Leaf cavity CO2 concentrations and CO2 exchange in onion,Allium cepa L.

Onion (Allium cepa L.) plants were examined to determine the photosynthetic role of CO₂ that accumulates within their leaf cavities. Leaf cavity CO₂ concentrations ranged from 2250 L L^–1 near the leaf base to below atmospheric (<350 L L^–1) near the leaf tip at midday. There was a daily fluctuation in the leaf cavity CO₂ concentrations with minimum values near midday and maximum values at night. Conductance to CO₂ from the leaf cavity ranged from 24 to 202 mol m^–2 s^–1 and was even lower for membranes of bulb scales. The capacity for onion leaves to recycle leaf cavity CO₂ was poor, only 0.2 to 2.2% of leaf photosynthesis based either on measured CO₂ concentrations and conductance values or as measured directly by ¹⁴CO₂ labeling experiments. The photosynthetic responses to CO₂ and O₂ were measured to determine whether onion leaves exhibited a typical C₃-type response. A linear increase in CO₂ uptake was observed in intact leaves up to 315 L L^–1 of external CO₂ and, at this external CO₂ concentration, uptake was inhibited 35.4±0.9% by 210 mL L^–1 O₂ compared to 20 mL L^–1 O₂. Scanning electron micrographs of the leaf cavity wall revealed degenerated tissue covered by a membrane. Onion leaf cavity membranes apparently are highly impermeable to CO₂ and greatly restrict the refixation of leaf cavity CO₂ by photosynthetic tissue.Abbreviations C_a external CO₂ concentration - C_i intercellular CO₂ concentration - CO₂ compensation concentration - PPFR photosynthetic photon fluence rate     

Characterisation of carbon dioxide and bicarbonate transport during steady-state photosynthesis in the marine cyanobacterium Synechococcus strain PCC7002

Net O₂ evolution, gross CO₂ uptake and net HCO _inf3 ^su– uptake during steady-state photosynthesis were investigated by a recently developed mass-spectrometric technique for disequilibrium flux analysis with cells of the marine cyanobacterium Synechococcus PCC7002 grown at different CO₂ concentrations. Regardless of the CO₂ concentration during growth, all cells had the capacity to transport both CO₂ and HCO _inf3 ^su– ; however, the activity of HCO _inf3 ^su– transport was more than twofold higher than CO₂ transport even in cyanobacteria grown at high concentration of inorganic carbon (C_i = CO₂ + HCO _inf3 ^su– ). In low-C_i cells, the affinities of CO₂ and HCO _inf3 ^su– transport for their substrates were about 5 (CO₂ uptake) and 10 (HCO _inf3 ^su– uptake) times higher than in high-C_i cells, while air-grown cells formed an intermediate state. For the same cells, the intracellular accumulated C_i pool reached 18, 32 and 55 mM in high-C_i, air-grown and low-C_i cells, respectively, when measured at 1 mM external C_i. Photosynthetic O₂ evolution, maximal CO₂ and HCO _inf3 ^su– transport activities, and consequently their relative contribution to photosynthesis, were largely unaffected by the CO₂ provided during growth. When the cells were adapted to freshwater medium, results similar to those for artificial seawater were obtained for all CO₂ concentrations. Transport studies with high-C_i cells revealed that CO₂ and HCO _inf3 ^su– uptake were equally inhibited when CO₂ fixation was reduced by the addition of glycolaldehyde. In contrast, in low-C_i cells steady-state CO₂ transport was preferably reduced by the same inhibitor. The inhibitor of carbonic anhydrase ethoxyzolamide inhibited both CO₂ and HCO _inf3 ^su– uptake as well as O₂ evolution in both cell types. In high-C_i cells, the degree of inhibition was similar for HCO _inf3 ^su– transport and O₂ evolution with 50% inhibition occurring at around 1 mM ethoxyzolamide. However, the uptake of CO₂ was much more sensitive to the inhibitor than HCO _inf3 ^su– transport, with an apparent I₅₀ value of around 250 M ethoxyzolamide for CO₂ uptake. The implications of our results are discussed with respect to C_i utilisation in the marine Synechococcus strain.Abbreviations Chl chlorophyll - C_i inorganic carbon (CO₂ + HCO _inf3 ^su– ) - CA carbonic anhydrase - CCM CO₂-concentrating mechanism - EZA ethoxyzolamide - GA glycolaldehyde - K_1/2 concentration required for half-maximal response - Rubisco ribulose-1,5,-bisphosphate carboxylase-oxygenase D.S. is a recipient of a research fellowship from the Deutsche Forschungsgemeinschaft (D.F.G.). In addition, we are grateful to Donald A. Bryant, Department of Molecular and Cell Biology and Center of Biomolecular Structure Function, Pennsylvania State University, USA, for sending us the wild-type strain of Synechococcus PCC7002.     

