Is HCO(3) Transport in Anabaena a Na Symport?

On the cradle of CCM research: discovery, development, and challenges ahead

Herein, 40 years after its discovery, I briefly and critically survey the development of ideas that propelled research on CO2-concentrating mechanisms (CCMs; a term proposed by Dean Price) of phytoplankton, mainly focusing on cyanobacteria. This is not a comprehensive review on CCM research, but a personal view on the past developments and challenges that lie ahead.

Isolation and characterization of mutants of two diazotrophic cyanobacteria tolerant to high concentrations of inorganic carbon

Diazotrophic heterocystous cyanobacteria Nostoc calcicola and Anabaena sp. ARM 629 were investigated for their ability to grow in presence of sodium bicarbonate (NaHCO3) or carbon dioxide (CO2) under cultural conditions. Maximum growth was observed in 75 mM NaHCO3 and 5% CO2 in N. calcicola and Anabaena ARM 629, respectively. Although their growth rate declined, N. calcicola and Anabaena sp. could tolerate upto 250 mM NaHCO3 and 20% CO2, respectively. N-methyl-N'-nitro N nitrosoguanidine induced mutants of these cyanobacteria were isolated which showed growth upto 1 M NaHCO3 (N. calcicola) or 50% CO2 (Anabaena sp.) in comparison to their wild types. The mutants also showed cross-resistance to either of the inorganic carbon compounds, which was not observed for wild type. It was concluded that mutants were altered in multiple properties enabling them to grow at elevated levels of inorganic carbon compounds.

Genes essential to sodium-dependent bicarbonate transport in cyanobacteria: function and phylogenetic analysis

The cyanobacterium Synechocystis sp. strain PCC 6803 possesses two CO(2) uptake systems and two HCO(3)(-) transporters. We transformed a mutant impaired in CO(2) uptake and in cmpA-D encoding a HCO(3)(-)transporter with a transposon inactivation library, and we recovered mutants unable to take up HCO(3)(-) and grow in low CO(2) at pH 9.0. They are all tagged within slr1512 (designated sbtA). We show that SbtA-mediated transport is induced by low CO(2), requires Na(+), and plays the major role in HCO(3)(-) uptake in Synechocystis. Inactivation of slr1509 (homologous to ntpJ encoding a Na(+)/K(+)-translocating protein) abolished the ability of cells to grow at [Na(+)] higher than 100 mm and severely depressed the activity of the SbtA-mediated HCO(3)(-) transport. We propose that the SbtA-mediated HCO(3)(-) transport is driven by DeltamuNa(+) across the plasma membrane, which is disrupted by inactivating ntpJ. Phylogenetic analyses indicated that two types of sbtA exist in various cyanobacterial strains, all of which possess ntpJ. The sbtA gene is the first one identified as essential to Na(+)-dependent HCO(3)(-) transport in photosynthetic organisms and may play a crucial role in carbon acquisition when CO(2) supply is limited, or in Prochlorococcus strains that do not possess CO(2) uptake systems or Cmp-dependent HCO(3)(-) transport.

Passive entry of CO2 and its energy-dependent intracellular conversion to HCO3- in cyanobacteria are driven by a photosystem I-generated deltamuH+

CO(2) entry into Synechococcus sp. PCC7942 cells was drastically inhibited by the water channel blocker p-chloromercuriphenylsulfonic acid suggesting that CO(2) uptake is, for the most part, passive via aquaporins with subsequent energy-dependent conversion to HCO3(-). Dependence of CO(2) uptake on photosynthetic electron transport via photosystem I (PSI) was confirmed by experiments with electron transport inhibitors, electron donors and acceptors, and a mutant lacking PSI activity. CO(2) uptake was drastically inhibited by the uncouplers carbonyl cyanide m-chlorophenylhydrazone (CCCP) and ammonia but substantially less so by the inhibitors of ATP formation arsenate and N, N,-dicyclohexylcarbodiimide (DCCD). Thus a DeltamuH(+) generated by photosynthetic PSI electron transport apparently serves as the direct source of energy for CO(2) uptake. Under low light intensity, the rate of CO(2) uptake by a high-CO(2)-requiring mutant of Synechococcus sp. PCC7942, at a CO(2) concentration below its threshold for CO(2) fixation, was higher than that of the wild type. At saturating light intensity, net CO(2) uptake was similar in the wild type and in the mutant IL-3 suggesting common limitation by the rate of conversion of CO(2) to HCO3(-). These findings are consistent with a model postulating that electron transport-dependent formation of alkaline domains on the thylakoid membrane energizes intracellular conversion of CO(2) to HCO3(-).

