Original Contribution |
From the Vascular Biology Unit, Department of Medicine, Boston University Medical Center, Boston, Mass.
Correspondence to Dr Victoria M. Bolotina, Vascular Biology Unit, R-408, Boston University Medical Center, 88 E Newton St, Boston, MA 02118. E-mail vbolotina{at}med-med1.bu.edu
| Abstract |
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Key Words: nitric oxide sarcoplasmic/endoplasmic reticulum Ca2+ ATPase cation influx Ca2+ platelets
| Introduction |
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Nitric oxide (NO), a potent inhibitor of thrombin-activated platelet aggregation,12 13 is known to decrease Ca2+cyt that is raised by agonists,14 although the mechanism is not well defined. It has been shown that NO inhibits thrombin- and IP3-stimulated Ca2+ release from internal stores in intact15 and permeabilized platelets.16 17 However, it is still unclear whether NO also inhibits capacitative cation influx. Brune et al17 found a significant inhibitory effect of the NO donor, sodium nitroprusside, on Mn2+ influx in TG-treated platelets. In contrast, Okamoto et al18 did not find an effect of the NO donor on TG-induced Ca2+ influx in human platelets and concluded that capacitative Ca2+ influx is resistant to NO.
The data presented here demonstrate that NO, indeed, is a potent inhibitor of capacitative cation influx in human platelets and that SERCA activity is required for this effect. This finding is consistent with the idea that NO inhibits capacitative cation influx indirectly by promoting SERCA-dependent refilling of intracellular Ca2+ stores.
| Materials and Methods |
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For experiments on permeabilized platelets, cells were obtained by gel filtration as follows. Prewashed Sepharose-2B gel (Sigma) was placed into the plastic column with the 70-µm nylon mesh attached to the bottom and equilibrated with a 3x volume of standard HEPES buffer of the following composition (in mmol/L): NaCl 137, KCl 2.7, MgCl2 · 6H2O 1, NaH2PO4 3.3, glucose 5.5, and HEPES 3.8 (pH 7.4). Ca2+ was not added to the buffer, but its residual concentration was 1 to 3 µmol/L as measured by Ca2+-sensitive electrode. Buffer was supplemented with 100 µmol/L aspirin and 6 mU/mL apyrase to prevent platelet activation with thromboxane A2 and traces of ADP, respectively. After collection, the platelet suspension was stored at 37°C and used during the next 3 to 4 hours. The cell number in the suspension used for experiments was 2 to 2.5x108/mL.
Fluorescence Measurements
The fluorescent probe fura-219 was used to
monitor changes in Ca2+cyt in
platelets. PRP was diluted with standard buffer to the final cell
number of
108/mL and centrifuged at
750g for 10 minutes. Platelets were resuspended in the
same buffer containing 2.5 µmol/L fura-2/AM and incubated at
37°C for 10 minutes. The platelet suspension was then
centrifuged at 750g for 10 minutes and resuspended
in 2 mL of buffer immediately before the fluorescence
measurements. Cells were loaded with fura-2 before each run. Each
experiment was done with 6 to 8x107 cells/mL.
Fluorescence (F) measurements were carried out at
37°C using a spectrofluorimeter (Hitachi F-4500) with excitation
wavelength alternating between 340 and 380 nm every 0.5 s and
emission wavelength 510 nm. Changes in
Ca2+cyt were estimated from the
F340/F380 ratio
(R340/380). Data collection, ratio
calculation, and analysis were performed with the Hitachi
software. All the recordings were corrected for the cell
autofluorescence determined in unloaded platelets. In some
experiments the initial rate of fall in Ca2+
concentration caused by NO in thrombin-stimulated platelets, and
after addition of IP3 or
Ca2+ in permeabilized
platelets, was estimated from the initial slope during the first 5
to 20 seconds. Importantly, control experiments showed no evidence for
a direct effect of NO either on response of fura-2 to
Ca2+ or on the fluorescence properties of
fura-2. To study cation influx, Mn2+ (100 to
300 µmol/L) was added to the platelets suspended in standard
buffer, and the rate of fura-2 quenching at an excitation and emission
wavelength of 360 and 510 nm, respectively, was determined. The rate of
Mn2+ influx was estimated from the slope during
the first 60 s after Mn2+ addition, and the
linear fit was performed with Microcal Origin software.