Inhibition by ethoxyzolamide of a photoacoustic uptake signal in leaves: Evidence for carbonic anhydrase catalyzed CO2-solubilisation

A photoacoustic pulse-modulation technique is applied for the study of a CO₂-stimulated gas uptake signal in leaves (Reising and Schreiber, Photosynthe Res 31: 227–238, 1992). It is shown that this uptake signal can be substantially suppressed by application of the carbonic anhydrase inhibitor, ethoxyzolamide, to leaf discs. This inhibitor does not affect the O₂-evolution signal in air or the chlorophyll fluorescence induction pattern at high CO₂, when non-saturating light intensities are used. On the basis of these findings it is concluded that at least a major part of the CO₂-stimulated photoacoustic uptake signal results from light-modulated CO₂-solubilisation catalysed by carbonic anhydrase. Modulated CO₂-solubilisation appears likely to be induced by light driven H⁺-translocation from the stroma into the thylakoid lumen. Comparison of the induction patterns of chlorophyll fluorescence quenching and the uptake signal suggests a correlation between membrane energisation and CO₂-uptake. The importance of O₂-dependent electron flow as a major cause of membrane energisation is discussed. It is proposed that in the absence of CO₂ the combination of Mehler- and ascorbate peroxidase reactions does not result in a photobaric signal, as O₂-uptake and O₂-evolution components cancel each other. Two main conclusions, which are of considerable importance for future practical applications of the photoacoustic method, are drawn from these findings: (1) When high CO₂ is applied to leaves, the photobaric uptake component may provide a unique means of monitoring the function of stromal carbonic anhydrase in vivo. (2) Brief flushing of the photoacoustic cell with air may prevent the occurrence of an uptake signal, thus allowing a straight-forward deconvolution into photothermal and O₂-evolution components.     

Arabidopsis thaliana carbonic anhydrase: cDNA sequence and effect of CO2 on mRNA levels

A full-length cDNA clone encoding carbonic anhydrase was isolated from an Arabidopsis thaliana (Columbia) leaf library. Comparison of the derived amino acid sequence obtained from this clone with those of pea and spinach reveals a considerable degree of identity. The carbonic anhydrase cDNA was used to probe the level of RNA encoding this protein in the leaves of plants grown in elevated CO₂ (660 ppm). We have found that under these conditions the steady-state level of carbonic anhydrase mRNA was increased in comparison with control plants grown in normal atmospheric concentrations of CO₂ (330 ppm). This raises the intruiging possibility that there exists in higher plants a mechanism for perceiving and responding to changes in environmental CO₂ concentrations at the genetic level.     

Active CO(2) Transport by the Green Alga Chlamydomonas reinhardtii

Mass spectrometric measurements of dissolved free ¹³CO₂ were used to monitor CO₂ uptake by air grown (low CO₂) cells and protoplasts from the green alga Chlamydomonas reinhardtii. In the presence of 50 micromolar dissolved inorganic carbon and light, protoplasts which had been washed free of external carbonic anhydrase reduced the ¹³CO₂ concentration in the medium to close to zero. Similar results were obtained with low CO₂ cells treated with 50 micromolar acetazolamide. Addition of carbonic anhydrase to protoplasts after the period of rapid CO₂ uptake revealed that the removal of CO₂ from the medium in the light was due to selective and active CO₂ transport rather than uptake of total dissolved inorganic carbon. In the light, low CO₂ cells and protoplasts incubated with carbonic anhydrase took up CO₂ at an apparently low rate which reflected the uptake of total dissolved inorganic carbon. No net CO₂ uptake occurred in the dark. Measurement of chlorophyll a fluorescence yield with low CO₂ cells and washed protoplasts showed that variable fluorescence was mainly influenced by energy quenching which was reciprocally related to photosynthetic activity with its highest value at the CO₂ compensation point. During the linear uptake of CO₂, low CO₂ cells and protoplasts incubated with carbonic anhydrase showed similar rates of net O₂ evolution (102 and 108 micromoles per milligram of chlorophyll per hour, respectively). The rate of net O₂ evolution (83 micromoles per milligram of chlorophyll per hour) with washed protoplasts was 20 to 30% lower during the period of rapid CO₂ uptake and decreased to a still lower value of 46 micromoles per milligram of chlorophyll per hour when most of the free CO₂ had been removed from the medium. The addition of carbonic anhydrase at this point resulted in more than a doubling of the rate of O₂ evolution. These results show low CO₂ cells of Chlamydomonas are able to transport both CO₂ and HCO₃⁻ but CO₂ is preferentially removed from the medium. The external carbonic anhydrase is important in the supply to the cells of free CO₂ from the dehydration of HCO₃⁻.     

