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-induced pH Changes in Mammalian Cells
:Evidence for an NO3
-H+ Cotransporter




From the * Division of Respiratory Medicine, Department of Medicine, University of Toronto; and
Division of Cell Biology, Research
Institute, The Hospital for Sick Children, Toronto M5G 1X8, Canada
The effect of NO3
on intracellular pH (pHi) was assessed microfluorimetrically in mammalian cells
in culture. In cells of human, hamster, and murine origin addition of extracellular NO3
induced an intracellular
acidification. This acidification was eliminated when the cytosolic pH was clamped using ionophores or by perfusing the cytosol with highly buffered solutions using patch-pipettes, ruling out spectroscopic artifacts. The NO3
-
induced pH change was not due to modulation of Na+/H+ exchange, since it was also observed in Na+/H+ antiport-deficient mutants. Though NO3
is known to inhibit vacuolar-type (V) H+-ATPases, this effect was not responsible for the acidification since it persisted in the presence of the potent V-ATPase inhibitor bafilomycin A1.
NO3
/HCO3
exchange as the underlying mechanism was ruled out because acidification occurred despite nominal removal of HCO3
, despite inhibition of the anion exchanger with disulfonic stilbenes and in HEK 293 cells,
which seemingly lack anion exchangers (Lee, B.S., R.B. Gunn, and R.R. Kopito. 1991. J. Biol. Chem. 266:11448- 11454). Accumulation of intracellular NO3
, measured by the Greiss method after reduction to NO2
, indicated
that the anion is translocated into the cells along with the movement of acid equivalents. The simplest model to
explain these observations is the cotransport of NO3
with H+ (or the equivalent counter-transport of NO3
for
OH
). The transporter appears to be bi-directional, operating in the forward as well as reverse directions. A rough
estimate of the fluxes of NO3
and acid equivalents suggests a one-to-one stoichiometry. Accordingly, the rate of
transport was unaffected by sizable changes in transmembrane potential. The cytosolic acidification was a saturable function of the extracellular concentration of NO3
and was accentuated by acidification of the extracellular
space. The putative NO3
-H+ cotransport was inhibited markedly by ethacrynic acid and by
-cyano-4-hydroxycinnamate, but only marginally by 4,4
-diisothiocyanostilbene-2,2
disulfonate or by p-chloromercuribenzene sulfonate. The transporter responsible for NO3
-induced pH changes in mammalian cells may be related, though not identical, to the NO3
-H+ cotransporter described in Arabidopsis and Aspergillus. The mammalian cotransporter may be important in eliminating the products of NO metabolism, particularly in cells that generate vast
amounts of this messenger. By cotransporting NO3
with H+ the cells would additionally eliminate acid equivalents from activated cells that are metabolizing actively, without added energetic investment and with minimal disruption of the transmembrane potential, inasmuch as the cotransporter is likely electroneutral.
Nitric oxide has been recently recognized as an important second messenger in a variety of cell types. The
generation of NO from L-arginine is catalyzed by NO-synthase in response to a number of stimuli including
bacterial lipopolysaccharide, tumor necrosis factor-
,
and
-interferon (see Kiechle and Malinski, 1993
; Anggard, 1994
; Weinberg et al., 1995
for review). NO is an
unstable intermediate compound which, in aerobic
aqueous solutions such as the cytosol, is rapidly metabolized primarily to nitrite (NO2
) and to a lesser extent
to nitrate (NO3
). In the presence of oxidizing species
such as oxyhemoproteins, NO2
is rapidly converted to
the more stable NO3
(Ignarro et al., 1993
; Veszelovszky
et al., 1995
). Lipopolysaccharide and cytokine-induced
formation of NO, NO2
, and NO3
in vitro has been
extensively reported in neutrophils, primary macrophages, and monocyte/macrophage cell lines (Iyengar et
al., 1987
; Miwa et al., 1987
; Schmidt et al., 1989
; Wright
et al., 1989
). In animal models, increased production
of NO3
has been reported in sepsis (Ohshima et al.,
1994
; Oudenhoven et al., 1994
; Wright et al., 1992
),
glomerulonephritis (Sever et al., 1992
), and graft rejection (Tanaka et al., 1995
; Winlaw et al., 1994
; Drobyski
et al., 1994
). In humans, acute graft vs. host disease,
bacterial and viral meningitis, acute gastroenteritis, and
sepsis have been associated with increased NO3
production (Jungersten et al., 1993
; Shi et al., 1993
; Milstien et al., 1994
; Weiss et al., 1995
).
The amounts of NO2
and NO3
generated from NO
are substantial. The cytosolic concentrations of NO2
and NO3
in stimulated macrophages were found to be
119.3 nmol/ml and 281.2 nmol/ml, respectively (Marletta et al., 1988
). These figures greatly underestimate
the amount produced, since NO2
and NO3
are not
retained within the cell and can be readily recovered in
the extracellular milieu. In in vitro experiments, 100-
200 nmol of NO2
and NO3
were recovered from the
medium bathing 106 stimulated macrophages (Stuehr
and Marletta, 1987a
, b
, c
; Miwa et al., 1991
). Plasma nitrate levels as high as 200 µM have been reported in
disease states such as acute gastroenteritis (Jungersten et al., 1993
). These findings imply that NO2
and NO3
must be transported effectively across the plasma membrane for subsequent disposal. However, the pathway(s)
for transport of NO2
and NO3
in mammalian cells
are poorly understood.
This report describes a NO3
transport system present
in a variety of mammalian cells. In the course of measurements of the anion dependence of the intracellular
pH of Chinese hamster ovary (CHO)1 cells, we made
the serendipitous observations that addition of extracellular NO3
induced a reproducible cytosolic acidification. The purpose of this study was to characterize
this NO3
-induced cytosolic acidification, to compare
the underlying mechanism with known pHi regulatory
systems, and to describe its pharmacological profile.
Materials and Media
Nigericin, 2
7
bis-(2-carboxyethyl)-5(and 6) carboxyfluorescein
(BCECF) free acid and acetoxymethyl ester were purchased from
Molecular Probes, Inc. (Eugene, OR). Antimycin A, 2-deoxy-D-glucose, 2-(N-morpholino)ethanesulfonic acid (MES),
-nicotinamide
adenine dinucleotide phosphate (NADPH), glucose-6-phosphate,
bafilomycin, 4,4
-diisothiocyanostilbene-2,2
disulfonate (DIDS),
-cyano-4-hydroxycinnamate (CHC), and p-chloromercuribenzene
sulfonate (pCMBS) were obtained from Sigma Chemical Co. (St.
