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ARTICLE |
Correspondence to Frank T. Horrigan: horrigan{at}mail.med.upenn.edu
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| INTRODUCTION |
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That Ca2+ and voltage act independently to regulate opening is evident from BK channel function and consistent with channel structure. BK channels can be fully activated by membrane depolarization in the absence of Ca2+ (Cui et al., 1997
), and Ca2+ facilitates opening in a nearly voltage-independent manner, indicating that Ca2+ and voltage sensor activation have energetically additive effects on opening (Cui and Aldrich, 2000
; Horrigan and Aldrich, 2002
). The transmembrane domain of BK channels, like voltage-gated K+ (Kv) channels, includes an S5–S6 pore domain and a charged S1–S4 voltage sensor (Ma et al., 2006
). Coupling between the voltage sensor and pore can occur presumably as in Kv channels, via interactions within the transmembrane domain (Fig. 1 A) (Lu et al., 2002
; Long et al., 2005b
).
In addition, BK channels contain a large C-terminal cytosolic domain that interacts with intracellular ligands and is directly attached to the S6 activation gate. The cytosolic domain of each
-subunit contains two putative RCK (regulator of K+ conductance) homology domains (RCK1, RCK2), like those in the prokaryotic channel MthK (Jiang et al., 2001
). In MthK, RCK domains from different subunits assemble into a gating ring structure that expands upon Ca2+ binding to pull open the gate (Fig. 1 B) (Jiang et al., 2002
; Ye et al., 2006
), suggesting that Ca2+ opens BK channels by increasing tension on the RCK1–S6 linker (Niu et al., 2004
). Thus models of BK channel structure support that voltage and Ca2+ sensors may act independently on the gate (Fig. 1 C) to exert additive effects on steady-state activation.
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Mg2+ has effects on BK channel gating that resemble those of Ca2+: increasing PO, slowing IK deactivation, and shifting the GK-V relation to more negative voltages with little change in shape (Shi and Cui, 2001
; Zhang et al., 2001
). Effects of Mg2+ and Ca2+ on the half-activation voltage (V0.5) are approximately additive and involve different binding sites (Shi et al., 2002
; Xia et al., 2002
). Consequently, Mg2+ has been proposed to act independently of Ca2+ but through a similar functional mechanism. Effects of Mg2+ on the GK-V relation can be reproduced by gating schemes that assume Mg2+ acts, like Ca2+, to enhance channel opening independent of voltage sensor activation (Shi and Cui, 2001
; Zhang et al., 2001
; Hu et al., 2006
). However, several lines of evidence suggest that Mg2+ and Ca2+ do not act through identical functional mechanisms. First, high concentrations of Ca2+ (>100 µM), which are known to occupy Mg2+ binding sites, have effects that differ qualitatively from those of low [Ca2+]i. While 0–100 µM Ca2+ produces a nearly voltage-independent increase in log(PO), 100–1,000 µM Ca2+ increases log(PO) in a voltage-dependent manner (Horrigan and Aldrich, 2002
). In addition, mutations in the voltage sensor, including R213Q in S4, disrupt Mg2+ sensitivity but not Ca2+ sensitivity, suggesting that the voltage sensor plays a critical role in Mg2+-dependent activation (Hu et al., 2003
). Indeed, recent evidence indicates that Mg2+ bound to the cytosolic domain interacts electrostatically with R213 (Yang et al., 2007
).
This study examines the functional interaction between Mg2+- and voltage-dependent activation of mSlo1 BK channels. Effects of 0–100 mM Mg2+ on the steady-state and kinetic properties of ionic and gating currents were examined over a wide voltage range in WT channels and channels where either the voltage sensor or a putative Mg2+-binding site in the RCK1 domain were mutated. The results show that Mg2+ at the RCK1 site acts primarily to strengthen the allosteric coupling of voltage sensor activation to channel opening. Only at high concentrations (>10 mM), involving an additional very low affinity binding site, does Mg2+ have direct effects on opening, like Ca2+. Our results together with the proposed electrostatic nature of Mg2+/voltage sensor interaction suggest that Mg2+ and the voltage sensor must interact in multiple states to account for the effects of Mg2+ on voltage sensor/gate coupling.