CO2 exchange characteristics during dark-light transitions in wild-type and mutant Chlamydomonas reinhardii cells

A burst of net CO₂ uptake was observed during the first 3–4 min after the onset of illumination in both wild-type Chlamydomonas reinhardii in which carbonic anhydrase was chemically inhibited with ethoxyzolamide and in a mutant of C. reinhardii (ca-1-12-1C) deficient in carbonic anhydrase activity. The burst was followed by a rapid decrease in the CO₂ uptake rate so that net evolution often occurred. After a 2–3 min period of CO₂ evolution, net CO₂ uptake again increased and ultimately reached a steady-state, positive rate. From [¹⁴CO₂]-tracer studies it was determined that CO₂ fixation proceeded at a nearly linear rate throughout the period of illumination. Thus, prior to reaching a steady state, there was a rapid accumulation of inorganic carbon inside the cells which apparently reached a supercritical concentration and the excess was excreted, causing a subsequent efflux of CO₂. A post illumination burst of net CO₂ efflux was also observed in ethoxyzolamide-inhibited wild type and ca-1 mutant cells, but not in the unihibited wild type. [¹⁴CO₂]-tracer experiments revealed that this burst was the result of a collapse of a large internal inorganic carbon pool at the onset of darkness rather than a photorespiratory post-illumination burst. These results indicate that upon illumination, chemical or genetic inhibition of carbonic anhydrase initially causes an accumulation of excess inroganic carbon in C. reinhardii cells, and that unknown regulatory mechanisms correct for this imbalance by first excreting the excess inorganic carbon and then, after several dampened oscillations, achieving an equilibrium between bicarbonate uptake, bicarbonate dehydration, and CO₂ fixation.     

Regulation of carbonic-anhydrase activity,inorganic-carbon uptake and photosynthetic biomass yield inChlamydomonas reinhardtii

The regulation of carbonic anhydrase by environmental conditions was determined forChlamydomonas reinhardtii. The depression of carbonic anhydrase in air-grown cells was pH-dependent. Growth of cells on air at acid pH, corresponding to 10 m CO₂ in solution, resulted in complete repression of carbonic-anhydrase activity. At pH 6.9, increasing the CO₂ concentration to 0.15% (v/v) in the gas phase, corresponding to 11 M in solution, was sufficient to completely repress carbonic-anhydrase activity. Photosynthesis and intracellular inorganic carbon were measured in air-grown and high-CO₂-grown cells using a silicone-oil centrifugation technique. With carbonic anhydrase repressed cells limited inorganic-carbon accumulation resulted from non-specific binding of CO₂. With air-grown cells, inorganic-carbon uptake at acid pH, i.e. 5.5, was linear up to 0.5 mM external inorganic-carbon concentration whereas at alkaline pH, i.e. 7.5, the accumulation ratio decreased with increase in external inorganic-carbon concentration. It is suggested that in air-grown cells at acid pH, CO₂ is the inorganic carbon species that crosses the plasmalemma. The conversion of CO₂ to HCO ₃ ^- by carbonic anhydrase in the cytosol results in inorganic-carbon accumulation and maintains the diffusion gradient for carbon dioxide across the cell boundary. However, this mechanism will not account for energy-dependent accumulation of inorganic carbon when there is little difference in pH between the exterior and cytosol.     

Effect of carbon dioxide and temperature on photosynthetic CO2 uptake and photorespiratory CO2 evolution in sunflower leaves

Using an open gas-exchange system, apparent photosynthesis, true photosynthesis (TPS), photorespiration (PR) and dark respiration of sunflower (Helianthus annuus L.) leaves were determined at three temperatures and between 50 and 400 l/l external CO₂. The ratio of PR/TPS and the solubility ratio of O₂/CO₂ in the intercellular spaces both decreased with increasing CO₂. The rate of PR was not affected by the CO₂ concentration in the leaves and was independent of the solubility ratio of oxygen and CO₂ in the leaf cell. At photosynthesis-limiting concentrations of CO₂, the ratio of PR/TPS significantly increased from 18 to 30°C and the rate of PR increased from 4.3 mg CO₂ dm^-2 h^-1 at 18°C to 8.6 mg CO₂ dm^-2 h^-1 at 30°C. The specific activity of photorespired CO₂ was CO₂-dependent but temperature-independent, and the carbon traversing the glycolate pathway appeared to be derived both from recently fixed assimilate and from older reserve materials. It is concluded that PR as a percentage of TPS is affected by the concentrations of O₂ and CO₂ around the photosynthesizing cells, but the rate of PR may also be controlled by other factors.Abbreviations APS apparent photosynthesis (net CO₂ uptake) - PR photorespiration (CO₂ evolution in light) - RuBP ribulose-1,5-bisphosphate - TPS true photosynthesis (true CO₂ uptake)     

