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Biophys J, April 2000, p. 1895-1905, Vol. 78, No. 4
Department of Physiology, University of Kentucky College of Medicine, Lexington, Kentucky 40536-0298 USA
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ABSTRACT |
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External pH (pHo) modifies T-type calcium
channel gating and permeation properties. The mechanisms of T-type
channel modulation by pH remain unclear because native currents are
small and are contaminated with L-type calcium currents. Heterologous
expression of the human cloned T-type channel,
1H, enables us to
determine the effect of changing pH on isolated T-type calcium
currents. External acidification from pHo 8.2 to
pHo 5.5 shifts the midpoint potential
(V1/2) for steady-state inactivation by 11 mV, shifts the V1/2 for maximal activation
by 40 mV, and reduces the voltage dependence of channel activation. The
1H reversal potential (Erev) shifts from
+49 mV at pHo 8.2 to +36 mV at pHo 5.5. The
maximal macroscopic conductance (Gmax) of
1H increases at pHo 5.5 compared to pHo 8.2. The Erev and Gmax
data taken together suggest that external protons decrease
calcium/monovalent ion relative permeability. In response to a
sustained depolarization
1H currents inactivate with a single
exponential function. The macroscopic inactivation time constant is a
steep function of voltage for potentials <
30 mV at
pHo 8.2. At pHo 5.5 the voltage dependence of
inact shifts more depolarized, and is also a more
gradual function of voltage. The macroscopic deactivation time constant
(
deact) is a function of voltage at the potentials
tested. At pHo 5.5 the voltage dependence of
deact is simply transposed by ~40 mV, without a
concomitant change in the voltage dependence. Similarly, the delay in
recovery from inactivation at Vrec of
80
mV in pHo 5.5 is similar to that with a
Vrec of
120 mV at pHo 8.2. We
conclude that
1H is uniquely modified by pHo compared to
other calcium channels. Protons do not block
1H current. Rather, a
proton-induced change in activation gating accounts for most of the
change in current magnitude with acidification.
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INTRODUCTION |
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Voltage-activated calcium channels are critical
for regulation of electrical and chemical signaling in the myocardium.
Calcium channels are responsible for the generation of action
potentials in pacemaker cells and shaping the plateau phase of the
cardiac action potential in myocytes. There are two classes of calcium channels expressed in the myocardium, the L- and the T-type calcium channels. These channels differ in their pharmacological, permeation, and gating properties. L-type channels are sensitive to block by
dihydropyridines and cadmium, have a greater permeability for barium
than calcium, activate at potentials positive to
20 mV, and L-type
channel gating regulation is complex (Hille, 1992
). L-type channel
gating is governed by voltage, calcium, and other intracellular
second messengers. In contrast, T-type channels are sensitive to block
by nickel (Lee et al., 1999
), conduct barium and calcium equally,
activate at potentials positive to
70 mV, and their gating is
strictly voltage-dependent. The current kinetics of both these channel
types are also dramatically different. L-type channels continually
reopen in response to depolarization and have a slow decay rate (Hille,
1992
). T-type channels open in brief bursts before inactivating.
Qualitatively, the T-type channel gating kinetics are sodium
channel-like (Droogmans and Nilius, 1989
). Both sodium and T-type
calcium channel current macroscopic kinetics are well described by the
Aldrich, Corey, and Stevens model for sodium channels (Aldrich et al.,
1983
). However, a major difference between
INa and
IT is that
IT is ~50-fold slower than INa.
Extracellular acidification commonly accompanies pathophysiological
events such as ischemic episodes (reviewed by Carmeliet, 1999
).
