Articles |
From the Department of Physiology, Emory University School of Medicine, Atlanta, Ga.
Correspondence to Dr Peter L. Becker, Department of Physiology, Emory University School of Medicine, 1648 Pierce Dr, Atlanta, GA 30322. E-mail plb@physio.emory.edu.
| Abstract |
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Key Words: Cl- current Ca2+ oscillations transient inward current Na+-Ca2+ exchanger rabbit ventricular myocytes
| Introduction |
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The first possibility, that of INa-Ca, was proposed by Kass et al5 in an examination of Iti in strophanthidin-poisoned Purkinje fibers. Because an increase in [Ca2+]i would cause a positive shift in the equilibrium potential of the exchanger,6 an inward current would be expected to result from a Ca2+ oscillation; ie, because of the 3 Na+:1 Ca2+ stoichiometry of the exchanger, a transient Ca2+ elevation would produce either increased inward current (by the exchanger operating in Ca2+ efflux mode) below ENa-Ca or decreased outward current (by the exchanger operating in Ca2+ influx mode) at higher potentials. Consistent with this hypothesis, Lipp and Pott7 failed to detect a reversal of Iti in voltage-clamped cultured guinea pig myocytes over a wide range of membrane potentials.
Other investigators have proposed the existence of Ca2+-activated cation currents in cardiac myocytes, most typically nonselective in nature.5 8 This conductance appears to persist even under ionic conditions in which Na+-Ca2+ exchange would seem unlikely, such as replacement of all external Na+ with isotonic CaCl2.9 More recently, Zygmunt and Gibbons10 have demonstrated ICl(Ca) in rabbit ventricular myocytes. However, as described by these authors, ICl(Ca) is strongly rectifying, making it unlikely to contribute significantly to Iti.
In this study, we describe the characteristics of the oscillatory current (Iosc) that is activated by spontaneous Ca2+ transients in rabbit ventricular myocytes. We examined this current to determine its ion selectivity and voltage dependence. When studied under conditions designed to block K+ currents, the whole-cell current activated by spontaneous Ca2+ transients appeared to consist of at least two separate currents, a nonreversing inward INa-Ca and a Ca2+-activated Cl--selective current. Under such conditions, we found no evidence to suggest the presence of a Ca2+-activated nonselective current. In contrast to the original characterization of ICl(Ca), we found that substantial inward current was present at potentials negative to ECl. The ICl(Ca) does not appear to be voltage gated. We conclude that both currents will contribute to the arrhythmogenic afterdepolarizations that result from spontaneous SR Ca2+ release.
| Materials and Methods |
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Electrophysiological
Recording
Cells were patch clamped in the ruptured-patch
whole-cell configuration13 using Corning 7052
borosilicate glass electrodes (2 to 5 M
) filled with one of the fura
2containing pipette solutions (4 through 7) listed in the
Table
, generally pipette solution 4 unless noted.
Voltage clamp was achieved with an AxoPatch-1D amplifier (Axon
Instruments). During recordings, the cell chamber contained one
of the bath solutions listed in the Table
, generally bath
solution 1
unless noted. When reversal potentials were measured under conditions
in which Cl- was varied, the liquid junction
potentials were measured and accounted for by using the method of
Neher14 for each of the pipette and bath solution pairs
employed. These measurements agreed to within 15% of the junction
potentials calculated using the computer program
JPCalc.15
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The magnitude of the transient current associated with the Ca2+ oscillations was taken as the change in the current from the mean holding current at any given potential. In general, the maximum current observed to be associated with a particular Ca2+ oscillation was used in assessments of the voltage dependence and drug dependence. The reversal potential for the Iosc for each particular cell was estimated by a linear interpolation between the inward and outward current data points that bracketed the reversal point, and the mean reversal potential was the average of these individual estimates.
