Plant Physiol. (1999) 119: 1115-1124
Light-Induced Changes in Hydrogen, Calcium, Potassium, and
Chloride Ion Fluxes and Concentrations from the Mesophyll and Epidermal
Tissues of Bean Leaves. Understanding the Ionic Basis of Light-Induced
Bioelectrogenesis1
Sergey Shabala* and
Ian Newman
School of Agricultural Science (S.S.), and School of Mathematics
and Physics (I.N.), University of Tasmania, G.P.O. Box 252-54, Hobart,
Tasmania 7001, Australia
 |
ABSTRACT |
Noninvasive, ion-selective vibrating
microelectrodes were used to measure the kinetics of H+,
Ca2+, K+, and Cl
fluxes and the
changes in their concentrations caused by illumination near the
mesophyll and attached epidermis of bean (Vicia faba L.). These flux measurements were related to light-induced changes in
the plasma membrane potential. The influx of Ca2+ was the
main depolarizing agent in electrical responses to light in the
mesophyll. Changes in the net fluxes of H+, K+,
and Cl
occurred only after a significant delay of about 2 min, whereas light-stimulated influx of Ca2+ began within
the time resolution of our measurements (5 s). In the absence of
H+ flux, light caused an initial quick rise of external pH
near the mesophyll and epidermal tissues. In the mesophyll this fast alkalinization was followed by slower, oscillatory pH changes (5-15
min); in the epidermis the external pH increased steadily and reached a
plateau 3 min later. We explain the initial alkalinization of the
medium as a result of CO2 uptake by photosynthesizing
tissue, whereas activation of the plasma membrane H+ pump
occurred 1.5 to 2 min later. The epidermal layer seems to be a
substantial barrier for ion fluxes but not for CO2
diffusion into the leaf.
 |
INTRODUCTION |
The onset of illumination triggers a cascade of electrical events
in thylakoid and PMs of green plant tissues (Vredenberg and Tonk, 1975
;
Fujii et al., 1978
; Hansen et al., 1987
, 1989
, 1993
; Elzenga et al.,
1995
; Johannes et al., 1997
). Enhanced H+
extrusion induced by light may be an important factor promoting leaf
enlargement through an increase in wall extensibility (Linnemeyer et
al., 1990
; Elzenga et al., 1995
). Activation of the
H+ pump by photosynthesis might also be relevant
to phloem loading and the removal of photosynthate from the mesophyll
cells (Marrè et al., 1989). To understand metabolic control at
the whole-plant level it is essential that such physiological
implications of light-induced electrical signaling be taken into
account.
Reports on the ionic basis of electrical responses to light in plants
are as controversial as they are numerous. Conclusions reported from
different species or under different experimental conditions are often
diametrically opposite. The shape of the responses, their magnitude,
and the number of phases depend strongly on the ionic composition
(Elzenga et al., 1995
; Johannes et al., 1997
) and pH (Fujii et al.,
1979
; Kura-Hotta and Enami, 1981
; Prins et al., 1982
; Remis et al.,
1994
) of the medium. The typical scenario is a quick initial
depolarization of the PM potential, followed in 1 to 2 min by a slower
repolarization, which often (but not always) results in the
hyperpolarization of the PM at the end of the transient response, 20 to
40 min after the onset of illumination (Fujii et al.,
1979
; Prins et al., 1980
; Tazawa et al., 1986
; Marrè et al.,
1989; Spalding et al., 1992
; Hansen et al., 1993
; Blom-Zandstra et al.,
1995
, 1997
; Johannes et al., 1997
).
In spite of a large number of experimental studies, mechanisms of
transient membrane potential changes and their ionic bases remain
obscure. Involvement of numerous ion transporters in electrical events
at the PM, including those for H+,
K+, Cl
, and
Ca2+, have been documented (Spalding et al.,
1992
; Blom-Zandstra et al., 1997
; Johannes et al., 1997
). However,
there is no clear answer about which ion is acting as the depolarizing
agent in the initial phases of PM depolarization. Most experiments have been carried out using ion-substitution protocols. So far no direct measurements of specific ion fluxes have been performed in relation to
membrane depolarization by light. In addition, contributions of various
ion transporters to the resulting electrical changes at the PM are very
different for epidermal and mesophyll cells (Elzenga et al., 1995
),
which complicates the problem even more. Direct ion-specific
measurements may provide a breakthrough in this old mystery.
Another question of specific interest is the involvement of the
plasmalemma H+ pump in PM electrical responses.
Proton pumps are central in maintaining the PM in its polarized state
(Spanswick, 1981
; Linnemeyer et al., 1990
). There are numerous reports
that the activity of the H+ pump is increased
after the onset of illumination (Prins et al., 1982
; Tazawa et al.,
1986
; Marrè et al., 1989, and refs. therein; Linnemeyer et al.,
1990
; Okazaki et al., 1994
; Remis et al., 1994
). However, it has also
been observed in many cases that light causes a brief initial
alkalinization of the medium (Atkins and Graham, 1971
; Neuman and
Levine, 1971; Hope et al., 1972
; Brinckmann and Lüttge,
1975; Prins et al., 1982
), not the acidification that would be
produced by the activation of H+-extrusion
pumping. For many years the apparent controversy between these two
groups of observations has remained a submerged rock threatening the
electrophysiological ship.
The reason for this controversy could be that there have been no direct
measurements of net H+ fluxes from plant tissues
caused by light changes. The conclusions presented in the literature
were based on inferring H+ movement from measured
pH changes, or on interpreting PM electrical activity suppressible by
specific inhibitors of ion transport. Because pH changes may not always
be accompanied by H+ transport, we needed a
direct comparative measurement of pH changes and
H+ fluxes caused by light.