Occlusion of coronary circulation, for example, can change external pH
(pHo) from a normal value of 7.2 to as low as 6.0 (Vanheel et al., 1990
; Clark et al., 1993
). Extracellular acidification attenuates inward currents measured from both native
low-voltage-activated calcium channels (LVA; Tytgat et al., 1990
) and
high-voltage-activated calcium channels (HVA), including
Ica,L (Prod'hom et al., 1987
; Krafte
and Kass, 1988
; Pietrobon et al., 1989
). Decreases in calcium current
with acidification may be caused by 1) block of the permeation pathway;
2) decrease in local calcium concentrations, and; 3) proton
modification of gating. An increase of external proton concentration
shifts the voltage dependence of HVA calcium channels gating to more
depolarized potentials (e.g., Krafte and Kass, 1988
; Kwan and Kass,
1993
). This shift effect is similar to that noted for voltage-gated
sodium channels (Woodhull, 1973
), and T-type calcium channels in
cardiac myocytes (Tytgat et al., 1990
).
In contrast to L-type calcium channel studies, only scant information
exists for regulation of T-type calcium channels.
pHo modulates native
IT differently than L-type channel
currents in cardiac myocytes (Tytgat et al., 1990
; Cohen et al.,
1992). Native myocyte T-currents, however, are difficult to
study because myocyte currents are small and hard to isolate. Most
native preparations that express IT
also express ICa,L. As a consequence,
native IT is often measured as a
subtraction current. Heterologous expression of cloned T-type calcium
channels provides a system where IT
can be studied in isolation with native-like kinetics (Satin and
Cribbs, 1999
). To better understand proton modification of T-type
channels, we examined the effect of acidification on the human cardiac
T-type channel,
1H (Cribbs et al., 1998
), stable-transfected in
human embryonic kidney cells (HEK) 293 cells. The major effect of
decreasing pHo on
1H is a shift of
steady-state activation gating, with a novel decrease of the voltage
dependence of channel activation gating. We also report the unique
finding that
1H maximal macroscopic slope conductance increases at
pHo 5.5, compared to 8.2. We conclude that the
decrease of inward T-type calcium currents, measured by sustained
depolarizations, are mainly due to proton modification of activation gating.
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MATERIALS AND METHODS |
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Cell culture
1H cDNA (Cribbs et al., 1998
) was used to generate a
stable-transfected HEK 293 cell line (Satin and Cribbs, 2000
). Cells are incubated in DMEM supplemented with 10% fetal bovine serum, 100 U/ml penicillin, 100 mg/ml streptomycin, and 1 mg/ml G-418.
Electrophysiology
Cells were digested with 0.125% trypsin and re-plated 1-3 days
before recording in the whole-cell clamp configuration. Culture media
were replaced with the extracellular bath solution immediately before
recording. The pipette solution contained (in mM): 110 potassium
gluconate, 40 CsCl, 1 MgCl2, 5 Mg-ATP, 5 EGTA, 5 Hepes for pHi 7.4. The extracellular bath
solution consisted of (in mM): 140 NaCl, 5CsCl, 2.5 KCl, 10 TEA-Cl, 2.5 CaCl2, 1 MgCl2, 5 glucose,
and 5 Hepes for pHo 8.2-6.8 or 5 MES for
pHo 6.8 to 5.5. The solutions were titrated with
CsOH to the appropriate pH. Recordings were initiated 5 min after patch
break to allow equilibration of the pipette solution with the cell
interior. The cells were recorded in a chamber with a static bath
volume of 250 µl. To change pHo we superfused 6 ml bath solution at 1.5 m/min. Experiments were performed at room
temperature (20-22°C). Pipettes were pulled from borosilicate glass
to resistance in pipette solution ranging from 1.5 to 2 M
. The small
spherical cells used for analysis had a mean capacitance of 23 pF ± 1.2 and we measured a mean series resistance of 4.2 ± 0.03 M
. Currents were filtered at 10 kHZ and sampled at 50 kHz. For
voltage steps used in tail current measurements, the capacitative
transient was complete in 100-200 µs. All tail current decays are
fitted to data after the peak to reduce any complexity introduced by slow settling time of the voltage clamp. Single-exponential
functions superimpose the current decay, consistent with a
constant VCommand during the
measurement. pClamp 6.04 and 8.02b programs (Axon Instruments) were
used for data analysis and acquisition. Nonlinear curve-fitting was
performed with Origins v.4.1 (Microcal Software). Data are reported as
mean ± SEM. Student's t-tests on independent groups were used to evaluate p-values.
