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* Advanced Research Institute for Science and Engineering, Waseda University, 3-4-1 Okubo Shinjuku-ku, Tokyo 169-8555, Japan;
Department of Molecular Behavioral Biology, Osaka Bioscience Institute, 6-2-4 Furuedai, Suita, Osaka 565-0874, Japan;
Department of Molecular Neurobiology, School of Human Sciences, Waseda University, 2-579-15 Mikajima, Tokorozawa, Saitama 359-1192, Japan;
School of Science and Engineering, Waseda University, 3-4-1 Okubo Shinjuku-ku, Tokyo 169-8555, Japan; ¶ Center for Research on Occupational and Environmental Toxicology, Oregon Health and Science University, Portland, Oregon 97201-3098, USA; and || Mitsubishi Kagaku Institute of Life Sciences, and Core Research for Evolutional Science and Technology (CREST), Japan Science and Technology Agency (JST), 11 Minamiooya, Machida-shi, Tokyo 194-8511, Japan
Correspondence: Address reprint requests to Tohru Yoshioka, PhD, Tel.: +81-3-5286-2761; Fax: +81-3-3205-6419; E-mail: yoshioka{at}human.waseda.ac.jp.
| ABSTRACT |
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| INTRODUCTION |
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The effects of D2O on cellular secretion have been extensively studied in various cell types without any consensus on the underlying mechanisms. For example, D2O significantly reduces insulin release from pancreatic islets (Malaisse-Lagae et al., 1971
; Freinkel et al., 1976
; Montague et al., 1976
; Hill and Rhoten, 1983
), amylase release from pancreatic fragments (Calderon et al., 1980
), and gastrin release from antral mucosal fragments (Harty et al., 1983
). D2O has been shown to modulate the amount and arrangement of microtubules (Malaisse-Lagae et al., 1971
; Houston et al., 1974
; Itoh and Sato, 1984
) and secretory granules are transported from the basal to the apical cytoplasm via microtubules (Lacy et al., 1968
; Malaisse et al., 1975
; Sasaki and Tashiro, 1976
), thus the D2O-induced decrease in secretion has been ascribed to the stabilization of microtubules (Malaisse-Lagae et al., 1971
; Montague et al., 1976
; Hill and Rhoten, 1983
). The mechanism underlying the effect of D2O may not be this simplistic, however, because it has been shown that D2O increases serotonin release from blood platelets (Bennett et al., 1979
) and spleen cells (Sulowska and Wyczolkowska, 1991
) and histamine release from mast cells (Fewtrell and Metzger, 1980
; Maeyama et al., 1986
) and basophilic leukemia cells (Urata et al., 1989
).
Theoretically, D2O has at least two independent physiological effects: i), an isotope exchange (hydrogen to deuterium) effect on functional proteins, and ii), a solvent isotope effect, meaning that the mobility of monovalent cations is reduced by
20%, whereas the dielectric constant is not changed in D2O buffer (Bass and Moore, 1973
). The computer simulation studies on the isotope exchange effect using the density functional theory demonstrated that with H2O to D2O exchange, the state of functional proteins changes quickly, but with D2O to H2O exchange, the state of proteins recovers very slowly, due to the stability of deuterated amino acids (Table 1). On the other hand, reported electrophysiological properties (membrane potential and channel conductances), which are under the influence of a solvent isotope effect, change reversibly and rapidly with the change from H2O to D2O and back again (Schauf and Bullock, 1979
; Schauf and Chuman, 1986
; Andjus et al., 1994
). Therefore, isotope exchange effects and solvent isotope effects are possibly distinguishable as temporal pattern of D2O actions. However, D2O actions on physiological processes such as exocytosis have not been analyzed from this biophysical point of view.
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With special cautions for the temporal coordinates of D2O actions, we found biphasic and bidirectional effects of D2O on high-K+-induced ß-endorphin secretions in AtT20 cells. The initial increase of secretion corresponds to the immediate redistribution of actin filaments, whereas the delayed inhibition of secretion corresponds to dysfunction of VSCCs upon D2O washout.
| MATERIALS AND METHODS |
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5 x 104 cells. The culture medium was exchanged every other day and on the day before the experiments.
