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MEMBRANE TRANSPORTERS, ION CHANNELS, AND PUMPS
Faculty of Life Sciences, The University of Manchester, Manchester, United Kingdom
Submitted 20 November 2006 ; accepted in final form 7 May 2007
| ABSTRACT |
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oxidant stress; pancreatitis; calcium pump
Although the pathophysiology of pancreatitis remains incompletely understood, increasing evidence points to a role of oxidative stress as an underlying mechanism. In several animal models of pancreatitis, there is clear evidence that antioxidants reduce the associated cell injury (12, 31, 39), which has also proved beneficial in the treatment of human chronic pancreatitis (46). What remains unclear is whether oxidative stress is the trigger or a downstream consequence of an inflammatory response, which promotes the release of further oxidants from activated neutrophils at the site of injury (22, 50). However, there is substantial evidence that acinar cells can be a source of oxidant generation (7, 17, 42). In addition, in some pancreatitis models, lipid peroxidation products were detected prior to any inflammatory changes, suggesting that oxidative stress is an early event, if not the trigger of the disease (32).
The aim of the present study was to characterize in detail the effects of increased oxidative stress, using hydrogen peroxide (H2O2), on [Ca2+]i homeostasis and CCK-evoked [Ca2+]i oscillations in acinar cells. The results show that low concentrations of H2O2 increased [Ca2+]i and profoundly altered the normal pattern of CCK-evoked [Ca2+]i oscillations. These changes were transformed into an irreversible sustained increase in [Ca2+]i, or Ca2+ overload, in an increasing number of cells as the H2O2 concentration was increased. This H2O2-evoked Ca2+ overload also corresponded to inactivation of the plasma membrane Ca2+ pump (PMCA), the last "gate keeper" in the control of normal [Ca2+]i homeostasis. This suggests that oxidant-induced inactivation of the PMCA may be an important early event underlying the pathology of pancreatitis.
| MATERIALS AND METHODS |
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Digital imaging of fura-2 fluorescence.
Cells were loaded with 4 µM fura-2 acetoxymethyl ester (fura-2 AM; TEF Labs/Stratech, Soham, UK) in HEPES-PSS for 30 min at room temperature. Dye-loaded cells were allowed to adhere to a glass coverslip that formed the base of a gravity-fed perfusion chamber, continually perfused with HEPES-PSS with automatic valves for rapid switching of solutions (Harvard Apparatus, Kent, UK). All fluorescence imaging experiments were performed using an inverted epifluorescence Nikon microscope with x40 oil immersion objective (numerical aperture 1.3), charge-coupled device (CCD) camera, and illumination device. Emitted fluorescence was separated from excitation light using a 400-nm diachronic mirror. Earlier experiments utilized a Nikon Diaphot microscope with a slow-scan CCD camera (Digital Pixel, Brighton, UK), xenon arc lamp (Nikon), and Lambda-10 filter wheel (Sutter Instruments, Novato, CA) controlled by Kinetic Imaging image acquisition and analysis software (KI, Nottingham, UK). Later experiments utilized a Nikon TE2000 microscope with a CoolSNAP HQ interline progressive-scan CCD camera (Roper Scientific Photometrics, Tucson, AZ), and Cairn monochromator illumination system (Cairn Research, Kent, UK) controlled by MetaFluor image acquisition and analysis software (Molecular Devices, Downington, CA). Background-subtracted 340-nm and 380-nm fluorescence images were captured with no binning at a rate of 1 Hz, and 340/380 ratiometric images were calculated offline. A x1 relay lens on the microscope side port leading to the camera was used to increase the field of view so that a typical field of view contained
20–35 cells. The fura-2 fluorescence was calibrated into "estimated" [Ca2+]i using the following equation: [Ca2+]i = Kd(R – Rmin)/(Rmax – R)(SF380/SB380) (18). Where Kd is the fura-2 dissociation constant (150 nM) (48), R is any given 340/380 ratio value, SF380/SB380 is the ratio of fluorescence measured for Ca2+-free and Ca2+-bound fura-2, and Rmin and Rmax are the minimum and maximum ratio values following in situ calibration experiments. This involved treating cells with 10 µM ionomycin, 0.5 µM carbonyl cyanide m-chlorophenylhydrazone (CCCP; to prevent mitochondrial Ca2+ uptake), and 30 µM cyclopiazonic acid [CPA; to prevent Ca2+ uptake into the endoplasmic reticulum (ER)] in Ca2+ free HEPES-PSS (with 1 mM EGTA) to obtain Rmin values and Ca2+-saturated media (2 mM Ca2+) to obtain Rmax values. Average values were obtained from periodic in situ calibration experiments throughout the study and for different microscopes and objective lenses. All experiments were carried out at room temperature (20–22°C).
