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Plant Physiol. (1998) 116: 1125-1132
Energy Sources for HCO3
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ABSTRACT |
|---|
|
|
|---|
Light-dependent inorganic C
(Ci) transport and accumulation in air-grown cells of
Synechococcus UTEX 625 were examined with a mass
spectrometer in the presence of inhibitors or artificial electron
acceptors of photosynthesis in an attempt to drive CO2 or
HCO3
uptake separately by the cyclic or
linear electron transport chains. In the presence of
3-(3,4-dichlorophenyl)-1,1-dimethylurea, the cells were able to
accumulate an intracellular Ci pool of 20 mm,
even though CO2 fixation was completely inhibited,
indicating that cyclic electron flow was involved in the
Ci-concentrating mechanism. When 200 µm
N,N-dimethyl-p-nitrosoaniline was used to
drain electrons from ferredoxin, a similar Ci accumulation was observed, suggesting that linear electron flow could support the
transport of Ci. When carbonic anhydrase was not present, initial CO2 uptake was greatly reduced and the
extracellular [CO2] eventually increased to a level
higher than equilibrium, strongly suggesting that CO2
transport was inhibited and that Ci accumulation was the
result of active HCO3
transport. With
3-(3,4-dichlorophenyl)-1,1-dimethylurea-treated cells, Ci
transport and accumulation were inhibited by inhibitors of
CO2 transport, such as COS and Na2S, whereas
Li+, an HCO3
-transport inhibitor,
had little effect. In the presence of
N,N-dimethyl-p-nitrosoaniline, Ci transport and accumulation were not inhibited by COS and
Na2S but were inhibited by Li+. These results
suggest that CO2 transport is supported by cyclic electron
transport and that HCO3
transport is
supported by linear electron transport.
Cyanobacteria grown under limited C conditions develop a mechanism
for the active transport of Ci, which can lead to
intracellular Ci concentrations in excess of 1000 times the extracellular Ci concentration (Kaplan
et al., 1980 Light supplies the energy for active Ci
transport, because no transport occurs in the dark (Shelp and Canvin,
1984 Somewhat puzzling was the observation that DCMU completely inhibited
Ci fixation but did not completely inhibit
Ci transport and the formation of the
intracellular Ci pool (Ogawa et al., 1985a To investigate the photosynthetic reactions that may be involved in
providing energy for CO2 and
HCO3 Organisms and Growth
![]()
INTRODUCTION
Top
Abstract
Introduction
Methods
Results
Discussion
References
; Shelp and Canvin, 1984
; Espie and Canvin, 1987
; Espie et
al., 1988a
; Miller et al., 1990
; Badger and Price, 1992
).
CO2 and
HCO3
are transported by
separate and independent systems (Espie et al., 1988a
, 1988b
; Miller et
al., 1988b
; Price et al., 1992
; Salon et al., 1996a
).
; Ogawa et al., 1985b
; Kaplan et al., 1987
; Sültemeyer et
al., 1993
). Action spectrum studies suggest that PSI is primarily
responsible for the supply of energy for transport, but a low level of
PSII activity is apparently required for activation of
Ci uptake (Ogawa et al., 1985a
; Kaplan et al.,
1987
).
;
Kaplan et al., 1987
; Miller et al., 1988c
; Ritchie et al., 1996
).
CO2 transport but not
HCO3
transport was inhibited
in a mutant with a defect in cyclic electron flow (Ogawa, 1993
). We
have also observed significant Ci transport and
accumulation when PSI electron acceptors such as PNDA and methyl
viologen are supplied (Li and Canvin, 1997b
), suggesting that some
transport can be supported by linear electron
transport.
transport and
accumulation, we examined Ci uptake in the
presence of inhibitors and artificial electron acceptors of
photosynthesis. Our results suggest that CO2
transport is supported by cyclic electron transport and
HCO3
transport is supported by
linear electron transport.
![]()
MATERIALS AND METHODS
Top
Abstract
Introduction
Methods
Results
Discussion
References
; Li
and Canvin, 1997a
). Cells were harvested 48 h after inoculation.
At that time, the Chl a concentration was between 4 and 5 µg Chl mL
1, the [Ci]
was 50 µm, and the pH of the medium was 9.6.