Immunofluorescent confocal imaging
To observe the effects of D2O on the cytoskeleton, AtT20 cells were incubated in H2O-based buffered salt solution (BSS) consisting of (mM) 128 NaCl, 5 KCl, 2.7 CaCl2, 1.2 MgCl2, 1 Na2HPO4, 10 glucose, and 10 HEPES/NaOH (pH 7.3) for 20 min, and the H2O BSS was replaced with 90% D2O BSS for 5 or 15 min. AtT20 cells were then fixed in 4% phosphate-buffered paraformaldehyde for 15 min and washed three times with phosphate-buffered saline (PBS) consisting of (mM) 137 NaCl, 2.7 KCl, 1.5 KH2PO4, and 8.1 Na2HPO4 (pH 7.4). The fixed sample was then dipped in acetone for 3 min and dried to facilitate staining of F-actin with rhodamine phalloidin (Molecular Probes, Eugene, OR). The dried sample was incubated for 2 h at room temperature (2426°C) with monoclonal antibodies against ß-tubulin (1:100, ICN Biomedicals, Aurora, OH) and neurofilament-M (1:100, Chemicon International, Temecula, CA) dissolved in PBS supplemented with 1% bovine serum albumin (BSA), 0.1% Triton-X, and 0.05% sodium azide. The sample was rinsed three times with PBS and incubated for 1 h at room temperature with fluorescein isothiocyanate-conjugated goat anti-mouse IgG (ICN Biomedicals, 1:200) and rhodamine phalloidin (1:200) dissolved in the bovine serum albumin-supplemented PBS. After washing out the secondary antibody with PBS, the sample was mounted with glycerol. A confocal imaging system (µ-Radiance, Bio-Rad, Hercules, CA) attached to a fluorescence microscope (AxioPlan2, Carl Zeiss, Oberkochen, Germany) was used with an argon/krypton laser and a 40x objective lens (Plan-Neofluar 40x/0.75, Carl Zeiss). The digital image was processed using Photoshop (Adobe) software. All staining experiments were repeated at least three times.
Ca2+ imaging
The culture medium was gently rinsed from dishes using BSS. The cells were then incubated in BSS supplemented with 5 µM fura-2 AM (Molecular Probes) for 30 min in a CO2 incubator. Before photometry, the cells were rinsed again with BSS, incubated at 37°C for 15 min, and then continuously perfused with BSS at 30°C at a flow rate of 3 ml/min. Fluorescence images were produced by alternating 340- and 380-nm ultraviolet pulses (143-ms duration) and the resulting pairs of images were projected onto a cooled CCD camera (C4880, Hamamatsu Photonics, Hamamatsu, Japan) at 36-s intervals. A cocktail of 10 µM nifedipine (Sigma, St. Louis, MO) and 100 nM
-conotoxin MVIIC (Alomone Labs, Jerusalem, Israel) was used to block VSCCs, because these VSCC blockers at these concentrations inhibit most VSCC subtypes in AtT20 cells (Loechner et al., 1996
). Tetrodotoxin (TTX; Alomone Labs) was applied at a concentration of 1 µM to estimate possible involvement of Na+ channels in the Ca2+ oscillations. The frequency of the Ca2+ oscillations was estimated by the number of peaks within 180-s blocks recorded during the control and TTX treatment periods. All drugs were bath-applied with the perfusate. Further details of the Ca2+ imaging technique have been described previously (Ikeda et al., 2001
; Nelson et al., 2001
).
