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Department of Physiology and Biophysics, University of Calgary, Calgary, Alberta, Canada
Correspondence: Address reprint requests to Dr. Gary J. Kargacin, Dept. of Physiology and Biophysics, University of Calgary, 3330 Hospital Dr. NW, Calgary, Alberta T2N 4N1 Canada. Tel.: 403-220-3873; Fax: 403-270-2211; E-mail: kargacin{at}ucalgary.ca.
| ABSTRACT |
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| INTRODUCTION |
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Electron micrographs reveal the presence of peripheral SR elements in close proximity (1025 nm) to the plasma membrane in smooth muscle cells (see Devine et al., 1972
; Somlyo, 1980
; Gabella, 1983
; Somlyo and Franzini-Armstrong, 1985
). This close apposition may extend for considerable distances (>1 µm) along the cell length and is thought to form a restricted diffusion space between the two membranes (discussed in Kargacin, 1994
). Thus, the superficial SR in smooth muscle cells is distributed in a way that would favor localized interactions between single plasma membrane ion channels and the SR proteins involved in Ca2+ regulation. This could facilitate coupling between localized Ca2+ influx events and the filling of peripheral SR Ca2+ stores in smooth muscle cells.
In previous work (Kargacin and Kargacin, 1995
), we estimated that the SR in smooth muscle is capable of taking up Ca2+ at a rate that is 5075% of the rate at which Ca2+ is removed from the cytoplasm after a contractile stimulus. Thus, a substantial portion of the Ca2+ entering a cell after the opening of a single plasma membrane Ca2+ channel could be taken up into the SR; however, the rate at which this occurs relative to the rate at which Ca2+ diffuses away from an influx site would be an important determinant of how fast and efficiently an SR store located near a site of Ca2+ influx could be replenished. It is also important to understand how uptake of Ca2+ by the SR influences the amplitude and time course of single-channel Ca2+ transients and the interaction of these transients with Ca2+-binding molecules. To better understand the coupling between events at the plasma membrane and SR function, we developed a three-dimensional mathematical model of Ca2+ diffusion and regulation in smooth muscle cells derived from the one- and two-dimensional models that we utilized in previous studies (Kargacin and Fay, 1991
; Kargacin, 1994
, 2003
; Kargacin and Kargacin, 1997
). We also carried out experiments to determine the maximum rate of SR Ca2+ uptake in saponin-permeabilized smooth muscle cells and used immunofluorescence microscopy to study the distribution of SR Ca2+ pumps in these cells. The three-dimensional models simulated a cell segment in which a portion of the SR was in close apposition to the plasma membrane. This allowed us to examine the influence of the density and localization of SR Ca2+ pumps on the magnitude and spatial and temporal characteristics of the Ca2+ transients resulting from the opening of single plasma membrane Ca2+ channels and the extent and time course of SR loading during these transients. We also examined the role that Ca2+ buffering is likely to play in coupling SR Ca2+ uptake to single-channel Ca2+ transients in the microenvironment between the plasma membrane and the SR.
