Vol. 279, Issue 1, H76-H85, July 2000
Mechanism of effect of extracellular pH on
L-type Ca2+ channel currents in human mesenteric
arterial cells
Sergey V.
Smirnov1,
Gregory A.
Knock1,
Andriy E.
Belevych2, and
Philip I.
Aaronson1
1 Division of Pharmacology and Therapeutics, Centre for
Cardiovascular Biology and Medicine, King's College London, London SE1
7EH, United Kingdom; and 2 Department of Nerve-Muscle
Physiology, Bogomoletz Institute of Physiology, Kiev-24, Ukraine
 |
ABSTRACT |
Extracellular pH (pHo) influences vasoconstriction partly
by modulating Ca2+ influx through voltage-gated
Ca2+ channels in the vasculature. The mechanism of this
effect of pHo is, however, controversial. Using the whole
cell voltage-clamp technique, we examined the influence of
pHo on L-type Ca2+ channel currents in isolated
human mesenteric arterial myocytes. Acidification to pH 6.2 and
alkalinization to 8.2 from 7.2 decreased by ~50% and increased by
25-30%, respectively, the peak amplitude of Ca2+ and
Ba2+ currents (1.5 and 10 mM), with an apparent
pKa of 6.8. Activation and inactivation of
Ca2+ and Ba2+ currents were shifted toward
positive membrane voltages during acidification and in the opposite
direction during alkalinization. The relationship between the current
amplitude and shifts in the gating parameters in solutions of different
pHo conformed closely to that predicted by the Gouy-Chapman
model, in which the divalent cation concentration at the outer surface
of the membrane varies with the extent to which protons neutralize the
membrane surface potential.
vascular smooth muscle cells; mesenteric artery; calcium
channels
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INTRODUCTION |
IT IS WELL KNOWN
that voltage-gated Ca2+ channel currents in a variety of
tissues are modified by alterations in extracellular pH
(pHo). Reduction of pHo below the control value
of 7.2-7.4 (acidification) caused a decrease in the
Ca2+ channel current amplitude in tunicate egg cells
(20), guinea pig ventricular myocytes (13,
17, 29), and hybridoma cells (11). Alkalinization caused the opposite effect. The
reduction/enhancement of the Ca2+ channel current during
acidification/alkalinization was explained by a decrease/increase in
the surface concentration of the charge-carrying ion near the
Ca2+ channel mouth because of alterations in surface
potential created by the interaction of protons with fixed negative
charges on the outer surface of the cell membrane (11,
17, 20). Simultaneous displacements of the
voltage dependencies of activation and inactivation were also ascribed
to surface potential effects (17, 20). In
addition, it has been shown that extracellular protons can have a
direct action on Ca2+ channel conductance state
(23).
Although it is known that acidosis is associated with vasodilatation,
the relative roles of intracellular pH (pHi) and
pHo in causing vascular relaxation are controversial
(5, 8, 12, 27).
Surprisingly, the effects of pHo on voltage-gated Ca2+ channel currents in single vascular smooth muscle
cells (SMCs) have received limited attention. Decreasing
pHo caused an inhibition of the Ba2+ current
through voltage-gated Ca2+ channels in guinea pig cerebral
arterial cells (30). Prominent changes in current kinetics
were also described, but significant shifts in the current-voltage
(I-V) relationship associated with changing pHo
were absent. On the other hand, alteration of pHo caused
changes in the Ca2+ channel current amplitude and in the
voltage dependencies of channel activation and inactivation in single
bovine pial and porcine coronary arterial myocytes (14).
These divergent observations may have reflected differences in the
regulation of activity of Ca2+ channels by pHo
in various vascular SMCs.
Therefore, to investigate the mechanism of the modulation of L-type
Ca2+ channels by extracellular protons in SMCs isolated
from human mesenteric arteries (HMAs), the effect of pHo on
the amplitude, kinetics, and voltage dependencies of activation and
inactivation of the Ca2+ channel current was examined. The
current was studied in the presence of physiological (1.5 mM) and high
(10 mM) concentrations of Ca2+ and also in the same
concentrations of Ba2+. The effect of pHo on
the noninactivating "window current" (25) measured in
the presence of 10 mM Ba2+ was also studied. Our results
suggest strongly that the alteration of the Ca2+ current by
pHo can be explained primarily by changes in the surface concentration of divalent cations in the vicinity of the mouth of the
Ca2+ channel in these cells.
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MATERIALS AND METHODS |
Human mesenteric (omental) arteries were obtained from the fat
attached to sections of stomach or small or large bowel removed during
routine surgery at St. Thomas's Hospital (London). This procedure was
approved by the St. Thomas's Ethical Committee.
Methods of SMC isolation, current recording, and data analysis have
been described in detail previously (25, 26).