Driving Forces for Bicarbonate Transport in the Cyanobacterium Synechococcus R-2 (PCC 7942)

Air-grown Synechococcus R-2 (PCC 7942) cultures grown in BG-11 medium are very alkaline (outside pH is 10.0) and use HCO3- as their inorganic carbon source. The cells showed a dependence on Na+ for photosynthesis, but low Na+ conditions (1 mol m-3) were sufficient to support saturating photosynthesis. The intracellular dissolved inorganic carbon in the light was greater than 20 mol m-3 in both low-Na+ conditions and in BG-11 medium containing the usual [Na+] (24 mol m-3, designated high-Na+ conditions). The electrochemical potential for HCO3- in the light was in excess of 25 kJ mol-1, even in high-Na+ conditions. The Na+-motive force was greater than -12 kJ mol-1 under both Na+ conditions. On thermodynamic grounds, an Na+-driven co-port process would need to have a stoichiometry of 2 or greater ([greater than or equal to]2Na+ in/HCO3-1 in), but we show that Na+ or K+ fluxes cannot be linked to HCO3- transport. Na+ and K+ fluxes were unaffected by the presence or absence of dissolved inorganic carbon. In low-Na+ conditions, Na+ fluxes are too low to support the observed net 14C-carbon fixation rate. Active transport of HCO3- hyperpolarizes (not depolarizes) the membrane potential.

Monensin Inhibition of Na+-Dependent HCO3- Transport Distinguishes It from Na+-Independent HCO3- Transport and Provides Evidence for Na+/HCO3- Symport in the Cyanobacterium Synechococcus UTEX 625

The effect of monensin, an ionophore that mediates Na+/H+ exchange, on the activity of the inorganic carbon transport systems of the cyanobacterium Synechococcus UTEX 625 was investigated using transport assays based on the measurement of chlorophyll a fluorescence emission or 14C uptake. In Synechococcus cells grown in standing culture at about 20 [mu]M CO2 + HCO3-, 50 [mu]M monensin transiently inhibited active CO2 and Na+-independent HCO3- transport, intracellular CO2 and HCO3- accumulation, and photosynthesis in the presence but not in the absence of 25 mM Na+. These activities returned to near-normal levels within 15 min. Transient inhibition was attributed to monensin-mediated intracellular alkalinization, whereas recovery may have been facilitated by cellular mechanisms involved in pH homeostasis or by monensin-mediated H+ uptake with concomitant K+ efflux. In air-grown cells grown at 200 [mu]M CO2 + HCO3- and standing culture cells, Na+-dependent HCO3- transport, intracellular HCO3- accumulation, and photosynthesis were also inhibited by monensin, but there was little recovery in activity over time. However, normal photosynthetic activity could be restored to air-grown cells by the addition of carbonic anhydrase, which increased the rate of CO2 supply to the cells. This observation indicated that of all the processes required to support photosynthesis only Na+-dependent HCO3- transport was significantly inhibited by monensin. Monensin-mediated dissipation of the Na+ chemical gradient between the medium and the cells largely accounted for the decline in the HCO3- accumulation ratio from 751 to 55. The two HCO3- transport systems were further distinguished in that Na+-dependent HCO3- transport was inhibited by Li+, whereas Na+-independent HCO3- transport was not. It is suggested that Na+-dependent HCO3- transport involves an Na+/HCO3- symport mechanism that is energized by the Na+ electrochemical potential.

Quenching of Chlorophyll a Fluorescence in Response to Na+-Dependent HCO3- Transport-Mediated Accumulation of Inorganic Carbon in the Cyanobacterium Synechococcus UTEX 625