Voltage protocols
Steady-state inactivation is measured by holding at
100 mV,
then pre-pulsing from
90 to
30 mV for 5 s, followed by a
Vtest to
20 mV. The peak current of
Vtest is plotted as a function of
pre-pulse potential. The data were fit with the Boltzmann distribution:
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(1) |
Activation gating was measured by holding at
100 followed by a
Vtest from
90 mV to +40 mV for 300 ms. The peak current is plotted as a function of
Vtest. We fit the current voltage
curves with the Boltzmann form:
|
(2) |
80 mV, after pre-pulsing from
85 to +90 for 9 ms from a holding
potential of
100 mV. The data are fit with a single exponential from
cursors set from the peak inward current until the end of the test
pulse. Current amplitudes are plotted as a function of pre-pulse
potential. The data are fit with Eq. 1.
To assess open channel permeation properties and
Erev we pre-pulsed cells from a
Vhold of
100 mV to +100 mV for a
duration corresponding to the peak of the outward current (3 ms for
pHo 8.2 and 6 ms for pHo
8.2; see Results). After the pre-pulse to +100 mV we measured current
amplitudes at Vtest ranging from
120 to +100 mV (see Fig. 3). Erev was
measured from the zero current or by linear extrapolation of voltage
steps 5 mV apart.
Deactivation kinetics were determined by holding at
100 mV followed
by a +25 mV pre-pulse for 20 ms, and then tails were measured
by stepping from
40 to
150 mV. The tails were fit with a
single exponential to obtain the time constant of current decay (
deact).
deact as a
function of test potential generates a curve that fits with a single exponential.
Recovery from inactivation is measured by pulsing 5 s to 0 mV
followed by a variable recovery interval at
Vrec
80 or
120 mV. The fraction of
recovery current was determined by measuring tails at
80 mV after a
9-ms pre-pulse to +75 mV. Tail currents are fit with a single
exponential to determine current amplitudes. The data plotted as a
function of recovery intervals are fit with a double exponential.
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RESULTS |
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pHo shifts the voltage dependence of steady-state inactivation
Two parameters define steady-state inactivation of
IT: the midpoint voltage of
steady-state availability (V1/2), and
the slope factor (k), which describes the voltage-dependent
availability of this process. External acidification from
pHo 8.2 to 5.5 shifts steady-state inactivation
to more depolarized potentials without affecting the slope factor of
the steady-state inactivation curve (Fig.
1). Fig. 1, A and B
show the available currents recorded at a
Vtest of
20 mV, after pre-pulsing
5 s from
120 to
30 mV, for pHo 8.2 and
5.5. At pHo 5.5 the inward currents are <8.2. The decrease of inward current at
Vtest
20 mV is a consequence of a
positive shift of activation gating and a change in the voltage dependence of channel activation (see below). The currents are normalized to the maximal inward currents and are plotted as a function
of pre-pulse potential. Fig. 1 C shows the change of the
relative current plotted as a function of pre-pulse potential from Fig.
1, A and B. The only effect of changing
pHo from 8.2 to 5.5 is a positive shift of the
V1/2 by 11 mV (n = 5).
Fig. 1 D summarizes the fitted midpoint as a function of
pHo over the range 8.2-5.5. The only statistically
significant shift of V1/2 occurs for
pHo 5.5. However, acidification to
pHo 6.0 shifts the mean
V1/2 by 4 to 5 mV.
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pHo modifies IT activation voltage dependence and permeation
We used two methods to determine the effects of external
acidification on macroscopic IT
activation. First, we measured current-voltage curves from peak inward
calcium current by stepping from a
Vhold of
100 mV followed by a
Vtest ranging from
90 mV to +40 mV
for 300 ms. This voltage protocol is restricted to measuring net inward current, and is useful for comparison to data in the literature. Fig.