The external solution had the following composition (mM): 130 NaCl, 1 CsCl, 1.2 MgCl2, 1.5 CaCl2, 4 tetraethylammonium chloride, 10 HEPES, and 10 glucose. NaOH was used to
adjust the pH of the solution to 6.2, 7.2, or 8.2. In some solutions,
1.5 mM Ba2+, 10 mM Ca2+, or 10 mM
Ba2+ replaced 1.5 mM Ca2+. In 10 mM
Ba2+- or Ca2+-containing solutions, NaCl was
reduced to 120 mM. At pH 9.2, 5 mM HEPES was replaced with 5 mM
2-(N-cyclohexylamino)ethanesulfonic acid in the
Ba2+-containing solution. The pH in this solution fell
during experiments to 9.15-9.02, probably because of a slow
precipitation of Ba2+ by hydroxide ions. This difference
was considered negligible. The pipette solution contained (mM) 135 CsCl, 2.5 MgCl2, 2 Na2ATP, 10 HEPES, and 10 EGTA, and its pH was adjusted to 7.2 with NaOH. Basic chemicals were
purchased from BDH (Poole, UK); HEPES,
2-(N-cyclohexylamino)ethanesulfonic acid, EGTA, and
tetraethylammonium chloride were obtained from Sigma Chemical (Poole, UK).
Ca2+ and Ba2+ currents through L-type
Ca2+ channels were measured in whole cell voltage-clamp
mode at room temperature and analyzed using pClamp 6.0 software (Axon
Instruments). We previously described T- and L-type voltage-gated
Ca2+ channel current in HMA myocytes. The L-type
Ca2+ channel current, which dominated in these cells, was
the main subject of the present investigation. T-type current was
eliminated by using a holding potential of
60 mV (25).
To compare activation for L-type Ca2+ channel currents, a
standard voltage protocol was applied. Cells were held at
60 mV, and
Ca2+ or Ba2+ current was recorded using 100-ms
depolarizing voltage steps applied at 5-mV increments from
70 to +80
mV. The I-V relationship was initially recorded at
pHo 7.2 and then repeated at the test pHo in
the same cell. Peak current amplitude was measured at each membrane
potential and converted to current density, which was calculated as the
ratio of the current amplitude to the cell membrane capacitance with
the assumption of a specific membrane capacitance of 1 µF/cm2. The cell membrane capacitance was determined from
the area under the capacitive transients elicited by a 10-mV
hyperpolarizing pulse of 5-ms duration recorded with 50-kHz filtering.
Values are means ± SE. The significance of an experimental value
was determined using Student's paired or unpaired t-test as
appropriate, with P < 0.05 considered to be
significant, unless otherwise stated.
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RESULTS |
Effects of acidification and alkalinization on activation and
inactivation of L-type Ca2+ currents.
Figure 1A shows families of
Ca2+ currents recorded in the same HMA cell at 6.2, 7.2, and 8.2 pHo. A decrease in pHo from 7.2 to 6.2 caused a diminution of the Ca2+ current from 57 to 33 pA at
+10 mV and from 40 to 10 pA at
10 mV. Alkalinization to
pHo 8.2 produced the opposite effect on the
Ca2+ current, increasing its amplitude by 1.4 and 1.9 times
at +10 and
10 mV, respectively. The effects of altering
pHo were completely reversible in this and all other
external solutions tested (data not shown).

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Fig. 1.
Effect of various extracellular pH (pHo)
levels on Ca2+ channel current (ICa)
at 1.5 mM external Ca2+. A:
ICa recorded at pHo 6.2, 7.2, and
8.2 at 10-mV increments between 40 and 0 mV (top) and +10
and +40 mV (bottom). Holding potential was 60 mV; dashed
lines, zero current. Currents at each pHo were recorded
from the same cell with a membrane capacitance of 45 pF. B:
averaged current-voltage (I-V) curves recorded at
pHo 7.2 (n = 8), 6.2 (n = 5), and 8.2 (n = 6) and expressed as current densities.
Vm, membrane potential. C:
mean I-V curves normalized to peak
ICa in each cell at pHo 6.2, 7.2, and 8.2.
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Figure 1B shows the mean I-V relationships for
the peak of the Ca2+ current recorded at each membrane
potential and converted to current density, as described in
MATERIALS AND METHODS. The maximal peak amplitude of the
Ca2+ current was decreased by 50 ± 4% during
external acidification to 6.2 and increased by 38 ± 5% when
pHo was increased to 8.2 in comparison to those measured at
pHo 7.2 in five and six cells studied, respectively. The
nadir of the I-V relationship also occurred at progressively
more-negative membrane potentials as the pHo was raised,
shifting from approximately +15 mV at pHo 6.2 to between +5
and 0 mV and between 0 and
5 mV at pHo 7.2 and 8.2, respectively (Fig. 1C). This suggested that channel
activation was affected by changes in pHo
(20). To determine the parameters of activation for
Ca2+ current at different pHo, each
I-V curve for Ca2+ current was normalized to its
peak, as shown in Fig. 1C, and was described using the
following equation
|
(1)
|
where I is the amplitude of the normalized
Ca2+ current, V and Er
are the membrane and apparent reversal potentials for Ca2+
current, g is a scaling factor, and m is the
Boltzmann function for activation described by the following equation
|
(2)
|
in which Vm is the half-activation
potential and km is the slope factor. Parameters
Er, Vm,
km, and g (the latter ranged between
0.02 and 0.06) were varied in each individual cell at each
pHo to obtain the best fit of the I-V curves.