Electrophysiology
Recordings were performed at 34 days after plating by placing a cover slip fragment into a recording chamber located on the stage of an upright microscope equipped with phase-contrast optics. The chamber was perfused at
1 ml/min with BSS. Microelectrodes, pulled in two stages (Narishige puller, Narishige, Tokyo, Japan) from thin-walled borosilicate glass (World Precision Instruments, Sarasota, FL), had resistances of 57 M
when filled with a (intracellular) solution, at pH 7.3 and 310 mOsm, consisting of (mM) Cs methanesulfonate 87, CsCl 20, CsOH 25, CaCl2 1, HEPES 10, EGTA 10, ATP 3, and GTP 0.3. For the recording of resting membrane potential of AtT20 cells, the current clamp mode of the whole-cell patch clamp method was used with EPC-8 patch amplifier (HEKA, Lambrecht/Pfalz, Germany). Membrane potential responses were filtered at 3 kHz and acquired using pCLAMP7 software (Axon Instruments, Foster City, CA). For the recording of K+ currents, the cells were held at -60 mV using the whole-cell configuration of the patch-clamp technique and the membrane voltage stepped to +50 mV once every 30 s. To activate voltage-gated Na+ currents the cells were voltage clamped at -83 mV and depolarizing steps (10-mV steps, 30 ms in duration) applied once each 4 s. For the recordings of Ba2+ currents, Ca2+-free BSS containing 10 mM BaCl2 and 0.5 µM TTX was used as the external solution and 3 µM QX-314 was added to the internal solution. For the recordings of Ca2+ currents, internal solutions consisting of (mM) CsCl 120, MgCl2 3, HEPES 10, EGTA 10, ATP 3, GTP 0.4 and creatine phosphate 14, and external solutions consisting of (mM) TEA-Cl 142, CaCl2 2.5, MgCl2 1, HEPES 15, and glucose 9.9 were used. To observe intracellular hydrogen/deuterium exchange effects, Ca2+ current recordings were initiated with the internal solution of 90% D2O, and thereafter the external solution was replaced to 90% D2O-BSS by the bath perfusion. Voltage-gated Ca2+ currents were activated from a holding potential of -80 mV with depolarizing pulses (10-mV steps, 50 ms) applied once each 8 s. These currents were recorded using an Axopatch 1C (Axon Instruments), filtered at 2 kHz (-3 dB) with an eight-pole Bessel filter and digitized at 10 kHz on-line using an ITC16 A/D interface (Instrutech, Port Washington, NY) and Pulse software (HEKA). The cell capacitance and series resistance (1530 M
, 80%) were compensated. All records were corrected for a liquid junction potential of -13 mV. Further details of the recording methods have been described previously (Suzuki et al., 1997a
,b
; Hirono et al., 1999
).
Radioimmunoassay for ß-endorphin release
AtT20 cells were seeded onto a 100-mm dish (1 x 106 cells/dish) and cultured at 37°C for 24 h in the growth medium. After washing out the growth medium with BSS, the cells were incubated in 4 ml H2O BSS, D2O BSS, 30 mM K+ H2O BSS, and/or 30 mM K+ D2O BSS at room temperature. ß-Endorphin concentrations in H2O BSS (3 min) or in 90% D2O BSS (3 min) were assayed as undepolarized controls. Three groups were depolarized with high-K+ concentration and treated with D2O. The first group (H2O) was stimulated with 30 mM K+ H2O BSS (3 min) without any D2O treatment. The second group (D2O) was stimulated with 30 mM K+/90% D2O BSS for 3 min. The third group (D2O wash out) was treated with 90% D2O BSS for 3 min and then depolarized with 30 mM K+ H2O BSS for 3 min during D2O wash out.
Radioimmunoassays of ß-endorphin in these samples were then performed by researchers fully blind to the sample conditions. The antiserum was prepared in a rabbit by several biweekly injections of ß-endorphin emulsified in complete Freund's adjuvant. The ß-endorphin was labeled using the chloramines-T method and assayed as described previously (Furui et al., 1984
). Briefly, the incubation buffer was mixed with 100 mg/ml silicic acid and vortexed vigorously for 5 min. After centrifugation at 3000 rpm at 4°C for 5 min, the pellet was rinsed twice with an equal volume of ice-cold distilled water. The pellet was then extracted with 80% acetone in 0.1 N HCl via vigorous mixing for 5 min and centrifuged at 3000 rpm for 5 min. The supernatant was decanted and evaporated under a flow of nitrogen. The extract was dissolved in 0.2 ml of assay standard buffer (0.1 M phosphate buffer, pH 7.5, containing 0.5% bovine serum albumin and 500 U/ml aprotinin). Standard and samples were each brought to a total volume of 0.25 ml with the addition of standard buffer to achieve the appropriate dilution of antiserum. After incubation for 72 h at 4°C, 125I-labeled ß-endorphin was added and the mixture was incubated for 24 h at 4°C. The 125I-ß-endorphin was precipitated by the addition of 0.1 ml 0.1% rabbit gamma globulin, 0.5 ml 25% polyethylene glycol, and 0.1 ml standard buffer, and then centrifuged at 3000 rpm for 5 min. The radioactivity of the pellets was used as a quantitative estimation of the net ß-endorphin concentrations.