Digital imaging of dichlorofluorescein fluorescence.
Cells were loaded with 10 µM dichlorodihydrofluorescein diacetate (H2DCF-DA) (Molecular Probes/Invitrogen, Paisley, UK) for 30 min at room temperature. Loaded cells exhibited minimal fluorescence until treated with H2O2, which oxidizes H2DCF to the fluorescent 2',7'-dichlorofluorescein (DCF). Images of DCF fluorescence were obtained on the same imaging system as fura-2 images, but they were obtained using a fluorescein filter set. Time courses of normalized DCF fluorescence (%
F/Fo, % change in fluorescence divided by the starting fluorescence) were then derived for each individual cell in the field with 4-s time resolution.
Simultaneous measurement of oxidative stress and cytosolic [Ca2+]i. For simultaneous DCF and fura-2 imaging, cells were loaded with 10 µM fura-2 AM for 20 min at room temperature, followed by dual loading with 10 µM fura-2 AM and 10 µM H2DCF-DA for 20 min at 37°C. These loading conditions were found empirically to be optimal for achieving a measurable fura-2 signal without compromising the DCF signal. Under these conditions, cells were more heavily loaded with fura-2 than cells in experiments measuring [Ca2+]i alone. However, there was no apparent difference in the pattern or frequency of CCK-evoked [Ca2+]i oscillations that would indicate excessive buffering.
For dual-dye imaging, 340 nm, 380 nm (for fura-2), and 490 nm (for DCF) excitation wavelengths were selected using either the filter wheel or monochromator. Emitted fluorescence was captured through the same FITC filter set used for recording DCF fluorescence alone, which captured
35–40% of the emitted fura-2 fluorescence. Ratiometric fura-2 [Ca2+]i images, and normalized DCF images, were calculated offline with 4-s time resolution and analyzed as described above.
Solutions. In all imaging experiments, cells were superfused with a HEPES-PSS. Solutions containing H2O2 were made up fresh each day and were periodically assayed using a fluorometric assay, which monitors the conversion of p-hydroxyphenylacetate to a stable colored product during the reduction of H2O2 by horseradish peroxidase (20). H2O2 was applied to the cells by perfusion of H2O2-containing HEPES-PSS. This ensured that the cells were always exposed to a fresh supply of H2O2 at the desired concentration, because H2O2 degradation by cellular enzymes can markedly alter H2O2 concentrations under static incubation conditions (49). For experiments with La3+ (1 mM) to block the PMCA, all SO42– and H2PO4– ions were replaced with Cl– to prevent precipitation of La3+ salts. Stock solutions (1 mM) of Ru360 (Calbiochem) were dissolved in deoxygenated water and used immediately before use.
Assessment of H2O2-evoked oxidation of CCK. Because some experiments involved simultaneous application of H2O2 and CCK to cells, it was necessary to consider the possibility that H2O2 might oxidize CCK rather than act directly on the acinar cell. To address this possibility, H2O2 (100 µM) was added to HEPES-PSS containing 20 pM CCK. After 5 min, catalase (50 U/ml) was added to remove the H2O2. Degradation of H2O2 was monitored by periodically assaying aliquots of the medium for H2O2 (as above). After all the H2O2 had been destroyed, the experimental medium was applied to acinar cells, where it proved equally as potent in eliciting [Ca2+]i oscillations as medium containing 20 pM CCK that had not been exposed to H2O2 (data not shown). This confirmed that H2O2 does not act by oxidizing CCK.