Experimental Procedure
Prior to experiments, cells were washed three times in 25 mm BTP-HCl, pH 8.0, as previously described (Li and Canvin, 1997a
2
s
1 light and allowed to fix contaminant
Ci in the buffer and reach the
CO2 compensation point (Miller and Canvin, 1989
2 s
1. The
[O2] during the experiments was maintained
between 80 and 100 µm.
MS
A membrane inlet mass spectrometer (model MM 14-80 SC, VG Gas Analysis Systems, Middlewich, UK) was used in these experiments. Concentrations of 16O2, 12CO2, and 13CO2 (m/z 32, 44, and 45, respectively), in the 6-mL reaction chamber were measured simultaneously. The output signal was directed to a computer (486, Altair, Kingston, Canada), and the mass spectrometer was controlled using software (Spectrascan 5.3.1, Petrasoft 5.3.2) from the same company as the spectrometer (VG Gas Analysis Systems). The suspension was stirred with a rotating magnetic bar. Gases and chemicals were introduced into the reaction chamber through a small port. A response time of 2.3 s was obtained with two masses, and 1.1 s was obtained with one mass.
. Calibration for
16O2 was made as described
previously (Miller et al., 1988a
; Li and Canvin, 1997a
). The value of
16O2 concentration in
equilibrium with air was taken as 240 µm. Rates of
16O2 evolution were
calculated from the slope of the 32 signal after the appropriate
corrections were made for leak rates (2% h
1)
during the course of the experiment (Miller et al., 1988a
).
Ci Uptake and Accumulation
The activity of CO2 uptake and the intracellular Ci pool size were measured using the mass spectrometer by following the [CO2] after the addition of 13Ci to the medium both in the presence and in the absence of CA. In the absence of added CA, the intracellular Ci pool was determined either by taking a sample or by injecting CA into the medium (Salon et al., 1996a
1 Chl (Miller et al.,
1988cChemicals
PNDA, Na2S, IAC, CA, and BTP were obtained from Sigma. K213CO3 (99 atom % 13C) was obtained from MSD Isotopes (Montreal, Canada). The K213CO3 was dissolved in BTP-HCl, pH 8.0, as a concentrated solution for addition to the reaction medium (Miller et al., 1988b| |
RESULTS |
|---|
|
|
|---|
Ci Uptake and Accumulation and Effect of DCMU and PNDA
For air-grown cells of Synechococcus UTEX 625 we showed previously that light-dependent Ci uptake and accumulation can be determined using a mass spectrometer equipped with a membrane inlet system that measures the extracellular concentration of dissolved CO2 (Miller et al., 1988c
|
-CO2
system prior to the addition of CA. The Ci taken
up by the cells was quantitatively released back into the medium when
the actinic light was turned off (Fig. 1F).
equilibrium, the disappearance of CO2 from the
medium represented transport and accumulation of total
Ci. The CO2 taken up by the cells was quantitatively released back into the medium when the actinic
light was turned off, and an intracellular Ci
pool of 19.7 mm was observed (Fig. 1B). A similar
intracellular Ci pool remained when DCMU was
added to the cells during Ci uptake (Fig. 1C).
were not in equilibrium,
because after a steady extracellular CO2 level
was observed, the addition of CA caused an increase in
[CO2]. When the lights were turned off, the
[CO2] returned to the initial level. The
calculated Ci pool sizes were 18.8 mm (Fig. 1G) for IAC-inhibited cells and 15.6 mm (Fig. 1H) for
noninhibited cells. In the latter case, the addition of DCMU prevented
any CO2 fixation.
was established and the
light was turned on, the [CO2] initially decreased. After a short time, however, the
[CO2] in the medium increased whether
CO2 fixation was inhibited with IAC (Fig. 1I) or
not inhibited (Fig. 1J). When CO2 fixation was
inhibited, the [CO2] increased to a constant
level that was much higher than the initial equilibrium
concentration. The addition of CA resulted in a decrease in the
[CO2], showing that the
[CO2] had been above the equilibrium value. The
extracellular [CO2] strongly suggests that
Ci accumulation was the result of active
HCO3
transport and that
CO2 transport was inhibited (Badger, 1985
; Salon
et al., 1996b
, 1997
). When the cells were darkened, the intracellular
Ci pool appeared in the medium and the
extracellular [CO2] returned to its initial
equilibrium value (Fig. 1I). The intracellular Ci
pool was 17.5 mm (Fig. 1I).
).