Temperature effects on the photosynthetic response of C3 plants to long-term CO2 enrichment

To assess the long-term effect of increased CO₂ and temperature on plants possessing the C₃ photosynthetic pathway, Chenopodium album plants were grown at one of three treatment conditions: (1) 23 °C mean day temperature and a mean ambient partial pressure of CO₂ equal to 350 bar; (2) 34 °C and 350 bar CO₂; and (3) 34 °C and 750 bar CO₂. No effect of the growth treatments was observed on the CO₂ reponse of photosynthesis, the temperature response of photosynthesis, the content of Ribulose-1,5-bisphosphate carboxylase (Rubisco), or the activity of whole chain electron transport when measurements were made under identical conditions. This indicated a lack of photosynthetic acclimation in C. album to the range of temperature and CO₂ used in the growth treatments. Plants from every treatment exhibited similar interactions between temperature and CO₂ on photosynthetic activity. At low CO₂ (< 300 bar), an increase in temperature from 25 to 35 °C was inhibitory for photosynthesis, while at elevated CO₂ (> 400 bar), the same increase in temperature enhanced photosynthesis by up to 40%. In turn, the stimulation of photosynthesis by CO₂ enrichment increased as temperature increased. Rubisco capacity was the primary limitation on photosynthetic activity at low CO₂ (195 bar). As a consequence, the temperature response of A was relatively flat, reflecting a low temperature response of Rubisco at CO₂ levels below its k_m for CO₂. At elevated CO₂ (750 bar), the temperature response of electron transport appeared to control the temperature dependency of photosynthesis above 18 °C. These results indicate that increasing CO₂ and temperature could substantially enhance the carbon gain potential in tropical and subtropical habitats, unless feedbacks at the whole plant or ecosystem level limit the long-term response of photosynthesis to an increase in CO₂ and temperature.Abbreviations A net CO₂ assimilation rate - C _a ambient partial pressure of CO₂ - C _i intercellular partial pressure of CO₂ - Rubisco Ribulose-1,5-bisphosphate carboxylase - VPD vapor pressure difference between leaf and air     

Carbonic anhydrase activity in acetate grown Methanosarcina barkeri

Cell extracts (27000xg supernatant) of acetate grown Methanosarcina barkeri were found to have carbonic anhydrase activity (0.41 U/mg protein), which was lost upon heating or incubation with proteinase K. The activity was inhibited by Diamox (apparent K _i=0.5 mM), by azide (apparent K _i=1 mM), and by cyanide (apparent K _i=0.02 mM). These and other properties indicate that the archaebacterium contains the enzyme carbonic anhydrase (EC 4.2.1.1). Evidence is presented that the protein is probably located in the cytoplasm. Methanol or H₂/CO₂ grown cells of M. barkeri showed no or only very little carbonic anhydrase activity. After transfer of these cells to acetate medium the activity was induced suggesting a function of this enzyme in acetate fermentation to CO₂ and CH₄. Interestingly, Desulfobacter postgatei and Desulfotomaculum acetoxidans, which oxidize acetate to 2 CO₂ with sulfate as electron acceptor, were also found to exhibit carbonic anhydrase activity (0.2 U/mg protein).     

Role of intracellular carbonic anhydrase in inorganic-carbon assimilation by Porphyridium purpureum

Air-grown cells of Porphyridium purpurem contain appreciable carbonic-anhydrase activity, comparable to that in air-grown Chlamydomonas reinhardtii, but activity is repressed in CO₂-grown cells. Assay of carbonic-anhydrase activity in intact cells and cell extracts shows all activity to be intracellular in Porphyridium. Measurement of inorganic-carbon-dependent photosynthetic O₂ evolution shows that sodium ions increase the affinity of Porphyridium cells for HCO ₃ ^- . Acetazolamide and ethoxyzolamide were potent inhibitors of carbonic anhydrase in cell extracts but at pH 5.0 both acetazolamide and ethoxyzolamide had little effect upon the concentration of inorganic carbon required for the half-maximal rate of photosynthetic O₂ evolution (K_0.5[CO₂]). At pH 8.0, where HCO ₃ ^- is the predominant species of inorganic carbon, the K_0.5 (CO₂) was increased from 50 M to 950 M in the presence of ethoxyzolamide. It is concluded that in air-grown cells of Porphyridium. HCO ₃ ^- is transported across the plasmalemma and intracellular carbonic anhydrase increases the steady-state flux of CO₂ from inside the plasmalemma to ribulose-1,5-bisphosphate carboxylase-oxygenase by catalysing the interconversion of HCO ₃ ^- and CO₂ within the cell.Abbreviations AZ acetazolamide - EZ ethoxyzolamide - K_0.5[CO₂] half-maximal rate of photosynthetic O₂ evolution     