In this study we addressed these two specific questions, the ionic
basis of transient depolarization of the PM potential and the apparent
inconsistency between initial alkalinization of the external medium
caused by illumination and light-induced activation of the
H+ pump in the PM. Using the noninvasive
ion-specific microelectrode ion-flux measurement technique, we
determined the kinetics of H+,
Ca2+, K+, and
Cl
fluxes and changes in their concentrations
near bean (Vicia faba) mesophyll and attached epidermis due
to illumination. It appears that the influx of
Ca2+ is the main depolarizing agent in mesophyll
electrical responses to light, whereas Cl
fluxes seem to be one of the major contributors to the subsequent repolarization. High temporal resolution (5 s) allowed us to find a
significant delay between observed pH and H+-flux changes near
the mesophyll tissue. We explain the initial alkalinization of the
medium as a result of CO2 uptake by
photosynthesizing tissue, whereas activation of the PM H+ pump
occurs 1.5 to 2 min later. The epidermal layer seems to be a
substantial barrier for ion fluxes but not for
CO2 diffusion into the leaf.
 |
MATERIALS AND METHODS |
Plant Material
Plants of bean (Vicia faba L. cv Early Long Pod;
Creswell's Seeds, New Norfolk, Australia) were grown from seeds in
0.5-L plastic pots containing a commercially available professional potting mixture (Debco, Tyabb, Australia). Growth conditions were 16 h/8 h light/dark (model M1500-A lighting unit, Thorne, Moonah, Australia; total irradiance = 150 W m
2 at the
leaf level) with temperature ranging from 20°C (dark) to 28°C
(light). Watering was four times per week with tap water. Plants were
used for measurements after 20 d.
Flux Measurements
Fluxes of specific ions were measured generally as described in
our previous papers (Shabala et al., 1997
; Shabala and Newman, 1997
;
Shabala et al., 1998
) using a noninvasive microelectrode ion-flux
measurement system (MIFE, Unitas Consulting, Hobart, Australia;
additional information is available at
http://www.phys.utas.edu.au/physics/biophys). Electrode blanks were
pulled from 1.5-mm borosilicate glass capillaries (GC150-10, Clark
Electromedical Instruments, Pangbourne, UK), dried in the oven at
220°C for 5 h, and silanized with tributylchlorsilane (catalog
no. 90796, Fluka). Cooled microelectrodes were backfilled with 500 mol
m
3 CaCl2 for
Ca2+, 500 mol m
3 KCl for
K+ and Cl
, and 15 mol
m
3 NaCl plus 40 mol m
3
KH2PO4 (adjusted to pH 6.0 using NaOH) for H+. Electrode tips were then
filled with commercially available ion-selective
H+ (95297), Ca2+ (21048),
K+ (60031), and Cl
(24902) cocktails (all from Fluka), and electrodes were calibrated in a
known set of standards. The average slope was 53 to 54 mV/pIon for
monovalent ions and 26 to 27 mV/pCa for Ca2+
electrodes.
The ion-selective electrodes were mounted on an electrode holder
(MMT-5, Narishige, Tokyo, Japan) providing three-dimensional positioning. Plant tissue was placed into the measuring chamber, filled
with solution, and electrodes were positioned in line 50 µm above the
leaf surface with their tips spaced 3 to 4 µm apart. Three different
ions were measured at the same time; in all measurements a
H+ electrode was used as a reference point to
make results comparable. The chamber was placed on a three-way
hydraulic micromanipulator (WR-88, Narashige) driven by a
computer-controlled stepper motor (MO61-CE08, Superior Electric,
Bristol, CT). During the flux measurements, the MIFE computer gently
moved the chamber up and down, providing virtual movement of electrode
tips between two positions above the plant tissue. In this study the
electrodes were moved in a 10-s square-wave cycle between 50 and 90 µm above the leaf surface. The concentration of each ion was
calculated from its electrochemical potential for each position. The
flux of each specific ion was calculated later from the measurements of
the difference in the electrochemical potential between these positions
(Shabala et al., 1997
). During analysis the 1st s of each half-cycle
was ignored (time required for both the movement and the
electrochemical settling of the electrodes).
Experimental Procedure
We used expanding leaves in positions 3 to 6 on the stem (leaf age
7-10 d) in the experiments. The leaf was excised with a razor
blade 4 to 5 h before measurements were taken. If fluxes were to
be measured near the intact epidermal tissue, we cut out leaf segments
of 5 × 8 mm from the apical part of the leaf, avoiding major
veins. For mesophyll measurements we removed the epidermal tissue
before cutting the segment. To do this, we first cut leaf strips 5 mm
wide and peeled off the lower epidermal layer using fine forceps. Cut
leaf or mesophyll segments floated peeled-side or abaxial-surface down
on the experimental solution under light from a fiber-optic light
source (40 W m
2; EK1, Euromex, Sydney,
Australia). No wounding effects were noticeable when fluxes were
measured 4 to 5 h after segments were cut (data not shown). After
3 to 3.5 h of floating, the cut segment was mounted and
transferred into the measuring chamber. During the measurements, local
pH values near the tissue varied slightly in the range of 5.3 to 5.5 depending on the magnitude and direction of H+
fluxes.
We used a Perspex holder that provided gentle bending of the plant
tissue to mount the cut leaf or mesophyll segment. This arrangement
allowed a clear view for electrode positioning compared with planar
leaf arrangement. As the 5- to 6-mm radius of the leaf bending was
close to that naturally occurring, it should not have affected the cell
ion exchange. A few control experiments with plane-mounted segments
showed the same steady fluxes in the dark (data not shown). The holder
was installed in a measuring chamber with a volume of 10 mL. The
chamber was filled with solution and fixed on the hydraulic
micromanipulator under the microscope. Dim-green microscope light of
about 12 W m
2 was used as the background
illumination tangential to the leaf surface. Experiments started 1 h after plants adapted to the dim light.
Our preliminary studies showed that ion fluxes can vary significantly
with position over a range of several millimeters, even for apparently
uniform mesophyll tissue in steady conditions (S. Shabala and I. Newman, unpublished data). To minimize the variability of flux
measurements, we chose to perform experiments in the regions where
initial flux values (dark level) were close to the average (near zero
for H+ flux in control). After a suitable spot on
the mesophyll tissue was selected, we measured ion fluxes for about 5 min (microscope light only) before the projector light was turned on.
We used a fiber-optic projector (Intralux 4000, Volpi AG, Urdorf,
Switzerland) providing 60 W m
2 illumination.
Although we used dark plastic tubes covering the chlorided wire region
of the electrode capillaries in most experiments, there was no special
need for electrode shielding from direct light. Flux measurements
continued for 40 to 60 min after the onset of illumination. The light
was then turned off, the measuring chamber removed, and a new leaf or
mesophyll sample was installed.
All experiments were performed in unbuffered solution containing 0.5 mol m
3 CaCl2 plus 1 mol
m
3 KCl, pH 5.4, at room temperature
(22°C-24°C). Arif et al. (1995)
have explained the reasons for not
using buffers in the bath. Heat emission from the light source was
negligible.