Louis, MO). Ethacrynic acid was purchased from Serva (Heidelberg, Austria) and phloretin from K+K (Hollywood, CA). Glucose-6-phosphate dehydrogenase and nitrate reductase were from Boehringer Mannheim (Indianapolis, IN). All other chemicals and salts were purchased from Sigma Chemical Co.
PBS contained (in mM): 140 NaCl, 10 KCl, 8 sodium phosphate, 2 potassium phosphate, pH 7.4. The sodium chloride solution contained (in mM): 117 NaCl, 1.66 MgSO4, 1.36 CaCl2, 5.36 KCl, 25 HEPES, 5.55 glucose. Sodium nitrate solution contained (in mM): 117 NaNO3, 6.2 MgSO4, 1.36 calcium gluconate, 5.36 potassium gluconate, 25 HEPES, 5.55 glucose. Sodium gluconate solution contained (in mM): 117 sodium gluconate, 6.2 MgSO4, 1.36 calcium gluconate, 5.36 potassium gluconate, 25 HEPES, 5.55 glucose. Potassium and N-methyl-D-glucammonium (NMG) solutions were made with equimolar substitution of the appropriate salts. To study the nitrate concentration dependence we used media with NaNO3 concentrations varying from 3.65 to 117 mM that were osmotically balanced with sodium gluconate. Sodium nitrite solutions containing 10-117 mM NaNO2 were prepared similarly. Unless otherwise indicated, all solutions were titrated to pH 7.5.
The composition of the low-buffer solution used to fill the patch pipettes was (in mM): 1 MES, 120 KCl, 1 MgCl2, 12 potassium gluconate, 50 glucose, 1 Mg-ATP, pH to 7.5 with NMG -OH. The high-buffer pipette solution contained (in mM): 50 HEPES, 50 Tris, 20 KCl, 1 MgCl2, 12 potassium gluconate, 50 glucose, 1 Mg-ATP, pH to 7.3 with HCl. All pipette solutions also contained 300 µM BCECF-free acid. External solutions used in patch clamp experiments were composed of (in mM): 120 KCl, 1 MgCl2, 12 KOH, 50 HEPES, pH 7.0. The potassium nitrate solution was made with equimolar substitution of KNO3 for KCl. All solutions were nominally bicarbonate-free and were adjusted to 290 ± 10 mosM with the major salt.
Cells
WT5 is a sub-line of wild-type CHO cells. AP1 is a cell line derived
from WT5 that is devoid of endogenous Na+/H+ activity (Rotin
and Grinstein, 1989
). HEK 293 is a human embryonic kidney cell
line (Lee et al., 1991
). J774 is a murine monocyte/macrophage cell line. Cells were grown in
-MEM (Ontario Cancer Institute, Toronto, ON) containing 25 mM NaHCO3 supplemented with
10% FCS, 100 U/ml penicillin, and 100 µg/ml streptomycin
(Life Technologies, Inc., Grand Island, NY) and were incubated
in a humidified environment containing 95% air and 5% CO2 at
37°C. Cultures were reestablished from frozen stocks regularly,
and cells from passages 3 to 20 were used for the experiments.
Where indicated, intracellular ATP was depleted by incubating
the cells for 10 min in glucose-free medium with 5 mM 2-deoxy- D-glucose and 1 µg/ml antimycin A, to inhibit both glycolysis and
oxidative phosphorylation. This protocol has previously been shown to deplete >90% of the ATP in CHO cells within 10 min
(Goss et al., 1994
). Subsequent fluorescence measurements were
performed in glucose-free media containing 5.5 mM 2-deoxy-
D-glucose.
Measurements of Cytosolic pH
Microfluorimetry
The cytosolic pH (pHi) of small groups of cells
was determined by microphotometry of the fluorescence emission of BCECF using dual wavelength excitation. Cells grown to
confluence on 25-mm glass coverslips (Thomas Scientific,
Swedesboro, NJ) were loaded with BCECF by incubation with 2 µg/ml of the precursor acetoxymethyl ester form for 10 min at
37°C. The coverslips were then mounted in a Leiden Coverslip
Dish (Medical System Corp., Greenvale, NY) and placed into a
thermostatted holding chamber heated to 37°C (Open Perfusion
Microincubator; Medical Systems Corp., Greenvale, NY) attached
to the stage of a Nikon Diaphot TMD inverted microscope (Nikon Canada, Toronto, ON). Cells were visualized using a Nikon Fluor 40×/1.3 N.A. oil-immersion objective and a Hoffman modulation contrast video system with an angled condenser (Modulation Optics) through a CCD-72 video camera and control unit
(Dage-MTI, Michigan City, IN) connected to a Panasonic monitor. Clusters of 6-12 cells from the confluent culture were selected for analysis with an adjustable diaphragm. The chamber
was continuously perfused at
0.5 ml/min to allow for complete
exchange of the bath solution once every minute using a gravity-driven system and a Leiden aspirator. Solutions could be
switched by opening solenoid valves (General Valve, Fairfield,
NJ). When rapid solution changes were required, 3 aliquots of 1 ml of the new medium were quickly pipetted (<15 s) into the
chamber and perfusion was continued using the new medium
(Kapus et al., 1994
).
Fluorescence Imaging For imaging of single cell pHi, cells were grown on round glass coverslips to 60-70% confluence and loaded with BCECF as described above. Ratio fluorescence imaging was performed on a Zeiss Axiovert 100 TV inverted microscope (Zeiss, Oberkochen, Germany) equipped with a 75 W Xenon lamp (XBO 75, Zeiss), a shutter/filter wheel assembly (Lambda 10, Sutter Instrument Co., Novato, CA), a NeoFluar 63×/1.25 N. A. objective and a high-resolution (1,317 × 1,025 pixels, KAF 1400, Kodak) cooled, digital CCD camera (TEA/ CCD 1317; Princeton Instruments, Trenton, NJ) interfaced to a Pentium 90 computer (Dell Inc., Toronto, ON, Canada) via a 12 bit, 1 MHz camera-controller (Princeton controller: ST-38; Princeton Instruments, Trenton, NJ). Image acquisition and excitation filter selection were controlled by the Metafluor software (Universal Imaging Corp., West Chester, PA). All measurements of pHi were performed at 37°C.
Electrophysiology and pHi Measurements in Voltage-clamped Cells
Cells were patch-clamped in the whole-cell configuration of the
patch clamp technique using an Axopatch-1D amplifier (Axon Instruments Inc., Foster City, CA), as described (Kapus et al., 1993
). Electrodes were made from filament-filled borosilicate glass capillaries (World Precision Instruments Inc., Sarasota, FL)
using a horizontal puller (P-87; Sutter Instrument Co., Novato, CA) and a microforge (MF-9; Narishige USA, Greenvale, NY). Pipette resistance ranged from 2 to 10 M
; seal resistance ranged
from 10 to 50 G
. Series resistance varied between 5 and 30 M
,
and cell capacitance was between 12 and 34 pF.