Data analysis and experimental design. Because of the nature of most experiments, an unpaired experimental design was utilized. Comparisons were made and statistical significance determined between groups of experiments (e.g., control vs. treatment) using, where appropriate, an unpaired Student's t-test or Mann-Whitney test. For any given parameter analyzed, an experimental average was determined from several cells in a particular experiment. These values were in turn averaged to give the true overall average expressed in the text as means ± SE.
| RESULTS |
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Effects of submillimolar H2O2 during CCK-evoked [Ca2+]i oscillations. We also examined the effects of low concentrations of H2O2 (50, 75, and 100 µM) during a train of CCK-evoked [Ca2+]i oscillations. Similarly, these effects were heterogeneous, and thus responses were categorized for analysis. In this case, the three main types of response observed were the following: a severely impaired response, whereby oscillations slowly diminished and fused into a sustained increase in baseline [Ca2+]i (group A, Fig. 3); a mildly impaired response, whereby oscillations slowed and diminished and baseline [Ca2+]i transiently increased (group B, Fig. 3); and finally, no observable change in either baseline [Ca2+]i or the oscillation pattern (group C, Fig. 3). Again, the effects of H2O2 appeared to be concentration dependent in terms of the number of cells exhibiting each response. Thus a large number of cells exhibited impaired [Ca2+]i oscillations (group A 57 ± 2% and group B 37 ± 2%; n = 8, 143 cells, Fig. 3) in response to the highest concentration of H2O2 (100 µM), whereas few cells were unaffected (group C, 6 ± 1%; n = 8, 143, Fig. 3). In contrast, when the concentration of H2O2 was reduced to 50 µM, the majority of cells were unaffected (78 ± 2%, n = 5, 152 cells). The intermediate concentration (75 µM) evoked more heterogeneous responses [29 ± 5% (A), 54 ± 3% (B), 18 ± 5% (C); n = 6, 133 cells, Fig. 3].
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Direct measurement of cellular oxidative stress with DCF fluorescence.
We next tested whether the observed heterogeneity to H2O2 (Figs. 2 and 3) was due to differences in cellular oxidative stress using the oxidizable fluorescein derivative, H2DCF (23, 42). Following optimization of loading conditions, it was found that cells loaded with H2DCF initially showed very weak fluorescence (Fig. 4Ai, fluorescent image at 0 min). Because oxidation of the dye is irreversible, normalization was achieved by expressing the data as
F/F0 (Fig. Aii, Bi, Bii, and C). On exposure to 3 mM H2O2, cellular fluorescence increased markedly to almost saturated levels (Fig. 4Ai, fluorescent image at 20 min), presumably reflecting intracellular oxidation of H2DCF to the fluorescent product, DCF [Fig. 4, A and B; (23, 42)]. Monitoring DCF fluorescence in individual cells revealed that the increase in DCF fluorescence was extremely heterogeneous (Fig. 4Aii). Although virtually all cells showed some increase in DCF fluorescence at this high H2O2 concentration, the rate of the increase varied considerably between different cells. It was also noticeable that, after
20 min of H2O2 exposure, cells often showed a large decrease in DCF fluorescence; sometimes they appeared as a single step (see open arrows in Fig. 4Aii) or as multiple steps. These decreases were not due to a decrease in oxidative stress because oxidation of the dye is irreversible, but rather they were due to cell lysis and thus loss of DCF from the cell. Inspection of phase-contrast images of the cells confirmed that at 40 min cells that had lost DCF fluorescence showed clear evidence of cell lysis (Fig. 4Ai, fluorescent image at 40 min and brightfield image after).
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Simultaneous measurement of oxidative stress and [Ca2+]i; H2O2-evoked oxidative stress correlates to the degree of impairment of CCK-evoked [Ca2+]i signaling. As indicated above, the changes in DCF fluorescence and [Ca2+]i evoked by H2O2 showed considerable cell-to-cell heterogeneity. It is tempting to speculate that this could have a common cause based on intercellular differences in antioxidant capacity, such that cells with low antioxidant capacity would exhibit a faster rise in DCF fluorescence and a more marked disturbance of [Ca2+]i signaling. This was tested by loading cells with both fura-2 and H2DCF to allow the simultaneous measurement of cellular oxidative stress and CCK-evoked [Ca2+]i oscillations in individual cells (Fig. 5). Similarly to the experiments shown in Fig. 3, these effects were categorized into three general responses (A to C, Fig. 5A): a severely impaired response, whereby oscillations fused into a sustained increase in baseline [Ca2+]i (group A, Fig. 5Ai); mildly impaired response, whereby the frequency or amplitude of oscillations decreased without any noticeable change in baseline [Ca2+]i (group B, Fig. 5Aii); and finally, no observable change in either baseline [Ca2+]i or the oscillation pattern (group C, Fig. 5iii).