The concentration of ß-endorphin measured from each sample (4 ml) after 1416 h was used to normalize experimental variations among flasks. One measurement from the H2O group (n = 6) and one from the D2O-pretreated group (n = 6) were rejected according to Smirnoff's normality test (5% confidence). Duncan's multiple range test after a one way analysis of variance (ANOVA) was used for the comparison among the groups. A Student's t-test was used for statistical comparison unless otherwise noted.
Quantum chemical method
Ab initio calculations were carried out based on the Kohn-Sham density function theory (Kohn and Sham, 1965
) using the Becke3-Lee-Yang-Parr (B3LYP) function (Becke, 1993
; Lee et al., 1988
) and the 6-31G(d,p) basis set. Among available functions, the B3LYP function has been widely used in density-function-theory-based calculations and proven to yield very good descriptions of the vibration frequencies of small organic molecules. Harmonic vibration frequencies were calculated via analytic second derivatives of the energy with respect to the nuclear coordinates. We calculated the zero-point vibration energy of specific amino acids and water molecules, and evaluated the changes in the zero-point vibration energy that accompany the substitution of hydrogen atoms with deuterium atoms. No scaling factor for the zero-point vibration energy was used. All calculations were carried out using Gaussian 98 software (Frisch et al., 1998
) on an AlphaSationXP1000 (Compaq Computer K.K., Tokyo, Japan) workstation.
| RESULTS |
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2 min in all cells examined (n = 4; Fig. 2 A). The mean resting membrane potential during the firing burst (-45.3 ± 1.2 mV, n = 4) was slightly hyperpolarized (-54.4 ± 3.4 mV, n = 4) immediately after D2O application.
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Effects of D2O on spontaneous Ca2+ oscillations
Spontaneous Ca2+ oscillations were observed in approximately half the cells examined (389 of 743 cells, number of experiments = 16). The oscillation frequency varied widely (0.10.01 Hz). Cells were treated with 90% D2O BSS for 90 s, and this resulted in a gradual inhibition of spontaneous Ca2+ oscillations for 46 min (Fig. 3 A). Longer treatment with 50% D2O BSS (3 min; Fig. 3 A) or with lower concentrations of D2O had little effect on the Ca2+ oscillations. Treatment with TTX (1 µM, for 10 min) had little effect on Ca2+ oscillations (n = 3), indicating that the Ca2+ oscillations were not directly driven by the action potentials.
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Effects of D2O on high-K+-induced membrane depolarization and Ca2+ influx
AtT20 cells that exhibited no spontaneous action potentials or infrequent Ca2+ oscillations were used in the following experiments. Exposure to 30 mM K+ depolarized the membrane potential from -69.0 ± 3.2 mV to -32.0 ± 3.6 mV (n = 4, Fig. 4, A and B). The resting membrane potential slightly depolarized (+4.4 ± 0.6 mV, n = 4) but high-K+-induced membrane depolarization was not significantly changed with treatment with 90% D2O BSS (n = 3, Fig. 4 A). In addition, it was observed that VSCCs were not a primary determinant of the resting membrane potential, because blocking VSCCs with 10 µM nifedipine and 100 nM
-conotoxin MVIIC failed to reduce the membrane potential (n = 3, Fig. 4 B). The K+ currents recorded at holding membrane potential of +50 mV (mean amplitude = 703 ± 42 pA) was reduced immediately by 90% D2O BSS perfusion (-37.5 ± 6.7%, p < 0.01 by a paired Student's t-test, n = 4) and recovered to the control levels 89 min after D2O washout (Fig. 4 C).