| MATERIALS AND METHODS |
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0.5–5 ng of cRNA, incubated at 18°C, and studied 3–7 d after injection. HEK cells were transfected with mSlo1 in an SR
vector using Lipofectamine (GIBCO BRL/Life Technologies Inc.) 2–3 d before recording as described previously (Horrigan and Aldrich, 2002
Electrophysiology and Data Analysis
Currents were recorded using the patch-clamp technique in the inside-out configuration (Hamill et al., 1981
) at 20 ± 1°C. For Ca2+ experiments, the external solution contained (in mM) 104 KMeSO3, 6 KCl, 2 MgCl2, 20 HEPES, and the internal solution contained 110 KMeSO3, 6 HCl, 20 HEPES, and 2 EGTA (0 Ca2+) or 5 HEDTA (Ca2+ solution). Ca2+ was added as CaCl2 and [Cl–]i was adjusted to 10 mM with HCl. Free [Ca2+] for the 2 µM Ca2+ solution was measured (1.8 µM) with a Ca2+ electrode (Orion Research Inc.). For Mg2+ experiments, the external solution contained (in mM) 225 KOH, 196 HCl, 2 MgCl2, 10 HEPES, and internal solutions contained 225 KOH, 5 EGTA, 10 HEPES, plus MgCl2 and HCl to obtain the desired [Mg2+] with [Cl–]i = 200 mM. 100 mM Mg2+ solution contained a total of 100 mM Mg2+ for an estimated free [Mg2+] of 96.1 mM. Total Mg2+ in other solutions was adjusted to obtain the indicated free [Mg2] (2, 5, 10, 21 mM) as calculated by MaxChelator (http://www.stanford.edu/
cpatton/maxc.html) (Patton et al., 2004
). Since free [Mg2+] was not measured, the purity of MgCl2 and EGTA stocks were assayed by pH-metric titration (Tsien and Pozzan, 1989
) against standardized solutions of EDTA and CaCl2, respectively. For gating currents (Ig) the external solution contained 130 tetraethyl ammonium (TEA)-OH, 100 NMDG, 196 HCl, 2 MgCl2, 10 HEPES, and internal solution contained 225 NMDG-MES, 10 HEPES, 5 EGTA, plus MgCl2 and HCl as above. The pH of all solutions was adjusted to 7.2 with MeSO3. Internal solutions contained 40 µM (+)-18-crown-6-tetracarboxylic acid (18C6TA) to chelate contaminant Ba2+ (Diaz et al., 1996
; Neyton, 1996
).
Data were acquired with an Axopatch 200B amplifier (Molecular Devices Corp.) in patch mode with the Axopatch's filter set at 100 kHz. Currents were filtered by an 8-pole Bessel filter (Frequency Device, Inc.) at 50 kHz (IK) or 20 kHz (Ig) and sampled at 200 kHz with an 18-bit A/D converter (Instrutech ITC-18). For gating currents, the voltage command was also filtered at 20 kHz. A p/4 protocol was used for leak subtraction (Armstrong and Bezanilla, 1974
) with a holding potential of –80 mV. Electrodes were made from thick-walled 1010 glass (World Precision Instruments, Inc.) and their tips coated with wax (KERR Sticky Wax). The electrode's resistance in the bath solution (0.5–1.5 M
) was used as an estimate of series of resistance (RS) for correcting the voltage at which macroscopic IK was recorded. Series resistance error was <15 mV for all data presented. A Macintosh-based computer system was used in combination with Pulse Control acquisition software (Herrington and Bookman, 1995
) and Igor Pro for graphing and data analysis (WaveMetrics, Inc.). A Levenberg-Marquardt algorithm was used to perform nonlinear least-squared fits. Data are presented as mean ± SEM.
Open probability (PO) was estimated by recording macroscopic IK when PO was high (
0.005–0.05) and unitary currents in the same patch when PO was low (
0.01–0.1). Macroscopic conductance (GK) was determined from tail currents at –80 mV following 50-ms voltage pulses, and was normalized by GKmax to estimate PO. GKmax was measured in 5–100 mM Mg2+ (0 Ca2+) at V > 200 mV from tail currents and was estimated at [Mg2+] < 5 mM as GKmax (10 Mg2+) {
K([Mg2+])/
K(10 Mg2+)} where
K([Mg2+]) is the single channel conductance at –80 mV and is reduced slightly (
5%) in 10 Mg2+ due to Mg2+ block. At more negative voltages, NPO was determined from steady-state recordings of 1–60 s duration that were digitally filtered at 5 kHz. NPO was determined from all-points amplitude histograms by measuring the fraction of time spent (PK) at each open level (K) using a half-amplitude criteria and summing their contributions NPo =
kPk. PO was then determined by estimating N from GKmax (N = GKmax/
K, where
K is the single channel conductance at –80 mV). Mean activation charge displacement (qa = kT d(ln(PO)/dV) was measured from the slope of the ln(PO)-V relation by linear regression over 60-mV intervals and plotted against mean voltage. Fits of the qa-V relation were similarly determined by linear regression of simulated data (Ma et al., 2006
).