Inorganic-carbon transport in some marine eukaryotic microalgae

Inorganic-carbon transport was investigated in the eukaryotic marine microalgaeStichococcus minor, Nannochloropsis oculata and aMonallantus sp. Photosynthetic O₂ evolution at constant inorganic-carbon concentration but varying pH showed thatS. minor had a greater capacity for CO₂ rather than HCO ₃ ^– utilization but forN. oculata andMonallantus HCO ₃ ^– was the preferred source of inorganic carbon. All three microalgae had a low affinity for CO₂ as shown by the measurement of inorganic-carbon-dependent photosynthetic O₂ evolution at pH 5.0. At pH 8.3, where HCO ₃ ^– is the predominant form of inorganic carbon, the concentration of inorganic carbon required for half-maximal rate of photosynthetic O₂ evolution [K _0.5 (CO₂)] was 53 M forMonallantus sp. and 125 M forN. oculata, values compatible with HCO ₃ ^– transport. Neither extra- nor intracellular carbonic anhydrase was detected in these three microalgal species. It is concluded that these microalgae lack a specific transport system for CO₂ but that HCO ₃ ^– transport occurs inN. oculata andMonallantus, and in the absence of intracellular carbonic anhydrase the conversion of HCO ₃ ^– to CO₂ may be facilitated by the internal pH of the cell.     

Effect of dissolved inorganic carbon on oxygen evolution and uptake by Chlamydomonas reinhardtii suspensions adapted to ambient and CO2-enriched air

Mass spectrometric measurements of ¹⁶O₂ and ¹⁸O₂ isotopes were used to compare the rates of gross O₂ evolution (E₀), O₂ uptake (U₀) and net O₂ evolution (NET) in relation to different concentrations of dissolved inorganic carbon (DIC) by Chlamydomonas reinhardtii cells grown in air (air-grown), in air enriched with 5% CO₂ (CO₂-grown) and by cells grown in 5% CO₂ and then adapted to air for 6h (air-adapted).At a photon fluence rate (PFR) saturating for photosynthesis (700 mol photons m^-2 s^-1), pH=7.0 and 28°C, U₀ equalled E₀ at the DIC compensation point which was 10M DIC for CO₂-grown and zero for air-grown cells. Both E₀ and U₀ were strongly dependent on DIC and reached DIC saturation at 480 M and 70 M for CO₂-grown and air-grown algae respectively. U₀ increased from DIC compensation to DIC saturation. The U₀ values were about 40 (CO₂-grown), 165 (air-adapted) and 60 mol O₂ mg Chl^-1 h^-1 (air-grown). Above DIC compensation the U₀/E₀ ratios of air-adapted and air-grown algae were always higher than those of CO₂-grown cells. These differences in O₂ exchange between CO₂- and air-grown algae seem to be inducable since air-adapted algae respond similarly to air-grown cells.For all algae, the rates of dark respiratory O₂ uptake measured 5 min after darkening were considerably lower than the rates of O₂ uptake just before darkening. The contribution of dark respiration, photorespiration and the Mehler reaction to U₀ is discussed and the energy requirement of the inducable CO₂/HCO₃ ^- concentrating mechanism present in air-adapted and air-grown C. reinhardtii cells is considered.Abbreviations DIC dissolved inorganic carbon - DCMU 3-(3,4-dichlorophenyl)-1,1-dimethylurea - E₀ rate of photosynthetic gross O₂ evolution - PCO photosynthetic carbon oxidation - PFR photon fluence rate - PS I photosystem I - PS II photosystem II - U₀ rate of O₂ uptake in the light - MS mass spectrometer     

Diurnal changes in the response of canopy photosynthetic rate to elevated CO2 in a coupled temperature-light environment

The relative increase with elevated CO₂ of canopy CO₂ uptake rate (A), derived from continuous measurements during the day, was examined in full-cover vegetative Lolium perenne canopies after 17 days of regrowth. The stands were grown at ambient (358±50 mol mol^-1) and increased (626±50 mol mol^-1) CO₂ concentration in sunlit growth chambers. Over the entire range of temperature and light conditions (which were strongly coupled and increased simultaneously), A was on average twice as large in high compared to ambient CO₂. This response (called M=A in high CO₂/A in ambient CO₂) could not be explained by changes in canopy conductance for CO₂ diffusion (GC). In spite of interaction and strong coupling between temperature and light intensity, there was evidence that temperature rather than light determined M. Further, high CO₂ treatment was found to alleviate the afternoon depression in A observed in ambient CO₂. A temperature optimum shift or/and a larger carbohydrate sink capacity through altered root/shoot ratio are proposed in explanation.Abbreviations A CO₂ uptake rate - C350 ambient CO₂ treatment - C600 elevated CO₂ treatment - E canopy evapotranspiration rate - GC canopy conductance for CO₂ diffusion - M high CO₂ modification factor     