Membrane Potential Measurements
We measured the electrical potential difference across the PM in
the standard way, by impaling the cell with a microelectrode filled
with 500 mol m
3 KCl. Impalements were made
using the same hydraulically driven, three-dimensional manipulator that
was used for flux measurements. Because the
membrane-potential-measuring electrode and the ion-selective electrodes
were mounted in the same holder, we were not able to move the
electrodes up and down to measure fluxes of ions while measuring
membrane potential. Therefore, we measured concentrations only at a
position about 60 µm above the leaf tissue.
For both flux and membrane-potential measurements, we used the same
reference electrode. A chlorided silver wire was inserted into a thin
plastic tube or glass microelectrode with a broken tip containing 1000 mol m
3 KCl in 2% agar. Because it was at least
6 cm from the measured leaf sample, the diffusion of
K+ ions from it to the leaf was negligible. We
based this conclusion on the absence of any measurable drift in
K+ concentration near the tissue in steady
conditions.
Statistics
We obtained most of the data shown in the figures from five to
eight segments taken from five or six individual plants. Because a
simple averaging could mask important features such as oscillations in
plant transient responses, we have in some cases shown the records for
several individual plants in each variant (see Fig. 4). Finally, we
felt that the simple averaging under genetic or physiological
variability could also mask the time delay between changes in PM
potential and changes in ion flux or concentrations. For this reason,
the data presented in Figures 1 and 2 are for experiments taken as
typical of this set of experimental conditions. The qualitative
character of these data was reproduced for leaf segments obtained from
several (four or five) individual leaves. Statistical information on
the magnitude and phase duration of such responses appears in the text.

View larger version (38K):
[in this window]
[in a new window]
| Figure 4.
Light-induced changes in pHo near the
mesophyll (A) and the attached epidermis (B). Five individual traces
for each variant are shown. Traces 1 to 5 were used for calculating the
means shown in Figure 3A.
|
|

View larger version (49K):
[in this window]
[in a new window]
| Figure 1.
Transient changes in mesophyll cell membrane
potential ( ) and pHo ( ), and
[Ca2+]o ( ),
[K+]o ( ), and
[Cl ]o ( ) caused by transition from dark
to light (at 2 min). The data shown are from two typical individual
plants (A and B). A, Changes in pHo and
[Ca2+]o measured with the membrane potential.
B, Changes in [K+]o and
[Cl ]o measured with the membrane potential.
Each point is the average of measurements over a 5-s interval. Both
[K+]o and [Cl ]o
started to decrease only after the PM was significantly depolarized,
with a delay of about 50 s after illumination.
|
|

View larger version (49K):
[in this window]
[in a new window]
| Figure 2.
Light-induced changes in net fluxes (inward
positive) of H+ ( ), K+ ( ), and
Cl ( ), and pHo ( ) near the mesophyll
tissue measured simultaneously for a typical bean plant. Each point is
the average of measurements over a 20-s interval. A, pHo
and H+ flux; B, K+ and Cl flux. A
significant delay of about 2 min can be observed for fluxes of all
three ions, although the pH change occurred immediately after the light
was turned on at 5 min.
|
|
 |
RESULTS |
Light-Induced Transients in Mesophyll Membrane Potential and
Solution Ion Concentration
Transition from dark to light triggered a multiphase, transient
change of the membrane potential in the mesophyll cells of bean leaves
(Fig. 1). The resting potential of the PM
was slightly more negative than
100 mV in the dark. The onset of
illumination caused a rapid (45-50 s) depolarization of 15 to 20 mV,
which was followed by a slower repolarization lasting 2 to 2.5 min. Afterward, the membrane potential fluctuated in a complex way (individually for each plant), showing several oscillatory cycles of 5 to 15 min each. Often (but not always) there was a significant hyperpolarization of up to
20 mV compared with the dark level 20 to 30 min after the light was turned on.
Changes in membrane potential were always accompanied by changes in
[H+]o,
[Ca2+]o,
[K+]o, and
[Cl
]o near the
mesophyll tissue. Figure 1 shows examples of individual records from
two typical plants. For one of them (Fig. 1A), changes in
pHo and
[Ca2+]o were measured
together with membrane potential; for the second plant, transient
changes in [K+]o and
[Cl
]o were recorded
(Fig. 1B).
Although the time course of membrane-potential transients was
qualitatively similar for all plants, concentration changes for the
different ions were different. pHo and
[Ca2+]o changes started
immediately (within the 5-s time resolution) after the light was turned
on (Fig. 1A). The onset of illumination caused an initial quick rise of
the pHo near the mesophyll tissue; this fast
alkalinization was followed by slower, transient
pHo changes. Oscillations of 5 to 15 min were
also evident (see Fig. 4A) for most plants. As in the case of membrane
potential, the number of oscillatory cycles and their durations varied
between individual plants. However, for each plant the final
pHo value in light was more alkaline by 0.16 ± 0.02 (n = 7) than it was before the onset of
illumination.
Changes in [Ca2+]o
generally were of similar form as changes in
[H+]o. There was an
immediate drop in the
[Ca2+]o of about 25 to 30 µM, followed by slow recovery in 1.5 to 2 min (Fig. 1).
Minimum [Ca2+]o always
occurred at the same time as maximum alkalinization of the adjacent
medium. Another regular feature of light-induced transients was a small
but significant delay between the first peak in membrane potential and
the pHo changes. For each plant, the first
extreme in pHo and
[Ca2+]o transients
occurred 25 to 30 s after the membrane-potential maximum.
However, unlike the pHo and
[Ca2+]o changes for the
similar membrane potential transient, noticeable changes in
[K+]o and
[Cl
]o occurred only
after a significant delay (Fig. 1B). Both
[K+]o and
[Cl
]o started to
decrease only when membrane potential reached its peak of
depolarization. Although between-plant variability in transient
[K+]o and
[Cl
]o responses was
much larger than that for pHo and
[Ca2+]o changes, it is
clear that K+ and Cl
are
not required as depolarizing agents for the PM in bean mesophyll cells.
Transient Ion-Flux Changes in the Mesophyll
In other experiments the net fluxes of H+,
Ca2+, K+, and
Cl
were measured in response to illumination.