Cyclic Electron Flow-Dependent Active CO2 Transport
and Linear Electron Flow-Dependent HCO3
1 Chl
h
1 was observed (Fig. 2B).

View larger version (16K):
[in a new window]
Figure 2.
Effect of [DCMU] (A) and [PNDA] (B) on the
rate of O2 evolution (
) and the intracellular
Ci pool (
). Cells (6-9 µg Chl mL
1) were
incubated in the presence of 25 mm NaCl and 25 µg
mL
1 CA and allowed to reach the
CO2-compensation point. IAC (3.3 mm) was added;
5 min later the cells were darkened and 100 µm Ci was injected. After about 1 min, Ci
transport and accumulation were initiated by turning on the light. DCMU
or PNDA was added to the cells after the internal Ci pool
had reached its maximum size. The Ci pool remaining after
DCMU and PNDA addition was calculated upon darkening the cells. The
control rate of O2 evolution was 256 µmol
mg
1 Chl h
1. The maximum size of the
internal pool was 56 mm. The data are given as means ± sd (n = 2-5).
Transport
proceeds via separate and
independent transporters (Espie et al., 1989
; Miller and Canvin, 1989
;
Salon et al., 1996a
). CO2 transport is inhibited
by COS or Na2S (Espie et al., 1988b
, 1989
; Miller
et al., 1989
), and HCO3
transport is inhibited by Li+ in air-grown cells
of Synechococcus UTEX 625 (Espie et al., 1988b
; Miller et
al., 1988b
, 1990
; Espie and Kandasamy, 1994
). Therefore, it was of
interest to determine the effects of these inhibitors on
Ci uptake and accumulation in DCMU- and
PNDA-treated cells.
The use of MS to monitor the free [CO2] in
the medium provides a direct measurement of the extent of
Ci uptake and accumulation (Badger, 1985 Received July 21, 1997;
accepted November 17, 1997.
Abbreviations:
BTP, 1,3-bis[tris(hydroxymethyl)methylamino]
propane.
CA, carbonic anhydrase (carbonate dehydratase, EC 4.2.1.1).
Chl, chlorophyll.
Ci, dissolved inorganic carbon
(CO2 + HCO3
Badger MR (1985) The fluxes of inorganic carbon species during
photosynthesis in cyanobacteria with particular reference to
Synechococcus sp. In WJ Lucas, JA Berry, eds,
Inorganic Carbon Uptake by Aquatic Photosynthetic Organisms. American
Society of Plant Physiologists, Rockville, MD, pp 39-52
Badger MR,
Kaplan A,
Berry JA
(1980)
Internal inorganic carbon pool of Chlamydomonas reinhardtii. Evidence for a carbon dioxide concentrating mechanism.
Plant Physiol
66:
407-413
Badger MR,
Price GD
(1992)
The CO2 concentrating mechanism in cyanobacteria and green algae.
Physiol Plant
84:
606-615
[CrossRef]
Badger MR,
Price GD
(1994)
The role of carbonic anhydrase in photosynthesis.
Annu Rev Plant Physiol Plant Mol Biol
45:
369-392
[CrossRef][ISI]
Elstner EF,
Zeller H
(1978)
Bleaching of p-nitrosodimethylaniline by photosystem I of chloroplast lamellae.
Plant Sci Lett
13:
15-20
[CrossRef]
Espie GS,
Canvin DT
(1987)
Evidence of Na+ independent HCO3
Espie GS,
Kandasamy RA
(1994)
Monensin inhibition of Na+-dependent HCO3
Espie GS,
Miller AG,
Birch DG,
Canvin DT
(1988a)
Simultaneous transport of CO2 and HCO3
Espie GS,
Miller AG,
Canvin DT
(1988b)
Characterization of the Na+ requirement in cyanobacterial photosynthesis.
Plant Physiol
88:
757-762
Espie GS,
Miller AG,
Canvin DT
(1989)
Selective and reversible inhibition of active CO2 transport by hydrogen sulfide in a cyanobacterium.
Plant Physiol
91:
389-394
Kaplan A,
Badger MR,
Berry JA
(1980)
Photosynthesis and the intracellular inorganic carbon pool in the bluegreen alga Anabaena variabilis: response to external CO2 concentration.
Planta
149:
219-226
[CrossRef]
Kaplan A,
Zenvirth D,
Marcus Y,
Omata T,
Ogawa T
(1987)
Energization and activation of inorganic carbon uptake by light in cyanobacteria.