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F/Fo) compared with both the mildly affected (8.9 ± 1%
F/Fo) and unaffected cells treated with H2O2 (4.3 ± 1.1%
F/Fo) in addition to untreated control cells (3.4 ± 1.2%
F/Fo). These data clearly demonstrate a correlation between the level of oxidative stress "seen" by the DCF and the degree of impairment of CCK-evoked [Ca2+]i signaling evoked by H2O2. Both the effects of H2O2 on CCK-evoked [Ca2+]i signaling and the rise in oxidative stress were completely abolished by DTT (Fig. 5Bii and 5C, column 5). For all the data in Figs. 2–5, the observed heterogeneity was also apparent within cells from the same experiment (see mean data) and sometimes from the same acinus in any given experiment. In addition the type of response observed did not seem to depend on the extent of cell isolation as it was also noticed that some single cells were relatively "protected" compared with cells that were part of a large acinus. However, these are qualitative observations, and it would be difficult to completely rule out the effect of cell isolation on the heterogeneity without comparing the responses with those in vivo, which is technically very demanding. Furthermore, any approach to prevent oxidative damage during the isolation procedure may artificially improve the cells' antioxidant capacity and therefore artificially eliminate any heterogeneity that may have existed in vivo.
H2O2 regulates PMCA activity.
We next attempted to identify the underlying mechanism responsible for the H2O2-evoked irreversible increase in [Ca2+]i (Ca2+ overload). Rather than identifying the source of the increase in [Ca2+]i, we reasoned that the mechanism of impaired [Ca2+]i removal may be more important in converting a "mildly" effected cell to a severely effected cell, thus facilitating irreversible Ca2+ overload. We therefore tested the effects of H2O2 on PMCA activity utilizing an in situ assay, similar to that used in previous studies in parotid acinar cells (6). This involved depleting ER Ca2+ stores by inhibition of SERCA with TBQ and CPA. This increases [Ca2+]i due to Ca2+ leak from the ER and activation of store-operated Ca2+ entry (SOCE) (36). Subsequent removal of [Ca2+]o, and thus the Ca2+ influx component, essentially isolates Ca2+ efflux due to PMCA activity (Fig. 6A). This was quantified by fitting the falling phase of the [Ca2+]i clearance to an exponential decay, which yielded an average time constant (
) of 90 ± 10 s (n = 4, 43 cells, Fig. 6A) Under these conditions, all other [Ca2+]i clearance pathways are either inhibited (SERCA) or are expected to contribute little to the [Ca2+]i clearance [Na+-Ca2+-exchanger (30) and mitochondria (10)]. To validate experimentally that the major [Ca2+]i clearance pathway under these conditions was PMCA activity, we used two basic experimental approaches. First, to test whether mitochondrial Ca2+ uptake contributed to the [Ca2+]i clearance, cells were preincubated with the specific mitochondrial Ca2+ uptake inhibitor, Ru360 (10 µM), for 30 min before starting the "[Ca2+]i clearance assay". This has been shown to markedly inhibit mitochondrial Ca2+ uptake in pancreatic (21) and parotid acinar cells (6). Although there appeared to be a slowing of the clearance rate in some cells, on average this did not reach statistical significance (
= 114 ± 27 s, n = 5, 57 cells; Fig. 6B), suggesting that mitochondrial Ca2+ uptake is not the major [Ca2+]i clearance pathway under the conditions of these experiments. Second, to further validate that the [Ca2+]i clearance is due to the PMCA, La3+ (1 mM) was used to inhibit the PMCA (3, 8). This was applied either before the addition of CPA/TBQ (Fig. 6C) or during the increasing phase of the CPA/TBQ-evoked Ca2+ response (Fig. 6D). At this concentration La3+ inhibits both Ca2+ influx and Ca2+ efflux, effectively "sealing" the cell so that Ca2+ remains trapped so that it can neither enter nor leave the cell. Therefore, in the continued presence of La3+, CPA/TBQ-evoked a substantial increase in [Ca2+]i that remained elevated despite the subsequent removal of external Ca2+, presumably due to complete inhibition of the PMCA (see Fig. 6C). However, removal of La2+ using EGTA, which binds La3+ with high affinity, slowly reversed the inhibition of the PMCA, which then started to rapidly clear Ca2+ from the cytosol (see Fig. 6A). Furthermore, on average CPA/TBQ evoked a much larger increase in [Ca2+]i in the presence of La3+ (407 ± 51 nM, n = 4, 54 cells; compared with control cells, 219 ± 34 nM, n = 4, 43 cells), suggesting that PMCA actively removes Ca2+ from the cytosol as Ca2+ continues to leak from the ER, thereby reducing the net magnitude of the CPA/TBQ-evoked [Ca2+]i response. Addition of La3+ during the rising phase of the CPA/TBQ-evoked [Ca2+]i response caused an initial decrease, probably due to the rapid inhibition of Ca2+ influx, followed by a further increase that then rapidly reached a steady state, presumably due to the gradual inhibition of the PMCA (see Fig. 6D). One possible explanation for these observations is that La2+ enters the cell and interferes with fura-2 fluorescence, because it is known to bind to fura-2 with pM affinity (25). This could occur either by leak of La3+ or by La3+ entry through SOCE channels. However, this is highly unlikely because addition of La3+ neither quenched nor saturated the fura-2 signal, which would be expected even if small amounts of La3+ entered the cell (25). Furthermore, La3+ is thought to inhibit SOCE channels by a similar mechanism to voltage-operated Ca2+ channels (VOCCs) by blocking the pore of the channel (33), and it has recently been shown that La3+ cannot enter chromaffin cells through VOCCs (25). Therefore, these data provide convincing evidence that the PMCA is the major [Ca2+]i clearance pathway under the conditions of the experiments shown in Fig. 6.