The mean Vm values at various pHo
levels are compared in Table 1. This
comparison showed that acidification had a significantly larger effect
on the half-activation potential for Ca2+ current than did
alkalinization. Under these conditions, km
varied between 6.2 and 10.3 mV in various HMA cells, with mean values of 8.1 ± 0.9 (n = 5), 7.8 ± 0.6 (n = 8), and 7.6 ± 0.6 (n = 6) mV
at pHo 6.2, 7.2, and 8.2, respectively, which were not
significantly different. Similarly, g and
Er values were also not significantly affected
by altering pHo.
The effect of pHo on the steady-state inactivation of the
Ca2+ current was studied in a separate set of experiments.
Cells were placed into an external solution with a given
pHo and were stimulated with a 30-s conditioning potential
applied in the voltage range of
100 to +20 mV in 10-mV increments
followed by a short (150-ms) test pulse to +20 mV (pHo 6.2)
or +10 mV (pHo 7.2 and 8.2; Fig. 2A). The steady-state
inactivation-potential relationships thus obtained were then normalized
with respect to the magnitude of Ca2+ current recorded
after the prepulse to
100 mV and fitted with the Boltzmann function
(similar to Eq. 2) in each cell at each pHo. The
averaged steady-state inactivation dependencies obtained at
pHo 6.2, 7.2, and 8.2 are presented in Fig. 2B.
These results, as well as the analysis of individual data (Table
2), showed that acidification caused a
significantly larger shift in inactivation dependencies for
Ca2+ current than did alkalinization.

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Fig. 2.
Modulation of steady-state inactivation for
ICa (1.5 mM) by pHo. A: a
family of ICa recorded at a 150-ms test
potential (Vt) to +10 mV (pHo 7.2 and 8.2) and +20 mV (pHo 6.2) after a series of 30-s
preconditioning steps to various voltages (Vc).
Cell membrane capacitance was 48 pF. Dashed lines, zero current.
Voltage protocol is shown at top. The interpulse interval
was 30 ms. B: steady-state inactivation dependencies for
ICa averaged for 5 (pHo 6.2), 13 (pHo 7.2), and 9 (pHo 8.2) cells. Solid lines,
theoretical fit according to the Boltzmann equation with
half-inactivation potentials (Vh) equal to
23.1, 32.4, and 36.3 mV and slope factors
(kh) equal to 11.3, 9.3, and 9.2 mV at
pHo 6.2, 7.2, and 8.2, respectively. Vertical dashed lines,
Vh.
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Effects of acidification and alkalinization on the Ca2+
channel current in high Ca2+- and
Ba2+-containing solutions.
Figure 3 presents the effect of varying
pHo on the I-V curves for the Ca2+
channel current recorded in 1.5 mM Ba2+, 10 mM
Ca2+, and 10 mM Ba2+. As described in
MATERIALS AND METHODS, the I-V relationship was
initially recorded at pHo 7.2 and then repeated at the test pHo in the same cell with the use of a standard voltage
protocol. For 1.5 mM Ba2+ and 10 mM Ca2+, the
pH was altered from the control pHo of 7.2 to 6.2 or 8.2; for 10 mM Ba2+, pHo was altered from 7.2 to
6.2, 8.2, or 9.2. In Fig. 3, the current recorded at pHo
7.2 is shown paired with the current obtained at one test
pHo. Figure 3 illustrates that the effect of changing pHo on the I-V curve was very similar for each
of the three external solutions examined and also closely resembled the
effect recorded in the solution containing 1.5 mM Ca2+
(Fig. 1).

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Fig. 3.
Effect of various pHo on L-type
ICa in the presence of low and high
concentrations of divalent cations. A and C:
Ba2+ currents (IBa) recorded in the
presence of 1.5 and 10 mM Ba2+, respectively; B:
ICa measured in 10 mM external Ca2+
with use of the same experimental protocol described in the legend of
Fig. 1. Currents are expressed as current densities. Data represent
means for 6 and 7 (A), 5 and 4 (B), and 10, 8, and 8 (C) paired human mesenteric arterial (HMA) cells
studied at pHo 6.2 and 8.2 (A and B)
and 6.2, 8.2, and 9.2 (C), respectively.
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Alteration of pHo caused no obvious changes in the decay of
the current, regardless of the external solution employed. The lack of
effect of pHo on current kinetics is apparent in Figs. 1
and 2 for the solution containing 1.5 mM Ca2+ and is
further emphasized by the fact that any particular alteration in
pHo always had very similar effects on the peak inward
current and the current at the end of a 100-ms depolarization. For
example, in 10 mM Ba2+ solution, at the nadir of the
I-V curve, the current measured at the end of the pulse was
0.4 ± 0.02, 1.4 ± 0.1, and 1.6 ± 0.1 times that at
pHo 7.2 for 10, 8, and 8 cells studied at pHo
6.2, 8.2, and 9.2, respectively. The peak inward current in these cells was 0.5 ± 0.02, 1.4 ± 0.1, and 1.6 ± 0.1 times that
measured at pHo 7.2 at pHo 6.2, 8.2, and 9.2, respectively.