Cytosolic pH in voltage-clamped cells was measured microfluorimetrically on the Photon Technologies Inc. photometric system described above, using pipette solutions with a low buffering power (1 mM MES) to maximize the NO3
-induced intracellular
pH changes. Cells were patch-clamped in the whole-cell configuration and loaded with BCECF-free acid by diffusion of the dye
from the pipette solution into the cytosol. Measurements were
initiated 5 min after attaining the whole-cell configuration to allow for equilibration of the cytosolic pH with the pipette pH and
for adequate BCECF loading. Cells were superfused at 0.5 ml/
min with the indicated solutions. Calibration of fluorescence ratio vs. pH was performed on single nonpatched cells, using the nigericin technique described above (Thomas et al., 1979
). One calibration curve was obtained every day by averaging data from 3 to 6 cells sequentially perfused with KCl media buffered at 3 different pH values ranging from 6.0 to 7.5. All patch clamp experiments were carried out at room temperature. Single-cell pHi
measurements were also performed microfluorimetrically in nonpatched cells at room temperature to ensure that the NO3
-induced cytosolic acidification was present under these conditions as well (data not shown).
Measurements of Intracellular Nitrate Content
AP1 cells were grown to confluence on 6-well plastic tissue culture dishes (Costar Corp., Cambridge, MA). Culture medium was aspirated and cells were incubated with isotonic NaNO3 solution at 0 or 37°C for the indicated times. Where indicated, the solution contained 100 µM DIDS. At the end of the incubation period, each well was rapidly washed 3 times with 10 ml of PBS at
4°C and subsequently the cells were lysed using 1 ml distilled water and repeated freeze-thawing. Whole cell lysates were centrifuged for 10 min in a microcentrifuge (Beckman Microfuge,
13,500 rpm; Beckman Instruments, Fullerton, CA) to remove cellular debris. The NO3
content of the resultant supernatant was
measured using the Greiss reaction after reduction of NO3
to
NO2
, as previously described (Green et al., 1982
; Verdon et al., 1995
; Gilliam et al., 1993
). Reduction of NO3
to NO2
was performed by incubating the supernatant with 1 µM NADPH, 0.16 U/ml glucose-6-phosphate dehydrogenase, 500 µM glucose-6-phosphate, and 0.80 U/ml nitrate reductase at room temperature for 45 min. A 500-µl aliquot of the sample was then incubated with 250 µl of 0.1% (N-1-naphthyl)-naphthylethylene diamine dihydrochloride and 250 µl of 1% sulfanilamide in 5%
phosphoric acid at 37°C for 10 min. Absorbance was measured
spectrophotometrically at 540 nm in a Hitachi U-2000 spectrophotometer. A calibration curve was constructed by adding increasing concentrations of NaNO3 to lysates of cells not exposed
to exogenous NO3
. A second aliquot of the cell lysate was used
for protein determination using the BioRad Protein Assay Kit
(BioRad Laboratories, Richmond, CA). Total cell number was estimated by normalizing the protein content in the whole cell lysate to that of a cell suspension containing a known number of
cells, determined electronically using the Coulter counter. The
cell suspension was prepared by addition of 1 ml of trypsin-EDTA
(GIBCO-BRL, Life Technologies Inc., Grand Island, NY) to AP1
cells grown to confluence in a 75-ml tissue culture flask. The volume of the suspended cells was determined with the Coulter-Channelyzer combination. The intracellular NO3
concentration
was then calculated by dividing the NO3
content of the cell lysate by the corresponding cellular volume.
Data Analysis and Statistics
Quantification of cell-associated fluorescence was performed using the Felix software package (Photon Technologies, Inc.) or
the Metamorph/Metafluor package (Universal Imaging, Inc.,
West Chester, PA). Mean H+(equivalent) flux was calculated by multiplying the rate of pHi change (
pHi/
time) by the buffering capacity of CHO cells, measured to be 25 mmol/pH/liter of cells in
the pH range of our measurements (Kapus et al., 1994
). The rate
of pHi change was derived by linear regression of the pHi vs. time
curve over 4-s intervals using the Origin software (MicroCal Software Inc., Northampton, MA). Data were graphed using the Origin software and are shown as mean ± one standard error (SE)
of the number of experiments indicated. Significance was calculated using Student's t test.
Effect of Nitrate on Intracellular pH
The effect of external NO3
on pHi was evaluated microfluorimetrically in CHO cells loaded with BCECF.
To facilitate the detection of NO3
-induced changes in
pHi, the contribution of other acid/base transporters, which might have a compensatory effect, was minimized. For this purpose, the initial experiments were
performed in nominally HCO3
-free and Na+-free solutions, to minimize Cl
/HCO3
exchange and Na+-dependent acid/base transport. As shown in Fig. 1 A, superfusion of the cells with an NO3
-rich solution induced a
sizable cytosolic acidification. The change in pHi cannot be attributed to removal of external Cl
, since substitution of Cl
with equimolar gluconate
did not significantly alter pHi. This finding also implies that Cl
/
HCO3
exchange activity is negligible, since the alkalinization predicted to result from uptake of HCO3
, in
exchange for exiting Cl
, was not detectable. It is therefore unlikely that the NO3
-induced acidification results from exchange with intracellular HCO3
via the
anion exchanger.
-induced cytosolic acidification in Chinese hamster ovary (CHO) cells. (A) CHO (AP1) cells grown to near confluence on glass coverslips were loaded with BCECF and used for microfluorimetric determination of pHi. The coverslip was perfused sequentially with the following K+-rich solutions, as indicated by the
bar at the bottom of the graph: Cl
, gluconate
, NO3
, and Cl
.