Plant Physiol
84:
210-213
Li Q,
Canvin DT
(1997a)
Oxygen photoreduction and its effect on CO2 accumulation and assimilation in air-grown cells of Synechococcus UTEX 625.
Can J Bot
75:
274-283
Li Q,
Canvin DT
(1997b)
Inorganic carbon accumulation stimulates linear electron flow to artificial electron acceptors of PSI in air-grown cells of the cyanobacterium Synechococcus UTEX 625.
Plant Physiol
114:
1273-1281
[Abstract]
MacKinney G
(1941)
Absorption of light by chlorophyll solutions.
J Biol Chem
140:
315-322
McEnery MW,
Pederson PL
(1986)
Diethylstilbestrol. A novel Fo-directed probe of the mitochondrial proton ATPase.
J Biol Chem
261:
1745-1752
Miller AG,
Canvin DT
(1989)
Glycolaldehyde inhibits CO2 fixation in the cyanobacterium Synechococcus UTEX 625 without inhibiting the accumulation of inorganic carbon or the associated quenching of chlorophyll a fluorescence.
Plant Physiol
91:
1044-1049
Miller AG,
Espie GS,
Canvin DT
(1988a)
Active transport of inorganic carbon increases the rate of O2 photoreduction.
Plant Physiol
88:
6-9
Miller AG,
Espie GS,
Canvin DT
(1988b)
Chlorophyll a fluorescence yield as a monitor of both active CO2 and HCO3
Miller AG,
Espie GS,
Canvin DT
(1988c)
Active transport of CO2 by the cyanobacterium Synechococcus UTEX 625. Measurement by mass spectrometry.
Plant Physiol
86:
677-683
Miller AG,
Espie GS,
Canvin DT
(1989)
The use of COS, a structural analog of CO2, to study active CO2 transport in the cyanobacteria Synechococcus UTEX 625.
Plant Physiol
90:
1221-1231
Miller AG,
Espie GS,
Canvin DT
(1990)
Physiological aspects of CO2 and HCO3
Miller AG,
Espie GS,
Canvin DT
(1991)
The effects of inorganic carbon and oxygen on fluorescence in the cyanobacterium Synechococcus UTEX 625.
Can J Bot
69:
1151-1160
Ogawa T (1993) Molecular analysis of the
CO2-concentrating mechanism in cyanobacteria.
In H Yamamoto, C Smith, eds, Photosynthetic Response to the
Environment, American Society of Plant Physiologists, Rockville, MD, pp
113-125
Ogawa T,
Inoue Y
(1983)
Photosystem I-initiated postillumination CO2 burst in a cyanobacterium, Anabaena variabilis.
Biochim Biophys Acta
724:
490-493
[CrossRef]
Ogawa T,
Miyano A,
Inoue Y
(1985a)
Biochim Biophys Acta
808:
77-84
[CrossRef]
Ogawa T, Omata T, Miyano A, Inoue Y (1985b) Photosynthetic
reactions involved in the CO2-concentrating
mechanism in the cyanobacterium, Anacystis nidulans. In WJ
Lucas, JA Berry, eds, Inorganic Carbon Uptake by Aquatic Photosynthetic
Organisms. American Society of Plant Physiologists, Rockville, MD, pp
287-304
Price GD,
Colman JR,
Badger MR
(1992)
Association of carbonic anhydrase activity with carboxysomes isolated from the cyanobacterium Synechococcus PCC7920.
Plant Physiol
100:
784-793
Ritchie R,
Nadolny C,
Larkum AWD
(1996)
Driving forces for bicarbonate transport in the cyanobacteria Synechococcus R-2 (PCC 7920).
Plant Physiol
112:
1573-1584
[Abstract]
Salon C, Li Q, Canvin DT (1997) Glycolaldehyde inhibition of
CO2 transport in the cyanobacterium
Synechococcus UTEX 625. Can J Bot (in press)
Salon C,
Mir NA,
Canvin DT
(1996a)
HCO3
Salon C,
Mir NA,
Canvin DT
(1996b)
Influx and efflux of inorganic carbon in Synechococcus UTEX 625.
Plant Cell Environ
19:
247-259
Shelp BJ,
Canvin DT
(1984)
Evidence for bicarbonate accumulation by Anacystis nidulans.