Patch-to-patch variation in V0.5 of the G-V and Q-V relationships are observed for Slo1 channels (Stefani et al., 1997
; Horrigan et al., 1999
). To compensate for the effect of such variation on mean Po-V and QC-V relations, V0.5 was determined for each patch and individual relations were shifted along the voltage axis by
V0.5 = (<V0.5> – V0.5) before averaging, where <V0.5> is the mean for all experiments at the same [Mg2+]. Patch to patch variation in PO at extreme negative voltages is also observed (Horrigan et al., 1999
). Therefore, mean log(PO)-V and
K-V relations for 0, 10, and 100 mM Mg2+ were constructed using only experiments in which both Mg2+ data and matching 0 Mg2+ controls exist. In this way, mean relations accurately reflect effects of Mg2+ that were observed in individual experiments.
Gating capacitance (Cg) was measured using admittance analysis as previously described (Horrigan and Aldrich, 1999
). In brief, gating currents were recorded in response to 0.5-s voltage ramps upon which a sinusoidal voltage command (781 hz, 60 mV peak to peak) was superimposed. Admittance was calculated for each cycle of the sinewave, and capacitance was determined after correcting for phase shifts due to instrumentation.
| RESULTS |
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10–7 by recording unitary current activity in macropatches containing hundreds of channels. Log(PO) is increased by 2 µM Ca2+ in a nearly voltage-independent manner, shifting the entire log(PO)-V curve upward by 1.2 log units (a 15-fold increase in PO) until channels are maximally activated at positive voltages. PO is increased 15-fold even at extreme negative voltages (
–100 mV) where voltage sensors are not activated and log(PO) is weakly voltage dependent (Fig. 2 C, dotted lines) (Horrigan and Aldrich, 2002
Why Is the Effect of Mg2+ Voltage Dependent?
Two different mechanisms could potentially account for the voltage dependence of Mg2+ action; the effect of Mg2+ could depend on the activation state of the voltage sensor, or Mg2+ binding could be intrinsically voltage dependent. Voltage-dependent binding must be considered because if Mg2+ interacts with the voltage sensor it could also lie within the membrane electric field; and a model assuming that Mg2+ traverses a fraction of the electric field (
= 0.2) to reach its binding site can reproduce the effect of 10 mM Mg2+ (Fig. 2, B and C, dotted curves, see legend for details). However, the effects of Mg2+ on two voltage sensor mutants (R207Q, R167E) in Fig. 2 D indicate that voltage sensor activation is critical to the effect of Mg2+ and probably sufficient to account for the voltage dependence of Mg2+ action.
R207Q in S4 and R167E in S2 shift voltage sensor activation to more negative and positive voltages, respectively (Ma et al., 2006
), such that log(PO)-V relations for these mutants are shifted along the voltage axis relative to the WT in 0 Mg2+ (Fig. 2 D, filled symbols). R207Q also shifts the Q-V relation by more than –250 mV, based on gating current measurements, such that even at –200 mV a significant fraction (
0.2) of voltage sensors are activated (Ma et al., 2006
). Both R207Q and R167E are readily activated by 10 mM Mg2+ at depolarized voltages (Fig. 2 D), suggesting these mutations do not disrupt Mg2+ binding nor interactions of Mg2+ with the voltage sensor (Hu et al., 2003
; Yang et al., 2007
). However the voltage dependence of Mg2+-dependent activation for the mutants is greatly altered relative to the WT, suggesting that Mg2+ action depends on the activation state of the voltage sensor. In the case of R167E, Mg2+ has no effect on PO at voltages up to +60 mV where the WT is strongly activated by Mg2+. Conversely, R207Q exhibits a robust 30-fold increase in PO at negative voltages (–120 to –200 mV) where the WT appears insensitive to Mg2+. The response of R207Q indicates that Mg2+ is capable of occupying its binding site even at extreme negative voltages. Thus, it is unlikely that Mg2+ binding is intrinsically voltage dependent; and the inability of the WT to be activated at negative voltages likely reflects that Mg2+ is incapable of increasing PO when voltage sensors are in the resting state. This hypothesis is supported by comparison of the WT and R167E data that show that channels are Mg2+ insensitive when PO is weakly voltage dependent.
Understanding the Action of Mg2+ in Terms of Allosteric Mechanisms
To determine how Mg2+ and voltage sensors interact mechanistically we interpreted our results in terms of a well-established allosteric gating scheme that accounts for the effects voltage on steady-state activation of BK channels (Fig. 2 E, Scheme 1) (Horrigan and Aldrich, 1999
; Horrigan et al., 1999
). Scheme 1 asserts that the opening of the gate can be described as a concerted, weakly voltage-dependent transition between an open and closed conformation (C-O) with zero-voltage equilibrium constant L0 and partial charge zL. In addition, voltage sensors in each of four independent and identical subunits can undergo a transition between a resting and activated conformation (R-A) characterized by equilibrium constant J0 and partial charge zJ. The coupling between voltage sensor and gate is described by an allosteric factor D, such that the C-O equilibrium constant increases D-fold for each voltage sensor activated and the voltage sensor equilibrium increases D-fold when the channel opens.