| MATERIALS AND METHODS |
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Three-dimensional model of Ca2+ diffusion and regulation in smooth muscle cells
The three-dimensional model of Ca2+ diffusion and regulation in a smooth muscle cell segment that was used in our simulations is shown diagrammatically in Fig. 1. The cell segment was cylindrical in shape (diameter = 2 µm; length = 10 or 20 µm). Diffusion and regulatory processes were modeled using the explicit finite-differences method described by Crank (1975)
to numerically solve the following partial differential equation:
![]() | (1) |
, and l are the radial, angular, and length dimensions in a cylindrical coordinate system, D is the diffusion coefficient, and F(r,
,l,[Ca],t) is a function describing the position, concentration, and time-dependent regulatory processes included in the model (see Eqs. 24 below). (Note that in this and the following equations, [Ca] refers to [Ca2+]i.) The modeled cell segment was divided into 40 radial elements (each one extending 25 nm in the radial direction), 20 or 40 length elements (each 500-nm long), and 20 (18°) angular elements. Near-membrane SR was represented by a segment of a cylindrical volume located 25 nm from the plasma membrane with a thickness in the radial direction of 50 nm, a length of 4 µm and spanning 54° in the angular direction (see Fig. 1). These dimensions are in keeping with those reported in the literature for segments of the near-membrane SR (see Devine et al., 1972
, 0) = Ca(r,
, 1) and Ca(r,
, L + 1) = Ca(r,
, L) where L is the total length of the cell segment). These boundary conditions did not affect the outcome of simulations reported here because the localized Ca2+ signals that were modeled did not reach the longitudinal boundaries of the cell segment (Kargacin, 2003
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0.3 µm in the angular direction) located between the plasma membrane and the SR membrane, immediately in front of the center of the SR segment (see Fig. 2 B). Ca2+ buffering in the cell segment was the same at all locations and was described by the equation
![]() | (2) |
Ca2+ uptake into the SR was described by the Hill equation,
![]() | (3) |
![]() | (4) |
Measurement of SR Ca2+ uptake in suspensions of isolated smooth muscle cells
Ca2+ uptake into the SR of saponin-permeabilized isolated rabbit stomach smooth muscle cells was measured using fura-2 as described previously (Pollock et al., 1998
; also see Kargacin and Kargacin, 1995
). Briefly, enzymatically dispersed cells were saponin-permeabilized in a rigor buffer (150 mM K-methanesulfonate, 1 mM Mg-methanesulfonate, 5 mM EGTA, 20 mM piperazine-n,n'-bis(2-ethanesulfonic acid; pH 7.0), centrifuged (10 x g), resuspended in uptake buffer (100 mM KCl, 10 mM MgCl2, and 20 mM HEPES at pH 7.0), and then centrifuged and resuspended three more times in uptake buffer. Suspensions of cells (50 µl) in uptake buffer (see below) were pipetted into a small (
75 µl) chamber on the stage of an inverted microscope. After measuring background fluorescence and light scatter at 340- and 380-nm excitation and 510-nm emission, fura-2 (7.5 µM, final concentration) was added to the chamber and SR Ca2+ uptake was initiated by the addition of MgATP (12 mM, final concentration) and an ATP regenerating system consisting of creatine phosphate and creatine phosphokinase (final concentrations of 12 mM and 19 U/ml, respectively). Solutions in the chamber were constantly stirred and fluorescence was measured at 510 nm with a photomultiplier through the side port of the microscope. Excitation light (alternating 340 nm and 380 nm), was provided by a fluorometer (SPEX CMX model; Edison, NJ) through the epifluorescence port of the microscope. 340:380 fluorescence ratios were obtained at 1-s intervals. Experiments were conducted at 22°C.
Raw 340:380 fluorescence ratios were corrected for light scatter and background fluorescence and converted first into [Ca2+]free using the equation of Grynkiewicz et al. (1985)
and then into [Ca2+]total by solving a set of simultaneous equations to account for Ca2+ binding to the various components in the uptake buffer (see Kargacin and Kargacin, 1995
; Pollock et al., 1998
). Uptake velocities were determined from the negative slopes of the [Ca2+]total vs. time curves during the time of most rapid Ca2+ uptake according to the equation
![]() | (5) |
Immunofluorescence labeling
Freshly isolated rabbit stomach smooth muscle cells were fixed (20 min) in 1% paraformaldehyde added to the isolation medium, washed 3x in phosphate buffered saline (PBS; 150 mM NaCl, 2.1 mM NaH2PO4, and 8.4 mM Na2HPO4 at pH 7.3), permeabilized for 45 min with 0.1% Triton X-100 in PBS, washed 2x in PBS and once in incubation buffer (PBS with 3% BSA and 0.05% Tween). Cells were incubated with anti-SERCA2 or anti-phospholamban overnight at 4°C in incubation buffer, washed 3x in incubation buffer and incubated 11.5 h at room temperature with a Cy3- or AlexaFluor 488-conjugated secondary antibodies in incubation buffer. Labeled cells were washed 3x in PBS and pipetted (6 µl aliquots) into drops of 95% glycerol on glass slides. For the dual-label experiments, the cells were incubated with one primary antibody overnight at 4°C, washed 3x in incubation buffer and incubated with the second primary antibody for 11.5 h at room temperature. After washing 3x with incubation buffer, the cells were then incubated with secondary antibodies (added together) and treated as described above. Immunofluorescence images were either recorded on 35-mm film and digitized later with a scanner, or directly collected with a digital camera.