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-conotoxin MVIIC) significantly reduced the amplitude of the high-K+-induced Ca2+ response (-89.5 ± 9.3%, number of experiments = 4, p < 0.01 in comparison with first Ca2+ response by a paired Student's t-test, Fig. 5 B). Treatment with 10% D2O BSS (unpublished data) or 50% D2O BSS (Fig. 5 C) for 3 min had no effect on the high-K+-induced Ca2+ influx. Interestingly, high-K+-induced Ca2+ influx during treatment with 90% D2O BSS was not changed, whereas the first few high-K+-induced Ca2+ responses during D2O washout were significantly inhibited (-99.8 ± 0.2%, number of experiments = 4, p < 0.01 in comparison with first Ca2+ response by a paired Student's t-test, Fig. 5 D). This inhibition of high-K+-induced Ca2+ influx was primarily dependent on the time elapsed after D2O treatment. A 1-min treatment with 90% D2O BSS was sufficient to inhibit high-K+-induced Ca2+ responses during D2O washout (
9-min period; Fig. 5 E), whereas longer treatment (up to 17 min) with 90% D2O BSS did not significantly affect high-K+-induced Ca2+ influx induced during the treatment, but did lengthen the time course of high-K+-induced Ca2+ influx (Fig. 5 F).
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Effects of D2O on ß-endorphin release
Treatment with 90% D2O BSS increased the release of ß-endorphin slightly (126.6 ± 20.6% of H2O control), but not to a statistically significant degree (p = 0.11; Fig. 7). Exposure to 30 mM K+ resulted in a significantly greater release of ß-endorphin compared with baseline levels both in H2O BSS (138.0 ± 8.6% of H2O control, n = 5, p < 0.05) and 90% D2O BSS (163.0 ± 24.3% of D2O control, n = 6, p < 0.05). The high-K+-induced ß-endorphin release was inhibited during washout of 90% D2O BSS (115.6 ± 9.2% of H2O control, n = 5, p > 0.05).
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ZPVE) for hydrophilic amino acids (Table 1). Within the hydrophilic amino acids, acidic amino acids were not analyzed in this simulation because they have only tight CH bounds at their side chains. Here we assume simple exchange reactions:
(A·A)OD + DOH (for Ser, Thr, and Tyr)
(A·A)ND + DOH (for Asn, Gln, Lys, Arg, and His).
These data show that a single deuterium substitution lowered the zero-point vibrational energy by 2.10 ± 0.02 kcal/mol and a dual deuterium substitution doubled the
ZPVE for several amino acids examined. Compared to a bond to hydrogen, a deuterium-containing bond has lower zero point energy. The activation energy is greater and the rate of the reaction is correspondingly less for the deuterated compounds. Within the Born-Oppenheimer approximation, deuterated and nondeuterated molecules are electronically identical, thus isotope effects arise primarily from the
ZPVE. These data indicate that for hydrophilic amino acids examined, the isotopic substitution of hydrogen by deuterium may be preferred over that of deuterium by hydrogen, which may result in slower deuterium to hydrogen exchange in these amino acids.
| DISCUSSION |
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Cellular responses under D2O exposure
Although classical interpretations of D2O-induced inhibition of cellular secretion have been based on D2O-mediated stabilization of microtubules (Malaisse-Lagae et al., 1971
; Montague et al., 1976
; Hill and Rhoten, 1983
), the effects of D2O on the cytoskeleton appear to be even more prevalent and varied. Zimmermann et al. (1988)
reported that D2O induces the redistribution of filamentous actin and a change in morphology of human neutrophil granulocytes. More recently, Omori et al. (1997)
examined the effects of D2O on actin filaments using fluorescent staining of BALB 3T3 cells and observed a transient increase in actin filaments. In addition, they examined the effects of D2O on actin polymerization in vitro and demonstrated that D2O accelerates purified globular actin polymerization immediately upon exposure to D2O, whereas the total amount of polymerized actin later during treatment with D2O is the same as that in H2O. Therefore, one possible mechanism underlying D2O-induced actin filament redistribution may involve the hydrogen to deuterium exchange in globular proteins (Hermans and Scheraga, 1959
; Scheraga, 1960
), which results in more stable protein structures (Sing and Wood, 1969
; Karasz and Gajnos, 1976
), and thus is caused by a typical isotope exchange effect.