Based on Scheme 1 there are four distinct mechanisms by which a ligand might alter Po. Ligand binding could (a) influence the intrinsic stability of the gate (L0), (b) perturb the voltage sensor equilibrium (J0), (c) alter voltage sensor/gate coupling (D-factor), or (d) alter the gating charge associated with voltage sensor activation (zJ) or channel opening (zL). The action of Ca2+ is mainly accounted for by an effect on the gate (L0) with a minor impact on voltage sensor activation (J0). This mechanism can be represented by an allosteric model (Fig. 2 F, Scheme 2) that successfully reproduces the effects of Ca2+ (Fig. 2, B and C, solid lines) in terms of a ligand-binding equilibrium (X-X·M2+) and allosteric factors C and E that describe the coupling of Ca2+ sensors to the gate and to voltage sensors, respectively (Horrigan and Aldrich, 2002
). Direct coupling between Ca2+ sensors and gate is evident from the ability of Ca2+ to increase PO whether or not voltage sensors are activated. Thus the insensitivity of PO to 10 mM Mg2+ when voltage sensors are in the resting state rules out a similar interaction between Mg2+ sensors and gate and indicates that L0 is unchanged, but leaves open the possibility that Mg2+ affects voltage sensor activation or coupling (Fig. 2 G, Scheme 3) or charge.
Mg2+ Has Little Effect on Voltage Sensor Activation when Channels Are Closed
To characterize effects of Mg2+ on the voltage sensor we recorded gating current from WT and mutant channels (Fig. 3).
The results indicate that Mg2+ has little effect on the voltage sensor equilibrium (J0) or gating charge (zJ).
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20% increase in peak IgON with little change in kinetics (Fig. 3 A, top). Application of 100 mM Mg2+, to activate very low affinity binding sites (Hu et al., 2006
gFast) for a single experiment (Fig. 3 C) reflect a small –21 mV shift in the
gFast-V relation to more negative voltages.
To better quantify small changes in VhC (
VhC) by Mg2+ we examined gating capacitance (Cg) (Fig. 3, D–F). Cg is the voltage-dependent component of membrane capacitance and reflects the derivative of gating charge with respect to voltage. The Cg-V relation was determined from admittance analysis by measuring Ig evoked by a sinusoidal voltage command superimposed on a 500-ms voltage ramp from –200 to +200 mV (see Materials and methods) (Horrigan and Aldrich, 1999
, 2002
). At voltages where steady-state PO is low (<0.1), the Cg-V relation approximates the derivative of QC-V (Horrigan and Aldrich, 1999
). Thus
VhC can be determined directly from shifts in the foot of Cg-V relation (Fig. 3 D). Because Cg-V is determined rapidly and with high voltage resolution, small VhC shifts are detectable, the effects of applying and washing out Mg2+ can be assessed rapidly, and errors in
VhC due to slow changes in VhC from channel oxidation or electrode potential drift are minimized. Cg-V analysis for the WT (Fig. 3 D) yielded
VhC values (10 Mg: 17.2 ± 1.5 mV [n = 6], 100 Mg: 36.1 ± 1.6 mV [n = 6]) similar to those determined from QC-V relations.
The effect of Mg2+ on VhC is comparable to that of micromolar Ca2+ (Horrigan and Aldrich, 2002
), consistent with a weak interaction between Mg2+ binding and voltage sensor activation in closed channels that increases the voltage sensor equilibrium constant J0 (e.g., E-factor in Schemes 2 and 3, Fig. 2, F and G). However, millimolar Mg2+ may also shift voltage-dependent parameters by nonspecific mechanisms such as screening of membrane surface charge (Hu et al., 2006
). Therefore, to assess the impact of the RCK1 Mg2+ site on J0 we compared effects of Mg2+ on the WT channel to those of a mutant (E374A/E399N) whose RCK1 site is disrupted (Shi et al., 2002
; Hu et al., 2006
). This mutation of putative Mg2+-coordinating residues, which reduces the GK-V shift in 10 mM Mg2+ by 80% to –14.0 ± 2.0 mV, also reduces effects of 10 or 100 mM Mg2+ on the Cg-V relation (Fig. 3, E and F). The difference in
VhC between the WT and mutant (
VhC =
VhC(E374A/E399N) –
VhC(WT)) was –9.5 ± 2.8 mV and –11.6 ± 2.8 mV for 10 and 100 Mg2+, respectively, likely representing the effect of RCK1 site occupancy on J0. The similar impact of mutation in 10 and 100 mM Mg2+ is consistent with the expectation that the RCK1 site is nearly saturated in 10 mM Mg2+(Hu et al., 2006
).