Trace is representative of 4 similar experiments. (B, left) A single
CHO cell was patched in the whole-cell configuration with a pipette filled with high buffer solution (50 mM HEPES, 50 mM Tris,
20 mM KCl) containing BCECF and used for microfluorimetric determination of pHi. After equilibration of the cytosol with the pipette buffer (~5 min), the extracellular bathing medium was
changed from KCl solution to KNO3 solution, as indicated. The
trace is representative of 2 experiments. (right) CHO cells grown to
near confluence on glass coverslips were loaded with BCECF and
used for microfluorimetric determination of pHi. The pHi of the
cells was clamped by incubation with 5 µM nigericin in a K+-rich
solution for 5 min. Where indicated, the main anion of the perfusing solution was switched from Cl
to NO3
, while keeping the K+
concentration constant at 140 mM. The trace is representative of 5 similar experiments. (C ) CHO cells were grown to 60-70% confluence on coverslips and loaded with BCECF for measurement of pHi
by ratio imaging. The cells were allowed to equilibrate with the isotonic Cl
-rich solution and one set of images was acquired (solid
bars). The solution was then substituted for a NO3
-rich medium,
and, after 5 additional min, another set of images was acquired
(open bars). Images were collected from multiple areas of the coverslip while continuously perfusing the coverslip with the indicated
solution. Quantification of cell-associated fluorescence ratio was
performed using the Metamorph/Metafluor package (Universal
Imaging, Inc.). Calibration of fluorescence ratio vs. pHi was performed on the same coverslip using the nigericin technique, as described in EXPERIMENTAL PROCEDURES. The histogram was built
using 153 and 174 cells perfused with isotonic Cl
-rich and NO3
-rich media, respectively.
It was important to ascertain that the NO3
-induced
acidification of the cells is neither artifactual nor the
result of a toxic effect. Cell morphology, which was
monitored continuously using Hoffman optics, was not
altered by addition of NO3
. Moreover, BCECF was retained by the cells throughout the observation period,
attesting to the viability of the cells. Finally, the effect of
external NO3
was reversible since reperfusion with the
Cl
-rich medium induced recovery of pHi (Fig. 1 A).
These observations argue against a deleterious effect of
NO3
.
In our experiments, pHi is estimated from the ratio
of BCECF fluorescence recorded at two excitation
wavelengths. Differential quenching of fluorescence at
one of these wavelengths by NO3
could mimic the appearance of acidification. Several experimental approaches were used to rule out this potential artifact.
We first compared the spectral properties of the free
acid of BCECF in vitro in isotonic KCl or KNO3 solutions, titrated to pH levels ranging from 5.84 to 7.56 with HCl or HNO3. Excitation and emission spectra acquired in Cl
and NO3
solutions were identical (data
not shown). That NO3
does not alter the behavior of
the dye inside cells was shown by clamping pHi with 5 µM nigericin, a K+/H+ ionophore, in cells bathed in
media containing 140 mM K+. Under these conditions
the fluorescence ratio was unaffected by substitution of
extracellular Cl
for NO3
(Fig. 1 B, right).
The effects of extracellular NO3
on pHi were also
eliminated when the buffering capacity of the cytosol
was greatly increased. This was accomplished by patch-clamping CHO cells in the whole-cell configuration
with pipettes filled with a high buffer (50 mM HEPES, 50 mM Tris) solution. Microfluorimetric measurements of the individual patched cells revealed no
change in pHi when extracellular Cl
was replaced by
NO3
and vice versa (Fig. 1 B, left). Together, these
findings indicate that NO3
does not artifactually alter
the fluorescence of BCECF and indicate that this anion
induces a bona fide change in pHi.
Microfluorimetric measurements like those of Fig. 1
A represent the average pHi of clusters of 6-12 cells. To
assess whether the NO3
-induced cytosolic acidification
occurs in all or most of the cells in the population and
to further validate the microfluorimetric observations,
the pHi of individual cells was measured by ratio fluorescence imaging, as described in EXPERIMENTAL PROCEDURES. For these experiments, CHO cells were
grown to submaximal confluence on glass coverslips, to
facilitate the demarcation of individual cells, and were
loaded with BCECF as described. Cells were perfused for 5 min in isotonic Cl
or NO3
solution before image acquisition, to allow adequate time for equilibration. As shown in Fig. 1 C, NO3
-induced cytosolic acidification occurred in virtually all the cells studied (n = 153 cells in Cl
-rich solution and n = 174 in NO3
-rich
solution). The mean pHi in Cl
solution was 7.55 ± 0.02, whereas 5 min after switching to NO3
, pHi had
decreased to 7.19 ± 0.02. These values were statistically different with P = 2.84 × 10
34 (Student's t test). It is
noteworthy that the recording systems used for the imaging and photometry experiments are entirely different, indicating that the pH changes recorded are independent of the optical path, detector, and analysis software used.
We also tested whether other cell types also display
the NO3
-induced changes in pHi. The murine monocyte-macrophage cell line J774 was tested since, as detailed in the INTRODUCTION, NO3
production is
greatly enhanced in stimulated phagocytes (Miwa et al.,
1987
; Iyengar et al., 1987
; Schmidt et al., 1989
; Wright et al., 1989
). When bathed in NO3
-rich media, J774
cells underwent a cytosolic acidification at a rate similar
to that observed in CHO cells (Table I).
|
Table I.
NO3 |
NO3
-induced Cytosolic Acidification Is Accompanied by
NO3
Uptake
NO3
could induce the observed pHi changes by acting
on an extracellular receptor, by altering the transmembrane potential or by driving the transport or generation of acid equivalents as it enters the cell. To test
whether the NO3
-induced intracellular acidification is
accompanied by entry of the anion into the cells, the
intracellular NO3
content was measured using the
Greiss method, after reduction of NO3
to NO2
(see
EXPERIMENTAL PROCEDURES). For these experiments,
CHO cells were incubated with isotonic NaNO3 for 2-10
min at 37°C. Extracellular trapping was estimated by exposing cells momentarily to ice-cold NaNO3 solution at
0°C (time = 0 in Fig. 2). Subtraction of this value from
the individual determinations also accounted for any endogenous NO3
or NO2
. Uptake of NO3
by the
cells was linear for at least 10 min. In cells incubated with 117 mM NO3
the initial rate of entry of the anion, derived from linear regression, averaged 6.75 ± 0.15 mmol/liter cells/min (n = 3 at 2 min; n = 6 for all
other time points; R = 0.995).
uptake by adherent CHO cells.
CHO cells were grown to near confluence on 6-well plastic tissue
culture dishes. The cells were exposed to NaNO3 solution for the
times indicated, then washed extensively in the cold. Following lysis using 1 ml distilled H2O and repeated freeze-thawing, the intracellular NO3
content was measured after reduction to NO2
as
described in EXPERIMENTAL PROCEDURES. Solid squares: control cells. Open triangles : the uptake medium contained 100 µM 4,4
-diisothiocyanostilbene-2,2
disulfonate (DIDS). Cell number and
cell volume were measured using the Coulter-Channelyzer in parallel samples of cells that were suspended by trypsinization. Data
are means ± SE of 3 determinations at 2 min and 6 experiments at
other time points. Lines were fitted by linear regression.