Figure 2 shows a typical example from one
individual plant, where net fluxes of H+,
K+, and Cl
were measured
simultaneously in the same experiment. As membrane-potential measurements were impossible with the moving electrode probe, transient
pHo changes have been used as a reference point
instead of membrane potential. These typical pHo
changes appear in Figure 2A and make these results comparable with
those reported in Figure 1.
The data presented in Figure 2 confirm our previous findings. Light
caused a significant influx of both K+ and
Cl
(which is in good agreement with the
decrease in [K+]o and
[Cl
]o shown in Fig. 1B), but only after a
significant delay of 2 to 3 min (Fig. 2B). The most surprising result
was that, in spite of the significant initial increase in
pHo near the mesophyll tissue, no significant
change in net H+ flux was observed during the
first 2 min after light application (Fig. 2A). The
H+ flux started to change only after the
pHo value had reached its first peak at 1.5 min
and had started to decrease.
We studied this last observation in more detail in the next
experiments. Figure 3A shows average
pHo and H+ flux changes
measured near the mesophyll tissues of eight individual plants after
the onset of illumination. As a result of the light-induced transient,
the average H+ flux decreased from a slightly
positive value of 1.7 ± 5.9 nmol m
2
s
1 (net influx) down to
20 nmol
m
2 s
1. The
H+ flux reached its minimum value 7 min after the
light was turned on, and slowly returned to its dark level (3.6 ± 4.3 nmol m
2 s
1) in the next 15 to 20 min.
The delay (
) between the start of the pHo rise and the
beginning of H+-flux change (see Fig. 3A) was 100 ± 13 s (n = 8). Afterward, pHo
changes were qualitatively consistent with those expected from the
measured H+ flux.

View larger version (42K):
[in this window]
[in a new window]
| Figure 3.
Average changes in ion fluxes (solid symbols) and
concentrations (open symbols) for five plants. A, pHo and
H+ flux; B, [Ca2+]o and
Ca2+ flux. Means are over 20-s intervals and the
SE for fluxes is shown in Figure 7. The SE for
concentration = 5.7 µM; the SE for pH
changes = 0.03.
|
|
There was no such delay between changes in Ca2+
flux and its concentration (Fig. 3B). Light application immediately
initiated Ca2+ uptake by the mesophyll. This
resulted in decreased
[Ca2+]o close to the
tissue (Fig. 3B). The Ca2+ influx lasted only 2 to 2.5 min, and was followed by transient efflux over the next 7 to 8 min. Ca+ fluxes stabilized at a slightly positive level
(9.7 ± 5.6 nmol m
2
s
1) 15 to 20 min after the onset of
illumination. Changes in the Ca2+ flux were
always qualitatively consistent with changes in
[Ca2+]o.
Effect of Epidermis on pHo and Ion Fluxes
When we measured pHo changes near the intact
leaf segment (with epidermis present), the qualitative course of
transient responses was very different from that measured near the
isolated mesophyll (Fig. 4). After the
onset of illumination, the pHo for the epidermis rose steadily for a few minutes before reaching a plateau (Fig. 4B).
Afterward, the pHo remained constant, without the
significant drop and subsequent fluctuations for the
pHo measured near the mesophyll. The magnitude of
the transient alkalinization was similar for both tissues (
pH
0.15 ± 0.02). The pHo saturation near the epidermis occurred later than the first peak in mesophyll pH changes (2.8 ± 0.25 and 1.7 ± 0.15 min, respectively). There was
also a slight delay of 30 ± 5 s (n = 6)
between the onset of illumination and the beginning of
pHo changes from the epidermis. We observed no
such delay for mesophyll tissue.
Even more pronounced was the difference between ion fluxes from
mesophyll and epidermis (Fig. 5). Both
H+ and Ca2+ fluxes from
epidermis were negligible, and, when the light was turned on, there was
a barely noticeable increase in H+ influx
measured near the epidermis. Changes in Ca2+
fluxes were less than the level of noise in the system.

View larger version (46K):
[in this window]
[in a new window]
| Figure 5.
Fluxes of H+ (A) and Ca2+
(B) induced by light near the mesophyll (solid symbols) and attached
epidermis (open symbols). Average data from five plants in each variant
are shown. Bars = ±SE.
|
|
 |
DISCUSSION |
The Ionic Basis of Electrical Events at the PM: Is Ca2+
a Depolarizing Agent?
In general, changes in membrane potential reflect underlying
changes in the conductance of ion channels and the activity of pumps.
For this reason, the ionic basis of the transient depolarization of the
PM seems to be a foundation for our understanding of light-induced bioelectrogenesis in plants. The involvement of all major ions, in
particular H+, K+,
Ca2+, and Cl
, has been
suggested previously by numerous researchers; however, the reported
data are controversial.
Prins et al. (1982)
reported a pause of approximately 5 min between the
reduction of [K+]o and the pHo rise near the
lower side of Potamogeton lucens. According to Fujii et al.
(1978)
, K+ and Cl
ions in
solution were not essential for light-induced membrane-potential changes, whereas such membrane responses were completely inhibited by
the absence of Ca2+. Johannes et al. (1997)
supported this point of view, showing that K+
influx was not crucial for membrane-potential depolarization, because
K+ could be removed from the bathing medium without
affecting the electrical response of the PM. According to these and
other findings, the crucial ion for PM depolarization is Ca2+;
when Ca2+ was omitted from the solution, membrane-potential
transients were abolished (Ermolayeva et al., 1996
; Johannes et al.,
1997
).
Remis et al. (1994)
challenged this point of view by showing that
transient changes in the PM depend strongly on the presence of
K+ in the bathing medium. When
K+ was present in the medium, light induced the
extrusion of H+ and the uptake of
K+ by Elodea densa, which caused
membrane hyperpolarization, not depolarization. However, in the absence
of K+, the PM was initially depolarized by the
onset of illumination (Marrè et al., 1989).
Similar controversy exists for other ions. Conductance changes for
Cl
have been suggested by Spalding et al.