Fura 2 Fluorescence Measurements
Fura 2 fluorescence was
measured with a
hightemporal-resolution microfluorimeter consisting of a
modified Zeiss IM-35 inverted fluorescence microscope outfitted
with a Hamamatsu model 3460-04 PMT. A special filter wheel (fabricated
by Omega Optical) controlled the excitation wavelengths. The filter
wheel has two large transmissive wedges (150° each) that pass 340 and
380 nm light, respectively. Two small opaque wedges (30° each) reside
between the larger transmissive sectors to prevent
simultaneous excitation with two different wavelengths. The
filter wheel is mounted to the shaft of a motor, which spins the filter
in the excitation light path of the microscope. The excitation light
from a xenon lamp source was thus rapidly alternated (
110 Hz)
between 340 and 380 nm. The fluorescence emission image of the
cell was focused onto the photocathode of a PMT. A dichroic reflecting
mirror in the emission path diverted the emission light (<590 nm) to
the PMT but allowed longer wavelengths to pass to the microscope
oculars. This technique allowed us to monitor the cell and its
environment with bright-field optics using red light without
significantly compromising the fluorescence detection
efficiency. An emission filter centered at 530 nm (bandwidth 40 nm) was
placed in front of the PMT to select the emission wavelengths. The
field stop diaphragm in the excitation path was narrowed to illuminate
only about two thirds of the cell (
100 to 150 µm). In addition, a
mask placed at an intermediate image plane in the emission path limited
the field of view that was focused on the PMT to limit the background
light signal. Generally, this mask was wider than a cell but about two
thirds of a cell length long and positioned so as not to image the fura
2filled patch pipette. Note that the recorded FI ratio
represents the spatially averaged signal from the illuminated
region of the cell. Thus, when the signal derives from propagating
Ca2+ waves, the characteristics of the recorded
transient are determined not only by the rate of Ca2+
release and reuptake but also by the path and propagation speed of the
wave front within the cell.
The PMT was connected to a custom-designed photon-counting circuit interfaced to an IBM-compatible computer. Control and data acquisition software was written to synchronize the operation of the photon counter to the revolution of the filter wheel. The program stored fluorescence data for each wavelength once per revolution, sampled and stored membrane potential and membrane current three times per revolution, and sampled and stored other parameters (eg, stimulus markers) once per revolution. The 340- and 380-nm fluorescence counts used to compute the 340/380 FI ratio were corrected for the background fluorescence and cell autofluorescence measured before rupturing the patch.
Miscellaneous Methods
DNDS was generously provided by Dr
Roger Worrell, Emory
University. DNDS was made as a 1-mmol/L extracellular solution and
applied locally to cells by pressure ejection from a pipette positioned
near the cell. Fura 2free acid was purchased from Molecular Probes.
All other reagents were obtained from Sigma Chemical Co. Except where
noted, values for various measurements are reported as the
mean±SEM.
| Results |
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10 µmol/L. This
elevated
[Ca2+]i leads to an enhanced accumulation
by
the SR and eventually to spontaneous SR Ca2+ release by a
mechanism that is not fully
understood.18 19 20
An example of
such an event is shown in Fig 1A
. Note
that when the membrane potential was stepped from -64 to +36 mV,
there was a relatively slow elevation of the
[Ca2+]i, as indicated by the increase
in the 340/380 FI ratio, due to the reverse
Na+-Ca2+ exchanger influx. This elevated
SR-pump substrate concentration led to Ca2+ loading of the
SR, followed by the initiation of spontaneous Ca2+
transients. Outward currents were associated with these
Ca2+ transients at +36 mV. Returning to negative
potentials
generally resulted in the suppression of the Ca2+
oscillations, although occasionally one or two transients
would occur before cessation. On these occasions, inward currents were
observed. Although it is not evident from the data shown in Fig
1
, the
[Ca2+]i elevation is not synchronous
throughout the cell. Rather, as many other investigators have
shown,18 20 21 the
[Ca2+]i rise
appears to be initiated in one discrete location and subsequently
propagates throughout the cell at a rate on the order of 100
µm/s.18 Such oscillations have been termed
"calcium waves," and they initiate contractile waves that follow
in their wake. Because fluorescence was recorded from a
rather large part of the cell on our setup, this relatively slow
propagation speed resulted in Ca2+ transient durations that
appear prolonged relative to transients that were initiated
synchronously.
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As is also evident in the example shown in Fig
1A
, these
Ca2+ oscillations are associated with
oscillations, or transients, in the membrane holding
current. As described below, the currents could be inward or outward
depending on the holding potential. Because of the common mechanism of
activation of the inward and outward components under these conditions,
we have chosen to refer to such currents as Iosc to reflect
this fact. Specifically, we have avoided the more familiar terms
Ito(Ca) and Iti that are commonly used to refer
to currents elicited under similar circumstances.
