EFFECTS OF CO2 ENRICHMENT ON THE BLOOM‐FORMING CYANOBACTERIUM MICROCYSTIS AERUGINOSA (CYANOPHYCEAE): PHYSIOLOGICAL RESPONSES AND RELATIONSHIPS WITH THE AVAILABILITY OF DISSOLVED INORGANIC CARBON1

Microcystis aeruginosa Kütz. 7820 was cultured at 350 and 700 μL·L ^{? 1} CO₂ to assess the impacts of doubled atmospheric CO₂ concentration on this bloom‐forming cyanobacterium. Doubling of CO₂ concentration in the airflow enhanced its growth by 52%–77%, with pH values decreased and dissolved inorganic carbon (DIC) increased in the medium. Photosynthetic efficiencies and dark respiratory rates expressed per unit chl a tended to increase with the doubling of CO₂. However, saturating irradiances for photosynthesis and light‐saturated photosynthetic rates normalized to cell number tended to decrease with the increase of DIC in the medium. Doubling of CO₂ concentration in the airflow had less effect on DIC‐saturated photosynthetic rates and apparent photosynthetic affinities for DIC. In the exponential phase, CO₂ and HCO₃ ^? levels in the medium were higher than those required to saturate photosynthesis. Cultures with surface aeration were DIC limited in the stationary phase. The rate of CO₂ dissolution into the liquid increased proportionally when CO₂ in air was raised from 350 to 700 μL·L ^{? 1}, thus increasing the availability of DIC in the medium and enhancing the rate of photosynthesis. Doubled CO₂ could enhance CO₂ dissolution, lower pH values, and influence the ionization fractions of various DIC species even when the photosynthesis was not DIC limited. Consequently, HCO₃ ^? concentrations in cultures were significantly higher than in controls, and the photosynthetic energy cost for the operation of CO₂ concentrating mechanism might decrease.     

THE INORGANIC CARBON REQUIREMENTS OF CHLAMYDOMONAS SEGNIS (CHLOROPHYCEAE) FOR CELL DEVELOPMENT IN SYNCHRONOUS CULTURES1

The time in the cell cycle when CO₂ provision was required for cell development and division was determined in synchronous cultures of Chlamydomonas segnis Ettl bubbled with air (0.03% CO₂) or air enriched with 5% CO₂ under continuous light at 25°C and pH 7. Provision of CO₂ (% in air v/v) during the G₁-phase was found to be essential for the completion of the cell cycle. There was no demand for CO₂ supply throughout the S-phase and mitosis. Using cultures adapted to CO₂ concentrations ranging from 0.03 to 5% in air, the apparent CO₂ concentration (K_m) required for the cells to develop during the G_-1-phase and to attain one half the maximal rates of photo-synthetic O₂ evolution was calculated as 0.05%. This value increased to 0.1 and 0.5% during the S-phase. For total protein and carbohydrate accumulation, which would reflect inorganic carbon (CO₂+ HCO₃^?) assimilation, the K_m (% CO₂) were ca. 0.1 and 0.14 throughout the cell cycle, respectively. The CO₂ concentration at which the cells exhibited the shortest generation time (6.7 h) was 0.1%. These results showed that during development, cells photosynthesizing (evolving O₂) at maximal rates but accumulating protein and carbohydrate at one half the maximal rates or less would complete their vegetative life cycle in the shortest time.     

Inorganic carbon acquisition in the acid‐tolerant alga Chlorella kessleri

The ability of the freshwater alga, Chlorella kessleri, to maintain a carbon concentrating mechanism when grown at acid pH was investigated. The alga grows over the pH range 4.0–9.0 and was found to take up bicarbonate and CO₂ actively when grown at pH 6.0. However, when grown at acid pH (below 5.5), it does not have active CO₂ uptake. The acidotolerant species maintained an internal pH of 6.1–7.5 over the external pH range 4.5–7.5, thus the pH difference between the cell interior and the external medium was large enough to allow for the diffusive uptake of CO₂ at acid external pH. Mass spectrometric monitoring of O₂ and CO₂ fluxes by suspensions of C. kessleri, grown at acid pH, and maintained at pH 7.5 showed that the rates of O₂ evolution did not exceed those of CO₂ uptake. The final CO₂ compensation concentrations of 14.0–17.7 µM reached by photosynthetic cells were above the CO₂ equilibrium concentration in the external medium, indicating a lack of active CO₂ uptake at acid pH. Chlorella kessleri accumulated CO₂ with internal concentrations that were 9.9, 18.7 and 22.7‐fold that of the external medium for cells grown, respectively, at pH 4.5, 5.0 and 5.5. The ability of C. kessleri cells to accumulate high intracellular concentrations of inorganic carbon at acid pH would provide a sufficiently high concentration of CO₂ at the active site of Rubisco thus allowing the alga to maintain growth rates similar to those at alkaline pH.     