The small effect of Mg2+ on gating current suggests that Mg2+ enhances voltage sensor/gate coupling (D). The –17.2 mV
VhC by 10 mM Mg2+ (Fig. 3 F) can account for a similar GK-V shift but is much too small to explain the observed –67-mV shift (Fig. 2 B). By contrast, an increase in the coupling factor D can shift V0.5 without affecting VhC. In addition, enhanced coupling should facilitate channel opening when voltage sensors are fully activated and facilitate voltage sensor activation when channels are open. These predictions are confirmed below by results in Figs. 4 and 5.
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D4 where
D = D(Mg2+)/D(control). This predicted facilitation of opening cannot be tested for the WT channel because in 0 Mg2+ PO is already nearly saturated (
1) at potentials >250 mV where voltage sensors are fully activated (compare GK-V in Fig. 2 B and Qc-V in Fig. 3 B). However, facilitated opening by Mg2+ can be observed in mutants with enhanced voltage sensor activation (R207Q, R210C; Fig. 4).
Fig. 4 A compares the log(PO)-V relations for WT, R207Q, and R210C channels in 0 Mg2+. R207Q shifts QC-V, as noted above, such that this relation is saturated and voltage sensors are fully activated at V
–20 mV (Ma et al., 2006
) (Fig. 4 A, labeled arrow). Over this voltage range, PO is weakly voltage dependent and well described by a Boltzmann function (dotted curve) as expected for channels with fully activated voltage sensors undergoing a two-state C-O transition with equilibrium constant L0D4 (Horrigan and Aldrich, 2002
). Importantly, the weak voltage dependence of L0 reduces PO to nonsaturating levels at potentials where the mutant voltage sensors are still fully activated (e.g., PO = 0.04 at –20 mV). The PO-V relation for R210C is indistinguishable from that of R207Q at V
–20 but extends the weakly voltage-dependent phase of PO to less than –200 mV, suggesting that R210C voltage sensors are constitutively activated (Ma et al., 2006
). The difference between WT and R207Q in Fig. 4 A is consistent with a 100-fold change in the voltage sensor equilibrium constant J0 (Horrigan and Aldrich, 1999
; Ma et al., 2006
) and illustrates qualitatively the effect expected if Mg2+ acts merely to promote voltage sensor activation. That is, an increase in J0 can shift the steepest part of the log(PO)-V relation to more negative voltages but cannot increase PO above the limiting relation defined by L0D4 (Fig. 4 A, dotted curve). By contrast, 10 mM Mg2+ markedly increases PO for R207Q (Fig. 4 B) and R210C channels (Fig. 4 C) when voltage sensors are fully activated, indicating that L0D4 is increased. This increase presumably reflects enhanced voltage sensor/gate coupling (increased D) because L0, although it cannot be measured directly for R207Q or R210C channels, is insensitive to 10 mM Mg2+ in WT and R167E (Fig. 2 D).
Analysis of the mutant data indicate that 10 mM Mg2+ produces an approximate twofold increase in the coupling factor D. Fig. 4 C shows that R210C channels are activated by 10 mM Mg2+ in a voltage-independent manner, consistent with the assumption that voltage sensors are constitutively activated. Mean log(P0)-V relations in the presence and absence of Mg2+ were fit by Boltzmann functions with identical charge (Fig. 4 C, dotted curves), as expected if Mg2+ increases the C-O equilibrium constant by a voltage-independent factor (
D4) and Mg2+ binding is not voltage dependent. A similar response is observed for R207Q at V
–20 mV (Fig. 4 B, dotted curves). The fits to R207Q and R210C yield
D4 values of 8.2 and 16.6, respectively, implying a 1.7–2.0-fold increase in D. A more direct estimate of
D4 is obtained from the Mg2+-dependent increase in PO for R210C at extreme negative voltage. Over a range of voltages (–200 to –140 mV) where PO is small (<0.1) and therefore approximates the C-O equilibrium constant, Mg2+ increases PO by an average of 21.6 ± 6.0-fold (
D4), indicating a 2.16 ± 0.13-fold increase in D, consistent with the Boltzmann fits.