2 A is a plot of the peak
inward current plotted as a function of
Vtest for pHo
8.2 and 5.5 in a representative cell. For this wide pH range the peak
inward current decreases, the I(V) curve shifts
depolarized, and the voltage dependence decreases. Fig. 2,
B-D summarize the Boltzmann distribution fit
parameters as a function of pHo ranging from 8.2 to 5.5. Changes in pHo from 8.2 to 6.8 have no
significant effect on conductance, midpoint, or slope of the
conductance-transformed I(V) curve. For pH < 6.8 the macroscopic conductance obtained from a linear fit of the ascending limb of the inward I(V) curve begins to
decline (Fig. 2 B), the
V1/2 for peak inward current shifts
from
51 ± 2 mV (pHo 8.2) to
17 ± 5 mV (pHo 5.5; n = 6) (Fig. 2
C), and the voltage dependence becomes more shallow,
changing from 4.6 ± 0.3 mV/e-fold at
pHo 8.2 to 8.8 ± 0.6 mV/e-fold
at pHo 5.5 (n = 6; Fig. 2
D).
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The potential range tested above may not adequately define changes in
the voltage dependence of channel activation and macroscopic conductance. We determined how pHo modifies both
inward and outward currents by stepping from a
Vhold of
100 to a
Vtest from
90 mV to +100 mV. This
extended range peak current-voltage curve shows that peak outward
current is greater for pHo 5.5 than for 8.2 (Fig.
3 A). Fig. 3 B is
the data in panel A expanded to show that external
acidification causes a hyperpolarizing shift of Erev. The
pHo-induced change in
Erev is unequivocal, because at the
same potential of +40 mV we measured inward current in
pHo 8.2 and outward current in
pHo 5.5. The reversal potential
(Erev) for
1H shifts from 49 ± 1.2 mV at pHo 8.2 to 36 ± 0.58 mV at pHo 5.5 (n = 4; p < 0.001).
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The shift of Erev for peak currents
elicited by sustained depolarizations suggests a change in selectivity.
Therefore, to assess open channel properties we activated channels and
measured tail currents elicited by voltage steps to potentials ranging from
120 to +100 mV. The pre-pulse duration was set to the peak of
the outward current measured at +100 mV for pHo
8.2 and 5.5. The open channel current-voltage curve is clearly
nonlinear (Fig. 3 C). The expanded voltage axis shows
unequivocal evidence for a pHo-induced change in
Erev (Fig. 3 D). The slope
of the open channel current-voltage curve reflects channel conductance.
Notice that the maximal slope is in fact slightly steeper for voltages corresponding to inward current at pHo 5.5 compared to 8.2 (Fig. 3 C). The dashed line in Fig. 3
C represents the data recorded at pHo
5.5 shifted by 15 mV, to normalize for the change in
Erev. This effect is subtle, but
reproducible in all cells tested (n = 4, p < 0.01). We conclude that acidification increases
macroscopic T-type channel slope conductance under our physiological
ionic conditions.
External acidification reduces IT activation voltage dependence
Determining pH effects on IT
activation voltage dependence from the peak inward I-V
relationship is problematic. To test the effects of external
acidification on activation we used a broad range of pre-pulse
potentials, followed by a step to a common test potential. We
voltage-clamped cells expressing
1H from
Vhold =
100 mV to potentials ranging
from
85 to +90 mV for 9 ms, and then measured the instantaneous tail
currents elicited by a return step to
80 mV. All tail currents are
well-fitted by a single exponential function. This is an important
minimal test of adequate voltage control. Fig.
4, A and B show raw
current traces from this tail current voltage protocol at
pHo 8.2 and 5.5. Different pre-pulse potentials
are shown in pHo 8.2 versus 5.5 because of the
dramatic difference in the maximal current activation range for these
two conditions (Fig. 4 C). In Fig. 4 A pre-pulses
to
80,
55,
45,
20, and 25 mV are shown. Fig. 4 B
shows pre-pulses of
80, 0, 25, 70, and 90 mV. Pre-pulses to +75 mV
are necessary for maximal current activation at
pHo 5.5 compared to
10 mV for pHo 8.2. The
V1/2 for maximal current activation is
shifted depolarized and the slope for maximal current activation is
about threefold more gradual for pHo 5.5 than
8.2. Fig. 4, D and E summarize the pooled data
obtained from Boltzmann fits of the tail I(V)
curves plotted as a function of pHo.