| RESULTS AND DISCUSSION |
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0.1 to 5 pA with open times ranging from
1 to 5 ms (see Benham et al., 1987
0.2 pA (at -40 mV in 2 mM extracellular Ca2+). Zou and co-workers (Zou et al., 1999
1 pA (at -80 mV in 2 mM extracellular Ca2+). Fig. 2 A shows the predicted [Ca2+] as a function of position along the length of the segment in the near-membrane space of the central plane of the modeled cell segment 3 ms after the opening of a single plasma membrane Ca2+ channel carrying a current of 0.1 pA. The relative positions of the influx site and the SR element in the model are shown diagrammatically in Fig. 2 B. Fig. 2 C shows the time course of a predicted Ca2+ transient in the volume element immediately adjacent to the plasma membrane in the model for the simulation shown in Fig. 2 A (open time for the channel was 4 ms). The [Ca2+]i in this volume element reached a maximum value of
35 µM. After the closing of the channel, [Ca2+]i, declined rapidly due to diffusion away from the influx site and binding to the Ca2+ buffer included in the model. For the simulation shown in Fig. 2, A and C, [buffer]free in the cytoplasm was 200 µM before the channel opened ([buffer]total = 230 µM); for this simulation, although the SR element was present in the model as a diffusion barrier, Ca2+ uptake into the SR was not included.
Influence of SR Ca2+ uptake on near-membrane [Ca2+]i in response to the opening of a single plasma membrane Ca2+ channel
To determine the extent to which SR Ca2+ uptake is likely to influence the [Ca2+]i reached in the restricted diffusion space between the plasma membrane and a near-membrane SR element, simulations were carried out with SR Ca2+ uptake included in the model. In the simulations, SR uptake was assumed to occur at all points on the surface of the SR facing the plasma membrane. To our knowledge, the density of Ca2+ pumps on the SR membrane of smooth muscle cells is not known. In previous work (Kargacin and Fay, 1991
; also see discussion in Kargacin and Kargacin, 1995
), however, based on 1), determinations of the rate at which Ca2+ is removed from the cytosol of smooth muscle cells after contractile stimulations (Becker et al., 1989
); 2), the Ca2+ extrusion rate per unit area of the smooth muscle plasma membrane surface (determined by Lucchesi et al., 1988
; also see Kargacin and Fay, 1991
); 3), the relative contributions of plasma membrane extrusion mechanisms and SR Ca2+ uptake to the Ca2+ removal process (Kargacin and Kargacin, 1995
; also see Kargacin and Fay, 1991
); and 4), the volume of the SR in smooth muscle cells (determined by Devine et al., 1972
), we computed an SR Ca2+ uptake rate per cm2 of SR surface area of
3 x 10-12 mol-Ca2+ cm-2 s-1.
For the following simulations, we used this value as a starting point and varied the uptake rate into the near-membrane SR element in the model about this value. The results in Fig. 3 A show the near-membrane Ca2+ transients predicted by the model after the opening of a single plasma membrane Ca2+ channel (4 ms open time; 0.1 pA Ca2+ current) when SR uptake was not included in the model (black trace) and when SR uptake was included and the maximum uptake velocity was 3, 15, 30, or 150 x 10-12 mol-Ca2+ cm-2 s-1. The amplitude of the near-membrane Ca2+ transient was not greatly affected by SR Ca2+ uptake except at the highest SR Ca2+ uptake velocity. Furthermore, the amount of Ca2+ reaching the central cytoplasm of the cell was not greatly influenced by the SR uptake except in the case of the highest uptake rate. After the opening of the plasma membrane Ca2+ channel, maximum [Ca2+]i in the same plane and longitudinal position as the Ca2+ channel but at a central cytoplasmic position (at a position 0.5 µm from the plasma membrane; see Fig. 3 C) increased from a resting level of 150 to 215 nM when SR uptake was not included in the model. When SR uptake was included, [Ca2+]i at this same cytoplasmic point reached levels of 213, 204, 195, and 152 nM, respectively, when simulations were run with SR uptake rates of 3, 15, 30, and 150 x 10-12 mol-Ca2+ cm-2 s-1.