Experiments on Permeabilized Cells
Before the experiment, platelets were resuspended in an
artificial cytoplasmic solution containing (in mmol/L): KCl
110, NaCl 10, KH2PO4 1,
KH2CO3 5, and HEPES 20 (pH
7.1) and supplemented with 1 µg/mL oligomycin, 2 µg/mL antimycin,
2 mmol/L MgATP, and an ATP-regenerating system containing 5
mmol/L creatine phosphate and 15 U/mL creatine kinase. There was no
Ca2+ added, and its residual concentration in the
cytoplasmic solution was 1 to 3 µmol/L (as measured by a
Ca2+-sensitive electrode). Fura-2
(K+ salt, 1 µmol/L) was added to this
solution to monitor the changes in free Ca2+.
During the experiment 20 µg/mL saponin was applied directly to the
recording chamber, causing permeabilization of the platelet
plasma membrane and resulting in sequestration of external
Ca2+ into the stores, lowering the free
Ca2+ concentration (see Figure 7A
). After
4 to 6 minutes, Ca2+ concentration stabilized at
a level of 200 to 250 nmol/L as calculated from the ratio
F340/F380
assuming a Kd for fura-2 of 224
nmol/L.19
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NO Solution
A standard 1-L intravenous bag was filled with
distilled water (750 mL) that had been bubbled with nitrogen gas to
remove oxygen. Approximately 30 mEq of Bio-Rad analytical-grade anion
exchange resin was mixed in the water before the bag was filled. The
resin retains any nitrites or nitrates that may be formed by the
reaction of NO with oxygen. The contents of the bag were bubbled with
nitrogen gas for another 30 minutes. The contents were then mixed
thoroughly, and the bag was placed in a refrigerator at 4°C. The
concentration of NO in the solution equilibrated to give a
3.1±0.6 mmol/L (n=5) saturated solution that was stable at least
for 1 week as measured by a chemiluminescent nitric oxide
analyzer (Sievers NOA model 270). The absence of contaminating
nitrite in saturated NO solution was confirmed by obtaining a similar
analysis in the presence and absence of a reducing agent in the
reflux chamber of the analyzer (KI in glacial acetic
acid). At the time of the experiment, subsequent dilutions were made
from the saturated NO solution by drawing off the solution from the bag
with a gas-tight syringe and dissolving it in sealed tubes filled with
deoxygenated solution (bubbled with nitrogen for 1
hour).
Materials
NO gas was from Matheson. Fura-2/AM and fura-2
(K+ salt) were from Molecular Probes. BHQ and
IP3 were from Calbiochem. All other drugs were
from Sigma.
Statistical Analysis
Each experiment was repeated 3 to 9 times. ANOVA and paired
t test were used to determine the statistical significance
of differences in obtained data. P<0.05 was considered
significant. The results on the bar graphs are expressed as
mean±SE.
| Results |
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Thrombin-Induced Cation Influx
To experimentally separate intracellular
Ca2+ release from cation influx from the
extracellular space, thrombin was applied at a submaximal concentration
(0.5 U/mL) to suspensions of fura-2loaded platelets in
Ca2+-free medium. Cation influx was then
analyzed following the addition of Ca2+
(1 mmol/L) or Mn2+ (100 µmol/L). A
typical experiment (Figure 1A
and 1B
)
shows that application of thrombin in the absence of extracellular
Ca2+ caused a very rapid increase in
Ca2+cyt that, after reaching a
maximum, declined to a lower steady-state level. Adding extracellular
Ca2+ after thrombin caused an immediate further
increase in Ca2+cyt, resulting
from Ca2+ influx (Figure 1A
and 1B
). The
amplitude of the maximal Ca2+ rise, determined
mainly by Ca2+ influx, depended on the period
between the addition of thrombin and Ca2+. Figure 2A
summarizes the time dependence
of thrombin-induced Ca2+ influx, showing that it
was maximal when Ca2+ was added 30 s after
thrombin and that it decreased as the period between addition of
thrombin and Ca2+ increased to 10 to 15 minutes.