Acidification from pHo 8.2 to 5.5 shifts the
V1/2 for activation by 50 mV. The
slope factor is approximately tripled at pHo 5.5 compared to 8.2 (16.0 ± 1.8 and 5.3 ± 1.6 for pH 8.2 and 5.5, respectively).
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External acidification shifts and decreases the voltage dependence
of
inact
To characterize the pHo modification of
channel kinetics we measured the effect of pHo on
macroscopic channel inactivation. The decaying phase of current for
various sustained depolarizations is well described by a single
exponential function for both pHo 8.2 and
5.5 (Fig. 5, A and
B). The plot of the time constant of inactivation
(
inact) as a function of
Vtest reveals a voltage-dependent and
a voltage-independent phase of
inact for all
pHo tested (Fig. 5 C). There is no
pHo-induced change in the voltage-independent
inact (Fig. 5 C, +60 mV). Native
IT can be described by an ACS-like model of gating (Droogmans and Nilius, 1989
). A fundamental principle is that for small depolarizations activation is the slow, rate-limiting transition, and therefore contributes to the macroscopic inactivation rate. Following this logic, we predict that acidification should shift
and decrease the voltage dependence of the inactivation time constant.
Fig. 5 C is a plot of the
inact as
a function of voltage for pHo 8.2 and 5.5. There
is not a simple 40-50-mV translation of the
inact(V) curve (dashed
line, Fig. 5 C). Consistent with the effects of
pHo modification of steady-state activation gating, the
inact(V) is both more
gradual and shifted depolarized at pHo 5.5 relative to 8.2 (Fig. 5 C).
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External acidification shifts deactivation kinetics on the voltage axis without an effect on voltage dependence
To characterize channel deactivation kinetics we activated
channels with a pre-pulse to +25 mV for 20 ms and returned the membrane
potential ranging from Vtest of
40
to
160 mV for pHo 8.2 and 5.5 (Fig.
6, A and B). For
all Vtest, and for all
pHo tested the current relaxed with a single
exponential (Fig. 6, C and D). The time constant
of deactivation (
deact) is a function of
voltage for the potential range tested. For pHo
5.5 the voltage-dependence of activation is shifted ~40-50 mV (Figs.
2 and 4). If the deactivation process involves the same
voltage-dependent rate transitions as the activation process, but in
the opposite net direction, then
deact(V) should be altered in
response to external acidification. Fig. 6 compares the effect of
pHo 8.2 and 5.5 on the voltage dependence of
deactivation. The single-exponential fit the of
deact(V) plot (Fig. 6 E)
yields the slope or voltage dependence of deactivation. Interestingly,
the voltage dependence of deactivation (slope = 49 ± 1.2 and
46 ± 1.0 mV/e-fold change for
pHo 8.2 and 5.5, respectively) was not
significantly affected by pHo. In fact, a 40-mV
shift of
deact(V) at
pHo 8.2 superimposes over the
deact(V) data at pHo 5.5 (Fig. 6 F). This is in
contrast to proton effects on the voltage dependence of
activation (Figs. 2 and 4). These data suggest that multiple
closed-state transitions of the activation pathway are differentially
modified by external pH.