The results of this study indicate that among several cytoskeletal components, D2O affected actin filaments specifically. The effect of D2O on the amount of actin filaments was transient (<15 min), which is consistent with Omori et al. (1997)
. Although we cannot exclude the possible action of D2O on microfilaments with a longer application of D2O, the results of our study indicate that it is possible to affect actin filaments selectively with our experimental protocol in AtT20 cells. In addition, we found a decrease in actin filaments in the cell processes immediately upon exposure to D2O in AtT20 cells. Secretory vesicles are transferred to the cell processes for exocytosis in AtT20 cells (Tooze and Burke, 1987
). The disassembly of the actin barrier at the plasma membrane is thought to be essential for the fusion of secretory vesicles (Pfeiffer et al., 1985
; Koffer et al., 1990
; Lejen et al., 2001
; Wilson et al., 2001
); therefore, D2O-induced disassembly of the actin barrier may be the one possible mechanism to facilitate vesicle fusion, and ß-endorphin release. Therefore, D2O-induced increases in secretion observed in this study and in various other cell types (Bennett et al., 1979
; Sulowska and Wyczolkowska, 1991
; Fewtrell and Metzger, 1980
; Maeyama et al., 1986
; Urata et al., 1989
) may be explained in part by actin-mediated mechanisms.
The D2O-induced reduction in spontaneous action potentials and slight hyperpolarization of the resting potential both rapidly returned to control values upon D2O washout. The direct action of D2O on Na+ channel gating has been demonstrated previously in Myxicola giant axons (Schauf and Bullock, 1979
; Schauf and Chuman, 1986
). Consistently, our study also demonstrated slow activation and inactivation of Na+ channel kinetics during D2O exposure in AtT20 cells. Since Na+ channel activity is directly modulated by actin polymerization (Mironov and Richter, 1999
; Negulyaev et al., 2000
), it is also possible that D2O indirectly effects on Na+ channels via actin filaments. In addition, a reduction in the mobility of Na+ in D2O buffer is known as the solvent isotope effects (Bass and Moore, 1973
). Therefore, both isotope exchange effects and solvent isotope effects may mediate the D2O effects on spontaneous action potentials.
During D2O exposure, we also found partial and reversible inhibition of spontaneous Ca2+ oscillations in AtT20 cells. Application of TTX did not inhibit spontaneous Ca2+ oscillations, indicating that these Ca2+ oscillations were not caused by voltage-dependent mechanisms. Since spontaneous Ca2+ oscillations were activated by caffeine and inhibited by dantrolene, the Ca2+ oscillations appears to be dependent on Ca2+ release from ryanodine-sensitive internal Ca2+ stores in AtT20 cells. D2O inhibited both spontaneous and caffeine-activated Ca2+ oscillations, whereas neither high-K+-induced Ca2+ influx nor voltage-dependent Ca2+ currents were affected during D2O exposure. Therefore, D2O may affect proteins regulating Ca2+ release from internal stores, although the specific sequence for the inhibition of spontaneous Ca2+ oscillations still needs to be analyzed.
In the presence of high-K+, exposure to D2O increased ß-endorphin release, whereas the D2O-induced enhancement of ß-endorphin release was not significant without high-K+ stimulation. Considering observed D2O actions on physiological processes underlying ß-endorphin secretion, two interpretations are possible: i), the modulation of actin filaments alone is not sufficient to increase ß-endorphin release, or ii), the inhibition of spontaneous action potentials and Ca2+ oscillations during D2O treatment masked a concomitant D2O-induced, actin-mediated increase in ß-endorphin release. However, the identification of primary D2O action for secretory activities during D2O exposure is difficult in living cells, since various solvent isotope effects and isotope exchange effects are simultaneously produced during D2O exposure and many of these effects are interrelated.