(1992)
, and were supported later by Blom-Zandstra et al. (1997)
as one
of the possibilities for PM depolarization. In their experiments in
pea, Elzenga et al. (1995)
found that in mesophyll cells the transient
depolarization depended on the [Cl
]o and was
unaffected by changes in the [Ca2+]o or
[K+]o. In contrast, when isolated epidermal tissue
was measured, the membrane depolarization was much smaller and was
enhanced by increasing the [Ca2+]o. They
concluded that the ionic basis of this depolarization differs
qualitatively between the epidermis and the mesophyll, and suggested
that light-induced depolarization of the PM in pea mesophyll seems to
be mediated by an increased efflux of Cl
, whereas
membrane-potential changes in the epidermis reflect changes in the
fluxes of Ca2+ and the activity of an
ATPase-dependent H+-pump in the PM (Elzenga et
al., 1995
).
The major reason for such controversy is that no direct flux
measurements have been performed so far (to our knowledge) to elucidate
the ionic basis of cell electrical responses to light. Because of the
numerous feedback loops and interaction between ion transporters,
reliable selective inhibition or enhancement of one of them is not
feasible. Furthermore, even when the experimental solution is initially
lacking one particular ion, it does not necessarily mean that there
will be no flux of that ion from the measured tissue. We have
previously observed that in a short time many ions
(K+ in particular) can be released from the cell
into the bath in concentrations large enough to produce flux able to
change the membrane potential by 20 to 30 mV in 1 min (S. Shabala and
I. Newman, unpublished data).
To our knowledge, the only reported data on light-induced flux
measurements were given by Johannes et al. (1997)
, who linked patch-clamp measurements on caulomal filaments of the moss
Physcomitrella patens with measurements of ion fluxes
induced by red light. According to their findings,
Ca2+, K+, and
anion-permeable channels were open at the peak of light-induced membrane depolarization. Ca2+ influx and anion
efflux coincided with the depolarizing phase, whereas
K+ influx occurred only for the first 30 s.
Dramatic transient K+ efflux associated with PM
repolarization took place later (unfortunately, the flux data are only
mentioned but not shown in that paper). In addition, Johannes et al.
(1997)
used absorption spectrometry applied to samples taken discretely
at 30-s or 1-min intervals for their flux measurements, and, because
the peak of membrane depolarization occurred within 2 to 15 s,
this rate of sampling was clearly inadequate and made their conclusions
on flux kinetics questionable.
Our study is the first to our knowledge to report direct measurements
of light-induced ion fluxes near green plant tissue. The peak of the
depolarization occurred at about 50 s, and the depolarization
process was clearly biphasic, with a typical shoulder at about 15 s (Fig. 1). All of this is in good agreement with membrane-potential
data reported previously (Spalding et al., 1992
; Elzenga et al., 1995
).
There were immediate changes in pHo and
[Ca2+]o after the light
was turned on (Fig. 1A). However, the immediate
pHo changes were not accompanied by any
significant change in net H+ flux near the tissue
(Fig. 2A). The statistically significant delay of 100 ± 13 s
(Fig. 3A) before H+ flux changed suggests that
activation of the PM proton pump began only after the PM was
depolarized.
Activities of K+ and Cl
transporters were also affected much later, when membrane potential
reached its peak of depolarization (Fig. 1B). These data are supported
by direct measurements of K+ and
Cl
fluxes near the mesophyll tissue (Fig. 2B).
We observed a delay of up to 2 min between the onset of illumination
and the beginning of changes in K+ and
Cl
fluxes. Although in some plants this delay
was not very pronounced (largely due to extremely high variability in
initial K+ fluxes), there is no doubt that
neither K+ nor Cl
flux is
required as a depolarizing agent in the PM of bean mesophyll cells.
Among the four different ions that we measured, the most likely
candidate for membrane depolarization is Ca2+.
There was an increase in the net Ca2+ uptake
immediately after the light was turned on (within the 5-s time
resolution) (Figs. 1A and 3B). If we assume a membrane capacitance of 2 µF cm
2, a Ca2+ influx
as small as 0.05 nmol m
2
s
1 would be enough to depolarize the membrane
by 25 mV in 50 s (the typical rate of depolarization shown in Fig.
1). In our experiments we observed a Ca2+ influx
of approximately 10 nmol m
2
s
1 (Fig. 5B) near the mesophyll tissue within
the first 2 min after the onset of illumination, which is 2 orders of
magnitude greater than that needed to produce the observed
depolarization of the PM. Thus, our data support the work of others in
considering Ca2+ to be a potent depolarizing
agent in the light-induced electrical responses at the PM (Weisenseel
and Ruppert, 1977
; Takagi and Nagai, 1988
; Spalding and Cosgrove, 1992
;
Elzenga et al., 1995
).
To explain our data, we suggest a scenario similar to the one proposed
by Johannes et al. (1997)
for phytochrome-mediated, red-light-induced
membrane-potential transients in P. patens. A
light-induced Ca2+ influx of about 10 nmol
m
2 s
1 would be expected
to cause a significant increase in
[Ca2+]cyt. Increased
[Ca2+]cyt can also
stimulate H+-ATPase activity, resulting in an
increased H+ efflux (Elzenga et al., 1995
). It
may take a while before
[Ca2+]cyt is elevated
high enough to make this activation possible, and this could be the
reason for the approximately 2-min delay between light application and
the beginning of the H+ efflux observed in our
experiments (Fig. 3A).
Another important observation is the initial increase in the net
Cl
influx (Fig. 2B) (not an efflux, as was
postulated by Elzenga et al. [1995]). Because inward Cl
movement in higher-plant cells is an active process mediated by a
Cl
pump (Felle, 1994
), we suggest that elevated
[Ca2+]cyt activates the Cl
pump in a manner similar to that suggested for the
H+ pump. This also provides a reason for the
2-min delay observed for Cl
-flux activation by light.
Together with the H+ efflux, this increased
Cl
influx causes PM repolarization. Therefore,
our data rule out Cl
participation in the PM
depolarization and indicate its involvement in the repolarization
process. K+ seems to function as the equilibrium
ion, moving passively to compensate for light-induced charge movement
of Cl
or H+, which is
consistent with other reports (Prins et al., 1982
; Staal et al., 1994
).
It is known that Ca2+ can directly activate a
Ca2+-dependent K+ channel
in some species (Elzenga and Van Volkenburgh, 1993
; Johannes et al.,
1997
). The subsequent membrane repolarization may trigger Ca2+-permeable channels to close, leading to a
decrease in the [Ca2+]cyt
and to a change in the net Ca2+ flux from
influx to efflux (Fig. 3B).