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Recovery from inactivation parallels the deactivation response to acidification
In parallel with voltage-gated sodium channels, T-type calcium
channels exhibit a delay in recovery from inactivation (Satin and
Cribbs, 1999
). The delay in the recovery from inactivation is
voltage-dependent. This delay is shorter for more hyperpolarized recovery potentials, and becomes negligible at recovery potentials negative to
120 mV. It has been postulated that the delay in recovery
from inactivation reflects a voltage-dependent deactivation step
necessary for recovery from inactivation (Kuo and Bean, 1994
). Because
acidification from pHo 8.2 to 5.5 shifts the
deact(V) relationship ~40 mV, we
wanted to determine whether the voltage dependence of the delay in
recovery from inactivation is also shifted by ~40 mV. Recovery from
inactivation is measured by pulsing 5 s to 0 mV, followed by a
variable recovery interval at recovery potentials
(Vrec) of
80 or
120 mV. The
fraction of recovery current was determined by measuring tail current
at
80 mV, following a 9-ms pre-pulse to +75 mV (Fig.
7). We pre-pulsed to +75 mV for 9 ms to
maximally activate IT for
pHo 8.2 and 5.5. Tail currents are fit with a
single exponential to determine current amplitudes. The data are
normalized to the maximal current recovered at 8 s for each
recovery potential. The relative current is plotted as a function of
recovery interval (Fig. 7). Fig. 7 A shows that there is no
significant difference between the fraction of current recovered at
Vrec =
120 mV for
pHo 8.2 and 5.5. For
Vrec =
80, the recovery fraction is
significantly smaller for recovery intervals <100 ms at
pHo 8.2 compared to pHo 5.5 (Fig. 7, B and C). Fig. 7 D shows that
the fraction of current recovered at pHo 8.2 and Vrec =
120 mV overlaps the fraction
of current recovered at pHo 5.5 and
Vrec =
80 mV. This result is
consistent with a 40-mV shift of deactivation for
pHo 5.5 compared to pHo
8.2.
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DISCUSSION |
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This study reports the novel finding that external acidification
reduces the
1H T-type calcium channel voltage dependence for
activation. Similar to most other voltage-dependent cation channels,
external acidification causes a reduction of the inward current through
1H. However, this reduction of inward current is only observed for
currents elicited by a sustained depolarization. The mechanism
underlying this reduction of inward current for the
1H channel is a
depolarizing shift and a decrease of the voltage dependence of
activation gating.
Paradoxically to the decrease of current elicited by a sustained depolarization, acidification from pH 8.2 to 5.5 actually increases macroscopic slope conductance. External acidification also hyperpolarizing shifts Erev. This is consistent with the postulate that this T-type calcium channel isoform becomes less calcium-selective relative to monovalent ions. It is well established that single calcium channel conductance for monovalent ions is larger than that for divalent cations. Therefore, our data suggest that protonation of the T-type calcium channel simultaneously slows activation gating and reduces calcium selectivity.
External acidification decreases the voltage dependence of
activation for
1H
An unexpected major finding of our study was that external protons
dramatically reduced the slope factor for the activation curve. To our
knowledge there are no reports of proton reduction of voltage
dependence in a variety of cation channels that have been extensively
studied. This result suggests that T-type channels have evolved unique
gating properties. To determine the effect of acidification on
activation kinetics we used an isochronal pre-pulse from
85 to +90 mV
for 9 ms, followed by a Vtest to
80
mV. For small depolarizations channel activation is underestimated, because current time-to-peak is >9 ms. The voltage dependence of
activation is also obscured by the temporal overlap of inactivation. Nevertheless, an increase in this activation curve slope factor, with
acidification, indicates a slowing of the activation rate. These
effects are distinct from sodium channel (Woodhull, 1973
; Begenisich
and Danko, 1983
; Daumas and Andersen, 1993
; Benitah et al., 1997
) or
HVA calcium channel modulation by protons in native (Zhou and Jones,
1996
) or heterologous expression systems. Both gating charge movement
and the energy transferred from the voltage sensor to the gating
machinery contribute to this slope factor. Because of the change in
slope it is tempting to suggest that external acidification titrates
some of the charge involved in voltage sensing, thus reducing the
overall gating charge movement. Our conclusion that pH modification
involves conformational changes of calcium channels is consistent with
the early finding from HVA calcium channels that pH modifies one or
more sites on the external surface (Prod'hom et al., 1989
).