Ca2+ (1 mmol/L) added to unstimulated
platelets resulted in only a minor increase in fura-2 ratio (Figure 2A
), indicating that leakage of the dye out of platelets and
passive thrombin-independent Ca2+ influx were
both negligible. Thrombin also elicited Mn2+
influx, measured as the rate of quenching of fura-2
fluorescence (Figure 1C
and 1D
). Similar to
Ca2+ influx, the rate of
Mn2+ influx depended on the time after thrombin
application. The Mn2+ influx was maximal after
30 s; however, after 5 minutes, thrombin caused almost no increase
in the rate of Mn2+ influx as compared with the
passive leak (Figure 2C
).
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BHQ-Induced Cation Influx
In Ca2+-free medium, BHQ caused a slower,
smaller, and more sustained increase in
Ca2+cyt (Figure 3B
) compared with that of thrombin.
Subsequent addition of external Ca2+ caused a
rapid increase in Ca2+cyt which,
after reaching a peak, declined to a steady-state level (Figure 3A
and 3B
). Unlike the thrombin-activated
Ca2+ influx, the amplitude of the BHQ-induced
Ca2+ influx increased with time following
application of BHQ (Figures 2B
and 3
), reaching a maximum
after 5 to 10 minutes.
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As with Ca2+ influx, BHQ-induced
Mn2+ influx increased during the period between
the addition of BHQ and Mn2+, being negligible
during the first 30 s and reaching a maximum in 5 minutes. Figure 2D
summarizes the relationship between the length of the period
between addition of BHQ and Mn2+ and the rate of
influx.
Effect of NO on Thrombin- and BHQ-Activated
Ca2+ and Mn2+ Influx
To determine whether authentic NO has an
inhibitory effect on capacitative cation influx in human
platelets, NO was applied 30 s before addition of
Ca2+ or Mn2+ in
platelets stimulated with thrombin or BHQ. When added after
thrombin-induced Ca2+ mobilization had reached
the peak, NO (1 µmol/L) significantly increased the initial rate
of decline in Ca2+cyt (from
0.007±0.002 ratio units/s before NO addition to 0.088±0.004 ratio
units/s after NO addition; n=6, P<0.001) (Figure 1A
;
see also Figure 4C
) and profoundly
inhibited the subsequent Ca2+ rise and
Mn2+ influx (Figure 1
). The effect of NO
did not depend on the time of incubation with thrombin (Figure 2A
and 2C
), decreasing Ca2+ concentration
and Mn2+ influx to a level that approximated the
level that could be attributed to passive Ca2+
leak. When added to the thrombin-stimulated cells after
Ca2+ influx reached equilibrium, NO decreased
Ca2+cyt to a level similar to
that reached when NO was added before Ca2+
(Figure 1A
and 1B
). When NO-containing solution was exposed to
the air for 1 hour and then applied to platelets, it produced no
effect on Ca2+cyt (not shown,
n=3), indicating that NO, rather than the products of its
degradation, was the active inhibitor of thrombin-induced
cation influx.
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Contrary to that induced by thrombin, the influx of
Ca2+ and Mn2+ induced by
BHQ was affected by NO only during the first few minutes of BHQ
treatment (Figure 3A
and 3C
). Summary data are shown in Figure 2B
and 2D
. However, after pretreatment of platelets with BHQ
for 5 to 10 minutes, NO did not affect the subsequent
Ca2+ and Mn2+ influx
(Figures 2B
and 2D
and 3B and 3D) significantly. These
results illustrate the time-dependent disappearance of the effect of NO
on capacitative cation influx during the progressive inhibition of
SERCA by BHQ. This points to the importance of SERCA-dependent store
refilling for NO-induced inhibition of influx.