Different Mg2+ Sites Have Distinct Effects on Gating
To further characterize the action of Mg2+ at both RCK1 and very low affinity binding sites we examined the effects on PO of different [Mg2+]i, up to 100 mM, in WT and mutant channels (Fig. 5). The RCK1 site with an estimated KD of 2.2–5.5 mM should be nearly saturated at 10 mM Mg2+, whereas a putative very low affinity site (KD: 40–136 mM) is not significantly affected until concentrations >10 mM (Hu et al., 2006
). The effects of high and low concentrations of Mg2+ appear similar in that GK-V relations are progressively shifted to more negative voltages with little change in shape (Fig. 5 A) (Shi and Cui, 2001
; Zhang et al., 2001
; Hu et al., 2006
). Increasing Mg2+ from 10 to 100 mM shifted the G-V by an additional –34 mV (Fig. 5 A). However, log(PO)-V relations reveal that 100 mM Mg2+ also increases PO significantly at extreme negative voltages (Fig. 5 B). Thus it appears that occupancy of very low affinity Mg2+ sites, unlike the RCK1 site, influence the gate (L0) to increase PO when voltage sensors are not activated.
The log(PO)-V relation in 100 mM Mg2+ appears to achieve a limiting slope between –160 and –140 mV, where PO is increased 2.9-fold relative to the control (Fig. 5 B, dotted lines), implying a 2.9-fold increase in L0. However measurements below –140 mV were difficult to obtain. Therefore, to confirm that 100 mM Mg2+ increases L0 we also compared log(PO)-V relations in 0, 10, and 100 mM Mg2+ for two mutant channels (Fig. 5, C and D).
Mutation of the RCK1 site (E374A/E399N) largely eliminates the response to 10 mM Mg2+ but leaves the PO increase by 100 mM Mg2+ intact (Fig. 5 C). The mutation reduces the GK-V shift (
V0.5) by 10 and 100 Mg2+ to –14.0 ± 2.0 mV and –34.6 ± 1.8 mV, respectively, similar to previous reports (Shi and Cui, 2001
; Hu et al., 2006
). The reduced shift allows log(PO)-V to achieve a limiting slope at more positive voltages than the WT (Fig. 5 C, dotted lines), indicating a 2.9-fold increase in L0 with 100 mM Mg2+, like the WT.
The response of E374A/E399N is important not only in verifying that L0 is increased by 100 mM Mg2+ but also in ruling out that Mg2+ occupancy of either the RCK1 site or Ca2+-binding sites contribute to L0. The insensitivity of L0 to 10 mM Mg2+ in the WT could conceivably reflect an ability of Mg2+ at the RCK1 site to decrease L0 that is masked by the action of Mg2+ at other sites. However, this possibility is unlikely since L0 is also insensitive to 10 mM Mg2+ in E374A/E399N. In addition this result indicates that high affinity Ca2+-binding sites, which are known to bind Mg2+ at millimolar concentrations, are not responsible for the L0 increase in 100 mM Mg2+ because such sites should already be nearly saturated in 10 mM Mg2+ (Shi and Cui, 2001
; Zhang et al., 2001
; Hu et al., 2006
). Thus the E374A/E399N results confirm that occupancy of a very low affinity Mg2+ site is required to increase L0.
The R167E mutant was used to better quantify the effects of Mg2+ on L0 (Fig. 5, D and E). R167E is activated strongly by 100 mM Mg2+ but achieves a limiting slope at voltages
100 mV more positive than the WT (Fig. 5 D, dotted lines). Thus L0 can be determined at voltages that are sufficiently negative to achieve a limiting slope but not too extreme to prevent steady-state recording. The effects on L0 of 10 and 100 mM Mg2+ were determined from the change in NPO at –80 mV in patches where Mg2+ was repeatedly applied and washed out. The results confirm that 10 mM Mg2+ has little or no effect on L0 (1.06 ± 0.05-fold change, n = 10), whereas 100 mM Mg2+ increased L0 by a factor of 2.24 ± 0.23 (n = 5)(Fig. 5 D, inset).
Mg2+ Enhances Voltage Sensor Activation when Channels Are Open
The voltage dependence of PO in the WT channel provides further evidence that Mg2+ enhances voltage sensor/gate coupling. According to Scheme 1, the equilibrium constant for voltage sensor activation when channels are open (J0D) is directly proportional to D. Therefore the charge–voltage relation for open channels (Qo-V), should be shifted to more negative voltages by Mg2+ if coupling is enhanced. Although BK channel voltage sensors can move when channels are open, determination of Qo from gating currents is difficult because channels close rapidly (Horrigan and Aldrich, 1999
). However, Qo can be assessed in a model-independent fashion from the logarithmic slope of the Po-V relation (Horrigan and Aldrich, 2002
). The mean activation charge displacement (qa = kTd(ln[Po])/dV) exhibits a bell-shaped dependence on voltage that is plotted in Fig. 5 E for 0, 10, and 100 mM Mg2+. qa is expected to approximate Qo at voltages where both PO and Qc are small (Horrigan and Aldrich, 2002
; Ma et al., 2006
). Thus the Qo-V relation is approximated by the foot of the qa-V relation at negative voltages, and is markedly left-shifted by Mg2+, indicating that voltage sensor activation is enhanced when channels are open.