These spontaneous
Ca2+ oscillations occurred
more frequently at positive potentials (where Ca2+ influx
via the Na+-Ca2+ exchanger is favored) and
were
absent or rare at negative potentials. However, by first holding the
cell for several seconds at a positive potential to load the SR, we
would often observe an oscillation on stepping back to a
more negative potential. By this method of using positive polarization
to initiate spontaneous Ca2+ oscillations, we
were able to examine the voltage dependence of this current. The result
from this series of experiments is shown in Fig 1B
. The average
reversal potential of Iosc was somewhere between +5 and
+15
mV, although it was different in each cell. A difficult variable to
control in these experiments was the change
in[Ca2+]i at different potentials. For
example, the [Ca2+]i oscillations
that occurred at negative potentials started at lower Ca2+
levels (because the [Ca2+]i would start
to
fall immediately on stepping to the negative potential; see Fig
1A
) and
were somewhat smaller in magnitude. Thus, one variable that affects
these currents (the [Ca2+]i) was not
independent of potential. Furthermore, even at a single potential,
there was marked variability in both the Ca2+ and current
magnitudes (eg, note the variability in the current magnitude in Fig
1A
on return to +36 mV). We attribute one aspect of this variability to
differences in the starting location and propagation path of the
Ca2+ wave. Because of this variability, the current
magnitudes plotted in Fig 1B
were normalized to the current
magnitude
observed during the immediately preceding +36-mV holding period. In
this way, we attempted to normalize for cell-to-cell
variability and to account, as best we could, for time-dependent
processes such as the degree of SR loading produced by holding the cell
at the positive potential. Because of the variations in the
Ca2+-transient signal observed at different potentials and
our inability to record the spatial characteristics of the
Ca2+ transients, we hesitate to draw firm conclusions from
the shape of the I-V relation. Nevertheless, it is clear that
Iosc can carry significant charge in either direction
depending on the membrane potential.
What is Iosc?
Iosc is undoubtedly a
current activated by the
elevated [Ca2+]i. A number of
Ca2+-activated currents have been described or
postulated in cardiac myocytes, including specific
K+22 and Cl-
currents,10 23 24 a nonselective cation
current,8 and
INa-Ca.5 6 7 Under
the conditions used in our study (eg, Cs+ and TEA on both
sides of the membrane), it is unlikely that the current
oscillations we observed were due even in part to
Ca2+-activated channels selective for
K+. From the data to be presented below, we feel
that it is likely that Iosc consists of at least two
distinct Ca2+-activated currents: a
Cl- current and INa-Ca.
ICl(Ca)
The existence of ICl(Ca)
has previously been
demonstrated in rabbit ventricular myocytes by Zygmunt and
Gibbons.10 We examined the involvement of a
Cl- conductance in these
Ca2+-activated current oscillations
with a number of approaches. We first examined the action of the
reversible anion channel blocker DNDS and found that it attenuated the
outward current observed with Ca2+ oscillations
at +36 mV. An example of such an experiment is seen in Fig
2
. A 1-mmol/L DNDS solution was pressure ejected from a
nearby pipette onto a cell that was exhibiting spontaneous
Ca2+ and current oscillations at a holding
potential of +36 mV. Shortly after the application of DNDS, there was a
reduction in the peak outward current amplitude. Overall, the mean peak
current amplitude fell to 45±10% of the pre-DNDS control value and
recovered within 2 minutes of terminating the DNDS application to
90±30% of control (six observations in five cells). Further, we also
observed that the holding current becomes less outward in the presence
of DNDS. This finding suggests that there was a sustained
Cl- conductance at +36 mV that contributed to the
holding current.
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The pressure and aim of the puffer pipette were adjusted to avoid disturbing the position of the cell with respect to the patch pipette. Thus, we are not confident that the DNDS was applied to the whole cell surface, nor can we be certain that the delivered concentration was sufficient to completely suppress Cl- currents. Indeed, because we rarely observed inward currents under these conditions (an expectation based on experiments to be described later), we feel it is likely that such application did not completely block the Cl- currents.