Can J Bot
62:
1398-1403
Sültemeyer DF,
Biehler K,
Fock HP
(1993)
Evidence for the contribution of pseudocyclic photophosphorylation to the energy requirement of the mechanism for concentrating inorganic carbon in Chlamydomonas.
Planta
189:
235-242
; Salon et al., 1996b
). The effects of COS and
Na2S were rapid, and we interpret the fast increase in the extracellular [CO2] as being
due to rapid leakage of the CO2 that had been
accumulated within cells. Darkening the cells after CA equilibration
did not result in any increase in the [CO2],
indicating that the previously accumulated Ci
pool had leaked from cells upon injection of COS or
Na2S (Fig. 3, A and B).

View larger version (28K):
[in a new window]
Figure 3.
Effects of COS (30 µm, A and E),
Na2S (200 µm, B and F), DES (10 µm, C and G), and Li+ (D and H) on
Ci uptake in the presence of DCMU (A-D) or PNDA (E-H).
Cell suspensions were incubated in the presence of 25 mm (A-G) or 5 mm NaCl (H) and allowed to reach the
CO2-compensation point. IAC (3.3 mm) was added,
and 5 min later cells were darkened and either 5 µm DCMU
(A-D) or 200 µm PNDA (E-H) and 100 µm
Ci was injected in the dark. After Ci
equilibration, the light was switched on as indicated (L) and
Ci was allowed to accumulate. The inhibitors were injected
either during Ci uptake, as indicated (A-C, G, and H) or
before the addition of Ci (D, E, and F). The effect of the
inhibitors was rapid, and there were no difference in terms of order of
addition. After CA addition the cells were darkened and the size of the
intracellular Ci pool (
) was determined. Results were
corrected for changes due to CA addition. The dashed lines indicate the
changes in m/z = 45 signal seen upon the addition of the inhibitor
in the absence of cells. [Chl] (in micrograms per milliliter) was
10.4 in A and C; 4.57 in B; 5 in D and G; 9 in H; and 5.75 in E and F. Chemicals other than NaCl added before the Ci are shown in
the figures without regard to time of addition.
transport
occurs in the absence of CO2 transport (Salon et
al., 1996b
). The results, therefore, indicated that
CO2 inhibitors had little effect on
Ci transport and accumulation in PNDA-treated cells.
), resulted in a rapid
increase in the extracellular [CO2] to above
the initial equilibrium level. The addition of CA to cells in the light
caused a decrease in [CO2] and a rapid
re-establishment of the
CO2-HCO3
equilibrium. As shown by the absence of an increase in the
extracellular [CO2] upon darkening, all or most
of the intracellular Ci had leaked from the cells
upon the addition of DES (Fig. 3C). When the same concentration of DES
was added to PNDA-treated cells, there was no burst of
CO2 and the cells still retained an intracellular pool of 16.9 mm (Fig. 3G).

View larger version (13K):
[in a new window]
Figure 4.
The effects of 1 µm DCMU (A) on
Ci uptake and accumulation with PNDA and 100 µm PNDA (B) on Ci uptake and accumulation
with DCMU in the absence of CA. Cell suspensions containing 25 mm NaCl with 100 µm Ci and 3.3 mm IAC were incubated as described in Figure 1, with 5 µm DCMU (B) or 200 µm PNDA (A). After
Ci equilibration, the light was switched on as indicated
(L) and Ci was allowed to accumulate. DCMU and PNDA were
injected as indicated, and CA was added either before the addition of
DCMU (A) or after the addition of PNDA (B) to maintain the
CO2-HCO3
equilibrium. The light
was turned off as indicated (D). [Chl] was 5.75 (A) and 3.9 µg
mL
1 (B).
![]()
DISCUSSION
Top
Abstract
Introduction
Methods
Results
Discussion
References
; Miller
et al., 1988c
; Salon et al., 1996a
, 1996b
). It has also allowed active
CO2 transport to be distinguished from HCO3
transport in air-grown
cyanobacteria (Espie et al., 1988a
, 1989
; Salon et al., 1996a
, 1996b
),
in which only Na+-dependent
HCO3
transport occurs. In the
present study the MS technique was used to determine the capacities to
which Ci uptake could occur in the presence of
inhibitors or artificial electron acceptors of photosynthesis to
identify the role of photosynthetic electron transport in the operation
of the Ci-concentrating mechanism.
