associated with this, the close packing in the hydrophobic patch is lost, potentially allowing water and ions to pass through the pore. In the S1000 simulation the radius of the pore increases to
1.2 nm (Fig. 6). Several mutagenesis studies have shown that hydrophilic substitutions in this region destabilize the closed state permitting the channel to gate at a lower membrane tension. The most effective "gain-of-function" mutations are substitutions of either Ile-14 or Val-21 (or both) by charged residues (Oakley et al., 1999
The membrane
The application of lateral tension and the structural changes in the pore result in a reorganization of the structure of the membrane. In particular, the thickness of the membrane (calculated as the distance between the peaks in the density plot of the lipid headgroups across the simulation box) tends to decrease from a value of 4.8 nm and 4.6 nm in simulations P100 and NP, respectively, to values of 4.0 nm and 2.7 in the stretching simulations S100 and S1000, respectively. Fig. 5 d shows that in the case of the S1000 simulation the thickness of the membrane is not uniform, but decreases away from the protein as the membrane is stretched. Close to the protein the membrane maintains its thickness, matching the dimensions of the protein. Although typical cells disrupt at pressures only slightly higher than the gating pressures (Levina et al., 1999
), during this set of simulations the membrane did not rupture even at the highest tension simulated. MD simulations of pure dipalmitoylphosphatidylcholine (DPPC) lipid bilayers, however, do show spontaneous rupture (on a ns time scale) for lateral pressures exceeding -200 bar (Tieleman et al., 2002
). The presence of the protein therefore seems to have a stabilizing effect on the surrounding membrane.
The mechanism of opening
The mechanism by which the MscL channel opens has been debated for some time. Some have proposed a concerted mechanism, in which tension within the membrane leads to a simultaneous motion of all helices in the TM1 and TM2 bundle away from the central axis opening the pore (Spencer et al., 1999
). Others have postulated that the outer TM2 helices act as a tension sensor, and can expand significantly before the internal part of the channel opens. This model considers that the periplasmic loops act as "strings" connecting the tension-sensing rim to the internal region of the complex. The channel opens when the tension-sensing rim transfers enough force via these loops to pull the internal TM1 bundle into the open state (Sukharev et al., 2001
).
Our simulations suggest a third possibility. When enough tension (mimicked by the "negative" pressure in the xy-plane in the S1000 simulation) is applied, a partial reorganization of the structure is observed. There is an increase in the tilt of the helices with respect to the axis of the pore, followed by the separation of two helices within the TM2 bundle. A TM1 helix then moves into the space that has been created, expanding the central cavity. At the same time, the hydrophobic cluster consisting of residues Ile-14 and Val-21 from each of the five subunits forming the TM1 bundle is disrupted, creating a channel through the pore. The intersubunit salt-bridges between Lys-33 from one subunit and Asp-36 (this bridge is present for more than 90% of the time in simulation S1000) from the next subunit remain stable, with the possible effect of maintaining the overall stability of the global structure of the protein.
A series of new experimental papers concerning the mechanism of MscL gating appeared after this work was first submitted for review (Perozo et al., 2002a
; Perozo et al., 2002b
; Betanzos et al., 2002
). In particular, Perozo and co-workers, using electron paramagnetic resonance (EPR) spectroscopy in combination with site directed spin labeling, obtained results which are consistent with the opening pathway being characterized by the tilting of the TM1 and TM2 helices. They find there is an increase in the tilt of the TM1 helix of 15 degrees and of the TM2 helix of 17 degrees. This is consistent with the magnitude of the changes shown in Fig. 4, which also shows a larger increase in tilt in the cases of the TM2 helices. The EPR experiments also suggest that the TM1 helix rotates around its principal axis by
70 degrees. We find that as the outer TM2 helix tilts, the associated TM1 helix changes its relative position and rotates away from the center of the pore. In the current set of simulations, however, only a single TM1 helix moves significantly, and more events would be required to test if such motion could explain the change observed in the EPR signal. Betanzos et al. (Betanzos et al., 2002
) provide convincing evidence that the pore opens with an iris-like action. In particular, they show that disulfide bonds engineered between TM1 and TM2 helices of adjacent subunits (Cys-32Cys-81) do not prevent gating, indicating that at least this region remains in contact during gating.