Also the effect of pHo on the Ca2+ channel
current was more prominent at negative than at positive membrane
voltages (Fig. 3). For example, in 10 mM Ba2+,
acidification decreased the density of Ba2+ current by
about sixfold, from 0.6 ± 0.1 to 0.1 ± 0.02 µA/cm2 (n = 10), at
10 mV but only by
twofold, from 1.0 ± 0.1 to 0.5 ± 0.1 µA/cm2
(n = 10, P < 0.05), at +40 mV.
Similarly, in the group of cells in which pHo was increased
from 7.2 to 9.2, Ba2+ current was significantly enhanced
from 0.7 ± 0.1 to 1.6 ± 0.2 µA/cm2
(n = 8) at
10 mV and showed only a nonsignificant
increase from 1.0 ± 0.2 to 1.4 ± 0.3 µA/cm2
(n = 8) at +40 mV (Fig. 3C). A similar
potential dependency of the effect of pHo on
Ca2+ current in 1.5 mM Ca2+ is also apparent in
Fig. 1.
The similarity between the effects of pHo on the
Ca2+ channel current recorded in each of the four solutions
is emphasized in Fig. 4, which compares
the extent to which the mean current density at the peak of the
I-V curve was altered by acidification and alkalinization in
each case. The effect of pHo on the current in 10 mM
Ba2+, the solution in which the widest range of
pHo was examined, was fitted using the equation shown in
the legend to Fig. 4. This curve predicted a 60% maximal enhancement
of current through L-type Ca2+ channels in HMA cells,
compared with the current measured at pHo 7.2, as a result
of strong alkalinization. The effects of pHo in each of the
other three solutions were virtually indistinguishable from those
observed in 10 mM Ba2+.

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Fig. 4.
Relationship between pHo and the peak L-type
ICa measured at the nadir of the I-V
curve. IP,pH/IP,7.2
represents the ratio of the peaks of ICa or
IBa at test pHo to that at
pHo 7.2, respectively, at each divalent cation
concentration. The line was drawn according to the following equation:
IP,pH/IP,7.2 = Amax/[1 + 10(pKa pH0)n],
where Amax, the maximal saturated ratio, was
1.6, the apparent pKa value was 6.8, and
n, the apparent Hill coefficient, was 0.6.
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The I-V curves from each of the individual experiments
carried out in 10 mM Ca2+ and in both concentrations of
Ba2+ were analyzed as described above for Ca2+
current in 1.5 mM Ca2+ to determine the effect of
pHo on the half-activation potentials. These are listed in
Table 1. The extent to which changing pHo affected the
steady-state inactivation of the Ca2+ channel current was
also studied in each of these three external solutions by use of the
voltage protocol described in Fig. 2, and the data are shown in Table
2. Neither km nor kh
(slope factor) values derived from activation and inactivation
experiments, respectively, were significantly affected by alterations
in pHo (data not shown). A comparison of the shifts in the
half-activation (Vm) and half-inactivation (Vh) potentials for the Ca2+ channel
current at different pHo showed in all cases that
alkalinization to pHo 8.2 caused smaller shifts in both
parameters than did acidification to pHo 6.2. Although
there was some variability in the extent to which changing
pHo altered Vm and
Vh in the different solutions, no clear trends
that would suggest that the effect of pHo on gating differed greatly between solutions were apparent.
Effects of changing pHo on the Ca2+ channel
window current.
Figure 5 depicts the normalized
steady-state inactivation dependencies together with the activation
curves (generated using the mean values of km
and Vm at each pHo) for the
Ca2+ channel current recorded in 10 mM Ba2+
physiological saline solution, the solution in which the greatest range
of pHo was studied. Figure 5 illustrates the extent to
which activation and inactivation of the Ca2+ channel
current were displaced to more-negative voltage ranges as
pHo was increased. The shift in the inactivation curve
would be expected to have little effect on the current, since even at pHo 9.2, Ba2+ current is almost completely
available at a holding potential of
60 mV. On the other hand, the
position of the activation curve is such that its displacement should
have an important effect on current amplitude, especially at negative
potentials.

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Fig. 5.
Effect of pHo on steady-state activation and
inactivation of IBa in 10 mM external
Ba2+. Activation and inactivation curves (lines) were
generated using Boltzmann equations, with mean
Vm and Vh values shown in
Tables 1 and 2, respectively. Mean km values
were 6.3, 6.4, 7, and 6.4 mV and mean kh values
were 8.1, 8.2, 9.5, and 10.5 mV at pHo 6.2, 7.2, 8.2, and
9.2, respectively. Symbols show IBa normalized
with respect to the current recorded after the conditioning potential
to 100 mV. Dashed lines, half-activation and half-inactivation
potentials.