NO Increases the Amount of Ca2+ Released by Ionomycin
in Thrombin-Activated Platelets
We conducted the following experiments to determine whether NO
affects Ca2+ stores in thrombin-activated
platelets. Figure 4
shows thrombin-induced
Ca2+ release in the absence of extracellular
Ca2+. Five minutes after thrombin application,
ionomycin (2 µmol/L) was applied to release the remaining
portion of Ca2+ from the stores. When ionomycin
was applied after thrombin, it caused a 2.5 times smaller rise in
Ca2+cyt than when it was applied
alone to unstimulated platelets (Figure 4A
; peak
R340/380 was 1.4±0.1 versus 3.5±0.3
ratio units, respectively; n=4, P<0.005). This indicates
that after release from the stores by thrombin,
Ca2+ is taken up into the stores and is also
extruded from the cells. To test whether NO can increase the amount of
Ca2+ in the stores after they were emptied by
thrombin, NO (1 µmol/L) was added at different times before or
after the agonist. When NO was applied 30 s before thrombin
(Figure 4B
), the amplitude of the thrombin response was slightly
suppressed (peak
R340/380 was 1.0±0.1
versus 1.3±0.1 ratio units in control; n=4, P>0.05), but
the initial rate of decline in
Ca2+cyt was significantly
accelerated (from 0.007±0.001 to 0.014±0.001 ratio units/s; n=4,
P<0.005). The amplitude of the ionomycin-induced
Ca2+ release in this case was
65% more than
that obtained without NO (peak
R340/380
was 2.2±0.1 compared with 1.4±0.1 ratio units without NO; n=4,
P<0.001). When added 1 minute after thrombin, NO greatly
accelerated the decline in
Ca2+cyt and increased the
response to ionomycin by 36% (peak
R340/380 was 1.7±0.1 ratio units; n=4,
P<0.05; Figure 4C
). When NO was applied 30 s
before ionomycin, it did not significantly increase the amplitude of
Ca2+ release by ionomycin (peak
R340/380 was 1.5±0.1 ratio units; n=4,
P>0.05; Figure 4D
).
These results suggest that after Ca2+ is released from the stores by thrombin, NO can promote its uptake into the stores, which can be a result of acceleration of Ca2+ back-sequestration or, alternatively, inhibition of Ca2+ release. To discriminate between these possibilities, the following experiments were performed.
Inhibition of SERCA Abolishes the Effect of NO on Thrombin-Induced
Ca2+ Release
In Ca2+-free medium, thrombin (0.5 U/mL)
caused a fast Ca2+ rise resulting from
Ca2+ release from the stores, followed by a
slower Ca2+ decline as a result of its uptake
into the stores and extrusion from the cell (Figure 5A
). Addition of NO (1 µmol/L)
30 s before thrombin (Figure 5A
) decreased the peak of
transient Ca2+ rise (from 1.4±0.1 ratio units to
0.9±0.1; n=5, P<0.05) and dramatically accelerated the
uptake/extrusion phase of Ca2+ transient
(0.014±0.002 ratio units/s in the presence of NO versus 0.008±0.001
in control; n=5 P<0.05). When platelets were pretreated
with 30 µmol/L BHQ for 5 minutes, Ca2+ was
partially released from the stores, and thrombin was applied after BHQ
released the remaining Ca2+ (Figure 5B
).
Pretreatment with BHQ eliminated the effect of NO on both peak
thrombininduced Ca2+ release (0.9±0.1 ratio
units in control versus 0.9±0.1 in the presence of NO; n=5,
P>0.05) and the rate of the subsequent uptake/extrusion
(0.008±0.001 ratio units/s versus 0.008±0.0011; n=5,
P>0.05). These experiments show that functional SERCA is
required for the effect of NO on both rising and falling phases of
thrombin-induced Ca2+ transient.
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Inhibition of Mitochondria Does Not Prevent the Effect of NO on
Ca2+cyt
By taking up Ca2+ during agonist-induced
activation, mitochondria could be involved in the regulation of
capacitative Ca2+ influx in different types of
cells.21 22 23 Inhibitors of mitochondrial
metabolism were therefore used to determine whether
mitochondria are involved in the inhibition of the thrombin-induced
Ca2+ rise in intact platelets caused by NO.
Figures 6A
and 6B
illustrate the effect
of NO on thrombin-activated Ca2+ release
and influx under control conditions (Figure 6A
) and in the
presence of the mitochondrial inhibitors (Figure 6B
)
oligomycin (1 µg/mL) and antimycin (2 µg/mL). As in the data
obtained in the Jurkat cell line,24 inhibition of
mitochondria decreased the amplitude of thrombin-induced
Ca2+ rise (from 1.8±0.2 to 1.4±0.1; n=3,
P<0.05). However, the inhibition by NO of the
thrombin-initiated Ca2+ release and influx was
unchanged. These results indicate that uptake of
Ca2+ into mitochondria is not involved in the
inhibitory effect of NO on
Ca2+cyt in platelets.