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Measurement of SR Ca2+ uptake in saponin-permeabilized isolated smooth muscle cells
Only the highest SR Ca2+ uptake rate used in the model (which would require an SR Ca2+ uptake velocity 50x greater than that computed in our previous studies; see Kargacin and Fay, 1991
) had a significant impact on 1) the predicted magnitude of the single channel Ca2+ transient, 2) the amount of Ca2+ reaching the central cytoplasm of the cell, and 3) the association of Ca2+ with the Ca2+ buffer in the modeled cell segment. The estimate of the SR uptake rate (3 x 10-12 mol cm-2 s-1) that we used as a starting point for the simulations discussed above was determined indirectly from the rate at which Ca2+ declines in smooth muscle cells during contractile signaling and the likely contribution of plasma membrane extrusion processes to this decline (see Kargacin and Fay, 1991
; Lucchesi et al., 1988
; Cooney et al., 1991
). To determine if this estimate was accurate, we measured Ca2+ uptake into the SR of saponin-permeabilized isolated rabbit stomach smooth muscle cells and computed a Ca2+ uptake rate per unit surface area of SR from these measurements. Fig. 4 A shows the raw fura-2 fluorescence data and a corresponding uptake curve showing the change in [Ca2+]total in the uptake buffer (Fig. 4 B) for a typical SR uptake Ca2+ experiment . The maximum rate of uptake for the curve shown (computed from the points on the curve shown by the filled circles in Fig. 4 B) was 22.6 nmol g-cell-protein-1 s-1. The mean uptake rate measured at 22°C for 76 such experiments from nine different isolated rabbit stomach smooth muscle cell preparations was 28 ± 2 nmol g-cell-protein-1 s-1. The highest mean uptake rate of the nine different isolated cell preparations we used for the experiments was 57 nmol g-protein-1 s-1. Assuming a specific gravity of 1 g ml-1, a Q10 for SERCA2 SR Ca2+ pumps of 2.5 (see Lundblad et al., 1986
), and a weight ratio of cell protein:cell water of 1:4, a mean uptake rate of 26 x 10-6 mol l-cell volume-1 s-1 at 37°C can be calculated from the measured mean uptake rate of 28 nmol g-cell-protein-1 s-1. Although Devine and co-workers (Devine et al., 1972
) did not determine the percentage of cell volume occupied by the SR for rabbit stomach smooth muscle cells, they did determine a value of
2% for rabbit Taenia coli. Using an SR volume:cell volume ratio of 0.02, a mean Ca2+ uptake rate per unit volume of SR of 13 x 10-4 mol l-SR-1 s-1 can be computed. The volume of the near-membrane SR segment in the model cell is 18 x 10-17 l and the surface area is
7 x 10-8 cm2. Therefore, the expected Ca2+ uptake rate of the SR element in the model per unit surface area, based on our uptake experiments (see Fig. 4), is 3.3 x 10-12 mol cm-2 s-1. The SR volume:cell volume estimates for smooth muscle by Devine and co-workers (Devine et al., 1972
) ranged from 2% to 6% for all of the smooth muscle cell types examined. If one uses the highest SR volume:cell volume estimate, a mean uptake rate of 1.1 x 10-12 mol cm-2 s-1 can be computed. If we use the highest mean uptake rate measured for our different cell preparations (57 nmol g-protein-1 s-1), our estimates of the uptake rate range between 2.2 x 10-12 and 6.6 x 10-12 mol cm-2 s-1 for the SR element in our simulations when the total SR volume ranged between 2% and 6% of the cell volume. Permeabilized toad stomach smooth muscle cells lose
30% of their soluble protein during isolation and permeabilization (see Kargacin and Fay, 1987
). A similar protein loss from the rabbit stomach smooth muscle cell preparations would result in an overestimate of Ca2+ uptake rates of
30%. Our measured mean SR Ca2+ uptake rates (ranging between 1.1 and 6.6 x 10-12 mol cm-2 s-1) are consistent with the uptake rate per unit area of SR membrane that we estimated indirectly in our previous work (Kargacin and Fay, 1991
). Thus it is unlikely that uptake rate per unit area of SR membrane (3 x 10-12 mol cm-2 s-1) that was used as a starting value in our simulations could be an order-of-magnitude lower than the mean SR Ca2+ uptake rate in smooth muscle cells in vivo. If the peripheral SR plays a major role in shaping Ca2+ transients in smooth muscle cells, flux of Ca2+ into the near-membrane SR would have to be much greater than the cellular average.