Photosynthetic metabolism of cyanate by the cyanobacterium Synechococcus UTEX 625

Intact cells of the unicellular cyanobacterium Synechococcus UTEX 625 degraded exogenously supplied cyanate (as KOCN) to CO₂ and NH₃ in a light-dependent reaction. NH₃ release to the medium was as high as 80 mol(mgChl)^-1h^-1 and increased 1.7-fold in the presence of methionine sulfoximine, a glutamine synthetase inhibitor. Cyanate also supporte photosynthetic O₂ evolution to a maximum rate of 188 mol O₂(mgChl)^-1h^-1 at pH 8 and 30°C. Cyanate decomposition in cell-free extracts, measured by mass spectrometry as ¹³CO₂ production from KO¹³CN, occurred in the soluble enzyme fraction, but not in the thylakoid/carboxysome fraction, and was enhanced by HCO₃ ^– and inhibited by the dianion oxalate. CO₂, rather, than HCO₃ ^–, was a product of cyanate decomposition. The ability to decompose cyanate was not dependent upon pre-exposure of cells to cyanate to induce activity. The collective results indicate that Synechococcus UTEX 625 possesses a constitutive, cytosolic cyanase (EC 4.3.99.1), similar in mechanism to that found in some species of heterotrophic bacteria. The reaction catalyzed was: OCN+HCO₃+2H⁺2CO₂+NH₃. In intact cells, the CO₂ produced by the action of cyanase on OCN^- was either directly fixed by the Calvin cycle enzyme ribulose-1,5-bisphosphate carboxylase/oxygenase, leading to O₂ evolution, or leaked into the medium where it was returned to the cell by the active CO₂/HCO₃ ^– transport systems for fixation. However, leakage of CO₂ from air-grown cells was only observed when the active CO₂ transport system was inhibited by darkness or the CO₂ analogue carbon oxysulfide.Abbreviations BTP bistrispropane - C _i inorganic carbon (=CO₂+HCO₃ ^-+CO₃ ^2-) - CA carbonic anhydrase - Chl chlorophyll - COS carbon oxysulfide - MSX methionine sulfoximine - PAR photosynthetically active radiation - Rubisco ribulose bisphosphate carboxylase/oxygenase     

Photosynthesis and apparent affinity for dissolved inorganic carbon by cells and chloroplasts of Chlamydomonas reinhardtii grown at high and low CO2 concentrations

Chloroplasts with high rates of photosynthetic O₂ evolution (up to 120 mol O₂· (mg Chl)^-1·h^-1 compared with 130 mol O₂· (mg Chl)^-1·h^-1 of whole cells) were isolated from Chlamydomonas reinhardtii cells grown in high and low CO₂ concentrations using autolysine-digitonin treatment. At 25° C and pH=7.8, no O₂ uptake could be observed in the dark by high- and low-CO₂ adapted chloroplasts. Light saturation of photosynthetic net oxygen evolution was reached at 800 mol photons·m^-2·s^-1 for high- and low-CO₂ adapted chloroplasts, a value which was almost identical to that observed for whole cells. Dissolved inorganic carbon (DIC) saturation of photosynthesis was reached between 200–300 M for low-CO₂ adapted chloroplasts, whereas high-CO₂ adapted chloroplasts were not saturated even at 700 M DIC. The concentrations of DIC required to reach half-saturated rates of net O₂ evolution (K_m(DIC)) was 31.1 and 156 M DIC for low- and high-CO₂ adapted chloroplasts, respectively. These results demonstrate that the CO₂ concentration provided during growth influenced the photosynthetic characteristics at the whole cell as well as at the chloroplast level.Abbreviations Chl chlorophyll - DIC dissolved inorganic carbon - K_m(DIC) coneentration of dissolved inorganic carbon required for the rate of half maximal net O₂ evolution - PFR photon fluence rate - SPGM silicasol-PVP-gradient medium     