Exchange of NO3
for Cl
(Simchowitz, 1988
; Simchowitz and Davis, 1989
; Zhang and Solomon, 1992
;
Kurtz et al., 1994
) has been documented to occur via
the stilbene-sensitive anion exchanger (AE). To determine whether this process contributes to NO3
uptake
in CHO cells, measurements were also performed in
the presence of 100 µM 4,4
-diisothiocyanostilbene-2,2
-disulfonate (DIDS), a concentration of the inhibitor that is expected to completely block the AE1 (Bruce
et al., 1994a
, b
) and AE3 (Lee et al., 1991
) isoforms and
largely block the AE2 isoform of the exchanger (Simchowitz and Davis, 1989
; Lee et al., 1991
). NO3
flux in
DIDS-treated cells was 2.66 ± 0.07 mmol/liter cells/ min (n = 3 at 2 min; n = 6 for all other time points;
R = 0.994). Thus 39% of the total NO3
flux was insensitive to stilbenes and may be, at least in part, coupled
to the translocation of H+ equivalents (see below).
Since the NO3
-induced pHi changes were reversible,
we tested the reversibility of the NO3
fluxes. In three
experiments, NO3
content was measured in cells incubated with the anion for 15 min, followed by incubation in a NO3
-free (Cl
-rich) medium for 10 min at
37°C. Upwards of 85% of the NO3
taken up by the
cells was lost during the washout period, implying that
transport of the anion is bi-directional (data not shown).
Jointly, these experiments indicate that NO3
is
transported across the membrane during the course of
the NO3
-induced pHi changes. The flux of NO3
may
alter pHi directly, by driving the transport of H+ equivalents across the membrane through a formerly unidentified pathway. Alternatively, the anion could conceivably modulate the activity of known acid/base transporters, such as Na+/H+ exchangers (NHE), anion
exchangers or vacuolar-type H+ pumps (V-ATPases).
These possibilities were considered experimentally below.
NO3
-induced Cytosolic Acidification Is Not Mediated by the
Na+/H+ Antiporter
In erythrocytes, NHE has been reported to be inhibited
by NO3
(Parker, 1983
; Parker and Castranova, 1984
;
Jennings et al., 1986
). Because NHE is thought to contribute to the maintenance of the steady-state pHi, inhibition of this transporter by NO3
could conceivably result in a cytosolic acidification like that illustrated in
Fig. 1 A. To test this hypothesis, we compared the effect
of NO3
on pHi changes in two clones of CHO cells,
the wild-type CHO cell (WT5) which expresses the
NHE-1 isoform of the exchanger and the CHO mutant
(AP1) which is devoid of NHE. As illustrated in Fig. 3 A,
WT5 cells recover readily from an acid load upon addition of extracellular Na+. Such recovery, which is inhibited by amiloride and its analogues (not shown), is the
hallmark of NHE activity. By contrast, AP1 cells failed
to recover when Na+ was reintroduced to the perfusate,
implying that they are devoid of NHE.
-induced cytosolic acidification is independent
of Na+/H+ exchange. (A) CHO cells grown to confluence on glass
coverslips were loaded with BCECF and used for fluorimetric determination of pHi. WT5 cells are wild-type CHO cells, while AP1
cells are antiport-deficient CHO mutants isolated by the H+-suicide technique (see EXPERIMENTAL PROCEDURES). Before the initiation of the trace, the cells were acid loaded by means of an ammonium pre-pulse (25 mM for 10 min). The trace starts upon perfusion of the ammonium-loaded cells with a Na+-free, NMG-Cl
solution (pH 7.5). Where indicated, the bathing medium was
switched to a Na+-rich solution (NaCl, pH 7.5). Representative of
5 experiments. (B and C ) pHi was measured fluorimetrically in
CHO cells loaded with BCECF, as in panel A. In B AP1 cells were
perfused initially with NaCl or NMG-Cl medium, as indicated.
Where noted, the media were changed to NaNO3 or NMG-NO3 solution, respectively. In C WT5 (top trace) or AP1 cells (lower trace)
were perfused initially with NMG-Cl medium. Where noted, the
perfusing medium was switched to NMG-NO3 solution. Traces in B
and C are representative of 6 experiments, respectively. Mean
NO3
- induced H+ flux of AP-1 cells was 2.54 ± 0.40 mmol/liter/
min in Na+-rich solution and 2.22 ± 0.45 mmol/liter/min in
NMG+-rich solution. Mean NO3
- induced H+ flux of WT5 cells in
NMG+-rich solution was 2.39 ± 0.39 mmol/liter/min.
Despite the absence of NHE, AP1 cells exhibited a cytosolic acidification upon addition of external NO3
.
The rate and extent of acidification were similar in the
presence and absence of extracellular Na+ (Fig. 3 B).
The mean NO3
- induced H+ flux was 2.54 ± 0.40 mmol/liter/min (n = 6) in Na+-rich solution and 2.22 ± 0.45 mmol/liter/min in NMG+-rich solution (n = 6).
These observations imply that NHE is not essential for
NO3
to induce cytosolic pH changes.
Furthermore, NO3
-induced cytosolic acidification
was observed in wild-type CHO cells bathed in the absence of external Na+ (mean NO3
- induced H+ flux in
NMG+-rich solution was 2.39 ± 0.39 mmol/liter/min;
n = 6). Under these conditions, forward NHE activity is
abrogated and only backward exchange can occur,
which can lead to cytosolic acidification. Inhibition of
this process by NO3
would be expected to have the
converse effect, namely, cytosolic alkalinization. However, as shown in Fig. 3 C, NO3
produced an acidification in WT5 cells that was indistinguishable from that
noted in AP1 cells. Together, the data using ion substitution and genetic deletion of the antiporter indicated
that the NO3
-induced cellular acidification is not mediated by inhibition of NHE.
NO3
-induced Cytosolic Acidification Is Not Mediated by the
Anion Exchanger
The Cl
/HCO3
exchanger has affinity for other anions, including NO3
(see Cabantchik and Greger,
1992
; Reinertsen et al., 1989
for review), and NO3
/
HCO3
exchange has been reported (Kemp and Boyd,
1993
; Humphrey et al., 1994
; Zhao et al., 1994
).
Though our experiments were conducted in the nominal absence of HCO3
, we cannot a priori exclude the
possibility that exchange of cellular HCO3
for external NO3
accounts for the acidification, particularly
considering the finding that DIDS inhibited a sizable
fraction of NO3
uptake. To address this possibility directly, the effect of NO3
on pHi was measured in the
presence of DIDS. As shown in Fig. 4 A, the NO3
-
induced acidification persisted when WT5 cells were
treated with 100 µM DIDS. The H+(equivalent) flux in control cells was 2.5 ± 0.5 mmol/liter/min and 2.7 ± 0.5 mmol/liter/min for DIDS treated cells (n = 4). No effect on the rate of cytosolic acidification was found using up to 1 mM of DIDS for 15 min (results not shown).