Apparent Inconsistency between Light-Induced Changes in
pHo and H+ Flux
If the initial alkalinization of the bath solution near the
mesophyll induced by light that we (Figs. 1, 2A, and 4A) and others (Atkins and Graham, 1971
; Neuman and Levine, 1971; Hope et al., 1972
;
Prins et al., 1982
) have observed is due to modified activity of
H+ transporters, it could be achieved by either a
decrease in the active H+ extrusion or an
increase in the activity of passive H+ inward
transporters. In each case, we would expect an increased H+ influx. But in our experiments, switching on
the light induced significant H+ efflux, which
occurred after a distinct time delay (nearly 2 min after
pHo changes started; see Fig. 3A). Alkalinization
of similar magnitude (Fig. 4B) was also evident near the attached epidermal tissue, where H+ fluxes were nearly
zero (Fig. 5A).
This apparent inconsistency cannot be explained by a methodological
fault in the flux measurements obtained by using the MIFE technique.
When measured at the same time as H+, changes in
Ca2+ flux and
[Ca2+]o were in good
agreement with each other and showed no delay after light onset (Fig.
3B). We also ruled out the effect of light on the measuring electrodes,
because there was no pHo change when the
electrodes were far away from the tissue (data not shown). Therefore,
this apparent inconsistency has a biological origin and means that, in
spite of the alkalinization of the medium, there is no net
H+ electrochemical gradient near the leaf surface
in the first 100 s after the dark-to-light transition.
We believe that the initial alkalinization of the medium near the leaf
tissue in the absence of net H+ fluxes observed
in bean is a result of quick CO2 uptake by
photosynthesizing tissue after the onset of illumination.
CO2 dissolved from the atmosphere is normally
present in solution (Lucas and Berry, 1985
; Arif et al., 1995
; Raven,
1997
). Following 1 h of dark adaptation, the amount of CO2
was expected to be significant. In solution, dissolved CO2
reacts with water to form HCO3
:
|
(1)
|
The combined pK of these reactions is 6.3 (Neumann and Levine,
1971
), which is above the pH of our experimental solution (5.3-5.5),
shifting the equilibrium toward CO2 formation.
When the light is turned on, the uptake of CO2 by
photosynthesizing cells would cause a decrease in the concentration of
H2CO3, which would cause an
association of H+ with
HCO3
, resulting in
H+ leaving the medium. If the
CO2 flux is much faster than the
H+ flux through the medium, there will be an
increase in medium pH with a net H+ flux near zero. This is
what we observed.
This explanation is in good agreement with reports that the direction
of light-induced pH changes is strongly dependent on the pH of the
external medium. Illumination of a Cyanidium caldarium cell
suspension caused a rapid alkalinization of the medium at pH 7.0, whereas a slower acidification occurred at pH 4.0 in the light
(Kura-Hotta and Enami, 1981
). Light-induced transient acidification of
the medium measured at pH 1.0 to 3.0 turned into a light-induced alkalinization in the range of pH 5.0 to 7.0 for the green alga Dunaliella acidophila (Remis et al., 1994
).
We also found evidence supporting this explanation when we pretreated
plants for 3 h at both pH 4.0 and pH 7.0 (data not shown). Changing the bathing solution to be more alkaline is known to shift the
equilibrium between CO2 and
HCO3
(see Eq. 1) toward
HCO3
formation (Yin et al.,
1996
). Therefore, one would expect
HCO3
-induced
pHo changes of the bath solution to be more
significant. In our experiments, pHo measured at
60 µm from the tissue increased by up to 0.63 ± 0.03 units
(compared with 0.15 ± 0.02 for the control at pH 5.4) in less
than 2 min after the light was turned on. On the other hand, a shift
into the more acidic region (pH 4.0) was expected to reduce
HCO3
formation and inhibit the
rapid, light-induced pH rise observed in our experiments. In such
experiments we found not only that the initial alkalinization was
completely suppressed, but that even the barely noticeable
alkalinization of the external solution took place 5 min after the
onset of illumination, when activity of the H+
pump was expected to start decreasing (data not shown).
Both CO2 and
HCO3
can be used by plants
during photosynthesis (Prins et al., 1982
; Lucas and Berry, 1985
;
Raven, 1997
). It seems reasonable to assume, however, that an efficient
mechanism of HCO3
transport
through the PM would be more appropriate for aquatic than for
terrestrial plant tissue. Most experiments with light-induced pH
changes have used aquatic plant species. However, even for some
cyanobacteria and microalgae, CO2 diffusion was
preferred to HCO3
uptake
(Lucas and Berry, 1985
, and refs. therein). Some aquatic organisms can
utilize only CO2 and not HCO3
(Prins et
al., 1982
, and refs. therein). We argue that CO2 transport is appropriate for the mesophyll tissues of terrestrial plants, in
which atmospheric CO2 is the normal source of inorganic
carbon.
Prins et al. (1980)
reported an immediate decrease in the
CO2 concentration after the onset of illumination
for some aquatic angiosperms that use CO2 as
their source of inorganic carbon for photosynthesis. The present study
provides evidence that a similar mechanism exists in the
mesophyll tissues of terrestrial plants. According to Hansen et
al. (1993)
, CO2 reaches the photosynthetic apparatus quite rapidly, within a few seconds. This can explain the
absence of a detectable delay in pHo rise close
to the tissue as a result of the dark-to-light transition in our
experiments.
Earlier we suggested that the nearly 2-min delay between light
application and the beginning of H+ efflux
observed in our experiments could be explained as the time required to
elevate [Ca2+]cyt to a
level that can stimulate H+-ATPase activity. This
delay may also be mediated by some other metabolic process involved in
the light signal transduction to the PM ATPase. Linnemeyer et al.
(1990)
discussed at least four different mechanisms for this process,
and there is clearly a need for more experiments in this direction. It
has been argued that light activation of H+
uptake from the stroma to the thylakoid lumen should result in alkalinization of the cytosol (Hansen et al., 1987
; Linnemeyer et al.,
1990
; Heber et al., 1994
; Okazaki et al., 1994
; Yin et al., 1996
).
According to the findings of Linnemeyer et al. (1990)
, this shift in
cytosolic pH from neutral to more alkaline should result in a
significant decrease in PM ATPase activity (the optimal pH for which is
close to 6.5 for bean mesophyll cells). Therefore, we can rule out the
direct control of PM ATPase activity by cytosolic pH as the sole factor
regulating the activity of the H+ pump. More
experiments are required to clarify this issue.