In the cyanobacterium Synechococcus UTEX 625, the yield of chlorophyll a fluorescence decreased in response to the transport-mediated accumulation of intracellular inorganic carbon (CO2 + HCO3- + CO32- = dissolved inorganic carbon [DIC]) and subsequently increased to a near-maximum level following photosynthetic depletion of the DIC pool. When DIC accumulation was mediated by the active Na+-dependent HCO3- transport system, the initial rate of fluorescence quenching was found to be highly correlated with the initial rate of H14CO3- transport (r = 0.96), and the extent of fluorescence quenching was correlated with the size of the internal DIC pool (r = 0.99). Na+-dependent HCO3- transport-mediated accumulation of DIC caused fluorescence quenching in either the presence or absence of the CO2 fixation inhibitor glycolaldehyde, indicating that quenching was not due simply to NADP+ reduction. The concentration of Na+ required to attain one-half the maximum rate of H14CO3- transport, at 20 [mu]M external HCO3-, declined from 9 to 1 mM as the external pH increased from 8 to 9.6. A similar pH dependency was observed when fluorescence quenching was used to determine the kinetic constants for HCO3- transport. In cells capable of Na+-dependent HCO3- transport, both the initial rate and extent of fluorescence quenching increased with increasing external HCO3-, saturating at about 150 [mu]M. In contrast Na+-independent HCO3- transport-mediated fluorescence quenching saturated at an HCO3- concentration of about 10 [mu]M. It was concluded that measurement of chlorophyll a fluorescence emission provided a convenient, but indirect, means of following Na+-dependent HCO3- transport and accumulation in Synechococcus.

The relationship between carbon and water transport in single cells of Chara corallina

The hydraulic resistance of the plasma membrane was measured on single internodal cells of Chara corallina using the method of transcellular osmosis. The hydraulic resistance of the plasma membrane of high CO2-grown cells was significantly higher than the hydraulic resistance of the plasma membrane in low CO2-grown cells. Therefore we tested the possibility that the "bicarbonate transport system", postulated to be present in low CO2-grown cells, serves as a water channel that lowers the hydraulic resistance of the plasma membrane. We were unable to find any correlation between agents that inhibited the "bicarbonate transport system" and agents that increased the hydraulic resistance of low CO2-grown cells. We did, however, find a correlation between the permeability of the cell to water and CO2. We propose that the reduced hydraulic resistance of the plasma membrane of the low CO2-grown cells is a function of a change in either the structural properties of the lipid bilayer or the activity of a CO2 transport protein so that under conditions of reduced inorganic carbon, the plasma membrane becomes more permeable to CO2, and consequently to other small molecules, including H2O, methanol and ethanol.

NMR studies on Na+ transport in Synechococcus PCC 6311

The freshwater cyanobacterium Synechococcus PCC 6311 is able to adapt to grow after sudden exposure to salt (NaCl) stress. We have investigated the mechanism of Na+ transport in these cells during adaptation to high salinity. Na+ influx under dark aerobic conditions occurred independently of delta pH or delta psi across the cytoplasmic membrane, ATPase activity, and respiratory electron transport. These findings are consistent with the existence of Na+/monovalent anion cotransport or simultaneous Na+/H(+)+anion/OH- exchange. Na+ influx was dependent on Cl-, Br-, NO3-, or NO2-. No Na+ uptake occurred after addition of NaI, NaHCO3, or Na2SO4. Na+ extrusion was absolutely dependent on delta pH and on an ATPase activity and/or on respiratory electron transport. This indicates that Na+ extrusion via Na+/H+ exchange is driven by primary H+ pumps in the cytoplasmic membrane. Cells grown for 4 days in 0.5 M NaCl medium, "salt-grown cells," differ from control cells by a lower vmax of Na+ influx and by lower steady-state ratios of [Na+]in/[Na+]out. These results indicate that cells grown in high-salt medium increase their capacity to extrude Na+. During salt adaptation Na+ extrusion driven by respiratory electron transport increased from about 15 to 50%.

Na-Independent HCO(3) Transport and Accumulation in the Cyanobacterium Synechococcus UTEX 625

The active transport and intracellular accumulation of HCO(3) (-) by air-grown cells of the cyanobacterium Synechococcus UTEX 625 (PCC 6301) was strongly promoted by 25 millimolar Na(+).Na(+)-dependent HCO(3) (-) accumulation also resulted in a characteristic enhancement in the rate of photosynthetic O(2) evolution and CO(2) fixation. However, when Synechococcus was grown in standing culture, high rates of HCO(3) (-) transport and photosynthesis were observed in the absence of added Na(+). The internal HCO(3) (-) pool reached levels up to 50 millimolar, and an accumulation ratio as high as 970 was observed. Sodium enhanced HCO(3) (-) transport and accumulation in standing culture cells by about 25 to 30% compared with the five- to eightfold enhancement observed with air-grown cells. The ability of standing culture cells to utilize HCO(3) (-) from the medium in the absence of Na(+) was lost within 16 hours after transfer to air-grown culture and was reacquired during subsequent growth in standing culture. Studies using a mass spectrometer indicated that standing culture cells were also capable of active CO(2) transport involving a high-affinity transport system which was reversibly inhibited by H(2)S, as in the case for air-grown cells. The data are interpreted to indicate that Synechococcus possesses a constitutive CO(2) transport system, whereas Na(+)-dependent and Na(+)-independent HCO(3) (-) transport are inducible, depending upon the conditions of growth. Intracellular accumulation of HCO(3) (-) was always accompanied by a quenching of chlorophyll a fluorescence which was independent of CO(2) fixation. The extent of fluorescence quenching was highly dependent upon the size of the internal pool of HCO(3) (-) + CO(2). The pattern of fluorescence quenching observed in response to added HCO(3) (-) and Na(+) in air-grown and standing culture cells was highly characteristic for Na(+)-dependent and Na(+)-independent HCO(3) (-) accumulation. It was concluded that measurements of fluorescence quenching provide an indirect means for following HCO(3) (-) transport and the dynamics of intracellular HCO(3) (-) accumulation and dissipation.