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35 µM immediately adjacent to a plasma membrane Ca2+ channel carrying a current of 0.1 pA during the 4-ms time period that the channel is open (see Fig. 2). A Ca2+ concentration of this magnitude (>100x the [Ca2+]50% of the smooth muscle SR Ca2+ pump
200 nM; see Materials and Methods) would be expected to saturate the SR Ca2+ pumps immediately facing the influx site. The Ca2+ gradient in the near-membrane space is predicted to be very steep; however (see Fig. 2 A), when cytoplasmic Ca2+ buffering is reduced, the higher [Ca2+] and the ability of Ca2+ to spread longitudinally and in the angular direction beyond the site of influx would allow the SR to take up additional Ca2+ at sites away from those opposing the channel. Thus reduced Ca2+ buffering in the near-membrane diffusion space would allow Ca2+ to more quickly reach SR pumps more distant from the influx site. For a channel carrying a 0.1 pA current with an open time of 4 ms the model predicted a maximum [Ca2+]i of 0.47 µM in the near-membrane space 2 ms after the channel closed when the starting cytoplasmic free buffer concentration was 200 µM. When the cytoplasmic buffer concentration was 100 µM, the predicted maximum [Ca2+]i was 0.62 µM and, when the cytoplasmic buffer concentration was 0, the predicted maximum [Ca2+]i was 1.56 µM. At this same time point, the widths of the Ca2+ signals at half-maximal Ca2+ concentration were
600 nm, 700 nm, and 800 nm, respectively, for starting free buffer concentrations of 200, 100, and 0 µM.
The Ca2+ buffers incorporated into the model were assumed to be immobile. This assumption may not hold for all Ca2+-binding molecules, however. Of the endogenous mobile Ca2+ buffers, most are likely to be proteins (e.g., calmodulin) which have cytoplasmic diffusion coefficients an order-of-magnitude less than the diffusion coefficient for Ca2+ (see Smith et al., 1996
). Thus, for the time periods considered in our simulations, the impact of assuming that these buffers are immobile would be minimal. Highly mobile Ca2+ buffers, on the other hand, could increase the apparent diffusion coefficient for Ca2+ in cells. Studies with small Ca2+-binding molecules introduced into cells exogenously (e.g., fluorescent Ca2+ indicators) suggest that such buffers can increase the apparent cytoplasmic Ca2+ diffusion coefficient by a factor of 2 or more (see Zhou and Neher, 1993
). Endogenous buffers of this type could facilitate SR Ca2+ loading by allowing Ca2+ to more rapidly move away from sites where the SR Ca2+ pumps are saturated. Whether endogenous highly mobile Ca2+ buffers are present in smooth muscle cells is unknown, however. In adrenal chromaffin cells, Zhou and Neher (1993)
were unable to obtain evidence of the presence of highly mobile endogenous buffers suggesting that these buffers did not contribute significantly to the Ca2+ binding capacity in these cells.