DNDS application also lowered the
overall 340/380 FI ratio and reduced
the amplitude of the fluorescence ratio transients associated
with the current oscillations. However, DNDS is
fluorescent at both 340 and 380 nm excitation; therefore, in
the presence of DNDS, the fura 2 FI ratio was no longer a reliable
indicator of the [Ca2+]i. However, there
is
good circumstantial evidence to suggest that the Ca2+
transients continued unabated in the presence of DNDS. All cells
exposed to DNDS continued to contract in a wavelike manner during DNDS
application, indicating that the [Ca2+]i
rise
was sufficient to initiate this process. Moreover, an examination of
the fluorescence resulting from excitation at both wavelengths
used to compute the FI ratio (ie, 340 and 380 nm) indicates that the
amplitude of the fluorescence change that occurred during the
oscillations in all these cells was not significantly
altered by DNDS. If these fluorescence transients were due
solely to the rise and fall of [Ca2+]i
(and
not, for example, to an abrupt change in DNDS concentration during the
time course of the transients) and if the DNDS did not significantly
affect the "resting" [Ca2+]i,
then the amplitude of the transients at any one wavelength should
remain proportional to the [Ca2+]i
change.
Although this assessment is problematic during the pressure
ejection period owing to movement of the cell with respect to the
illumination spot, an analysis of the 380-nm
fluorescence during oscillations that followed the
termination of DNDS confirms that the Ca2+ transients were
not significantly attenuated. The mean
380 FI for the three
transients (labeled with dot pairs) that occurred immediately after the
termination of the DNDS ejection in Fig 2
was 96% of the mean
380
FI of the three transients (labeled with single dots) just before DNDS
application, whereas the mean peak current amplitude was attenuated
50%. Thus, DNDS application significantly reduced the peak outward
current amplitude but did not appear to significantly alter the
Ca2+ transient amplitude. This fact strongly suggests the
presence of a Cl- conductance that was
activated by the elevated
[Ca2+]i.
INa-Ca
Although this evidence suggests
that Iosc involves
ICl(Ca), the reversal potential indicated in Fig 1B
(ranging between +5 and +15 mV) is significantly more positive than
the
-2-mV ECl under these conditions. Further, while
ICl(Ca) can account for the outward component of
Iosc, ICl(Ca) has been described as a
strongly outwardly rectifying current in rabbit ventricular
myocytes. Another current that should be altered by a change in the
[Ca2+]i is
INa-Ca.5
Indeed, such currents have previously been found to correlate to
spontaneous [Ca2+]i rises.7
INa-Ca is in the direction of the movement of
Na+ (since the exchange is believed to be three sodium ions
for one calcium ion25 ), and so an increase in the
[Ca2+]i would either attenuate an outward
current or enhance an inward current, depending on in which direction
the exchanger was operating when the
[Ca2+]i
changed. Hence, the change in INa-Ca with an abrupt
increase in the [Ca2+]i will always be in
the
inward direction, regardless of the holding potential or the gradients
of the two ions. To examine the contribution of INa-Ca to
Iosc, we conducted a series of experiments in the
absence of extracellular or intracellular Cl-
(Table
;
solutions 2 and 5, respectively). Although we were concerned about the
accuracy of the voltage measurements under these conditions (Ag/AgCl
electrodes were used for both pipette and bath coupling), the voltage
dependence of the L-type Ca2+ current indicated that it was
close: peak ICa normally occurs at +10 mV, and in these
experiments in the absence of Cl-, we found it
was within 10 mV of this value. As shown in Fig 3
, when
we eliminated Cl- and then elicited Ca2+
oscillations (by intermittent voltage-clamp intervals
at positive potentials), an inward Iosc was observed at all
potentials (from -88 mV to +72 mV). As was the case in the
presence of Na+ and Cl- (Fig
1
), the peak
current magnitude was variable from transient to transient even in
the same cell. However, although the current magnitude demonstrated
considerable variability, no reversal potential or strong voltage
dependence was evident, a result that would be expected if the current
was due to the Na+-Ca2+ exchanger.
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Do Other Currents Contribute to Iosc?
In
the presence of Cs+ and TEA, it appears that
Iosc might consist of just two components,
ICl(Ca), as has been described by Zygmunt and
Gibbons,10 and INa-Ca. To test this
hypothesis, we examined Iosc in the presence of
Cl- under conditions that block the
Na+-Ca2+ exchanger. We reasoned that if these
two currents are solely responsible for Iosc, then
eliminating INa-Ca should leave just ICl(Ca).