The subsequent decrease in H+ efflux 7 min after
the onset of illumination (Fig. 3A) could reflect the feedback
mechanism of cytoplasmic pH homeostasis of the living cell. Its details
are unknown but may include slowing down the activity of the
H+ pump via a substrate-depletion effect (Hansen
et al., 1987
). Participation of other ion-transport systems should also
be considered (Marrè et al., 1989; Blom-Zandstra et al., 1997
).
Effect of the Epidermis
The epidermal layer seemed to be an effective barrier for ion
fluxes in our experiments (Fig. 5). Only a slight, light-induced H+ influx was discernible outside the epidermis
(Fig. 5A), and no changes in Ca2+ flux could be
seen (Fig. 5 B). At the same time there was a significant initial
alkalinization of the medium near the epidermis (Fig. 4B), of about the
same magnitude as that observed near the isolated mesophyll tissue
(
pH 0.15 ± 0.02). Unlike the classical multiphase transients
from the mesophyll, however, the pHo near the
attached epidermis rose steadily before reaching its saturation level
about 3 min after the light application.
In spite of earlier reports on the lack of light-induced changes of the
membrane potential in epidermal tissues (Lüttge and Pallaghy,
1969
), it seems to be accepted now that chlorophyll-deficient tissues
also exhibit electrical changes in response to light. Fujii et al.
(1978)
and Johannes et al. (1997)
have also reported phytochrome-mediated, light-induced membrane-potential changes. Mechanisms of the light-induced depolarization in mesophyll and epidermis seem to be very different (Elzenga et al., 1995
).
Although we also observed membrane-potential changes from epidermal
cells in our experiments (data not shown), we measured the fluxes of
H+ and Ca2+ at nearly zero
levels outside the epidermis (Fig. 5). The epidermal layer (with its
cuticule present) was an effective barrier for ion fluxes but not for
CO2 diffusion into the leaf. Further experiments should take this point into account. Working on the isolated epidermis, an alternative method could measure fluxes from the inside of the
strip, where the cutinized layer is absent.
 |
conclusion |
The first mention of plant bioelectric responses to light appeared
in a study over 100 years ago (Haake, 1892
), and hundreds of papers
have been published on this subject since that time. Having been
obtained from different plant materials and using different
experimental conditions and techniques, these results are often quite
contradictory. The interaction and interdependence of the numerous ion
transporters are far from well understood. Recent publications on
whole-cell, patch-clamp measurements from plant protoplasts have
revealed the advantages of that technique in studying the mechanisms of
ion-channel responses to light variations (Blom-Zandstra et al., 1995
,
1997
; Johannes et al., 1997
). In this paper we have shown the value of
noninvasive, specific ion-flux measurements in addressing the same
problem. A combination of the two techniques may be ideal in casting
more light on this old and mysterious problem of the mechanisms of
light-induced plant bioelectrogenesis.
 |
FOOTNOTES |
1
This work was supported by an Australian Research
Council grant to I.N.
*
Corresponding author; e-mail sergey.shabala{at}utas.edu.au; fax
61-3-6226-2642.
Received June 26, 1998;
accepted December 4, 1998.
 |
ABBREVIATIONS |
Abbreviations:
[Ca2+]cyt, cytosolic
free Ca2+ concentration.
[XX]o, external
concentration.
pHo, external pH.
PM, plasma membrane.
 |
ACKNOWLEDGMENTS |
We are grateful to Dr. Bruce Scott for his helpful discussion of
this work. We also thank Mrs. Svetlana Shabala for her technical assistance in the preparation of the manuscript.
 |
LITERATURE CITED |
Arif I,
Newman IA,
Keenlyside N
(1995)
Proton flux measurements from tissues in buffered solution.
Plant Cell Environ
18:
1319-1324
[CrossRef]
Atkins CA,
Graham D
(1971)
Light-induced pH changes by cells of Chlamydomonas reinhardii: dependence on CO2 uptake.
Biochim Biophys Acta
226:
481-485
[Medline]
Blom-Zandstra M,
Koot HTM,
van Hattum J,
Vogelzang SA
(1995)
Isolation of protoplasts for patch-clamp experiments: an improved method requiring minimal amounts of adult leaf or root tissue from monocotyledonous or dicotyledonous plants.
Protoplasma
185:
1-6
Blom-Zandstra M,
Koot HTM,
van Hattum J,
Vogelzang SA
(1997)
Transient light-induced changes in ion channel and proton pump activities in the plasma membrane of tobacco mesophyll protoplasts.
J Exp Bot
48:
1623-1630
Elzenga JTM,
Prins HBA,
Van Volkenburgh E
(1995)
Light-induced membrane potential changes of epidermal and mesophyll cells in growing leaves of Pisum sativum.
Planta
197:
127-134
[ISI]
Elzenga JTM,
Van Volkenburgh E
(1993)
Ion channels in the plasma membrane of epidermal and mesophyll cells of growing pea leaves.
Plant Physiol
102:
S106
Ermolayeva E,
Hohmeyer H,
Johannes E,
Sanders D
(1996)
Calcium-dependent membrane depolarization activated by phytochrome in the moss Physcomitrella patens.
Planta
199:
352-358
[ISI]
Felle HH
(1994)
The H+/Cl
symporter in root-hair cells of Sinapis alba.
Plant Physiol
106:
1131-1136
[Abstract]
Fujii S,
Shimmen T,
Tazawa M
(1978)
Light-induced changes in membrane potential in Spirogyra.
Plant Cell Physiol
19:
573-590
[Abstract/Free Full Text]
Fujii S,
Shimmen T,
Tazawa M
(1979)
Effect of intracellular pH on the light-induced potential change and electrogenic activity in tonoplast-free cells of Chara australis.
Plant Cell Physiol
20:
1315-1328
[Abstract/Free Full Text]
Haake O
(1892)
Über die ursachen electrischer ströme in pflanzen.
Flora
75:
455-487
Hansen U-P,
Dau H,
Vanselow KH,
Fisahn J,
Stein S,
Kolbowski J
(1989)
Thylakoid and plasma fluxes.
In
J Dainty,
MI DeMichelis,
E Marrè,
F Rasa-Caldogno,
eds, Plant Membrane Transport: The Current Position.