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The overlap of the activation and inactivation curves was also
increased and shifted to more-negative potentials as pHo
was increased. This would predict that the noninactivating window current, which we previously demonstrated in these cells
(25), should be progressively suppressed as
pHo is reduced. To evaluate this more directly, the
noninactivating window current in the 10 mM Ba2+ solution
was measured using 30-s membrane depolarizations to
10 and 0 mV from
a holding potential of
60 mV at control pHo 7.2 and at
two test pHo, 6.2 and 8.2. This solution was used because it gave the largest and most stable Ca2+ channel current.
The result of one such experiment, where Ba2+ current was
recorded during membrane depolarization to
10 mV, is shown in Fig.
6A. The whole cell inward
Ba2+ current was blocked by 0.5 mM Cd2+ at the
end of the experiment, and the window Ba2+ current was
measured as the Cd2+-inhibitable sustained current
(25). The example shown in Fig. 6A demonstrates
that alkalinization of the external solution increased the window
Ba2+ current by 33%, whereas acidification inhibited this
current by 57%. The sustained current measured in five cells under
these conditions at test potentials of
10 and 0 mV was converted to current density and is plotted against pHo in Fig.
6B. The lines connect the mean current density calculated at
each pHo. The current amplitude measured during such
prolonged membrane depolarizations at various pHo in the
same cell may be underestimated because of a subsequent rundown of the
current (from 5 to 40%) often observed during prolonged cell
stimulation.

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Fig. 6.
Effect of pHo on the window
IBa. A: IBa
(10 mM) measured using 30-s steps to 10 mV from the holding potential
of 60 mV at pHo 6.2, 7.2, and 8.2 and in the presence of
0.5 mM Cd2+. Cell capacitance = 32 pF. B:
window IBa (measured as
Cd2+-sensitive current at the end of 30-s voltage step and
presented as current densities) recorded at test potentials of 10 and
0 mV at pHo 6.2, 7.2, and 8.2. Each symbol represents a
different HMA cell. Solid lines connect mean values calculated for each
pHo.
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Role of pHi.
Although the pipette solution contained 10 mM HEPES to buffer
pHi, it is possible that the changes in pHo
were causing corresponding alterations in pHi that
contributed to the observed effects of different pHo on the
Ca2+ channel current. To evaluate this possibility, the
concentration of HEPES in the pipette solution was increased to 100 mM
(the concentration of CsCl was reduced to 80 mM accordingly). Effects of pHo 6.2, 7.2, and 8.2 on activation and inactivation of
Ba2+ current in 10 mM Ba2+ were then compared
using the same experimental approach described above. Acidification of
the external solution to 6.2 decreased the peak Ba2+
current amplitude by 46 ± 7% (n = 4), and
alkalinization increased the peak current by 38 ± 3%
(n = 6; data not shown). These values were not
significantly different from those measured with 10 mM HEPES in the
pipette solution (54 ± 2 and 42 ± 7%, n = 10 and 8, respectively). In addition, similar shifts in activation and inactivation dependencies were found (Tables 1 and 2). These results
strongly suggest that changes in the pHi either did not occur in 10 mM HEPES or did not affect the properties of the current we
recorded. This implies that the observed changes in the
voltage-dependent characteristics during external acidification or
alkalinization were entirely caused by the effects of external protons
on L-type Ca2+ channels.
Apparent voltage dependence of the effect of pHo is due
to the shift in activation gating.
As noted above, the effect of pHo on Ca2+
channel currents was more prominent at negative than at positive
potentials. A comparison of the pHo dependency of
Ca2+ (1.5 mM Ca2+) and Ba2+ (10 mM
Ba2+) current ratios at
10 and +10 mV is presented in
Fig. 7 (left). Ca2+ and Ba2+ currents were clearly more
pHo dependent at
10 than at +10 mV. This is unlikely to
be due to differences in the concentration of divalent cations at the
membrane surface (see below), since the surface potentials at
10 and
+10 mV should be the same for any given pHo. One possible
explanation could be that the current amplitude at any one potential
would be influenced by the pHo-mediated shifts in current
activation that we have described above (effects on current
availability with a holding potential of
60 mV were small enough to
be ignored). To examine this possibility, we divided Ca2+
or Ba2+ current at
10 mV by the fraction of
Ca2+ channels activated at this potential (calculated using
Eq. 2). This was done at each pHo tested. The
resulting currents thus adjusted for activation or inactivation were
then expressed as a fraction of the adjusted current at pHo
7.2. This process was then repeated for both currents at +10 mV. The
resulting corrected pHo dependencies for Ca2+
and Ba2+ currents are shown in Fig. 7 (right)
and represent effects of pHo on the current that were
independent of shifts in current activation. This correction resulted
in the pHo dependencies of the current at
10 and +10 mV
becoming almost superimposable (Fig. 7, right). Once
corrected as described, the pHo dependency of the current
amplitude at various potentials followed closely that shown in Fig. 4
for the peak current. Similar results were also obtained from the
analysis of Ca2+ and Ba2+ recorded in 10 mM
Ca2+ and 1.5 mM Ba2+, respectively (not shown).
These results therefore suggest that the apparent potential dependence
of the effect of pHo on Ca2+ and
Ba2+ current amplitudes is mainly due to the shift in
current activation.

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Fig. 7.