-induced cytosolic acidification is independent
of the anion exchanger. (A) pHi was measured fluorimetrically in
CHO cells (WT5) loaded with BCECF. The cells were perfused initially with NMG-Cl medium and, where noted, the perfusing medium was switched to NMG-NO3 solution. For the lower trace the
cells were pre-treated with 100 µM DIDS for 2 min before the initiation of the trace and the same concentration of the stilbene was
present throughout the measurement period illustrated. (B) Microfluorimetric measurement of pHi in HEK cells. The cells were
initially bathed in NMG-Cl solution and, where indicated, the medium was switched to NMG-NO3 solution. Traces in A and B are
representative of 6 experiments, respectively.
To further assess the role of the anion exchanger in
the NO3
-induced pH changes, we tested a human embryonic kidney (HEK) cell line which has been reported to lack endogenous Cl
/HCO3
exchange activity (Lee et al., 1991
). As shown in Fig. 4 B, perfusion of
HEK cells with external NO3
promoted a robust acidification, at a rate that was in fact greater than that observed in CHO cells (Table I). Jointly, these data suggest that the anion exchanger is not responsible for the
NO3
-induced cytosolic acidification.
NO3
-induced Cytosolic Acidification Is Not Mediated by the
V-ATPase
The V-ATPase, a H+-pump whose primary function is
acidification of intracellular organelles (see Gluck,
1993
for review), also plays a role in the homeostasis of
pHi in some cell types (Swallow et al., 1991
). In osteoclasts as well as in organelles studied in vitro, NO3
has
been reported to inhibit the V-ATPase (Chatterjee et
al., 1993
; Dschida and Bowman, 1995
). Because the
V-ATPase continuously removes H+ from the cytosol,
inhibition of this enzyme by NO3
could result in acidification. Two approaches were used to evaluate this
possibility. In the first, the pump was inhibited by depleting cells of ATP by inhibiting glycolysis and oxidative phosphorylation using 2-deoxy-D-glucose and antimycin A. In CHO cells this results in depletion of
>90% of the cellular ATP within 10 min (determined using luciferin-luciferase; Goss et al., 1994
). As illustrated in Figs. 5, A and B, such ATP-depleted cells exhibited cytosolic acidification when exposed to extracellular NO3
. The mean H+ flux of ATP-depleted cells
was comparable to that of control cells (2.38 ± 0.31 mmol/liter/min and 2.03 ± 0.42 mmol/liter/min, respectively; n = 4).
-induced cytosolic acidification is independent
of the V-ATPase. (A) pHi was measured fluorimetrically in CHO
cells (AP1) loaded with BCECF. The cells were perfused initially
with NMG-Cl medium and, where noted, the perfusing medium
was switched to NMG-NO3 solution. For the lower trace the cells
had been ATP depleted by preincubation for 10 min in glucose-free solution with 5 mM 2-deoxy-D-glucose and 1 µg/ml antimycin
A. The fluorescence measurements were performed in glucose-free solutions. Traces are representative of 4 determinations. (B)
Quantitation of the NO3
-induced cytosolic acidification in CHO
cells. (left) WT5 cells. Where specified (stippled bar), the cells were
treated with 50 nM bafilomycin for 2 min before, and also during
the pHi measurements in KCl or KNO3 solutions. (right) AP1 cells.
Where specified (stippled bar), the cells were ATP depleted as
above. The pHi measurements were performed in NMG-Cl and
NMG-NO3 solutions. H+(equivalent) flux was calculated by multiplying
the rate of pHi change (
pHi/
time) by the buffering capacity of
CHO cells, measured to be 25 mmol/pH/liter of cells in the pH
range of our measurements (Kapus et al., 1994
A second approach to evaluate the possible role of
the V-ATPase used bafilomycin A1, a macrolide antibiotic which is a potent and specific inhibitor of the
pump (Crider et al., 1994
; Zhang et al., 1994
). In these
experiments, WT5 cells were pre-incubated for 2 min
in a Cl
-rich, NO3
-poor solution, with 50 nM bafilomycin, a concentration shown previously to fully inhibit
V-ATPases in a variety of cell types (Zhang et al., 1994
;
Crider et al., 1994
). Subsequently, pHi was microfluorimetric measured upon exposure of cells to isotonic NO3
-rich solution. Comparison of four experiments
in bafilomycin-treated cells with their respective controls revealed no differences in H+(equivalent) flux (1.46 ± 0.41 and 1.42 ± 0.32 mmol/liter/min in control and
bafilomycin-treated cells, respectively; Fig. 5 B). Jointly,
the results of the ATP depletion and bafilomycin studies suggest that the NO3
-induced cytosolic acidification is not mediated by the inhibition of the V-ATPase.
Furthermore, the NO3
-induced cytosolic acidification
appears to be an ATP-independent process.
Possible Role of NO2
and Other Nitrogen Oxides in
NO3
-induced Cytosolic Acidification
Solutions of NO3
can contain small amounts of NO2
and/or other nitrogen oxides. Of relevance, addition
of NO2
to pancreatic acinar cells was recently shown to
induce a sizable cytosolic acidification (Zhao et al.,
1994
). This pH change was attributed, to a small extent, to the generation and permeation of HNO2, a
weak acid with pKa of 3.2. The majority of the acidification, however, was seemingly due to the reaction between poorly defined nitrogen oxides (possibly NO,
N2O3, and/or N2O4, intermediates in the oxidation of
NO2
to NO3
) and intracellular H2O or OH
. In acinar cells, the latter reaction was found to be catalyzed by carbonic anhydrase (Zhao et al., 1994
). These observations raised the possibility that a similar mechanism
might underlie the NO2
-induced acidification in CHO
cells. Experiments designed to explore this possibility
are illustrated in Fig. 6. The effect of NO2
on pHi was
compared with that of acetate, another weak acid with somewhat higher pK (pKa = 4.7). Acetate produced a
rapid acidification, as expected from the permeation of
the uncharged protonated species, acetic acid. An
equimolar concentration of NO2
induced a somewhat
smaller and slower acidification (
0.27 ± 0.05 pH
U/min; n = 3), consistent with the >10-fold lower concentration of the protonated species. In both cases, the
pHi changes were rapidly reversed upon removal of the
weak acids.
and NO2
on pHi
and assessment of the role of carbonic anhydrase. (A) pHi was
measured fluorimetrically in CHO cells (AP1) loaded with BCECF.