Low-CO2-inducible protein synthesis in the green alga Dunaliella tertiolecta

In the green marine alga Dunaliella tertiolecta, a CO₂-concentrating mechanism is induced when the cells are grown under low-CO₂ conditions (0.03% CO₂). To identify proteins induced under low-CO₂ conditions the cells were labelled with ³⁵SO₄ ^2–, and seven polypeptides with molecular weights of 45, 47, 49, 55, 60, 68 and 100 kDa were detected. The induction of these polypeptides was observed when cells grown in high CO₂ (5% CO₂ in air) were switched to low CO₂, but only while the cultures were growing in light. Immunoblot analysis of total cell protein against pea chloroplastic carbonic anhydrase polyclonal antibodies showed immunoreactive 30-kDa bands in both high- and low-CO₂-grown cells and an aditional 49-kDa band exclusively in low-CO₂-grown cells. The 30-kDa protein was shown to be located in the chloroplast. Western blot analysis of the plasmamembrane fraction against corn plasma-membrane AT-Pase polyclonal antibodies showed 60-kDa bands in both high- and low-CO₂ cell types as well as an immunoreactive 100-kDa band occurring only in low-CO₂-grown cells. These results suggest that there are two distinct forms of both carbonic anhydrase and plasma-membrane ATPase, and that one form of each of them can be regulated by the CO₂ concentration.Abbreviations CA carbonic anhydrase - DIC dissolved inorganic carbon (CO₂+ HCO₃ ^–) - CCM CO₂-concentrating mechanism - low CO₂ air containing 0.03% CO₂ - high CO₂ air supplemented with 5% CO₂ (v/v) We thank Prof. John Coleman for providing antibodies raised against pea chloroplast CA, Dr. James V. Moroney for providing antibodies raised against the 37-kDa periplasmic carbonic anhydrase of CO₂ Chlamydomonas reinhardtii, and Prof. Leonard T. Robert for a gift of corn plasma-membrane 100-kDa ATPase antibodies. We thank Dr. Jeanine Olsen (University of Groningen, the Netherlands) for style comments. This work was supported by the Institute Tecnológico de Canarias (Spain).     

Active uptake of CO2 during photosynthesis in the green alga Eremosphaera viridis is mediated by a CO2-ATPase

Mass spectrometry was used to investigate the uptake of CO₂ in Eremosphaera viridis DeBary. Upon illumination, cells preincubated at pH 7.5 with 100 M dissolved inorganic carbon (DIC) rapidly depleted almost all the free CO₂ from the medium. Rapid equilibrium between HCO ₃ ^- and CO₂ occurred upon addition of bovine carbonic anhydrase (CA) to the medium, showing that CO₂ depletion resulted from a selective uptake of CO₂ rather than an uptake of all inorganic carbon species. Glycolaldehyde (10 mM) completely inhibited CO₂ fixation but had little effect on CO₂ transport. Transfer of glycolaldehyde-treated cells to the dark caused a rapid efflux of CO₂ from the unfixed intracellular DIC pool which was found to be at least threeto sixfold higher in concentration than that of the external medium. These results indicate that E. viridis actively transports CO₂ against a concentration gradient. No external CA was detected in these cells either by potentiometric or mass-spectrometric assay. In the absence of external CA, the rate of photosynthetic O₂ evolution in the pH range 7.5 to 8.0 did not exceed the calculated rate of CO₂ supply, indicating a limited capacity for HCO₂ uptake in these cells. Electrophysiological measurements indicate that CO₂ uptake is electrically silent and thus is not a consequence of H⁺-CO₂ symport activity. Microsomal membranes isolated from Eremosphaera showed ATPase activity which was enhanced by CO₂. These results indicate that active CO₂ uptake is mediated by an ATPase.Abbreviations BTP 1,3-bis[tris(hydroximethyl)-methylamino]-propane - CA carbonic anhydrase - Chl chlorophyll - DIC dissolved inorganic carbon - [¹⁴C]DMO 5,5-dimethyl-[2-¹⁴C]-oxaz-didine-2,4-dione - WA Wilbur-Anderson units This work was supported by grants to B.C. and R.R.L. from the Natural Sciences and Engineering Research Council of Canada. We thank the Department of Biology, Queen's University, Kingston, Ontario for the use of the mass-spectrometer facility. We are indebted to A.G. Miller for his expert advice on operating the mass spectrometer and to Ms. Shahebina Samji for running the Bradford assays.     