;
Shelp and Canvin, 1984
; Miller et al., 1990
). Photosynthesis supplies
energy for the concentrating mechanism (Badger et al., 1980
; Ogawa et
al., 1985b
; Kaplan et al., 1987
), although the reactions involved in
providing the energy for this process are not known. It has been
suggested that PSI-driven cyclic electron flow is the source of energy
(Ogawa and Inoue, 1983
; Ogawa et al., 1985a
, 1985b
; Ogawa, 1993
).
However, the fact that DCMU inhibits the accumulation of
Ci and the enhanced Mehler reaction in
low-CO2 cells suggests the involvement of linear
electron transport (pseudocyclic photophosphorylation) in the operation
of the Ci-concentrating mechanism (Miller et al.,
1988a
, 1991
; Sültemeyer et al., 1993
).
), and the high
rate of O2 evolution that was observed even in
the presence of IAC indicates that it is an efficient acceptor of
PSI-derived electrons (Fig. 1, D, E, I, and J). The rate of
O2 evolution was higher in noninhibited than in
inhibited cells. Significant Ci accumulation
occurred even upon the addition of a high concentration of PNDA. These
observations are consistent with the results obtained by Li and Canvin
(1997b)
.
-CO2
equilibrium, and when the cells were darkened the intracellular Ci pool appeared in the medium (Fig. 1, I and J).
also observed this CO2
release in cells treated with CO2 transport
inhibitors. In this case, cells continued to transport
HCO3
, which was converted to
CO2, which leaked from the cells because it could
not be retransported. The differences in the patterns between DCMU- and
PNDA-treated cells in the absence of added CA can be explained. In the
presence of PNDA, active HCO3
transport was responsible for the accumulation of the intracellular Ci pool and the increase in the extracellular
[CO2] was due to rapid leakage of
CO2 from cells. The observation that
Ci uptake and accumulation in DCMU-treated cells
were inhibited by CO2-transport inhibitors such
as COS and Na2S, whereas the
HCO3
-transport inhibitor
Li+ inhibited Ci
accumulation in PNDA-treated cells supports this interpretation (Fig.
3, A, B, E, and F).
). In the
present study, 10 µm DES completely inhibited
CO2 accumulation in DCMU-treated cells,
indicating that CO2 transport was fueled by ATP
(Fig. 3C). HCO3
transport and
accumulation, however, could proceed in the presence of the same
concentration of DES in PNDA-treated cells (Fig. 3H). These results
suggest that PNDA-dependent linear electron flow was responsible for
the Ci accumulation, and the linear electron flow
may be more important than its coupling to ATP formation. We do not
know how linear electron transport supplies the energy for
HCO3
transport or why
CO2 transport appears to be driven only by ATP generated through cyclic phosphorylation (Ogawa, 1993
). Linear electron
transport should also generate ATP, but it does not appear to be
available to drive CO2 transport. If it drives
HCO3
transport, the ATPase
involved would not be sensitive to DES. Further speculation on energy
coupling is possible, but any firm conclusions concerning the subject
cannot be made at the present time.
1
This work was supported in part by grants from
the Natural Sciences and Engineering Research Council of Canada.
![]()
FOOTNOTES
*
Corresponding author; fax 1-613-545-6617.
![]()
ABBREVIATIONS
+ CO32
).
DES, diethylstilbestrol.
IAC, iodoacetamide.
PNDA, N,N-dimethyl-p-nitrosoaniline.
![]()
LITERATURE CITED
Top
Abstract
Introduction
Methods
Results
Discussion
References
uptake by the cyanobacterium Synechococcus leopoliensis.
Plant Physiol
84:
125-130
transport distinguishes it from Na+-independent HCO3
transport and provides evidence for Na+/HCO3
symport in the cyanobacteria Synechococcus UTEX 625.
Plant Physiol
104:
1419-1428
[Abstract]
by the cyanobacterium Synechococcus UTEX 625.
Plant Physiol
87:
551-554
transport in the cyanobacterium Synechococcus UTEX 625.
Plant Physiol
86:
655-658
transport by cyanobacteria: a review.
Can J Bot
68:
1291-1302
and CO2 leakage from Synechococcus UTEX 625.
Plant Cell Environ
19:
260-274
[CrossRef]
Copyright Clearance Center: 0032-0889/98/116/1125/08
© 1998 American Society of Plant Physiologists
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