Apparent potential dependency of the effect of
pHo on L-type ICa. A and
B: normalized ICa (1.5 mM) and
IBa (10 mM), respectively, recorded at test
potentials of 10 and +10 mV before (left) and after
(right) correction for activation. The current amplitude at
each test potential at a given pHo was normalized to that
at pHo 7.2 and presented on left as
ICa,pH/ICa,7.2
(A) or
IBa,pH/IBa,7.2
(B). In each cell at each test potential, the current was
divided by the fraction of channels activated at that potential
(calculated using Eq. 2) to correct current amplitude for
activation. The resulting values at each pHo were
normalized to that at pHo 7.2 and are expressed as
ICa,pH*/ICa,7.2*
for ICa (A) and
IBa,pH*/IBa,7.2*
for IBa (B).
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Role of the surface potential in the effects of pHo on
Ca2+ channel currents.
It is generally accepted that the shift in I-V relationships
for voltage-gated Ca2+ channels, caused by changing the
extracellular concentration of divalent cations or protons, is due to
the interaction of these cations with negative membrane surface charges
that form a surface potential in the vicinity of the channel
(6, 7, 20, 31). Increasing the concentration of protons, for example, results in a
decline of the surface potential due to binding to and/or screening of
negative surface charges. This leads to an increased transmembrane
potential (as the potential between the bulk extra- and intracellular
solutions remains the same) and, as a result, a shift of activation and
inactivation dependencies toward more-positive voltages.
Another theoretically predicted effect of decreasing or increasing the
surface potential is an alteration of the local concentration of
divalent cations near the Ca2+ channel mouth. This would
therefore affect the amplitude of the Ca2+ channel current
carried by these cations. As previously described (20),
there is an exponential relationship between the surface membrane
divalent cation concentration (SC) and the surface
potential (
o)
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(3)
|
where z is the valency (equal to 2), CC is
the bulk concentration of divalent cation, and F,
R, and T have their usual thermodynamic definitions. As reported previously (20),
Vm or Vh can be chosen as
a measure of changes of
o. In case of shifts in
Ca2+ channel activation,
o =
Vm + B, where B is a
constant (20). If the peak amplitude of Ca2+
and Ba2+ currents at different pHo shown in
Fig. 4 is directly related to the SC, Eq. 3
predicts a linear relationship between the shift in the
voltage-dependent characteristics of L-type Ca2+ channels
and changes in the logarithm of the peak current amplitude with a slope
of RT/2F, equal to 25 mV. Figure
8 shows semilogarithmic plots of the
relationship between the peak current amplitude and its relative shifts
in activation and inactivation for each of the four solutions used. The
line in each panel depicts the exponential relationship predicted by
Eq. 3, and it is apparent that, in general, most of the data
points lay very close to this line.

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Fig. 8.
Correlation between ICa and
IBa peak amplitudes and the shifts in activation
( Vm) and inactivation
( Vh) dependencies in the presence of low (1.5 mM; A and C) and high (10 mM; B and
D) concentrations of divalent cation. Shifts in activation
for L-type ICa (mean ± SE) were determined
using the differences between Vm at a given
pHo and that at pHo 7.2 measured in individual
cells. Shift in inactivation is presented as the difference between the
mean Vh at a given pHo and that at
pHo 7.2. The current peak ratio
(ICa,pH/ICa,7.2 and
IBa,pH/IBa,7.2) was
normalized with respect to that at pHo 7.2. The correlation
between the normalized peak IBa amplitude and
the relative shifts in activation (open symbols) and inactivation
(closed symbols) was plotted using a logarithmic ordinate. Lines in
each plot show the predicted theoretical relationship described in
Eq. 3 with a slope of 25 mV.
|
|
Do these changes in the current amplitude correlate with the changes in
SC predicted to occur as a result of pHo
modulation of
o? Because the absolute value of
o is unknown, it is impossible to calculate
SC directly by Eq. 3 at each particular
pHo (20). However, it is possible to calculate
relative changes with respect to a particular pHo (e.g.,
7.2). In this case, Eq. 3 becomes
|
(4)
|
Because CC at each tested pHo and 7.2 is
the same, its ratio will be equal to 1. Figure
9 illustrates the mean changes in SC, normalized relative to pHo 7.2, based on
the shift in activation calculated in each cell and inactivation, for
each of the four conditions tested. The mean changes in the peak
current amplitude at different pHo, again normalized
relative to pHo 7.2, are also shown. It is apparent from
Fig. 9 that the peak current amplitude during acidification and
alkalinization conforms closely to that which would be predicted on the
basis of pHo-mediated changes in
o and
resulting alterations in SC.

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Fig. 9.