The cells were perfused initially with 117 mM NaCl medium and,
where noted, with solutions containing 10 mM sodium acetate
(Act
), 10 mM NaNO2 or 117 mM NaNO3. The sodium acetate
and NaNO2 solutions were osmotically balanced with 107 mM Na-gluconate. (B) AP1 cells were preincubated for 5 min with 0.1 mM
methazolamide in NaCl solution before fluorimetric measurement
of pHi. Where noted, cells were perfused with solutions containing
10 mM NaNO2 or 117 mM NaNO3, as described in panel A, supplemented with 0.1 mM methazolamide. Traces in A and B are representative of 4 experiments each.
To determine whether nitrogen oxides contributed
to the acidification by a carbonic anhydrase-mediated
process, the cells were treated with methazolamide, an
inhibitor of the anhydrase. A representative experiment is shown in Fig. 6 B. Neither the rate nor the extent of the NO2
-induced acidification were noticeably
altered by methazolamide (
pHi =
0.27 ± 0.05 in
control cells and
0.29 ± 0.07 in cells treated with methazolamide; n = 3). Similarly, the more gradual acidification induced by NO3
was unaffected by inhibition of
carbonic anhydrase (
pHi =
0.11 ± 0.03 in control
cells and
0.10 ± 0.04 in cells treated with methazolamide; n = 3). Thus, it appears that H+ release by reaction of nitrogen oxides with H2O or OH
is not an important component of the NO2
or NO3
response in
CHO cells.
To ensure that the NO3
-induced acidification observed in CHO cells was not due to reduction of extracellular NO3
to NO2
, the NO2
content of solutions
containing 29 to 117 mM NO3
was measured using the
Greiss method (as described in EXPERIMENTAL PROCEDURES). NO2
content in the solutions was found to be
negligible (mean [NO2
] = 0.44 ± 0.05 µM, n = 8).
Similarly, intracellular NO2
levels were found to be
negligible up to 10 min after exposure to extracellular
NO3
(results not shown). Jointly, these results suggest
that neither permeation of HNO2 nor metabolism of
contaminating nitrogen oxides are responsible for the
acidification induced by NO3
.
Properties of the NO3
-induced H+ Flux
The results summarized above confirmed that the pH
changes promoted by NO3
are not due to modulation
of the predominant homeostatic pathways and are accompanied by transport of NO3
across the membrane.
The simplest model to explain the effects of the anion
is therefore the cotransport of NO3
with H+, or its
equivalent, NO3
/OH
counter-transport. For simplicity, and by analogy with the system described in plants
and fungi (Downey and Gedeon, 1994
; Mehrag and
Blatt, 1995
), we will tentatively assume hereafter that
NO3
-H+ cotransport is responsible for the observed
pHi changes.
The kinetic properties of the putative NO3
-H+
cotransport were investigated next. The extracellular
[H+] dependence was determined in AP1 cells suspended in NaNO3 solutions titrated between pH 6.0 to
7.5. Because reducing the extracellular pH (pHo) is expected to reduce pHi by pathways other than the NO3
-H+ cotransporter, the NO3
-independent component
of the pH change was also measured by perfusing the
cells in NaCl solution titrated to the appropriate pH.
The NO3
-independent H+ flux at pH 6.0, 6.5, and 7.0 was 4.11 ± 0.88, 1.71 ± 0.93, and 1.36 ± 0.77 mmol/
liter/min, respectively. The NO3
-independent component was then subtracted from the total change recorded in the presence of NO3
at an identical pHo.
The results of these determinations are illustrated in
Fig. 7. Increasing external [H+] in the pH 7.5-6.0
range increased the rate of NO3
-induced cytosolic
acidification, consistent with NO3
-H+ cotransport.
More extreme levels of pHo were not studied for fear of
inducing cell damage. In the range studied, the half
maximal rate of acidification was attained at [H+] = 0.09 ± 0.01 µM.
-induced cytosolic acidification. pHi was measured fluorimetrically in CHO cells
(AP1) loaded with BCECF. The pHi change was measured upon
introduction of a NO3
-rich solution of the indicated external
[H+] (corresponding to a pHo range of 6.0-7.5). The rate of pHi
change was estimated over a 60 s period and the H+(equivalent) flux
was calculated as in Fig. 5. The NO3
-independent acidification,
due solely to the reduction in extracellular pH was estimated using
Cl
-rich solutions of identical pH, and was subtracted from the
equivalent measurements performed in NO3
-rich media (see EXPERIMENTAL PROCEDURES). NO3
-independent H+ flux at pHo of
6.0, 6.5, 7.0 was 4.11 ± 0.88, 1.71 ± 0.93 and 1.36 ± 0.77 mmol/
liter/min, respectively. Data are means ± SE of 5 experiments.
To assess the external NO3
concentration ([NO3
]o)
dependence of the putative cotransporter, pHi was
measured in AP1 cells perfused with isotonic solutions
containing 3.65-117 mM NO3
. These experiments
were performed at both pHo 6.5 and 7.5, and the solutions were osmotically balanced with gluconate
since
this anion was shown earlier to have no discernible effect on pHi (Fig. 1 A). The rate of H+(equivalent) flux increased with increasing external NO3
concentration at
both pHo. The apparent NO3
affinity and maximal velocity of the putative cotransporter can be inferred by
fitting the data with an Eadie-Hofstee plot (Fig. 8). At
pHo 7.5, Vmax and Km were 5.81 ± 0.58 mmol/liter/min
and 86.2 ± 12.6 mM, respectively (R =
0.98). At pHo
6.5, Vmax and Km were 10.7 ± 1.3 mmol/ liter/min and
40.1 ± 10.6 mM, respectively (R =
0.97). Because the
apparent affinity of the transporter for NO3
is modified by [H+]o, we conclude that binding of the ions to
the transporter cannot occur independently in random
order. The altered affinity is consistent with an allosteric effect of protons on the conformation of the NO3
binding site(s).
concentration dependence: Eadie-Hofstee plot.
pHi was measured fluorimetrically in CHO cells (AP1) loaded with
BCECF. The cells were equilibrated in Cl
-rich medium and pHi
changes were measured upon introduction of solutions of varying
NO3
concentration (from 6.65 to 117 mM). The solutions were
osmotically balanced using gluconate. No significant pHi change
was induced by gluconate itself (e.g., Fig. 1). The rate of pHi
change was estimated over a 60 s period and the H+(equivalent) flux
was calculated as in Fig. 5. These experiments were performed at
pHo = 7.5 (closed squares) and pHo = 6.5 (open triangles). Data are
means ± SE of 4 determinations. Vmax and Km, derived by linear regression from the Eadie-Hofstee plot were 5.8 ± 0.6 mmol/liter/
min and 86.2 ± 12.6 mM for pHo = 7.5 (R =
0.98) and 10.7 ± 1.3 mmol/liter/min and 40.1 ± 10.6 mM for pHo = 6.5 (R =
0.97).