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, as shown previously (6) and in Fig. 6. However, if [Ca2+]i clearance slowed substantially, as was the case following treatment with 1 mM H2O2 (Fig. 7A), then the rate no longer accurately fitted a single exponential decay but rather approached a linear relationship. Therefore, [Ca2+]i clearance was also quantified by measuring the initial maximum rate over a 30-s window following the removal of [Ca2+]o (see crosshairs in Fig. 7A), expressed as change in [Ca2+]i per minute (nM/min).
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from 90 ± 10 to 60 ± 6 s (P < 0.047; see Fig. 7B), and 50 µM H2O2 decreased
to 45 ± 6 s (P = 0.013; see Fig. 6B). Another interesting observation from these experiments, which could explain such increases in rate, was that H2O2 (50 µM) also enhanced the CPA/TBQ-evoked increase in [Ca2+]i (475 ± 48 nM, compared with 219 ± 34 nM control; P < 0.05), suggesting that H2O2 may promote passive Ca2+ leak from the ER. Therefore, the increase in [Ca2+]i clearance following treatment with 10–50 µM H2O2 could be due to the simple fact that the initial [Ca2+]i from which clearance was measured (shown as the crosshairs in Fig. 7A) was higher, and therefore so was the maximum rate of clearance (see Fig. 7C). However, at these concentrations H2O2 elevated [Ca2+]i (either transiently or sustained) in a large proportion of cells (50 µM,
84%; 10 µM,
30%, Fig. 2), which is known to increase PMCA activity (13, 14) and thus "upregulate" PMCA activity for several minutes afterward (3, 9), such that during the subsequent clearance assay PMCA activity remains high.
The most important observation from these experiments was that there was a transition at or above 100 µM H2O2, whereby [Ca2+]i clearance, and thus PMCA activity, was dramatically reduced despite a further increase in preclearance start [Ca2+]i (see Fig. 7C). Higher concentrations of H2O2 reduced [Ca2+]i clearance from 140 ± 16 nM/min (control, n = 4, 43 cells) to 87 ± 16 nM/min (300 µM H2O2, n = 4, 46 cells, P = 0.057) and 42 ± 11 nM/min (1,000 µM, n = 4, 52 cells, P < 0.001; see Fig. 7C). Similar exponential decay data revealed that 300 µM H2O2 significantly increased
from 90 ± 10 s to 327 ± 67 s (P = 0.0012; see Fig. 6B), and the data with 1 mM H2O2 could not be fitted to a single exponential decay, suggesting almost complete inactivation of the PMCA. The effect of 100 µM H2O2 on PMCA activity (
= 112 ± 46, Fig. 7B; maximum rate = 239 ± 56 nM/min; n = 4, 42 cells) was not significantly different from the control using either analytic method. However, this effect was likely a mixture of responses from two subpopulations of cells, whereby H2O2 either increased or decreased PMCA activity. It is also worth noting that the progressive increase in preclearance start [Ca2+]i was due to a greater extent to an increase in resting [Ca2+]i (>100 µM), rather than an enhanced CPA/TBQ-evoked Ca2+ leak (10–50 µM). This suggests that the irreversible nature of the H2O2-evoked Ca2+ overload response was due to inhibition of the PMCA.