To estimate the increase in voltage sensor/gate coupling by Mg2+ we fit the foot of the mean qa-V relations with a function predicted by Scheme 1 to describe Qo: Qo = zl + 4zJB(V), where B(V) is a Boltzmann function with charge zJ and half activation voltage VhO (Fig. 5 E, solid curves). The fits indicate that VhO is shifted by –60 ± 3 mV and –92 ± 4 mV in 10 Mg2+ and 100 Mg2+, respectively. Changes in the coupling factor D can be determined by comparing the shift in QO (
VhO) to that in QC (
VhC). QO depends on both D and J0, whereas QC depends only on J0. Therefore the quantity 
VCO = [
VhC –
VhO], plotted in Fig. 5 F for WT and E374A/E399N channels, should depend only on D (i.e.,
D = exp(zJ
VCO/kT), based on Scheme 1). Fig. 5 F indicates 
VCO = 43 ± 3 mV in 10 mM Mg2+, corresponding to a 2.7-fold increase in D. 100 mM Mg2+ produces a larger 
VCO (56 ± 4 mV), corresponding to a 3.6-fold increase in D, that probably represents the effect of saturating the RCK1 site. 
VCO for the E374A/E399N mutant is not significantly different from 0 (P < 0.05, t test) in 10 or 100 Mg2+ (Fig. 5 F), implying that all changes in voltage sensor/gate coupling can be attributed to the RCK1 site.
Modeling the Effects of Mg2+ on Steady-State Activation
The above results suggest that 10 mM Mg2+ acts primarily at the RCK1 binding site to enhance voltage sensor/gate coupling (D) with a minor effect on the voltage equilibrium (J0), and that 100 mM Mg2+ causes additional increases in D, J0, and L0 that reflect action at both RCK1 and very low affinity binding sites. To confirm that these parameter changes are sufficient to describe the effects of Mg2+ on steady-state activation and to better quantify the changes in D we fit simultaneously the log(PO)-V, qa-V, and PO-V relations for 0, 10, and 100 mM Mg2+ using Scheme 1, as defined by Eq. 1:
![]() | (1) |
The 0 Mg2+ data were fit by setting charge parameters to values determined previously (zJ = 0.58 e, zL = 0.3 e) (Horrigan and Aldrich, 2002
) and allowing all other parameters (J0, L0, D) to vary, yielding results (Table I, WT 0 Mg2+) similar to previous reports (Horrigan and Aldrich, 2002
; Ma et al., 2006
).
To fit the Mg2+ data, the change in J0 relative to 0 Mg2+ was set by gating current measurements (
VhC, Fig. 3 F), while L0 and D were allowed to vary. Excellent fits to the log(PO)-V and qa-V relations were obtained in this way (Fig. 5, B and E, dotted curves), with 10 Mg2+ increasing D by a factor of 2.14, and 100 Mg2+ causing a greater increase in D (2.83-fold) together with a 2.43-fold increase in L0 (Table I, WTA parameters). A similar procedure was used to fit the E374A/E399N data (Fig. 5 C, dotted curves), yielding values of D (Table I, E374A/E399N parameters) that vary by <15% relative to the control, which is within the resolution of our measurement (Ma et al., 2006
). Thus, shifts in Vhc determined from gating currents together with an increase in L0 in 100 Mg2+ appear sufficient to account for the changes in log(PO)-V when the RCK1 site is disrupted.
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To account explicitly for the effects of Mg2+ binding on the parameters in Scheme 1 we modeled the effects of very low affinity and RCK1 binding sites in terms of Schemes 2 and 3, respectively (Fig. 2, F and G). These allosteric mechanisms assume that Mg2+ can bind to any state of the channel defined by Scheme 1 and that effects of Mg2+ on the relative stability of different states therefore reflect the relative affinity of Mg2+ for these states. This principal is illustrated in Fig. 5 (G and H) by alternative representations of Schemes 2 and 3 that include the four states (CR, OR, CA, OA) and equilibrium constants defined by Scheme 1 for a single subunit, where boxes and associated allosteric factors indicate the states that are stabilized relative to the CR state by ligand binding. In Scheme 2, the action of Mg2+ is defined by its dissociation constant for the CR state (KD) and two allosteric factors (C and E). C defines the increase in affinity associated with channel opening, such that KD is reduced C-fold for the OR and OA states (Fig. 5 G, labeled box). Likewise, E defines the change in KD associated with voltage sensor activation (Fig. 5 G, CA and OA states). These changes in affinity can account for effects of Mg2+ on the equilibria for channel opening (L0) and voltage sensor activation (J0). However, voltage sensor/gate coupling (D) is unchanged in Scheme 2 because the effects of C and E are independent and neither alters binding in a manner that depends on the state of both the voltage sensor and gate. By contrast, in Scheme 3, D is increased F-fold upon ligand binding by assuming that the affinity of the open-activated state (OA) is increased relative to all other states by an allosteric factor F. Scheme 3 also includes an independent effect of voltage sensor activation on Mg2+ affinity (E-factor) as in Scheme 2, to account for effects on J0.