SR loading after Ca2+ influx through a single plasma membrane Ca2+ channel carrying a current of 1 pA
Although the SR Ca2+ pumps facing a plasma membrane Ca2+ channel are predicted to saturate after the single channel openings discussed above, spreading of Ca2+ in the near membrane space longitudinally and in the angular dimension would allow additional uptake to occur by pumps at more distal sites even if the SR pumps nearest the channel were saturated. The simulations shown in Fig. 7 A compare SR Ca2+ loading after 4-ms openings of single channels passing 0.1 and 1 pA Ca2+ currents. Although the amplitude of the predicted Ca2+ transient was an order-of -magnitude greater for the 1 pA current (not shown), the amount of Ca2+ taken up into the near-membrane SR element was only increased by a factor of 2 during the 4-ms time period that the channel was open (Fig. 7 A). This indicates that the SR Ca2+ pumps proximal to the influx site were working at maximum velocity, limiting the ability of the SR to take up additional Ca2+ at this site. During the following 15 ms of the simulation shown in Fig. 7 A, the rate of SR uptake continued to remain high, however, for the simulations that included the 1-pA channel as more distal uptake sites contributed to the SR loading.
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5000 channels per cell (Yatani et al., 1987
0.54 channels per µm2 of surface area. The area of the membrane overlying the SR element in our model was 3.8 µm2. Thus, one could expect 214 channels in this area if the channels in the cell are distributed uniformly. Although there is evidence for Ca2+ channel-mediated influx of Ca2+ into smooth muscle cells at rest (Ganitekvich and Isenberg, 1990
0.0003 at -40 mV, and
0.002 at -20 mV; Rubart et al., 1996
It has been suggested that L-type Ca2+ channels in vascular smooth muscle cells may be found in clusters (Klöckner and Isenberg, 1994a
,b
). If this is the case, the probability that more than one channel in a 4-µm2 area of plasma membrane could be open in a resting smooth muscle cell could be increased especially if localized changes in membrane potential due to the opening of one channel results in the opening of other nearby voltage-dependent channels. The probability of having more than one channel open would also increase during contractile activation (Quayle et al., 1993
, estimated a smooth muscle Ca2+ channel open probability of 0.44 under depolarizing conditions suggesting that, even under these conditions, based on the channel densities discussed above, 16 channels would be the maximum number of channels expected to be open in the membrane overlying the SR in our model). The results in Fig. 7 A for a single channel current of 1 pA are equivalent to those that would be obtained if there were 10 channels each carrying a current of 0.1 pA opening at the same time at a point on the plasma membrane overlying the center of the SR element in the model. As also noted above, the efficiency with which the near-membrane SR was able to take up Ca2+ after the influx event was limited by saturation of the SR pumps underlying the influx site. We also examine the effect of having a number of channels organized in a cluster about a central channel so that the transient signal was distributed over a wider area overlying the near-membrane SR. Fig. 7 B shows the results of simulations in which four channels were arranged in three different configurations about a central channel. As the mean distance from the central channel to the four other channels was increased, SR uptake was also increased. The most spacious configuration of five channels resulted in SR uptake that was approximately the same as that seen when 10 channels were confined to an area overlying the center of the SR element (compare Fig. 7, A and B).
| SUMMARY AND CONCLUSIONS |
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100 µm in length and 12 µm in diameter. Assuming a cylindrical central portion 50 µm in length and two conical shaped ends, the cell volume of a 2-µm diameter cell is
0.2 pl. Devine et al. (1972)
8 x 10-5 pl (see Methods). This volume represents at most 2% of the total SR volume expected to be present in a 100-µm-long, spindle-shaped smooth muscle cell with a radius of 2 µm. Based on these considerations, it would require a considerable number of single channel openings to significantly increase the overall SR Ca2+ content in a smooth muscle cell. This is unlikely to occur on a millisecond timescale, but could conceivably occur over several seconds or minutes.