Although under control conditions the major [Ca2+]i clearance pathway appears to be due to the PMCA (Fig. 6), evidence from Fig. 7 suggests that H2O2 may promote a greater ER Ca2+ leak, which could influence the clearance rate. Therefore, to test the direct effect of H2O2 on PMCA activity, the following experimental approach was applied (see Fig. 8). First, cells were preincubated with 10 µM Ru360 (similarly to Fig. 6) to inhibit mitochondrial Ca2+ uptake and subsequent Ca2+ release. Cells were then treated with CPA/TBQ in the absence of external Ca2+ to deplete ER Ca2+ (similarly to Fig. 1B), and following the recovery of [Ca2+]i, H2O2 was applied before external Ca2+ was added back which increased [Ca2+]i due to SOCE (Fig. 8). [Ca2+]i clearance (and thus PMCA activity) was then measured following a further removal of external Ca2+. The direct effects of 50 µM and 1 mM H2O2 was assessed because these concentrations caused the maximum effect on [Ca2+]i clearance in Fig. 7. Under these conditions 50 µM H2O2 had no direct effect on [Ca2+]i clearance (rate = 90 ± 16 nM/min,
= 49 ± 5 s; n = 5, 62 cells) compared with control cells (rate = 86 ± 5 nM/min;
= 41 ± 4, n = 6, 99 cells). This suggests that the increased [Ca2+]i clearance following treatment with 50 µM H2O2 (observed in Fig. 7) was Ca2+-dependent due to enhanced Ca2+ leak from the ER. However, 1 mM H2O2 significantly inhibited [Ca2+]i clearance (rate = 8 ± 3 nM/min; n = 4, 47 cells), consistent with experiments in Fig. 7 and the conclusion that inactivation of the PMCA is responsible for the H2O2-evoked irreversible Ca2+ overload.
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| DISCUSSION |
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Ca2+ overload is a common pathological precursor that mediates a variety of disease states, such as excitotoxicity during neurodegeneration (1). A common strategy for understanding this Ca2+ overload, either during excitotoxicity or during pancreatitis, has been to identify the sources of the [Ca2+]i increase, including most notably, mitochondria (15, 34) and Ca2+ entry pathways (1, 37). However, the irreversible nature of this Ca2+ overload suggests that perhaps a critical mechanism underlying this response is impairment of [Ca2+]i clearance pathways. In the present study, we have demonstrated that a critical concentration of H2O2 (>100 µM) dramatically and irreversibly inhibits or inactivates Ca2+ efflux. Interestingly, this corresponds to the H2O2 concentration that produced an irreversible Ca2+ overload in the vast majority of cells.
Oxidant-mediated regulation of PMCA has been directly demonstrated in neuronal and liver membranes (54) and has been suggested to occur in pancreatic acinar cells (34). The mechanism could be due to direct redox modulation of critical thiol groups within the PMCA or within calmodulin (CaM) (54) both of which could inhibit Ca2+/CaM-dependent activation of the PMCA (13). Another possibility is that the H2O2-evoked increase in [Ca2+]i activates Ca2+-dependent proteases, such as caspases or calpain, which are known to cleave and thus inactivate the PMCA (40). A similar mechanism has been described in neurons, whereby caspase cleavage of the Na+/Ca2+ exchanger, was shown to mediate the Ca2+ overload during the excitotoxicity associated with brain ischemia (2). Moreover, and of direct relevance to the present study, two groups have demonstrated that Ca2+-dependent activation of calpain leads to activation of the cytokine transcription factor, NF-KB, and pancreatic acinar cell injury (47, 51). In addition, cell injury associated with cerulean-induced pancreatitis was markedly ameliorated by calpain inhibitors (47, 52). Finally, there is now evidence that H2O2 can directly activate calpain, and that this leads to similar cell injury to that observed during pancreatitis (51). However, the time frame over which calpain became significantly activated (60-min exposure to 0.5 mM H2O2) in these experiments (51) occurred much later than when we observed PMCA inactivation (10-min exposure to 1 mM H2O2).