We used NMDG as a Na+ substitute in the extracellular and
electrode solutions (Table
, solutions 3 and 6) to prevent
Na+-Ca2+ exchange. Although this approach
prevented us from overloading the SR by reverse
Na+-Ca2+ exchange, we found that a short train
of repetitive 300-millisecond depolarizations (
10 at 2 Hz) from a
holding potential of -80 to +10 mV to activate the inward
ICa was sufficient to overload the SR to the point of
inducing Ca2+ oscillations. In fact, we found
that the oscillations induced under these conditions
occurred with a remarkably regular frequency and with an amplitude that
was for the most part independent of voltage, and the subsequent
current transients were less variable as a result. Fig 4A
shows
a representative series of
currents activated by spontaneous Ca2+ transients
at a range of holding potentials in the absence of Na+
under conditions of approximately symmetrical Cl-
(ECl=-2 mV). Although the magnitude of the
Ca2+ transients was fairly invariant with potential, the
associated Iosc varied in both magnitude and direction. Fig
4B
shows the I-V relation from this series of experiments. As
anticipated, the current was outward at potentials more positive to
ECl. Moreover, the current reversed very close to
ECl (-3±2 mV, n=3) and appeared to be only
somewhat
outwardly rectifying. Note that it was clearly inward at negative
potentials. This sizable inward component was not expected, as
ICl(Ca) described by Zygmunt and Gibbons10 in
rabbit ventricular myocytes was quite strongly outwardly
rectifying.
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We considered two possible explanations for the persistence
of an
inward current in the absence of Na+: either an additional
Ca2+-activated inward current was also present
or ICl(Ca) can indeed carry significant inward current in
rabbit ventricular myocytes. To further clarify this
question, we tried shifting ECl to see how the reversal
potential of Iosc changed. ECl was set equal to
-33 mV in the absence of Na+ using solutions 3 and 7
from the Table
, and Ca2+ oscillations were
induced as described above. Fig 5
shows the resulting
I-V relation from this series of experiments. Iosc was
observed to reverse at -32±4 mV (n=4 cells), very close to
the
new ECl. In contrast to the situation of approximately
symmetrical Cl-, the current under these
conditions was more strongly rectifying, but it was again clearly
inward at more negative potentials. Comparing the observations in Figs
4B
and 5
, for a -31-mV shift in
ECl, the
reversal potential of Iosc shifted -29 mV. No other
ionic species experienced an appreciable change in its equilibrium
potential except the Cl- substitute aspartate. These
observations are entirely consistent with the hypothesis that
Cl- is the charge carrier of this current under these
conditions and argue against the significant involvement of other
conductances. Further, in a separate series of experiments, under
Cl- conditions where Iosc was found to
reverse at -49±2 mV (n=4; data not shown), the
isoproterenol-induced time-independent
ICl(cAMP)26 was found to reverse at
-51±4 mV (n=3), indicating that these two currents have a
similar Cl- selectivity. Collectively, these data
strongly support the hypothesis that, in the absence of Na+
and in the presence of the K+ channel blockers
Cs+ and TEA, Iosc is the ICl(Ca).
Therefore, it appears that ICl(Ca) can carry inward current
in rabbit ventricular myocytes when activated at a
potential more negative to ECl.
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[Ca2+]i Sensitivity of
Iosc
Our fluorescence recordings of the
[Ca2+]i changes lack the spatial
information
required to make precise correlations between the current and the
[Ca2+]i, and thus we did not explore
this relation in detail. However, several observations are worth
noting. We monitored the averaged fura 2 fluorescence in only
about two thirds of the cell volume, although the voltage clamp
amplifier should measure a current whenever and wherever it is
activated. Thus, if a spontaneous Ca2+ wave was
initiated at the nonilluminated end of the cell, the current would be
detected immediately, but the fluorescence signal would change
only after the wave reached the illuminated portion of the cell.
Knowing this, our expectation would be that if Iosc was
proportional simply to the mean [Ca2+]i
indicated by the fura 2 FI ratio, then the duration of the current
transient should be either equal to or longer than the Ca2+
transient. But, to the contrary, the current transients (measured as
the deflection from the mean holding current) were shorter in duration
than Ca2+ transients. This occurrence is evident in several
of the records presented here (eg, Figs 1A
and
2
) and is
true even in the absence of the Na+-Ca2+
exchanger (eg, see Fig 4A
), which suggests that either the
current
inactivates or is sensitive to a higher
[Ca2+]i than is indicated by the fura 2
FI
ratio. Although our data don't rule out inactivation as a mechanism
for this difference in time course, we note that in addition to
suppressing the transient current, DNDS also attenuated the basal
holding current recorded at +36 mV, suggesting that a
Cl- conductance was present even at times between
the Ca2+ transients. Since holding at +36 mV elevated the
mean "resting" [Ca2+]i, it is
possible that the ICl(Ca) was partially activated
by this modest [Ca2+]i elevation.