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Inhibitor of cGMP Production, H-(1,2,4)
Oxadiazolo(4,3-a) Quinoxallin-1-one (ODQ), Attenuates but Does Not
Prevent the Effect of NO on Ca2+ Influx
To evaluate the role of cGMP formation in the effect of NO on
Ca2+ influx, specific guanylate
cyclase inhibitor, ODQ,25 26 was used. At
the concentration used in these experiments, ODQ has been shown to
completely prevent the NO-induced cGMP rise in
platelets.27 The effect of NO (1 µmol/L) on the
rate of Ca2+ removal from the cytoplasm and on
Ca2+ influx was compared in control platelets
(preincubated with the vehicle, 0.1% DMSO) and in the platelets
preincubated with ODQ (10 µmol/L) for 1 hour (Figure 6C
and 6D
). Pretreatment with ODQ did not alter the kinetics of the
Ca2+-release phase or amplitude of the maximal
Ca2+ influx following platelet stimulation
with thrombin. However, it resulted in a small but significant
attenuation of the inhibitory effect of NO on the
Ca2+ increase associated with
Ca2+ influx. The rates of the NO-induced
acceleration of the falling phase of Ca2+
transient in control and ODQ-pretreated platelets were 0.051±0.003
ratio units/s and 0.039±0.003, respectively (n=5, P<0.05),
which corresponds to a 24% decrease. The amplitude of the
thrombin-induced Ca2+ influx phase was inhibited
by NO by 82% in the cells preincubated with vehicle (1.46±0.17 ratio
units versus 0.26±0.02; n=5, P<0.01) and only by 67% in
ODQ-treated cells (1.44±0.16 ratio units versus 0.47±0.06; n=5,
P<0.01). Thus, the effect of NO (1 µmol/L) on
Ca2+ influx in platelets is partially
mediated by cGMP formation. These experiments also indicate the
possible existence of another, cGMP-independent mechanism of NO-induced
inhibition of capacitative cation influx in platelets.
NO Accelerates Ca2+ Uptake by the Stores in
Permeabilized Platelets
To directly monitor the process of filling and emptying of
internal Ca2+ stores and to eliminate the
involvement of the IP3 cascade and plasma
membrane-associated regulatory proteins (plasma membrane
Ca2+-ATPase [PMCA] or
Na+/Ca2+ exchanger), the
free-Ca2+ level was measured in suspensions of
permeabilized platelets. Addition of saponin (20
µg/mL) to the platelets resuspended in cytoplasmic solution
caused an immediate decrease in free Ca2+ (Figure 7A
), which was completely prevented by
BHQ (30 µmol/L) added 2 minutes before saponin (not shown). In
the presence of 2 mmol/L ATP, cytoplasmic
Ca2+ decreased from 1 to 3 µmol/L to a
stable level or set point28 29 of 200 to 250 nmol/L and
remained at the same low level for at least 10 minutes. When
Ca2+ (1 µmol/L) was added to
permeabilized cells, it was rapidly taken up by the
stores, and the same level of free Ca2+ was
restored (Figure 7A
). This decrease in free
Ca2+ concentration was used in our experiments as
a measure of Ca2+ uptake by the stores.
Application of IP3 (250 µmol/L) caused the
rapid release of stored Ca2+, which also was
almost completely resequestered into the stores. Inhibition of SERCA
with BHQ caused slow and irreversible release of
Ca2+ from the stores into the cytoplasmic
solution. Heparin, a blocker of IP3
receptors,30 31 completely abolished
IP3-induced Ca2+ release
but was without any effect on the Ca2+ rise and
uptake after exogenously added Ca2+ (Figure 7B
), indicating that these processes do not involve
IP3-sensitive channels.
NO (1 µmol/L) significantly increased the rate of
Ca2+ uptake after
IP3-induced release (0.077±0.006 versus
0.024±0.003 ratio units/s in control; n=5, P<0.001; Figure 7C
), but it had no effect if applied after BHQ (Figure 7D
). Because the effect of NO on
IP3-induced Ca2+ release
could be due either to inhibition of IP3-induced
Ca2+ release or to acceleration of uptake into
the stores, the effect of NO on Ca2+
sequestration in the absence of IP3 was
determined.