Effect of CO2 on uninfected Sf‐9 cell growth and metabolism

A problem in the mass production of recombinant proteins and biopesticides using insect cell culture is CO₂ accumulation. This research investigated the effect of elevated CO₂ concentration on insect cell growth and metabolism. Spodoptera frugiperda Sf‐9 insect cells were grown at 20% air saturation, 27^°C, and a pH of 6.2. The cells were exposed to a constant CO₂ concentration by purging the medium with CO₂ and the headspace with air. The population doubling time (PDT) of Sf‐9 cells increased with increasing CO₂ concentration. Specifically, the PDT for 0‐37, 73, 147, 183, and 220 mm Hg CO₂ concentrations were 23.2 ± 6.7, 32.4 ± 7.2, 38.1 ± 13.3, 42.9 ± 5.4, and 69.3 ± 35.9 h (n = 3 or 4, 95% confidence level), respectively. The viability of cells in all experiments was above 90%, i.e., while increased CO₂ concentrations inhibited cell growth, it did not affect cell viability. The osmolality for all bioreactor experiments was observed to be 300–360 mOsm/kg, a range that is known to have a negligible effect on insect cell culture. Elevated CO₂ concentration did not significantly alter the cell specific glucose consumption rate (2.5–3.2 × 10^?17 mol/cell s), but slightly increased the specific lactate production rate from ?3.0 × 10^?19 to 10.2 × 10^?19 mol/cell s. Oxidative stress did not contribute to CO₂ inhibition in uninfected Sf‐9 cells as no significant increase in the levels of lipid hydroperoxide and protein carbonyl concentrations was discovered at elevated CO₂ concentration. © 2016 American Institute of Chemical Engineers Biotechnol. Prog., 32:465–469, 2016     

PHYSIOLOGICAL CHARACTERISTICS OF PHOTOSYNTHESIS IN PORPHYRIDIUM CRUENTUM: EVIDENCE FOR BICARBONATE TRANSPORT IN A UNICELLULAR RED ALGA1

Various physiological characteristics of photosynthesis in the unicellular red alga Porphyridium cruentum Naegeli have been investigated. The rate of photosynthesis was optimal at 25° C and pH 7.5 and was not inhibited by 21% oxygen over a temperature range of 5 to 35° C. Kinetics of whole cell photosynthesis as a function of substrate concentration gave a K_1/2, (CO₂) of 0.3 μM. CO₂ compensation point, measured in a closed system at pH 7.5, was a constant 6.7 m?L · L^?1 over the temperature range 15 to 30° C and was unaffected by O₂ concentration. Whole cell photosynthesis, measured in a closed system at alkaline pH, showed that the rates of oxygen evolution were greatly in excess of the rate of CO₂ supply from the spontaneous dehydration of HCO₃^? in the medium. This indicates that bicarbonate is utilized by the cell to support this photosynthetic rate. These physiological characteristics of Porphyridium cruentum are consistent with the hypothesis that this alga transports bicarbonate across the plasmalemma.     

UPTAKE,EFFLUX, AND PHOTOSYNTHETIC UTILIZATION OF INORGANIC CARBON BY THE MARINE EUSTIGMATOPHYTE NANNOCHLOROPSIS SP.1

Uptake, efflux and utilization of inorganic carbon were investigated in the marine eustigmatophyte Nannochloropsis sp. grown under an air level of CO₂. Maximal photosynthetic rate was hardly affected by raising the pH porn 5.0 to 9.0. The apparent photosynthetic affinity for dissolved inorganic carbon (DIC) was 35 μM DIC between pH 6.5 to 9.0, but increased approximately threefold at pH 5.0 suggesting that HCO₃- was the main DIC species used from the medium. No external carbonic anhydrase (CA) activity could be detected by the pH drift method. However, application of ethoxyzolamide (an inhibitor of CA) resulted an a significant inhibition of photosynthetic O₂ evolution and carbon utilization, suggesting involvement of internal CA or CA-like activity in DIC utilization. Under high light conditions, the rate of HCO₃^? uptake and its internal conversion to CO₂ apparently exceeded the rate of carbon fixation, resulting in a large leak of CO₂ from the cells to the external medium. When the cells were exposed to low DIC concentrations, the ratio of internal to external DIC concentration was about eight. On the other hand, in the presence of 2 mM DIC, conditions prevailing in the marine environment, the internal concentration of DIC was only 50% higher than the external one.     