pH modification of channel kinetics and gating distinguish effects on specific transitions
The change in voltage dependence (slope factor) induced by protons
may be separable from the midpoint shift. A number of emerging schemes
of T-type channel gating allow us to interpret our shift and
voltage-dependent effect with respect to channel state transitions. T-type calcium channels gate with similar features as posed by the ACS
model (Aldrich et al., 1983
) for a variety of sodium channels. The
cloned T-type channels
1G,
1H, and native T-type current share
several similar macroscopic kinetic features (Chen and Hess, 1990
;
Satin and Cribbs, 1999
; Serrano et al., 1999
). These include voltage-dependent and independent phases of inactivation and
deactivation. The voltage-dependent phase of activation can be derived
from a slow rate of transfer between closed states at small
depolarizations. This would argue that pH effects on steady-state
activation should also be reflected in the kinetics of macroscopic
inactivation for small depolarizations. This contention is supported by
our data.
The voltage-dependent phase of deactivation is dominated by transitions
through closed states proximal to the open state. However, in contrast
to pH modification of inactivation kinetics, there is only a shift on
the voltage axis of the time course of deactivation; pH does not alter
the voltage dependence of deactivation. The simplest explanation for
these results is that protons slow the voltage dependence of closed
transitions distal to opening only. The finding that the proton-induced
depolarizing shift is similar for all measures is consistent with a
reduction of negative surface potential by protons (Hille et al.,
1975
). Alternatively, Armstrong and colleagues recently posed the
intriguing mechanism that apparent surface potential shifts can in fact
be due to intrapore ion binding in sodium channels (Armstrong, 1999
;
Armstrong and Cota, 1999
). The crux of Armstrong's hypothesis is that
intrapore calcium in the sodium channel facilitates open-to-close
gating of the sodium channel. Lower pH shifts
Erev away from
ECa; presumably, this reduces calcium
occupancy. Although a surface potential mechanism is consistent
with our data, we cannot eliminate a connection between changes in pore
properties and channel gating. Future experiments varying ionic
conditions are necessary to test whether intrapore ions stabilize
individual channel states.
Recovery from inactivation of IT is
distinct from sodium channel recovery in that there is no voltage
dependence of the rate of recovery from inactivation (Chen and Hess,
1990
; Satin and Cribbs, 1999
; Serrano et al., 1999
). However, in
parallel with sodium channel gating schemes (Kuo and Bean, 1994
), there
is a voltage dependence to the delay in the onset of recovery from inactivation of IT (Satin and Cribbs,
1999
). The interpretation is that this delay reflects the deactivation
through the inactivated states. Our pH modification results are
entirely consistent with this scheme for T-type channels. Protons have
the same shift effect on voltage dependence of the onset of recovery
from inactivation as observed for deactivation.
Native studies of T-type calcium channels suggest that inactivation is
linked to channel activation (Droogmans and Nilius, 1989
). Therefore,
changes in activation gating should be reflected in inactivation
gating. The effect on the V1/2 for
activation is significant at pHo 6 or less. While
we did not find a significant difference in the
V1/2 for inactivation at
pHo 6.0, there is an ~5 mV mean
V1/2 depolarizing shift. At
pHo 5.5 this shift achieves statistical significance.
External acidification decreases calcium selectivity and increases inward ionic conductance
The explanation for the increase of maximal macroscopic
conductance (Gmax) is simple in the
context of established models of calcium channel selectivity (reviewed
by Hille, 1992
; also see Deng and McCleskey, 1999). Our
experiments were performed in physiological external ionic conditions
with respect to calcium and sodium. We show a change in
Erev that is consistent with a decrease in relative calcium selectivity (Fig. 3). We also note that
the conductance of inward currents is greater at
pHo 5.5 compared to pHo
8.2. Together, these data suggest that protons are decreasing the
affinity of calcium to the pore and increasing monovalent permeation.
An increase in monovalent permeation increases conductance, because
monovalent ions do not bind to the pore with high affinity (reviewed by
Hille, 1992
).