In addition, low concentrations of H2O2 (10–50 µM) transiently increased baseline [Ca2+]i in a large proportion of cells, and it is also worth noting that pretreatment of similar concentrations significantly increased PMCA activity in a Ca2+-dependent manner due to enhanced CPA/TBQ-evoked Ca2+ leak (see Fig. 7). Such Ca2+- and time-dependent modulation of the PMCA has been observed previously in other cells (3) and is thought to be due to increased CaM binding (13). This Ca2+-dependent modulation of the PMCA makes physiological sense; low-level oxidants increase PMCA activity in an attempt to restore low resting [Ca2+]i in the face of other impaired Ca2+ transport pathways, thereby preventing cell injury. However, as oxidative stress increases further, the PMCA becomes irreversibly inactivated, leaving the cell unable to restore resting [Ca2+]i and thereby leading to "Ca2+ overload" and thus substantial cell injury.
It is not surprising that millimolar concentrations of H2O2 produced such pathologically clear-cut responses. However, the striking observation was that lower concentrations of H2O2 (10–100 µM) produced markedly heterogeneous responses such that there was a population shift in favor of the most severe [Ca2+]i response with increasing concentrations of H2O2. Furthermore, the degree of impairment of [Ca2+]i signaling in any given cell was directly proportional to the increase in cellular oxidative stress, suggesting that the heterogeneity was due to differences in cellular antioxidant capacity. This suggests that the concentration of H2O2 that produces any given response is less important than the proportion of cells that exhibit that response. This has important pathological implications, because only a fraction of cells with low antioxidant capacity may be sufficient to cause significant tissue damage within the whole organ in the face of an oxidant insult. This is because these highly sensitive cells would likely undergo an irreversible Ca2+ overload in response to low-level oxidant stress, causing cell lysis and necrotic cell death. This may cause inflammatory cytokine release and infiltration of activated neutrophils that further release oxidants (22, 50), culminating in a spiral of self-perpetuating cytotoxic tissue damage and ultimately organ failure, the hallmarks of severe acute pancreatitis (38). It is tempting to hypothesize that low level oxidants released from within acinar cells (7, 17, 42) could conceivably initiate pancreatitis if the antioxidant capacity of those cells or neighboring cells is low. It is also of interest that a lowered pancreatic antioxidant capacity has been suggested to be a predisposing factor for chronic pancreatitis (4).
The major source of the oxidant-evoked [Ca2+]i increase in the present study is likely to be due to Ca2+ leak from agonist-sensitive Ca2+ stores, such as the ER. The is because pretreatment with H2O2 enhanced the CPA/TBQ-evoked [Ca2+]i increase and the direct H2O2-evoked increase in [Ca2+]i was completely abolished under conditions where ER Ca2+ was depleted and Ca2+ influx was prevented. However, under similar conditions if cells were first stimulated with CCK, which evokes oscillatory [Ca2+]i signals and thus substantial mitochondrial Ca2+ uptake (17), H2O2 caused mitochondrial Ca2+ release that was abolished by the mitochondrial uncoupler, CCCP. This is consistent with other studies that showed oxidant-evoked mitochondrial depolarization and release of mitochondrial Ca2+ via the opening of the permeability transition pore (15, 16, 34). However, in naive unstimulated resting cells, where mitochondrial Ca2+ uptake does not occur, mitochondria are unlikely to be a major source of the oxidant-evoked [Ca2+]i increase.
The exact nature of the H2O2-evoked ER Ca2+ release in rat pancreatic acinar cells is unclear from the present study. We observed [Ca2+]i oscillations in response to another oxidant, thimerosal (Fig. 2, inset), in rat pancreatic acinar cells and also in response to low concentrations of H2O2 in mouse pancreatic acinar cells (3–30 µM, data not shown), consistent with other studies (16, 44). However, we never observed [Ca2+]i oscillations in response to H2O2 at any of the concentrations tested (10 µM-1 mM) in rat pancreatic acinar cells, suggesting that the nature of the response to oxidants depends on type of oxidant and the species in which it is tested. In fact, the time course of the H2O2-evoked increase in [Ca2+]i in rat pancreatic acinar cells was more reminiscent of a slow leak of Ca2+ from the ER, caused either by inhibition of SERCA (26, 29), or a direct effect on the passive leak pathway, due most likely to the translocon complex (27). However, further work is required to verify this mechanism and is beyond the scope of this study.