Exogenous Ca2+ was added to the suspension of
platelets after the cells were permeabilized and
the set point was allowed to reestablish. The rate of uptake of
exogenously added Ca2+, as well as the lowest
free-Ca2+ level reached after
Ca2+ addition and uptake, was highly dependent on
the ATP concentration (Figure 8A
and 8B
).
When added 30 s before Ca2+, NO
significantly accelerated the rate of Ca2+
sequestration into the stores (Figure 8C
). However, the effect
of NO was strongly dependent on the rate of sequestration observed in
the absence of NO, which, in turn, depended on ATP concentration
(Figure 8C
and 8D
). For example, at the higher rate of
Ca2+ uptake typical for 2 mmol/L ATP (Figure 8B
), there was no effect of NO (Figure 8D
; 0.042±0.005
ratio units/s under control conditions and 0.044±0.006 ratio units/s
in the presence of NO; n=4, P>0.1). However, at lower ATP
concentrations (100 to 200 µmol/L ATP), NO significantly
accelerated Ca2+ uptake (Figure 8C
), but
this was observed only in those experiments in which the control rate
was lower than 0.03 ratio units/s (Figure 8E
). For these
experiments, NO significantly increased the rate of
Ca2+ uptake into the stores from 0.015±0.003 in
control to 0.022±0.003 ratio units/s in the presence of NO (n=7,
P<0.05), representing an average 47% increase.
Figure 8E
summarizes the dependence of the effect of NO on the
control rate of Ca2+ uptake measured in
platelets from different platelet donors at 3 different ATP
concentrations (100 µmol/L, 200 µmol/L, and 2
mmol/L). At low concentrations of ATP, when only part of the added
Ca2+ was taken into the stores (Figure 8A
and 8B
), NO also increased the percentage of Ca2+
uptake from 49±11 to 68±8 (n=7, P<0.01). Thus, NO was
able to increase the rate and quantity of Ca2+
uptake into the stores, but only when the uptake was submaximal under
our experimental conditions.
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| Discussion |
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Nonselective Cation Influx in Platelets Depends on the
Stores
Our data are consistent with a close correlation of cation
influx in human platelets with the filling state of the
stores.4 5 6 Thrombin causes a fast release of
Ca2+ from IP3-sensitive
Ca2+ stores in platelets, which is followed
by partial back-sequestration into the stores and
Ca2+ extrusion from cells via PMCA and
Na+/Ca2+
exchanger.33 Under our experimental conditions
Ca2+ and Mn2+ influx is
maximally activated during the first 30 s after thrombin
application and then gradually decreases. This decrease most probably
results from the time-dependent partial back-sequestration of
Ca2+ into the stores. However, we cannot rule out
the involvement of other possible reasons, including desensitization of
the thrombin receptor signaling cascade or inactivation of plasma
membrane cation channels.
When Ca2+ was released slowly with BHQ (as was
seen to occur in permeabilized platelets in Figure 7D
), the amplitude of Ca2+ influx as well
as the rate of Mn2+ influx increased gradually
with time, reaching a maximum after 5 minutes (Figure 2B
and 2D
). The absence of back-sequestration of Ca2+ in
the presence of BHQ might explain why the maximal amplitude of the
BHQ-induced Ca2+ rise was
2.5 times higher
than that induced by thrombin (Figure 2A
and 2B
). The rates of
Mn2+ influx in thrombin- and BHQ-treated
platelets were comparable (Figure 2C
and 2D
), suggesting
that SERCA-dependent Ca2+ back-sequestration into
the stores in the presence of thrombin, which is absent in BHQ-treated
cells, can effectively reduce Ca2+ influx. Thus,
the maximal Ca2+ and Mn2+
influx in platelets coincides with the maximal emptying of the
stores, consistent with a mechanism of capacitative cation
influx.
NO Inhibits Capacitative Cation Influx in Human Platelets, but
SERCA-Dependent Store Refilling Is Required
Our data indicate that SERCA-dependent refilling of the stores is
required for NO to inhibit Ca2+ and
Mn2+ influx. When
Ca2+/Mn2+ influx was
activated by thrombin, NO was very effective and blocked this
influx almost completely and independently of the time after thrombin
application (Figures 1
and 2
). In BHQ-treated
platelets, however, NO was able to partially inhibit
Ca2+ and Mn2+ influx and
the rise in Ca2+cyt only during
the first few minutes after BHQ application. During this initial phase,
presumably, SERCA is only partially inhibited and some
back-sequestration of Ca2+ into the stores can
still occur. After 5 to 10 minutes, when the process of SERCA
inhibition by BHQ is apparently complete and maximal cation influx has
developed (Figure 2
), the inhibitory effect of NO on
Ca2+cyt disappears. The absence
of the inhibitory effect of NO on maximum
Ca2+ and Mn2+ influx after
a 10-minute treatment with BHQ suggests that NO does not have a direct
effect on plasma membrane cation channels, which are responsible for
such influx.