Comparison between pHo-dependent changes in
the peak L-type ICa and predicted changes in the
surface membrane concentration of divalent cations. Filled symbols and
lines, ICa ( in A,
in B) and IBa
( in C, in D;
IP,pH) in the presence of 1.5 (A and
C) and 10 (B and D) mM divalent
cation. Open symbols, predicted changes in the surface membrane
concentration for Ca2+ and Ba2+
(SC,pH). The ratio SC,pH/SC,7.2 was
calculated according to Eq. 4 by using the mean shifts in
activation, calculated using the differences between
Vm at the test pHo and at 7.2 in
individual cells ( ), and in inactivation, determined as
the difference between the mean Vh at a given
pHo and at pHo 7.2 ( ). The peak
amplitude of ICa or IBa
measured at a given pHo was normalized with respect to that
at pHo 7.2.
|
|
 |
DISCUSSION |
These experiments provide the first detailed measurements of the
effect of changing pHo on the vascular smooth muscle L-type Ca2+ channel in the presence of a physiological
concentration of Ca2+ (1.5 mM). The results suggest that in
the presence of a normal or raised (10 mM) concentration of external
Ca2+, as well as in the same concentrations of
Ba2+, the degree of inhibition or enhancement of the
Ca2+ channel current during acidification or alkalinization
in HMA cells can be mainly explained in terms of the effect of protons on the surface membrane potential.
As described by the Gouy-Chapman equation (10,
11, 20), an increase in the proton
concentration should screen negative membrane surface charges in the
vicinity of the Ca2+ channel, resulting in a decrease in
the surface potential and a consequent increase in the genuine
transmembrane potential (since the potential between the bulk extra-
and intracellular solutions is clamped). This would decrease the number
of open Ca2+ channels in the physiological range of
membrane potentials because of the shift of the activation to the right
along the voltage axis (a "stabilizing" effect of protons on the
cell membrane). Channel inactivation would also be shifted in a
depolarizing direction. Opposite effects on gating would be expected
for alkalinization. As summarized in Tables 1 and 2, alteration of
pHo shifted the activation and inactivation curves in HMA
cells as expected in each of the four solutions examined. The magnitude
of the shifts was comparable to those measured previously in a number
of types of cells, including other vascular smooth muscles
(14, 17, 28, 33).
This type of shift in gating parameters should not greatly affect the
amplitude of the current at the peak of the I-V curve, since
this should be little affected by shifts in activation gating and since
steady-state inactivation at a holding potential of
60 mV is almost
pHo insensitive (Fig. 5). However, in addition to modifying
the voltage dependency of channel gating, acidification-mediated diminution of the surface potential should also reduce the
concentration of divalent cations near the extracellular channel mouth,
depressing the current amplitude (3, 9). This
phenomenon has been visualized as a reduction in the amplitude of the
unitary current on the single Ca2+ channel level, in, for
example, guinea pig ventricular (29) and bovine and
porcine vascular myocytes (14). Similarly, acidification of the trans-chamber, which corresponds to the external
side, reduced the unitary conductance of the cardiac and skeletal
sarcoplasmic reticulum Ca2+ release channels incorporated
into planar lipid bilayers (24).
The extent of this reduction in the divalent cation concentration at
the external surface of the membrane can be predicted using the shift
in gating parameters, as described by Eq. 4, and assuming
also that the channel mouth and the gating mechanism "see" similar
surface potentials. If it is assumed that the current amplitude is
linearly related to the surface concentration of divalent cation, it is
possible to compare the observed effects of pHo on peak
current amplitude with the effects that are expected on the basis of
surface potential-mediated changes in the surface divalent cation
concentration. As illustrated in Fig. 9, a generally good correlation
between changes in peak current amplitude and the predicted changes in
the surface concentration near the channel mouth was found for both
concentrations of Ca2+ and Ba2+ tested. This
result is analogous to the similarity between the observed change in
the unitary channel conductance and the surface divalent cation
concentration calculated from the shift in activation dependencies that
was previously found in bovine pial and porcine coronary arterial cells
(14).
An alternative explanation for the effect of pHo on
Ca2+ channel currents is that a competition between protons
and divalent cations for binding to negatively charged sites near or
within the channel pore would directly or indirectly block the movement of Ca2+ through the channel. However, most of the reports
that have considered this type of interaction have concluded that
significant alterations in Ca2+ permeation would not occur
unless pHo is decreased to <6 or unless highly artificial
conditions are employed (e.g., Ca2+-free conditions in
which a monovalent cation is used as the permeant species)
(14, 17, 21-23,
33). On the other hand, Klöckner et al.
(16) more recently observed a progressive decrease in the
conductance of the human cardiac L-type channel at pHo > 6 when 10 mM Ba2+ was used as the charge carrier, which
was abolished by replacement with alanine of one of the array of four
glutamate residues thought to constitute the intrapore Ca2+
selectivity filter (32). This study (16)
therefore suggested that a direct effect of protons on the permeation
mechanism might occur with physiological levels of pHo and
extracellular Ca2+ concentration.