Cellular responses during D2O washout
During D2O washout, the high-K+-induced Ca2+ influx was completely inhibited for several minutes and gradually recovered (Fig. 5). In contrast, the high-K+-induced membrane depolarization of the membrane potential was not significantly affected during or after D2O exposure and agreed well with that predicted by the Nernst equation for K+ (Fig. 4 A). Although K+ channel conductance estimated by the voltage-clamp recordings was partially reduced upon D2O exposure, no further reductions in K+ currents were observed upon D2O washout (Fig. 4 C). Therefore, complete inhibition of the high-K+-induced Ca2+ influx upon D2O washout appears to involve VSCCs themselves and not via the effects on K+ channels. Because secretion from AtT20 cells depends on Ca2+ dynamics that are regulated largely by VSCCs in AtT20 cells (Richardson and Schonbrunn, 1981
; Richardson, 1983
), it is reasonable to assume that the inhibition of high-K+-induced ß-endorphin release may be associated with the reduction of the high-K+-induced Ca2+ influx.
To further clarify the effects of D2O on VSCCs, we examined Ba2+ and Ca2+ current recordings by the voltage clamp electrophysiology. Interestingly, with the conventional whole-cell patch-clamp recordings with an electrode pipette filled with H2O internal solution, we could not observe any significant reductions in the current amplitudes during or after D2O exposure (Fig. 6 A). However, when the D2O was dialyzed into the cells by the patch electrode, the current-voltage relationship of Ca2+ currents was modulated with a significant decrease in the inward currents (Fig. 6 B). The results suggest that asymmetric distribution of D2O (intracellular) and H2O (extracellular) across the plasma membrane is critical for the inhibition of VSCCs. Since intracellular D2O concentration in intact cells is higher than the extracellular D2O concentration during D2O washout, the inhibition of high-K+-induced Ca2+ influx may be explained by the asymmetric distribution of D2O that was produced exclusively during D2O washout.
Andjus et al. (1994)
reported that asymmetric distribution of D2O (extracellular) and H2O (intracellular) across the plasma membrane of freshwater alga activated Ca2+ channels in these cells. This effect of D2O may involve direct activation of Ca2+ channels, because the open channel probability of Ca2+ channels reconstituted in lipid bilayers is also increased in D2O. The authors suggested that transient osmotic-like stress produced by the more rapid transmembrane diffusion of D2O may mediate the activation of Ca2+ channels (Brooks, 1937
). However, we could not find any cell shape changes during and after the D2O exposure (Fig. 3), and thus the involvement of stress-sensitive mechanisms in the high-K+-induced Ca2+ influx can be ruled out. In addition, solvent isotope effects cannot explain the delayed D2O effects on high-K+-induced Ca2+ influx. Therefore, replacement of hydrogen with deuterium in constitutive proteins of VSCCs or in their regulatory proteins asymmetrically across plasma membrane may be the most considerable mechanism for the modulation of VSCCs.
Despite the significant inhibition of high-K+-induced Ca2+ influx during D2O washout, the same was not observed when the cells were treated in the presence of 90% D2O BSS, even with long incubation periods (up to 17 min), suggesting that the inhibition of Ca2+ flux was not associated with the onset of exposure to D2O or the duration of D2O treatment but with the return to H2O. Consistently, Ca2+ currents recorded with equable D2O substitutions in intracellular and extracellular solutions displayed normal current-voltage relationship (Fig. 6 B). These results suggest that the Ca2+ conductance of VSCCs is greatly affected in the intermediate state of isotope exchange effects when the constitutive proteins of VSCCs or their regulatory proteins contain asymmetrically deuterated amino acids during D2O washout, but not in the steady state when amino acids are completely deuterated during D2O treatment in the constitutive proteins of VSCCs or in their regulatory proteins (models in Fig. 8).
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ZPVE was found in tyrosine that is known as a critical residue for the voltage sensor of L-type Ca2+ channels (Bodi et al., 1997There are many known sites and mechanisms of action for D2O on cellular secretion. Both D2O-induced inhibition and activation of secretion have been reported in many different cell types. The results of this study demonstrated biphasic and bidirectional effects of D2O on ß-endorphin release that may be linked to the effects of D2O on actin filaments and VSCCs. Since the D2O concentration is only 1/6700 of H2O in our environment, hydrogen/deuterium exchange effects on natural living systems may be negligible. However, the results answered the complex D2O actions on cellular secretions in experimental models that were controversial for decades.
| ACKNOWLEDGEMENTS |
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| FOOTNOTES |
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Submitted on December 5, 2002; accepted for publication September 10, 2003.
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