Perozo and co-workers find there is an increase in the accessibility of the hydrophobic residues lining the pore, indicated by spectral broadening for residues Ile-24 and Ala-28. Our calculations show that, during opening, the hydrophobic core obstructing the pore is disrupted and the accessibility of this area to solvent increases, as indicated in Fig. 5. The average solvent surface accessible area for Ile-24 and Ala-28 increases from 1 to 3 nm2 passing from simulation NP to simulation S1000. Perozo and co-workers attempted to model the process of opening based on their experimental observations. Treating the helices as rigid subunits, they generated a series of intermediate states that had an overall appearance and an increase in the tilt of the helices comparable to that found in our simulations. It should be noted, however, that unlike the simulations, such modeling studies inforce that the structural changes occur in a concerted manner. Thus, Perozo and co-workers generate idealized models. As they acknowledge, additional intermediate states would be needed to explain, among other things, the multiple subconducting states detected using patch-clamp methods (Perozo et al., 2002a
).
What has been simulated in this study is just the first stage of the transition from a closed to a fully opened pore. Nevertheless, the mechanism implied by the simulations could explain the step-like partial or staged opening observed in patch-clamp experiments (Sukharev et al., 2001
). Moreover, this picture is consistent with much of the most recent experimental data obtained by Perozo et al. (Perozo et al., 2002a
). Clearly, the tension (
= 500 mN/m) at which the gating is observed in the S1000 simulation is nonphysiological, being more than an order of magnitude larger than that required experimentally (Sukharev et al., 1999
; Moe et al., 2000
). However, the opening threshold defined by Moe et al. (Moe et al., 2000
) for Tb-MscL is the pressure at which single channel openings were observed every 2 s. This timescale is well beyond that which can be simulated in atomic detail. Opening on a shorter timescale would correspond to a more negative threshold pressure. The large lateral pressure in the S1000 simulation was therefore needed to observe the process of opening on the timescale of MD. This will induce artifacts. In fact, simulation S1000 was terminated after 22 ns, as it was considered that the changes induced in the membrane and the partial fraying of the TM1 and TM2 helices made the simulation progressively less reliable. We note, however, that this fraying primarily occurs after the main opening event and most likely does not influence the observed mechanism. As the nature of the pore opening mechanism is mechanical, it is assumed that the basic features involved in the initial stages of the gating of MscL in the simulations will be similar to those under physiological conditions. It is also worth noting that some expansion of the structure (partial opening) is already evident at the end of simulation S100. There is some disruption of the hydrophobic lock and a noticeable increase in water within the pore (Figs. 5 c and 6 c). This is occurring at a tension of
= 50 mN/m, much closer to the physiological gating conditions.
In contrast to the previous simulation studies of Gullingsrud et al. (Gullingsrud et al., 2001
), who applied radial forces to an isolated MscL complex, in the absence of water and membrane lipids, the current simulations incorporate a detailed representation of the whole system. In particular, we have shown that water does not have a dramatic effect in terms of stability of the secondary structure elements and that the disruption of the hydrophobic core is a consequence of the mechanical reorganization of the helices, thus providing a detailed view of the mechanism by which MscL opens.
| CONCLUSIONS |
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| ACKNOWLEDGEMENTS |
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The research was supported by a Marie Curie fellowship, contract number CT-2000-00606.
Submitted on April 15, 2002; accepted for publication November 26, 2002.
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F. Y. Jiang, Y. Bouret, and J. T. Kindt Molecular Dynamics Simulations of the Lipid Bilayer Edge Biophys. J., July 1, 2004; 87(1): 182 - 192. [Abstract] [Full Text] [PDF] |
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B. Martinac Mechanosensitive ion channels: molecules of mechanotransduction J. Cell Sci., May 15, 2004; 117(12): 2449 - 2460. [Abstract] [Full Text] [PDF] |
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C.-S. Chiang, A. Anishkin, and S. Sukharev Gating of the Large Mechanosensitive Channel In Situ: Estimation of the Spatial Scale of the Transition from Channel Population Responses Biophys. J., May 1, 2004; 86(5): 2846 - 2861. [Abstract] [Full Text] [PDF] |
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H. Leontiadou, A. E. Mark, and S. J. Marrink Molecular Dynamics Simulations of Hydrophilic Pores in Lipid Bilayers Biophys. J., April 1, 2004; 86(4): 2156 - 2164. [Abstract] [Full Text] [PDF] |
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