Elsevier, Amsterdam, pp 345-351
Hansen U-P,
Kolbowski J,
Dau H
(1987)
Relationship between photosynthesis and plasmalemma transport.
J Exp Bot
38:
1965-1981
[Abstract/Free Full Text]
Hansen U-P,
Moldaenke C,
Tabrizi H,
Ramm D
(1993)
The effect of transthylakoid proton uptake on cytosolic pH and the imbalance of ATP and NADPH/H+ production as measured by CO2- and light-induced depolarization of the plasmalemma.
Plant Cell Physiol
34:
681-695
[Abstract/Free Full Text]
Heber U,
Wagner U,
Kaiser W,
Neimanis S,
Bailey K,
Walker D
(1994)
Fast cytoplasmic pH regulation in acid-stressed leaves.
Plant Cell Physiol
35:
479-488
[Abstract/Free Full Text]
Hope AB,
Lüttge U,
Ball E
(1972)
Photosynthesis and apparent proton fluxes in Elodea canadensis.
Z Pflanzenphysiol
68:
63-72
Johannes E,
Ermolayeva E,
Sanders D
(1997)
Red light-induced membrane potential transients in the moss Physcomitrella patens: ion channel interaction in phytochrome signalling.
J Exp Bot
48:
599-608
Kura-Hotta M,
Enami I
(1981)
Light-induced H+ efflux from intact cells of Cyanidium caldarium.
Plant Cell Physiol
22:
1175-1183
[Abstract/Free Full Text]
Linnemeyer PA,
Van Volkenburgh E,
Cleland RE
(1990)
Characterization and effect of light on the plasma membrane H+-ATPase of bean leaves.
Plant Physiol
94:
1671-1676
[Abstract/Free Full Text]
Lucas WJ,
Berry JA
(1985)
Inorganic carbon transport in aquatic photosynthetic organisms.
Physiol Plant
65:
539-543
Lüttge U,
Pallaghy CK
(1969)
Light triggered transient changes of membrane potentials in green cells in relation to photosynthetic electron transport.
Z Pflanzenphysiol
61:
58-67
Marre MT,
Albergoni FG,
Moroni A,
Marre E
(1989)
Light-induced activation of electrogenic H+ extrusion and K+ uptake in Elodea densa depends on photosynthesis and is mediated by the plasma membrane H+-ATPase.
J Exp Bot
40:
343-352
[Abstract/Free Full Text]
Neumann J,
Levine RP
(1971)
Reversible pH changes in cells of Chlamydomonas reinhardtii resulting from CO2 fixation in the light and its evolution in the dark.
Plant Physiol
47:
700-704
[Abstract/Free Full Text]
Okazaki Y,
Tazawa M,
Iwasaki N
(1994)
Light-induced changes in cytosolic pH in leaf cells of Egeria densa: measurements with pH-sensitive microelectrodes.
Plant Cell Physiol
35:
943-950
[Abstract/Free Full Text]
Prins HBA,
Harper JR,
Higinbotham N
(1980)
Membrane potentials of Vallisneria leaf cells and their relation to photosynthesis.
Plant Physiol
65:
1-5
[Abstract/Free Full Text]
Prins HBA,
Snel JFH,
Zanstra PE,
Helder RJ
(1982)
The mechanism of bicarbonate assimilation by the polar leaves of Potamogeton and Elodea: CO2 concentrations at the leaf surface.
Plant Cell Environ
5:
207-214
Raven JA
(1997)
CO2-concentrating mechanisms: a direct role for the thylakoid lumen acidification?
Plant Cell Environ
20:
147-154
Remis D,
Treffny B,
Gimmler H
(1994)
Light-induced H+ transport across the plasma membrane of the acid-resistant green alga Dunaliella acidophila.
Plant Physiol Biochem
32:
75-84
Shabala SN,
Newman IA
(1997)
Proton and calcium flux oscillations in the elongation region correlate with root mutation.
Physiol Plant
100:
917-926
[CrossRef][Medline]
Shabala SN,
Newman IA,
Morris J
(1997)
Oscillations in H+ and Ca2+ ion fluxes around the elongation region of corn roots and effects of external pH.
Plant Physiol
113:
111-118
[Abstract]
Shabala SN,
Newman IA,
Whittington J,
Juswono U
(1998)
Protoplast ion fluxes: their measurement and variation with time, position and osmoticum.
Planta
204:
146-152
[CrossRef]
Spalding EP,
Cosgrove DJ
(1992)
Mechanism of blue-light-induced plasma-membrane depolarization in etiolated cucumber hypocotyls.
Planta
188:
199-205
[CrossRef][ISI][Medline]
Spalding EP,
Slayman CL,
Goldsmith MHM,
Gradmann D,
Bertl A
(1992)
Ion channels in Arabidopsis plasma membrane. Transport characteristics and involvement in light-induced voltage changes.
Plant Physiol
99:
96-102
[Abstract/Free Full Text]
Spanswick RM
(1981)
Electrogenic ion pumps.
Annu Rev Plant Physiol
32:
267-289
[ISI]
Staal M,
Elzenga JTM,
Van Elk AG,
Prins HBA,
Van Volkenburgh E
(1994)
Red and blue light-stimulated proton efflux by epidermal leaf cells of the argenteum mutant of Pisum sativum.
J Exp Bot
45:
1213-1218
[Abstract/Free Full Text]
Takagi S,
Nagai R
(1988)
Light-affected Ca2+ fluxes in protoplasts from Vallisneria mesophyll cells.
Plant Physiol
88:
228-232
[Abstract/Free Full Text]
Tazawa T,
Shimmen T,
Mimura T
(1986)
Spectrum of light-induced membrane hyperpolarization in Egeria densa.
Plant Cell Physiol
27:
163-168
[Abstract/Free Full Text]
Vredenberg WJ,
Tonk WJM
(1975)
On the steady-state electrical potential difference across the thylakoid membranes of chloroplasts in illuminated plant cells.
Biochim Biophys Acta
387:
580-587
[Medline]
Weisenseel MH,
Ruppert HK
(1977)
Phytochrome and calcium ions are involved in light-induced membrane depolarization in Nitella.
Planta
137:
225-229
[CrossRef][ISI]
Yin ZH,
Huve K,
Heber U
(1996)
Light-dependent proton transport into mesophyll vacuoles of leaves of C3 plants as revealed by pH-indicating fluorescent dyes: a reappraisal.
Planta
199:
9-17