Mass Spectrometric Measurement of Intracellular Carbonic Anhydrase Activity in High and Low C(i) Cells of Chlamydomonas: Studies Using O Exchange with C/O Labeled Bicarbonate

By measuring ¹⁸O exchange from doubly labeled CO₂ (¹³C¹⁸O¹⁸O), intracellular carbonic anhydrase activity was studied with protoplasts and chloroplasts isolated from Chlamydomonas reinhardtii grown either on air (low inorganic carbon [C_i]) or air enriched with 5% CO₂ (high C_i). Intact low C_i protoplasts had a 10-fold higher carbonic anhydrase activity than did high C_i protoplasts. Application of dextran-bound inhibitor and quaternary ammonium sulfanilamide, both known as membrane impermeable inhibitors of carbonic anhydrase, had no influence on the catalysis of ¹⁸O exchange, indicating that cross-contamination with extracellular carbonic anhydrase was not responsible for the observed activity. This intracellular in vivo activity from protoplasts was inhibited by acetazolamide and ethoxyzolamide. Intracellular carbonic anhydrase activity was partly associated with intact chloroplasts isolated from high and low C_i cells, and the latter had a sixfold greater rate of catalysis. The presence of dextran-bound inhibitor had no effect on chloroplast-associated carbonic anhydrase, whereas 150 micromolar ethoxyzolamide caused a 61 to 67% inhibition of activity. These results indicate that chloroplastic carbonic anhydrase was located within the plastid and that it was relatively insensitive to ethoxyzolamide. Carbonic anhydrase activity in crude homogenates of protoplasts and chloroplasts was about six times higher in the low C_i than in high C_i preparations. Further separation into soluble and insoluble fractions together with inhibitor studies revealed that there are at least two different forms of intracellular carbonic anhydrase. One enzyme, which was rather insoluble and relatively insensitive to ethoxyzolamide, is likely an intrachloroplastic carbonic anhydrase. The second carbonic anhydrase, which was soluble and sensitive to ethoxyzolamide, is most probably located in an extrachloroplastic compartment.     

Carbonic anhydrase activity in leaves as measured in vivo by18O exchange between carbon dioxide and water

Carbonic anhydrase activity of intactCommelina communis L. leaves was measured using mass spectrometry, by following the¹⁸O-exchange kinetics between¹⁸O-enriched carbon dioxide and water. A gas-diffusion model (Gerster, 1971, Planta97, 155–172) was used to interpret the¹⁸O-exchange kinetics and to determine two constants, one (k) related to the hydration of CO₂ and the other (k_e), related to the diffusion of CO₂. Both constants were determined inCommelina communis L. leaves after stripping the lower epidermis to remove any stomatal influence. The hydration constant (k) was 17200 +2200 ·min^–1 (mean±SD, 12 experiments), i.e., about 8 600 times the uncatalyzed hydration of CO₂ in pure water, and was specifically inhibited by ethoxyzolamide, a powerful inhibitor of carbonic anhydrases, half-inhibition occurring around 10^–5 Methoxyzolamide. The diffusion constant (k_e) was 1.18±0.28·min^–1 (mean±SD, 12 experiments) and was only slightly inhibited (about 20%) by ethoxyzolamide. Carbonic anhydrase activity of stripped leaves was not affected by the leaf water status (up to 50% relative water deficits), was strongly inhibited by monovalent anions such as Cl^– or NO ₃ ^– , and decreased by about 50% when the photon flux density during growth was increased from 100 to 500 mol photons·m^–2·s^–1. By studying the effect of ethoxyzolamide (10^–4 M) on photosynthetic O₂ exchange, measured using¹⁸O₂ and mass spectrometry, we found that inhibition of carbonic anhydrase activity by 92–95% had little effect on the response curves of net O₂ evolution to increased CO₂ concentrations. Ethoxyzolamide had no effect on the photosynthetic electron-transport rate, measured as gross O₂ photosynthesis at high CO₂ concentration (>350 l·^–1), but was found to increase both gross O₂ photosynthesis and O₂ uptake at lower CO₂ levels. The chloroplastic CO₂ concentration calculated from O₂-exchange data was not significantly modified by ethoxyzolamide. We conclude from these results that, under normal conditions of photosynthesis, most of the carbonic anhydrase activity is not involved in CO₂ assimilation. Measurement of carbonic anhydrase activity using¹⁸O-isotope exchange therefore provides a suitable model to study the in-vivo regulation of this chloroplastic enzyme in plants submitted to various environmental conditions.Abbreviations CA carbonic anhydrase - C_cc chloroplastic CO₂ concentration - C_e external CO₂ concentration - EZA ethoxyzolamide - k CO₂ hydration rate constant - k_e CO₂ diffusion rate constan - PPFD photosynthetic photon flux density - Rubisco ribulose-1,5 bisphosphate carboxylase oxygenase - RWD relative water deficit The authors wish to thank P. Carrier for technical assistance with mass-spectrometric experiments and Dr. P. Thibault for helpful suggestions and comments. Dr. A. Vavasseur is gratefully acknowledged for supplyingCommelima communis. cultures. P.C., P.T. and A.V. are all from the CEA, Département de Physiologie Végétale et Ecosystèmes, Cadarache, France.