It is unlikely, however, that this type of interaction can explain the
effects we have demonstrated in HMA cells, at least in the
pHo range of 6.2-9.2. The most striking finding of
this study is that the relationship between pHo and the
amplitude of the Ca2+ channel current at the peak of the
I-V curve was very similar in Ca2+ and
Ba2+ and at 1.5 and 10 mM. Under conditions in which a
competition between protons and divalent cations is influencing the
permeation mechanism, the effect of pHo on channel
conductance should be sensitive to the identity and concentration of
the divalent cation. The affinity of Ba2+ for the binding
sites within the L-type channel that govern permeation is lower than
that of Ca2+ (3, 9), and protons
should be less able to competitively displace Ca2+ and
Ba2+ from common binding sites when these divalent cations
are present at higher concentrations. Thus, if protons compete for
binding sites related to the permeation mechanism, it would be
predicted that the effect of pHo on the peak current
amplitude should be larger in Ba2+ than in Ca2+
and should also be larger at the lower concentration of both ions.
Instead, the effect of pHo was similar, even when the
extreme cases of 1.5 mM Ba2+ and 10 mM Ca2+
were compared. This finding is therefore consistent with the previous
suggestions that a competition between protons and Ca2+ for
the permeation pathway does not make an important contribution to the
effect of pHo on the Ca2+ current under normal
conditions. By the same token, this invariance of the effects of
pHo on the current through L-type Ca2+ channels
under all conditions tested further suggests that
pHo-dependent changes in the concentrations of divalent
cation at the outer mouth of the channel are likely to be due to
screening of the surface potential rather than a competition for
binding sites.
In summary, our overall results suggest that the inhibition or
enhancement of Ca2+ channel currents during extracellular
acidification or alkalinization in HMA myocytes occurs mainly via
alteration of the membrane surface potential, resulting in a shift in
potential-dependent channel gating and in changes in the concentration
of divalent cation near the external Ca2+ channel mouth.
The proposed explanation of the effects of pHo on the
Ca2+ channel currents in HMA myocytes can be directly
related to the regulation of vascular tone in general, since the
mechanism of action of pHo described above reflects a
common feature of Ca2+ channels in a number of different
tissues. It has been shown that Ca2+ channels are slightly
activated at the resting membrane potential in vascular SMCs and that
this activation is likely to play a role in the regulation of vascular
tone by vasoconstrictors and vasodilators (19). We
previously described in HMA cells a window current that could
contribute to a steady-state Ca2+ influx over the
physiological range of the membrane potentials (25). The
results of the direct measurement of the effect of pHo on
the noninactivating window Ba2+ current through L-type
Ca2+ channels showed that this occurs in HMA myocytes (Fig.
6). An analogous effect on the window Ca2+ current would be
also predicted, since a similar pHo dependence of the peak
amplitude of Ca2+ current and significant shifts in its
activation dependencies were observed. In this case, even a quite small
effect of pHo on the voltage dependency of current
activation that we have measured will lead to marked alterations in
Ca2+ influx.
Despite the well-known fact that acidosis causes vasodilatation and
alkalosis causes vasoconstriction in isolated arteries and also in vivo
(1), controversy exists as to whether these effects are
due to changes in pHo or in pHi. Under our
experimental conditions, the effects of pHo were
independent of the changes of pHi, as our results with 10 and 100 mM HEPES in the pipette solution demonstrated. In intact
vessels, however, effects on pHi associated with changes in
pHo (4) could also have an important impact on
the overall effects of acidification and alkalinization. It has been
recently shown that intracellular acidification also suppresses the
Ca2+ current in vascular SMCs, largely by reducing channel
availability (15). It is interesting, however, that Iino
et al. (12) showed a marked suppression of the
voltage-gated Ca2+ current in rabbit portal vein cells
during intracellular acidification with propionate and, at the same
time, reported that high K+ depolarization-mediated
increases in intracellular Ca2+ concentration and tension
development in the intact tissue are paradoxically enhanced under these
conditions (12). Tian and co-workers (27)
showed that reduction of pHo under conditions where
pHi was kept constant caused vasodilatation. Furthermore, although application of the sodium salts of the weak acids lactate and
butyrate caused vasodilatation of rat mesenteric resistance arteries,
this response persisted even if the resulting intracellular acidification was prevented by simultaneous addition of ammonium chloride to the solution (2, 18). These
observations point to a predominant role of pHo, rather
than pHi, in mediating the vasodilating effects of
acidosis. In agreement with this possibility, the present results and,
in particular, the steep dependency on pHo of the
Ca2+ channel window current (Fig. 6) indicate that
physiologically relevant levels of acidification are likely to result
in significant inhibition of Ca2+ influx and a resulting
vasodilatation. The relative contribution of pHi vs.
pHo to the control of vascular tone during acidification and alkalinization remains, therefore, a subject worthy of additional investigation.
 |
ACKNOWLEDGEMENTS |
This work has been supported by the British Heart Foundation and
the Special Trustees of St. Thomas's Hospital.
 |
FOOTNOTES |
Address for reprint requests and other correspondence: S. V. Smirnov, Div. of Pharmacology and Therapeutics, King's College London, St. Thomas's Hospital, Lambeth Palace Rd., London SE1 7EH, UK (E-mail: sergey.smirnov{at}kcl.ac.uk).
The costs of publication of this
article were defrayed in part by the
payment of page charges. The article
must therefore be hereby marked
"advertisement"
in accordance with 18 U.S.C. §1734 solely to indicate this fact.
Received 4 June 1999; accepted in final form 10 January 2000.
 |
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