Uptake and utilization of inorganic carbon by cyanobacteria

In the cyanobacteria, mechanisms exist that allow photosynthetic CO2 reduction to proceed efficiently even at very low levels of inorganic carbon. These inducible, active transport mechanisms enable the cyanobacteria to accumulate large internal concentrations of inorganic carbon that may be up to 1000-fold higher than the external concentration. As a result, the external concentration of inorganic carbon required to saturate cyanobacterial photosynthesis in vivo is orders of magnitude lower than that required to saturate the principal enzyme (ribulose bisphosphate carboxylase) involved in the fixation reactions. Since CO2 is the substrate for carbon fixation, the cyanobacteria somehow perform the neat trick of concentrating this small, membrane permeable molecule at the site of CO2 fixation. In this review, we will describe the biochemical and physiological experiments that have outlined the phenomenon of inorganic carbon accumulation, relate more recent genetic and molecular biological observations that attempt to define the constituents involved in this process, and discuss a speculative theory that suggests a unified view of inorganic carbon utilization by the cyanobacteria.

Inorganic carbon transport in biological systems

1. The flux of inorganic carbon (Ci) is an important biological process. 2. CO2 crosses membranes through passive diffusion and, perhaps active transport while HCO3- crosses membranes via facilitated diffusion and active transport mechanisms. 3. Carbonic anhydrase is ubiquitous and enhances the flux of Ci. 4. Generally, Ci crosses membranes through passive and facilitated diffusion when the flux of Ci, per se, is important and crosses membranes via active transport when cells are regulating their intracellular pH and/or ion levels.

Energization and activation of inorganic carbon uptake by light in cyanobacteria

The requirement of the inorganic carbon (C(i)) transport system for light in cyanobacteria was investigated in Anabaena variabilis by the filtering centrifugation technique and in a mutant (E(1)) isolated from Anacystis nidulans using a gas exchange system. C(i) transport capability increased with time of preillumination and decreased following darkening. Full activity could not be obtained by operating either photosystem II (PSII) or photosystem I alone. 3(3,4 Dichlorophenyl)-1,1 dimethylurea strongly inhibited C(i) uptake. Very low activity of PSII was sufficient to activate C(i) uptake. However, in the presence of dithiothreitol PSII activity was not required. We conclude that light may be required to activate as well as to energize C(i) uptake in cyanobacteria.

Evidence for Na-Independent HCO(3) Uptake by the Cyanobacterium Synechococcus leopoliensis

At low levels of dissolved inorganic carbon (DIC) and alkaline pH the rate of photosynthesis by air-grown cells of Synechococcus leopoliensis (UTEX 625) was enhanced 7- to 10-fold by 20 millimolar Na(+). The rate of photosynthesis greatly exceeded the CO(2) supply rate and indicated that HCO(3) (-) was taken up by a Na(+)-dependent mechanism. In contrast, photosynthesis by Synechococcus grown in standing culture proceeded rapidly in the absence of Na(+) and exceeded the CO(2) supply rate by 8 to 45 times. The apparent photosynthetic affinity (K((1/2))) for DIC was high (6-40 micromolar) and was not markedly affected by Na(+) concentration, whereas with air-grown cells K((1/2)) (DIC) decreased by more than an order of magnitude in the presence of Na(+). Lithium, which inhibited Na(+)-dependent HCO(3) (-) uptake in air-grown cells, had little effect on Na(+)-independent HCO(3) (-) uptake by standing culture cells. A component of total HCO(3) (-) uptake in standing culture cells was also Na(+)-dependent with a K((1/2)) (Na(+)) of 4.8 millimolar and was inhibited by lithium. Analysis of (14)C-fixation during isotopic disequilibrium indicated that standing culture cells also possessed a Na(+)-independent CO(2) transport system. The conversion from Na(+)-independent to Na(+)-dependent HCO(3) (-) uptake was readily accomplished by transferring cells grown in standing to growth in cultures bubbled with air. These results demonstrated that the conditions experienced during growth influenced the mode by which Ssynechococcus acquired HCO(3) (-) for subsequent photosynthetic fixation.