There is considerable variation in the size of, the function of, and the mechanisms thought to regulate various types of smooth muscle cells. For this study, we developed a model that was general enough to allow us to make broadly applicable predictions. The results we obtained could be modified in specific smooth muscle cell types or for specific cellular morphologies, however. In the present model, for example, because relatively little is known about the role of the Na+/Ca2+ exchanger in smooth muscle Ca2+ regulation (discussed in Sanders, 2001
), we included Na+/Ca2+ exchange as part of a plasma membrane Ca2+ extrusion mechanism that also included the contribution of the plasma membrane Ca2+ ATPase. Arnon and co-workers (Arnon et al., 2000
) have proposed that Na+/Ca2+ exchangers are clustered as sites overlaying the SR in cultured arterial myocytes, however. If this is the case, Na+/Ca2+ exchange might play a role in modulating single channel Ca2+ transients depending upon the relative location of Ca2+ channels and these clusters on the plasma membrane. Exchangers located within a few nm of an influx site would experience a high Ca2+-dependent driving force. This could reduce the amplitude of intracellular Ca2+ transients arising at such sites. Although the role of calcium-induced calcium release in regulating smooth muscle contraction has not been well determined, ryanodine receptors are known to be present in the SR membrane in smooth muscle cells. If these receptors are located in close proximity to overlying plasma membrane Ca2+ channels, net SR Ca2+ release (as the result of calcium-induced calcium release) rather than SR uptake could result from the opening of single plasma membrane Ca2+ channels. Evidence both for and against the coupling of plasma membrane Ca2+ channel activity to SR Ca2+ release has appeared in the literature (reviewed by Sanders, 2001
). The steep Ca2+ gradient that develops near a site of Ca2+ influx would limit the spatial range over which coupling could occur between single channel events and Na+/Ca2+ exchange or ryanodine receptor-mediated SR Ca2+ release. One would also expect the plasma membrane to depolarize near a Ca2+ influx site. This would decrease the driving force for Ca2+ entry through the membrane and reduce the amplitude of localized Ca2+ transients and, consequently, the amount of Ca2+ taken up into the near-membrane SR at such sites. On the other hand, estimates of single channel currents from L-type Ca2+ channels in smooth muscle cells range over an order of magnitude (from
0.1 to
1 pA) and currents at the higher end of this range would be expected to result in higher SR uptake amounts (see Fig. 7 B).
Our experimental results, when incorporated into our model, predict that uptake of Ca2+ by the near-membrane SR in smooth muscle is unlikely to greatly influence either the magnitude of the Ca2+ transients arising from the opening of single plasma membrane Ca2+ channels or diffusion of Ca2+ away from these channels even when diffusion is restricted by the physical presence of the SR. These results appear to contradict the buffer-barrier hypothesis that has been proposed for smooth muscle cells. This hypothesis (reviewed recently by Sanders, 2001
) suggests that the close proximity of the SR to the plasma membrane at some locations allows the SR to take up a substantial amount of the Ca2+ entering a cell through the plasma membrane, thereby reducing the amount of Ca2+ that is able to reach the central cytoplasm of the cell unless the SR is fully loaded or SR Ca2+ uptake is inhibited. The results of our simulations suggest that, for such a mechanism to be operative, additional regulatory processes or structural entities that are presently not known (and were, therefore, not included in the model) would have to be present in cells. More comprehensive experimentally-derived knowledge of the microenvironments that exist between the plasma membrane and the SR membrane at sites where these two membranes are in close apposition in smooth muscle cells is required to further evaluate or model the signaling that is likely to occur in these regions. In addition to more precise knowledge of single-channel Ca2+ currents and the localization and the functioning of the Na+/Ca2+ exchanger and the plasma membrane Ca2+ pump, information about the possible clustering of SR Ca2+ pumps, about other mechanisms that could couple plasma membrane ion channel activity to SR function, and about structural proteins or cytoskeletal elements that could further limit diffusion in the near-membrane microenvironment is required for understanding the mechanisms involved in locally regulating Ca2+ in smooth muscle cells.
| ACKNOWLEDGEMENTS |
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This work was supported by the American Heart Association, the Heart and Stroke Foundation of Alberta, and the Canadian Institutes of Health Research. G.J.K. is an Alberta Heritage Foundation for Medical Research Senior Scholar.
Submitted on December 17, 2002; accepted for publication April 10, 2003.
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