Effect of Monovalent Cations on NO3
-induced
Cytosolic Acidification
Some anion transporters are cation dependent (Roos
and Boron, 1981
; Schron et al., 1985
; Shrode et al.,
1995
). To assess whether cationic species affect the rate
of NO3
-induced cytosolic acidification, pHi was measured in isotonic NO3
-rich solutions containing Na+,
K+, or NMG+ as the principal cation. The cells were initially equilibrated with Cl
-rich solutions of the same
cationic composition and then switched to NO3
media. AP1 cells were used for these measurements to
eliminate possible confounding effects due to NHE. As
summarized in Table II, no statistically significant differences in rate of H+ flux were observed in K+ or
NMG+ solutions when compared with Na+ solutions.
|
Table II.
Cationic Dependence of NO3 |
Voltage Sensitivity of the NO3
-induced
Cytosolic Acidification
The DIDS-insensitive rate of NO3
influx into AP1 cells
was 2.66 ± 0.07 mmol/liter/min (Fig. 2). Under comparable experimental conditions, the rate of H+(equivalent)
flux was calculated to be 2.63 ± 0.99 mmol/liter/min (Table III). The apparent stoichiometry of the putative
NO3
-H+ cotransporter derived from these flux rates is
therefore one-to-one. This calculation assumes that all
the stilbene-insensitive NO3
flux is coupled to H+
transport, a premise that has not been validated experimentally. An alternative approach to estimate the stoi-chiometry of the cotransport process is to analyze its
voltage sensitivity. An electroneutral one-to-one exchanger is likely to be voltage insensitive, whereas
changes in voltage are more likely to affect a transporter with unequal stoichiometry.
|
Table III.
Effects of Pharmacological Agents on the Rate of
NO3 |
To gain further insight into the mechanism of NO3
-H+ cotransport, we evaluated its electrical properties in
cells patch-clamped in the whole cell configuration. We
estimated that it would be difficult to measure a current mediated by the transporter, since this was calculated to be as low as 4.2 or 8.4 pA if assuming a stoichiometry of 2:1 or 3:1, respectively. Instead, we assessed whether the NO3
-induced pHi changes would be affected by drastic changes in the membrane potential. A
pipette solution with low buffering capacity (1 mM
MES) was used to maximize the NO3
-induced pHi
changes. A representative pHi measurement in a voltage-clamped cell is shown in Fig. 9. The cell was initially
clamped at
60 mV and superfused with a Cl
-rich solution. Under these conditions, pHi was unaffected by a
sudden depolarization to 0 mV, confirming that CHO
cells have a comparatively low H+(equivalent) conductance
at physiological pHi and at normal resting membrane
potential (Demaurex et al., 1995
). Cytosolic acidification was observed when NO3
replaced Cl
in the bathing solution. The occurrence of an acidification in voltage clamped cells implies that the effect of NO3
on
pHi is not mediated by, and does not require changes
in membrane potential. Moreover, the rate of pHi
change was not affected by sequentially stepping the
membrane potential up from
60 to +40 mV; only the
normal exponential decay was noted. A comparable decay was observed when the order of the voltage changes
was reversed, from depolarized to repolarized (not illustrated). The data in patch clamped cells indicate
that the NO3
-induced cytosolic acidification is voltage
insensitive, consistent with an electrically neutral process. This conclusion is compatible with the tentative
estimates of stoichiometry of one-to-one.
-induced cytosolic acidification. An AP1 cell was voltage clamped in the whole-cell configuration of the patch-clamp technique, using a pipette
filled with low buffer, KCl-rich solution containing BCECF. pHi was
measured microfluorimetrically on the photometric system described in METHODS. Over 5 min were allowed at a holding potential of
60 mV for adequate fluorophore loading and for equilibration of the cytosol with the pipette solution before initiation of the
pH measurements. The cell was initially superfused with KCl solution and subsequently with KNO3 solution, as noted. The holding
voltage was stepped to values ranging from
60 mV to +40 mV, as
indicated. Representative of 4 similar experiments.
Effect of Inhibitors on the NO3
-induced
Cytosolic Acidification
To establish possible analogies with other mammalian
transporters, we tested a variety of compounds known
to inhibit other plasmalemmal ion transport systems.
Ethacrynic acid (Poole and Halestrap, 1993
; Koechel,
1981
; Palfrey and Leung, 1993
), a dichlorophenoxyacetic acid derivative, is a potent alkylating reagent that
has loop diuretic action. It is known to inhibit several
ion carriers, including the Na+/K+/Cl
cotransporter
(Palfrey and Leung, 1993
). NO3
-induced cytosolic
acidification was 67% inhibited by 100 µM ethacrynic acid (Table III). The mean H+(equivalent) flux in ethacrynic
acid treated-cells was 1.01 ± 0.48 mmol/liter cells/min
(n = 4) compared with 3.06 ± 0.43 mmol/ liter cells/min
in paired controls (n = 19). Inhibition by ethacrynic acid was almost complete at 200 µM (not shown).
-Cyano-4-hydroxycinnamate (CHC) inhibits both
the anion exchanger (Simchowitz, 1988
) and the
monocarboxylate transporter (Poole and Halestrap,
1993
) in other cells. CHC (1 mM) inhibited NO3
-
induced cytosolic acidification to 20% of the control
rate (Table III). H+(equivalent) flux in CHC-treated cells
was 0.62 ± 0.49 mmol/liter cells/min (n = 4).
Phloretin, the aglycone of phlorizin, is a reversible,
relatively nonspecific inhibitor of several membrane
transport processes, including urea transport, monocarboxylate transport and Cl
/HCO3
exchange (Wang
et al., 1993
; Melnik et al., 1977
; Chou and Knepper, 1989
). In our experiments, 100 µM phloretin was
found to have no effect on the rate of NO3
-induced cytosolic acidification (Table III).
pCMBS, an organomercurial sulfhydryl reagent, irreversibly inhibits the monocarboxylate transporter (Munzel et al., 1995
) but does not affect the Cl
/HCO3
exchanger (Poole and Halestrap, 1993
; Zhang and Solomon, 1992
). NO3
-induced cytosolic acidification was
unaffected by 250 µM pCMBS (Table III). Similarly,
NO3
-induced cytosolic acidification was not affected
by furosemide (data not shown), a loop diuretic that inhibits several anion transport systems, including the
Cl
/HCO3
exchanger (Cabantchik et al., 1978
), the
monocarboxylate transporter (Poole and Halestrap,
1993
) and the SO42
/OH
exchanger (Schron et al.,
1985
) which is reportedly distinct from the SO42
/Cl