In any case, the discrepancy between the time course of the current and
Ca2+ transients indicates that the magnitude of the current
may be more indicative of the ongoing release process, perhaps
reflecting the surface area of the Ca2+ wave front (where,
as a consequence of the release process, the
[Ca2+]i gradient is large) rather than of
the
fraction of the cell volume that has an elevated
[Ca2+]i. In further support of this
hypothesis, we note that the current observed is often variable and
"spiky" in amplitude (eg, see initial five current transients in
Fig 2
). Recently, Lipp and Niggli,21 using
confocal
microscopy to obtain detailed spatial information, noted the sometimes
rather complex and tortuous paths that Ca2+ waves can
travel within cells. The variability and spikiness of the currents we
measure would be qualitatively consistent with the variations
in Ca2+ wave front surface observed by these
investigators.
| Discussion |
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We have deliberately avoided using the terms "Iti" and "Ito(Ca)" that are commonly used to classify the transient currents observed in cardiac cells. Over the last several years, it has become increasingly evident that several underlying currents are common to both, and thus such classifications based on the experimental parameters used to elicit them appear increasingly artificial. We feel it is reasonable to conclude that Iti consists of an inward INa-Ca along with (depending on species and tissue) ICl(Ca) and/or a Ca2+-activated cationic current. Ito very likely consists of outward manifestations of the Cl- and cationic currents (if present in Iti) and INa-Ca (possibly varying in direction with time), in addition to a 4-aminopyridinesensitive transient K+ current.
The use of spontaneous Ca2+ oscillations to study Ca2+-dependent currents presents a number of advantages for assessing the voltage and ionic dependence of these currents. The most important as it relates to this investigation is that detection of the Ca2+-activated transient currents was not complicated by capacitance transients or by the simultaneous activation of voltage-dependent transient currents. Thus, the subtraction of current measurements made in the presence of blockers was not required to reveal the specific Ca2+-activated component. This made the task of estimating the reversal potential of the current rather straightforward and less uncertain. On the other hand, activation of the current is not spatially and temporally uniform, since it occurs as a consequence of a relatively slowly propagating wave of Ca2+ release, which in turn often had different characteristics at different potentials. Because our hightime-resolution recording apparatus was not capable of recording the spatial characteristics of the Ca2+ transients, we were unable to assess directly how these characteristics modulated the current. This variability in the underlying Ca2+ transients undoubtedly contributes to the variability in the general appearance of the I-V relation; therefore, assessments of the degree of rectification of the currents are less reliable when they are activated in this way.
Characteristics of ICl(Ca)
In the absence of
Na+, Iosc
appeared to be exclusively ICl(Ca). The current was
moderately outwardly rectifying under conditions of approximately
symmetrical Cl- and more strongly rectifying when
ECl was -33 mV. The reversal potential under either
Cl- gradient condition was virtually identical to
ECl. Since no other ion gradient changed in a manner that
would be consistent with this observation, we conclude that the
current in the absence of Na+ is likely to be almost
exclusively ICl(Ca). Our results also demonstrate that
ICl(Ca) can be activated at all
physiological potentials. Under approximately
symmetrical Cl- gradient, the current appeared
somewhat outwardly rectifying, but not extremely so. Thus, voltage does
not appear to alter the gating characteristics of the underlying
channels significantly. Therefore, this current will be present
whenever [Ca2+]i is elevated,
irrespective of
the reason.
Our observations demonstrate that ICl(Ca) is briefer in duration than the associated Ca2+ transient indicated by the average fura 2 FI ratio. We suggest that this is largely because of the lower sensitivity to [Ca2+]i for activating this current, such that it is activated to a significant extent primarily by the very high [Ca2+]is that exist for a brief time at the Ca2+ release sites. Nonetheless, a small current may be activated by elevations in the resting [Ca2+]i that can be achieved by reverse Na+-Ca2+ exchange influx at positive membrane potentials, as indicated by the ability of DNDS to attenuate the outward holding current observed at +36 mV.