Na-Stimulation of Photosynthesis in the Cyanobacterium Synechococcus UTEX 625 Grown on High Levels of Inorganic Carbon

Photosynthesis of washed cells of Synechococcus UTEX 625 grown on 5% CO(2) was markedly stimulated (647 +/- 50%) at pH 8.0 by the addition of low concentrations of NaCl (concentration required for half-maximal response, K((1/2),) = 18 micromolar). Studies with KCl and Na(2)SO(4) showed that the stimulation was due to Na(+). Photosynthesis at pH 6.1 was only slightly stimulated by Na(+). The response of photosynthesis at pH 8.0 to [Na(+)] was strongly sigmoidal for dissolved inorganic carbon ([DIC] </= 500 micromolar). Cells grown with high total [DIC], but air-levels of CO(2), at pH 9.6 showed the same response to low [Na(+)]. The absence of Na(+) could be partially, but not completely overcome, by higher [DIC]. Various methods for examining CO(2) or HCO(3) (-) use (K((1/2)) (CO(2) ) determination; isotopic disequilibrium; and consideration of HCO(3) (-) dehydration rate) were consistent with CO(2) use by the cells, but HCO(3) (-) use could not be ruled out. Isotopic disequilibrium studies showed that CO(2) use was stimulated by Na(+). Cells grown on 5% CO(2) accumulated DIC against a concentration gradient by a process (or processes) dependent on Na(+). No evidence for uptake of Na(+) concomitant with DIC uptake could be found. The lack of O(2) evolution during the initial and most rapid period of DIC accumulation suggested that the required energy was obtained from cyclic photophosphorylation.

Early Responses of Sodium-Deficient Amaranthus tricolor L. Plants to Sodium Application

Effects of sodium application on sodium-deficient Amaranthus tricolor L. cv Tricolor seedlings were studied. Thirty-day-old A. tricolor seedlings grown without sodium received either 0.5 millimolar of NaCl or KCl, and the changes in the growth rate, chlorophyll concentration, photosynthetic oxygen evolution, and dark-oxygen consumption, and some enzyme activities were compared. Following the sodium treatment, the sodium concentration in the leaves increased from the initial value of 0.4 millimolar to 2 to 3 millimolar within 24 hours, and also the relative growth rate and O(2) evolution were enhanced within 24 hours. The stimulation of O(2) evolution was greater in the upper leaves than in the lower leaves. Although total chlorophyll concentration did not increase significantly, the increase in the chlorophyll a/b ratio was apparent within 24 hours. There were not significant increases in the C(4) photosynthetic enzyme activities; however, nitrate reductase activity increased by 350% by the sodium treatment within 24 hours, and this increase is considered not to be one of the consequences of the improved photosynthesis. Results suggest that the sodium treatment promoted CO(2) and nitrate assimilation resulting in the growth enhancement, and that sodium can be involved in some other functions than C(4) photosynthesis in A. tricolor plants.

Inorganic-carbon uptake by the marine diatom Phaeodactylum tricornutum

Air-grown cells of the marine diatom Phaeodactylum tricornutum showed only 10% of the carbonic-anhydrase activity of air-grown Chlamydomonas reinhardtii. Measurement of carbonic-anhydrase activity using intact cells and cell extracts showed all activity was intracellular in Phaeodactylum. Photosynthetic oxygen evolution at constant inorganic-carbon concentration but varying pH showed that exogenous CO2 was poorly utilized by the cells. Sodium ions increased the affinity of Phaeodactylum for HCO 3 (-) and even at high HCO 3 (-) concentrations sodium ions enhanced HCO 3 (-) utilization. The internal inorganic-carbon pool (HCO 3 (-) +CO2] was measured using a silicone-oil-layer centrifugal filtering technique. The internal [HCO 3 (-) +CO2] concentration never exceeded 15% of the external [HCO 3 (-) +CO2] concentration even at the lowest external concentrations tested. It is concluded that an internal accumulation of inorganic carbon relative to the external medium does not occur in P. tricornutum.