The time-dependent loss of the effect of NO on cation influx demonstrated in the presence of the SERCA inhibitor could explain why some researchers18 34 failed to detect the inhibition of TG-induced cation influx in platelets by NO donors, while others17 reported such an inhibition. The variability in the effect of NO could be also related to the incomplete inhibition of all SERCA isoforms by TG under different experimental conditions or to the differences between BHQ- and TG-sensitive Ca2+ stores and their role in the regulation of cation channels.
NO Promotes SERCA-Dependent Back-Sequestration of Ca2+
Into the Stores
The absence of an effect of NO on capacitative cation influx when
SERCA is inhibited shows that NO does not inhibit the influx directly
and suggests the importance of functional SERCA for the NO-induced
inhibition of cation influx. To determine whether NO indeed can
accelerate the refilling of Ca2+ stores in a
SERCA-dependent manner, the following 2 approaches were used. In the
first approach, ionomycin was used at a high concentration to release
Ca2+ from all the stores to determine whether NO
can promote the refilling of the stores emptied by thrombin. In
thrombin-activated platelets, NO was shown to significantly
increase the total intracellular Ca2+ pool
released by ionomycin. The effect of NO was maximal if it was added
before initiation of Ca2+ release by thrombin,
apparently because it promotes back-sequestration of
Ca2+ released by IP3. When
NO was added later, most of the released Ca2+ was
already removed from the cytoplasm, which explains the insignificant
increase in the Ca2+ stores (Figure 4
).
Permeabilized platelets were used in the second
approach, which allows direct observations of the
Ca2+ movements in and out of intracellular
stores. Using this method, NO was found to accelerate uptake of
Ca2+ either after it was released from the stores
with IP3 or after exogenous
Ca2+ was added (Figure 8
). The effect of
NO disappeared in the presence of BHQ. The strong dependence on ATP
concentration of Ca2+ uptake in
permeabilized platelets (Figure 8
) points to
the involvement of an ATP-using process, which, most logically, is
SERCA. Importantly, the effect of NO strongly depends on the initial
rate of Ca2+ uptake (Figure 8
). At a
maximal rate of Ca2+ sequestration, the
possibility of a further increase of SERCA activity by NO is unlikely.
Under physiological conditions, one would expect
SERCA to work at a lower, submaximal rate that would allow its further
acceleration by NO. In permeabilized platelets, NO
had a stimulatory effect only when the rate of
Ca2+ uptake was experimentally decreased (by
decreasing the concentration of ATP) (Figure 8C
and 8E
). These
results provide a possible explanation of the fact that some
investigators did not observe an effect of NO on SERCA.35
Indeed, SERCA activity is usually measured under experimental
conditions providing its highest activity (at high
Ca2+ and/or ATP concentrations), which might
exclude its further acceleration by NO.
Role of IP3-Induced Ca2+ Release,
PMCA, Na+/Ca2+ Exchanger, and Mitochondria in
the Effect of NO on Ca2+cyt in Human
Platelets
NO has been shown to inhibit the transient
Ca2+ rise caused by agonists in a variety of
cells, including platelets,14 16 which theoretically
can be mediated through NO-induced inhibition of
IP3 production by phospholipase C
or suppression of IP3-induced
Ca2+ release, on one hand, and a rapid
acceleration of Ca2+ back-sequestration into the
stores, on the other hand.
Although we cannot completely exclude an effect of NO exerted by
changes in the production or action of
IP3, there are several reasons why
back-sequestration of Ca2+ into the stores by
SERCA appears to be the major physiological
mechanism for the NO-induced decrease in
Ca2+cyt in human platelets.