The characteristics of this current as observed here differ in one important respect from the initial description by Zygmunt and Gibbons10 : we observed substantial inward current at potentials negative to ECl, whereas those investigators did not. Zygmunt and Gibbons activated the current by step depolarizations that activated ICa and then quantified the SITS-sensitive component of the tail currents evident on repolarization to more negative potentials. They observed a strongly outward-rectifying current; indeed, they observed no current at potentials more negative to +20 mV under conditions in which ECl was as negative as -23 mV, which implied a voltage dependence to the gating of these channels. It is unclear what the explanation is for this difference in our observations. In contrast to our protocol, the subtraction of current records made at different times in the presence of the irreversible anion channel blocker SITS was required to account for other components of the tail current, and one possibility is that perhaps rundown of ICa (and its tail current) might have obscured ICl(Ca) at these potentials at which its magnitude was small. On the basis of the close agreement we observed between ECl and the reversal potential of Iosc under conditions of different internal Cl-, we feel it is unlikely that another Ca2+-activated current is responsible for the inward component.
Since their initial report on rabbit ventricular myocytes, Zygmunt and Gibbons24 and Zygmunt23 have characterized similar Cl- currents in rabbit atria and in canine ventricular cells. In both studies, these investigators did observe inward ICl(Ca) that reversed at potentials close to ECl. In light of our observations, it is reasonable to assume that ICl(Ca) in rabbit ventricular myocytes is the same channel present in rabbit atrial myocytes and that this channel is very similar to that expressed in canine ventricular myocytes.
INa-Ca
In the absence of Cl-, the
observed
current was always inward, even at potentials more positive than +70
mV. With the exception of Ca2+, all other ionic
species had an equilibrium potential more negative than this;
therefore, the observed current is unlikely to represent the
flux of a single ion species. On the other hand, an apparent inward
transient current would be expected from the
Na+-Ca2+ exchanger, with a transient elevation
of the internal [Ca2+]i, although the
observed current may not necessarily represent a true inward
current.5 7 ENa-Ca is equal to 3
ENa-2 ECa,25 and thus
the effect of a [Ca2+]i elevation would
be to
shift this equilibrium potential in the positive direction. If the
[Ca2+]i rose when the membrane potential
was
held more negative than ENa-Ca, there should be an
enhancement of the inward current. However, if the
[Ca2+]i rose when the membrane potential
was
held more positive than ENa-Ca, a decrease in the
outward current would be expected (perhaps becoming inward, depending
on the potential and the extent of
[Ca2+]i
rise). In all cases, however, a deflection from the steady state
current in the inward direction would be expected. As we showed in Fig
3
, elimination of chloride ions did result in a current that
was inward
at all potentials examined.
Contribution of Other Ca2+-Activated Currents
to Iosc
The role of other Ca2+-activated
currents
cannot be completely excluded by our results, although we feel the
evidence makes it unlikely that other such currents were present
under the conditions employed. The existence of a
Ca2+-activated K+ current has not been
convincingly documented in rabbit ventricular myocytes, and
because of the use of TEA and Cs+ in our pipette and
bathing solutions, they likely would not have contributed to the
currents we observed if they did exist. We are confident that under the
zero Na+ conditions, the current we observe is
overwhelmingly ICl(Ca): the current's reversal potential
shifted with a change in the Cl- gradient, and under
both conditions, it reversed very close to the calculated
ECl. The cardiac nonselective cationic channel described by
Ehara et al8 does conduct Cs+. Therefore, the
inability of Cs+ to influence the reversal potential of the
transient current in our hands suggests that either such a conductance
is absent in rabbit ventricular myocytes or it is blocked
by TEA. However, we cannot completely rule out the contribution of
other currents under conditions in which Na+ was
present. Cannell and Lederer9 proposed the existence
of a Ca2+-activated nonselective current that can
pass K+ and Ca2+ in sheep Purkinje fibers on
the basis of behavior of "delayed afterdepolarization" currents.