The data in Fig. 5 (A and B) were fit (red curves, Table II parameters) by a two-site model that assumes the channel contains a single RCK1 (site 1, Scheme 3) and a very low affinity (site 2, Scheme 2) binding site in each of four identical subunits, yielding Eq. 2 (see below), where L, J, and D are defined as in Eq. 1; E1, F1 and C2, E2 are allosteric factors for sites 1 and 2, respectively; and Ki = [Mg2+]/KDi (i = 1,2), where KDi is dissociation constant for each binding site in the CR state.
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VhC attributed to the RCK1 site, whereas a larger F1-factor of 2.0 was required to explain the enhancement of voltage sensor/gate coupling. The site 2 (very low affinity) parameters were not as well constrained because few concentrations >10 mM were tested and the effect of saturating this site was not determined.
Effects of Mg2+ on Ig Kinetics and the Deactivation Pathway
Although gating current is relatively insensitive to Mg2+ when channels are closed (Fig. 3), the ability of Mg2+ to shift the Qo-V relation implies that Ig kinetics must be altered when channels are open. Such an effect is evident from OFF gating currents (IgOFF) following pulses of different duration (0.05–20 ms, +200 mV) in 0 and 10 mM Mg2+ (Fig. 6 A).
Normalized IgOFF traces (Fig. 6 B) show that OFF kinetics following brief pulses (
0.1 ms, red traces), that are comparable to the delay in IK activation (Horrigan et al., 1999
) and open few channels, are similar in 0 or 10 Mg2+. However, as pulse duration increases and channels open, voltage sensor deactivation is slowed, reflecting that Qo-V is shifted to more negative voltages than Qc-V (Horrigan and Aldrich, 1999
). The slowing of IgOFF occurs in 0 Mg2+ but is more prominent in 10 Mg2+ (Fig. 6 B) because Mg2+ increases the difference between QO and QC (Fig. 5 F) and the fraction of channels that open at +200 mV (Fig. 2 B).
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Fast,
Med,
Slow) reflecting the predicted pathways of voltage sensor deactivation (Horrigan and Aldrich, 1999
Fast) representing the deactivation of voltage sensors in closed channels (C4 to C0 transitions in Scheme 1*). QOFF for open channels is characterized by a component representing the deactivation of voltage sensors when channels are open (Fig. 6 D, Med) and another that is rate limited by channel closing (Fig. 6 D, Slow). Therefore, QOFF following prolonged depolarizations to +200 mV (0, 10 Mg [open], Fig. 6 C) are well fit by triple exponential functions where the fast component is small because most channels are open. This analysis confirms that voltage sensor deactivation in open channels (
Med, Fig. 6 C, dotted red lines) is slowed (2.3-fold) by 10 mM Mg2+. In addition
Slow (Fig. 6 C, solid red lines) is increased 1.5-fold, consistent with a slowing of channel closing by Mg2+.
Further insight into the mechanism of Mg2+ action is provided by plotting the amplitude of the three OFF components (QFast, QMed, QSlow) versus pulse duration (Fig. 6 E). As pulse duration increases, QFast is reduced while QMed and QSlow increase, following the exponential time course of channel opening (solid curves Fig. 6 E) (Horrigan and Aldrich, 1999
, 2002
). These kinetics are similar in the presence and absence of Mg2+ because 10 mM Mg2+ has little effect on activation kinetics (Shi and Cui, 2001
; Zhang et al., 2001
). However the relative amplitudes of QMed and QSlow are reversed by Mg2+. The change in relative amplitude of QMed and QSlow by Mg2+ is qualitatively similar to the effect of recording IgOFF at a more positive voltage in 0 Mg2+ (Horrigan and Aldrich, 1999
), supporting that Mg2+ shifts Qo to more negative voltages. In the absence of Mg2+, QMed is greater than QSlow because voltage sensors can completely deactivate at –80 before channels close (Fig. 6 D, 0 Mg2+ light blue arrow). That is, the Qo-V relation in 0 Mg2+ indicates that voltage sensors equilibrate to the resting state at –80 mV (Fig. 5 E). By contrast, in 10 Mg2+ more than 25% of voltage sensors should remain activated at –80 mV wh