First, inhibition of SERCA with BHQ (which prevents
Ca2+ back-sequestration, but not
IP3-induced Ca2+ release)
completely abolished the effect of NO on the thrombin-induced transient
Ca2+ rise (Figure 5
). Second, even without
involvement of IP3 in
permeabilized platelets, NO significantly increased
uptake of externally added Ca2+, accelerating the
rate of uptake and lowering the free Ca2+ level
(Figure 8
). Third, the effect of NO depended on ATP
concentration (Figure 8
), pointing to the regulation of an
ATP-dependent process such as SERCA.
PMCA and Na+/Ca2+ exchanger
have been proposed to be targets for NO action in other cells (for
review, see Reference 3636 ). In human platelets, we found no evidence
for a significant role of these Ca2+-removal
mechanisms in the effects of NO. Indeed, when SERCA was inhibited by
BHQ, Ca2+ (released by thrombin) was successfully
removed from the cytoplasm (Figure 5
), pointing to the activity
of PMCA, Na+/Ca2+
exchanger, or both. However, NO did not affect
Ca2+ removal when SERCA was inhibited. Also,
there was no effect of NO on the peak Ca2+ rise
in BHQ-treated platelets, although such extrusion mechanisms as
PMCA and Na+/Ca2+ exchanger
are expected to work under these conditions.
By taking up Ca2+ during agonist-induced
activation, mitochondria could be involved in the regulation of
capacitative Ca2+ influx in different types of
cells.21 22 23 Our experiments with mitochondrial
inhibitors (Figure 6
) show that the effect of NO on
intracellular Ca2+ does not depend on oxidative
metabolism by, or Ca2+ uptake into,
mitochondria.
Thus, IP3-induced Ca2+ release, PMCA, Na+-Ca2+ exchanger, and mitochondria, although they are potential targets for NO, seem not to play an important role in the effects of NO on Ca2+cyt in human platelets.
Role of cGMP Production in the Effect of NO on
Ca2+ Influx in Human Platelets
It is well known that NO37 and NO
donors27 38 stimulate cGMP production in human
platelets leading to the activation of cGMP-dependent protein
kinase and inhibition of agonist-induced
Ca2+cyt rise and platelet
aggregation.37 39 In rat aortic smooth muscle cells, this
effect was partially attributed to the phosphorylation
of the SERCA-regulatory protein phospholamban and thus the increased
sensitivity of SERCA to Ca2+.40 It
is tempting to look for a similar explanation for the effect of NO in
platelets. In fact, a phospholamban-like 22-kDa protein,
thrombolamban, found in platelets,41 has been shown to
regulate the activity of Ca2+ uptake by the ER
vesicles. However, comparative analysis of phospholamban and
thrombolamban revealed differences in their structural and physical
properties, as well as in the mechanisms for activation of the
respective Ca2+ pumps.42 Moreover,
no phosphorylation of thrombolamban by sodium
nitroprusside or cGMP analogs was found in
platelets.39 43 Thus, it seems unlikely that
cGMP-dependent stimulation of platelet SERCA by NO is mediated by
thrombolamban.
Inhibition of guanylate cyclase by ODQ has been shown to
eliminate the cGMP rise caused by NO donors and to prevent their effect
on platelet aggregation.27 However, there are some
indications that cGMP might not account for all the effects of
authentic NO on Ca2+cyt. It was
shown recently that inhibition of cGMP production with ODQ
suppresses, but does not eliminate, the effects of authentic NO on
intracellular Ca2+ in smooth muscle
cells,44 as well as the effect of the NO donor
S-nitrosoglutathione in platelets.45
Similarly, we found that pretreatment of human platelets with
10 µmol/L ODQ for 1 hour only partially blocked the
inhibitory effect of NO on capacitative
Ca2+ influx (Figure 6
). This result points
to the possibility that along with a cGMP-dependent pathway there is
also another, cGMP-independent mechanism of NO effect on
Ca2+ influx in human platelets. Indeed,
direct NO-induced nitrosylation of critical thiols is known to be
responsible for cGMP-independent effects of NO on some other
proteins.46 47 48 Further studies of the effects of NO on
SERCA need to be done to fully understand this
physiologically important pathway for
regulation of capacitative cation influx and intracellular
Ca2+ in platelets and other nonexcitable
cells.
| Acknowledgments |
|---|
Received July 17, 1998; accepted November 19, 1998.
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