However, this earlier work did not consider the possibility of the more
recently described ICl(Ca), and some of their
cationic substitutions resulted in [Cl-] changes as
well. In a more recent study, Han and Ferrier27 detected
the Cl- dependence of this
Ca2+-activated current in rabbit Purkinje fibers
but noted that the reversal potential was also altered by changes in
the calcium ion gradient, supporting the view that a
Ca2+-activated cationic conductance capable of
passing Ca2+ was also present. Although there are
significant methodological differences between these studies and ours,
it seems reasonable to conclude that Purkinje fibers differ from
ventricular cells in this respect. Our results showing (1)
virtual identity of the current's reversal potential to
ECl under two different Cl- gradients and
(2) the similarity of the reversal potential of ICl(Ca) and
the sustained ICl(cAMP) are not compatible with the
presence of a significant Ca2+-activated cationic
conductance in rabbit ventricular cells under the
conditions of our study.
Role of Ca2+-Activated Currents
Although
Ca2+-activated transient currents
undoubtedly influence the characteristics of the normal
ventricular action potential, perturbations in
Ca2+ cycling make them especially likely to contribute to
triggered activity under pathological conditions. Estimates of the
internal Cl- activity in rabbit heart range from
15 to 20 mmol/L.28 Thus, ECl is likely to
be in the range of
-40 mV. Under these conditions, one would
expect that an outward ICl(Ca) would normally be
transiently activated shortly after the initial action
potential depolarization. However, because this current is most
sensitive to the high [Ca2+]is that exist
at
moments of SR Ca2+ release, it would probably subside
within a few tens of milliseconds, well before the mean
[Ca2+]i declined. As a consequence, this
current should contribute to the initial repolarization after the
action potential spike, and perhaps for a short period it would also
contribute to a lowering of the plateau potential. This
ICl(Ca) will subside later during the plateau phase of the
action potential as the internal Ca2+ release process is
terminated and thus will likely have only a minor influence on the
latter part of the action potential waveform.
On the basis of thermodynamic calculations of ENa-Ca, it has been postulated that this transporter might operate in reverse mode early in depolarization (before a significant Ca2+ rise),29 30 and experimental evidence,30 31 albeit controversial,32 has led to the suggestion that this influx of Ca2+ could contribute to triggering SR Ca2+ release. In reverse mode, INa-Ca would be outward, but on SR Ca2+ release, the magnitude of this outward current should be attenuated and likely reversed. Thus, as a consequence of the SR Ca2+ release (however triggered), a net inward current will be activated, having the effect of driving the membrane potential more positive. The simultaneous activation of ICl(Ca) would tend to oppose this action of the change in INa-Ca. One possible consequence of this effect would be to enhance the magnitude of ICa. During the action potential, the initial depolarization of the cell membrane is likely sufficient to activate most available Ca2+ channels. By acting to keep the membrane potential less positive, the electrochemical driving force for Ca2+ would be enhanced, resulting in a larger current for a given number of open Ca2+ channels, and possibly a larger SR Ca2+ release.23
Delayed afterdepolarizations are frequently observed after repolarization under conditions favoring SR Ca2+ overload. These afterdepolarizations have been the focus of a number of studies, and results from several laboratories have implicated the Na+-Ca2+ exchanger and a Ca2+-activated cation current as possible contributors to the depolarization. Because the Ca2+-activated Cl- conductance was not thought to carry inward current in rabbit ventricular cells, it seemed unlikely to contribute to these events. However, our results clearly indicate that this current can carry inward current, and thus a role for this current in afterdepolarizations is likely.
The presence of a Ca2+-activated current has special implications for ICa and [Ca2+]i studies that require or rely on quantitative assessment of the magnitude and time course of ICa. As was illustrated by Zygmunt and Gibbons,10 the apparent rate of ICa inactivation will be altered due to activation of ICl(Ca). This alteration will frustrate efforts to quantify the net Ca2+ entry from the ICa time course. Precautions should therefore be taken in such studies on cardiac preparations that exhibit this current, such as setting ECl close to the typical command potentials employed. So far, ICl(Ca) has been confirmed in rabbit atria,24 ventricles,10 and Purkinje fibers,27 34 in dog ventricles,23 in ferret ventricles,35 and in cultured chick myocytes.36 On the other hand, Cl- substitutions had little effect on the reversal potential of Iti in bovine Purkinje fibers.5 In preliminary experiments, we have observed little evidence for a significant ICl(Ca) in rat ventricular myocytes.
| Selected Abbreviations and Acronyms |
|---|
|
| Acknowledgments |
|---|
Received May 4, 1995; accepted January 11, 1996.
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