Comparison to native cardiac T-type calcium current
There is substantial apparent block by protons of
IT and
Gmax in both native ventricular
myocytes (Tytgat et al., 1990
) and atrial cardiac myocytes (Cohen et
al., 1992). In the study on ventricular myocytes
Gmax analysis was based on currents
elicited by a sustained depolarization (Tytgat et al., 1990
; cf., Fig. 1 in our study). Complications with such an interpretation are highlighted in our present study. Although single-channel currents were
recorded, the ionic conditions were different. Given our finding that
pH modifies selectivity it may be difficult to simply extrapolate
single-channel results to macroscopic recordings under mixed ionic
conditions. In atrial myocytes (Cohen et al., 1992) the data are
qualitatively consistent with our findings with respect to the decrease
of slope factor and shift of V1/2 in
response to protonation. However, atrial T-type channel
Gmax decreases with acidification. In
this sole study on atrial myocytes the bath solution contained
Ba2+ as the charge carrier and no permeant
monovalent ions. Therefore, the discrepant decrease of
Gmax from our study may be related to
differences in charge carrier. We performed our studies in physiological ionic conditions with respect to sodium and calcium. This
simply cannot be done in native tissues because of the overlap of
sodium and L-type calcium currents with
IT. In addition, an important
limitation of native T-type calcium channel studies is that they rely
on subtraction currents. Significant contamination of L-type channels
may distort data analysis.
Physiological implications
Although pHo 5.5 seems extreme,
acidification of local external myocardium can reach levels as low as
5.9 after coronary artery occlusion (Axford et al., 1992
; Yan and
Kleber, 1992
). Cardiac hypertrophy is common in patients with ischemic
episodes. Native IT increases in
response to hypertrophy (Nuss and Houser, 1993
).
1H is a human
cardiovascular T-type calcium channel (Cribbs et al., 1998
). Therefore,
1H channels may be important pharmacological targets under such
pathophysiological conditions. Cardiac hypertrophy and heart failure
share the feature of prolonged action potential duration. In both
conditions, early after depolarizations (EADs) or spontaneous
subthreshold depolarizations (coined SD by Nuss et al., 1999
) may
generate arrhythmias. While EADs are in part promoted by increased
ICa,L activity (January and Riddle,
1989
; Zeng and Rudy, 1995
), SDs occur in the subthreshold voltage range where IT is active (Nuss et al.,
1999
). The hyperpolarized range of IT
activation is well suited for initiating and sustaining subthreshold
oscillatory potentials. There is evidence for this in the myocardium
(Hagiwara et al., 1988
; Sen and Smith, 1994
; Zhou and Lipsius, 1994
).
If IT contributes to SD, then local
acidification may actually be, in part, protective against abnormal
rhythm generation due to attenuation of
IT.
| |
ACKNOWLEDGMENTS |
|---|
We thank Leanne Cribbs for the
1H clone and for expert advice,
Yi Zhang and the UK Cardiovascular Journal Club members for stimulating
discussions, and Alison Nemes and Oscar Crawford for technical assistance.
This work was supported in part by a grant from the National Science Foundation.
| |
FOOTNOTES |
|---|
Received for publication 7 September 1999 and in final form 4 January 2000.
Address reprint requests to Brian P. Delisle, Dept. of Physiology, MS-508, University of Kentucky College of Medicine, Lexington, KY 40536-0298. Tel.: 606-323-1146; Fax: 606-323-1070; E-mail: bpdeli00{at}pop.uky.edu. or jsatin1{at}pop.uky.edu.
| |
REFERENCES |
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1H from human heart, a member of the T-type calcium channel gene family.
Circ. Res.
83:103-109[Abstract/Full Text].
1H.
Biophys. J.
77:3034-3042[Abstract/Full Text].
1G T-type calcium channel.
J. Gen. Physiol.
114:185-201[Abstract/Full Text].
Biophys J, April 2000, p. 1895-1905, Vol. 78, No. 4
© 2000 by the Biophysical Society 0006-3495/00/04/1895/11 $2.00
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