The H2O2-evoked increase in [Ca2+]i was also dependent on Ca2+ influx, since the response was markedly attenuated by removal of external [Ca2+]. However, this is likely due to depletion of ER Ca2+ and an indirect activation of SOCE. A direct effect on SOCE channels is unlikely since addition of H2O2 failed to affect the rate of [Ca2+]i increase when external Ca2+ was added back to ER-depleted cells, an assay routinely used as an indirect measure of SOCE (36). Notwithstanding this, a direct effect of H2O2 on noncapacitative Ca2+ influx pathways cannot be completely ruled out.
An alternative possibility is an effect of cellular ATP depletion, which is classically viewed as one of the earliest changes in oxidative injury (41). Depletion of 90% of cellular ATP has been reported to increase basal [Ca2+]i and inhibit [Ca2+]i oscillations in pancreatic acinar cells (45). However, studies on cultured intestinal epithelial cells suggest that even high millimolar concentrations of H2O2 do not deplete cellular ATP significantly over the first few minutes of exposure (49). In addition, 31P NMR measurements have shown that intracellular ATP levels in rat pancreas change by no more than 20% even during maximal agonist stimulation, when metabolic energy demand is presumably high (28). Given that H2O2 increased [Ca2+]i almost immediately, albeit relatively slowly, it seems unlikely that global ATP depletion is the primary mechanism for the increase in [Ca2+]i or inhibition of the PMCA, although local changes in ATP cannot be ruled out.
Low concentrations of H2O2 (10–100 µM) also profoundly altered CCK-evoked [Ca2+]i oscillations. As indicated above, ER store depletion and inactivation of the PMCA are also likely explanations for the most severe cases of Ca2+ overload under these conditions. In addition, under the conditions of these experiments, impaired mitochondrial function likely contributes to the impaired CCK-evoked [Ca2+]i oscillations consistent with other studies (16). Furthermore, the oxidant, tert-butylhydroperoxide, was also shown to impair carbachol-evoked [Ca2+]i oscillations, which fused into a sustained response in pancreatic acinar cells (43). These observations also corresponded to a marked impairment of agonist-evoked fluid and amylase secretion from the perfused pancreas (43).
Another interesting observation from the present study was that there were striking differences in the proportion of cells showing moderate to severe damage when H2O2 was applied during CCK-evoked [Ca2+]i oscillations compared with when H2O2 was added to resting cells. In particular, 50 µM H2O2 produced a Ca2+ overload response in approximately half of resting cells compared with none of the stimulated cells. These observations may be important pathologically, because they suggest that cells are more protected from the effects of H2O2 when stimulated with CCK. To our knowledge, this is a novel finding that suggests either that CCK couples to or enhances an antioxidant pathway within the cells, or that some aspect of the Ca2+ signaling machinery confers use-dependent protection from oxidant attack. However, further work is required to fully elucidate the mechanism, which is clearly beyond the scope of this study.
In summary, the present study shows that lower concentrations of H2O2 transiently increased [Ca2+]i due in the most part to depletion of ER [Ca2+] and activation of Ca2+ influx (SOCE). In addition, H2O2 also profoundly altered the normal pattern of CCK-evoked [Ca2+]i oscillations, reducing the amplitude and frequency of oscillations that are sometimes superimposed over a rising baseline. Disruption of mitochondrial Ca2+ handling is also likely to contribute to these responses. Similarly, the enhanced ER Ca2+ leak evoked by pretreatment with these low concentrations of H2O2 also indirectly increased the activity of the PMCA, which is the last gatekeeper for the control of low resting [Ca2+]i. During oxidant attack, we suggest that the PMCA works hard to maintain [Ca2+]i homeostasis in the face of disregulated Ca2+ transport pathways. However, at a critical H2O2 concentration (depending on the antioxidant capacity of the cell), PMCA activity rapidly and irreversibly declined. This likely converts the cell from a mildly effected cell, that can maintain [Ca2+]i homeostasis to some degree, to a severely effected cell, where [Ca2+]i is uncontrolled and thus irreversibly elevated. This mechanism may therefore be important in facilitating the Ca2+ overload, thereby resulting in a spiral of self-perpetuating cellular injury.
Finally, the effects of lower concentrations of H2O2 gave rise to a large degree of cellular heterogeneity that was likely due to differences in cellular antioxidant capacity. This further illustrates that the transition from a "mildly" effected to a "severely" effected cell potentially need only occur in a fraction of cells with low antioxidant capacity to trigger a cytotoxic inflammatory response. Inactivation of the PMCA may be a critical mechanism underlying these events and may well be important during the pathology of pancreatitis.
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