INDUCIBLE MECHANISMS FOR HCO3– UTILIZATION AND REPRESSION OF PHOTORESPIRATION IN PROTOPLASTS AND THALLI OF THREE SPECIES OF ULVA (CHLOROPHYTA)1

Thalli of Ulva reticulata Forskaal, Ulva rigida C. Ag., and Ulva pulchra Jaasund were incubated at different concentrations of dissolved CO₂. Incubation at a high CO₂ concentration resulted in decreased oxygen evolution rate and lower affinity for inorganic carbon at high pH conditions, i.e. the ability to use HCO₃^– as a carbon source was reduced. This effect was reversible, and plants regained this HCO₃^– uptake capacity when transferred to air concentrations of CO₂. The phytosynthetic oxygen evolution rate of plants grown at high CO₂ concentration was reduced by high O₂ concentrations, whereas thalli and protoplasts from cultures grown at air concentration were not affected. This is interpreted as a deactivation of the carbon-concentrating mechanism during conditions of high CO₂ resulting in high photorespiration when plants are exposed to high O₂ concentrations. Protoplasts were not affected by high O₂ to the same extent and were not able to utilize HCO₃^– from the medium. The algae were able to grow at very low CO₂ concentrations, but growth was suppressed when an inhibitor of external carbonic anhydrase was present. Assay of carbonic anhydrase activities showed that external and internal CA activities were lower in plants grown at a high CO₂ concentration compared to plants grown at a low concentration of CO₂. Possible mechanisms for HCO₃^– utilization in these Ulva species are discussed.     

PHOTOSYNTHETIC INORGANIC CARBON ACQUISITION IN AN ACID‐TOLERANT,FREE‐LIVING SPECIES OF COCCOMYXA (CHLOROPHYTA)1

The processes of CO₂ acquisition were characterized for the acid‐tolerant, free‐living chlorophyte alga, CPCC 508. rDNA data indicate an affiliation to the genus Coccomyxa, but distinct from other known members of the genus. The alga grows over a wide range of pH from 3.0 to 9.0. External carbonic anhydrase (CA) was detected in cells grown above pH 5, with the activity increasing marginally from pH 7 to 9, but most of the CA activity was internal. The capacity for HCO₃^? uptake of cells treated with the CA inhibitor acetazolamide (AZA), was investigated by comparing the calculated rate of uncatalyzed CO₂ formation with the rate of photosynthesis. Active bicarbonate transport occurred in cells grown in media above pH 7.0. Monitoring CO₂ uptake and O₂ evolution by membrane‐inlet mass spectrometry demonstrated that air‐grown cells reduced the CO₂ concentration in the medium to an equilibrium concentration of 15 μM, but AZA‐treated cells caused a drop in extracellular CO₂ concentration to a compensation concentration of 27 μM at pH 8.0. CO₂‐pulsing experiments with cells in the light indicated that the cells do not actively take up CO₂. An internal pool of unfixed inorganic carbon was not detected at the CO₂ compensation concentration, probably because of the lack of active CO₂ uptake, but was detectable at times before compensation point was reached. These results indicate that this free‐living Coccomyxa possesses a CO₂‐concentrating mechanism (CCM) due to an active bicarbonate‐uptake system, unlike the Coccomyxa sp. occurring in symbiotic association with lichens.     

EVOLUTIONARY RESPONSES OF A COCCOLITHOPHORID GEPHYROCAPSA OCEANICA TO OCEAN ACIDIFICATION

The ongoing ocean acidification associated with a changing carbonate system may impose profound effects on marine planktonic calcifiers. Here, we show that a coccolithophore, Gephyrocapsa oceanica, evolved in response to an elevated CO₂ concentration of 1000 μatm (pH reduced to 7.8) in a long‐term (～670 generations) selection experiment. The high CO₂‐selected cells showed increases in photosynthetic carbon fixation, growth rate, cellular particulate organic carbon (POC) or nitrogen (PON) production, and a decrease in C:N elemental ratio, indicating a greater upregulation of PON than of POC production under the ocean acidification condition. Cells from the low CO₂ selection process shifted to high CO₂ exposure showed an enhanced cellular POC and PON production rates. Our data suggest that the coccolithophorid could adapt to ocean acidification with enhanced assimilations of carbon and nitrogen but decreased C:N ratios.     

INTERACTION OF LEUCINE, GLUCOSE, AND KETONE METABOLISM IN RAT BRAIN IN VITRO

Brain cortex slices from fed, 48 h and 120 h fasted rats were incubated and ¹⁴CO₂ was measured from (a) [U-¹⁴C]glucose (5 mm ) either alone or in the presence of l -lcucine (0.1 or 1 mm ), and (b) [U-¹⁴C]leucine or [l-¹⁴C]leucine at 0.1 or 1 mm with or without glucose (5 mm ). In other experiments, sodium dl -3-hydroxybutyrate (3-OHB) or acetoacetate (AcAc) at 1 or 5 mm were added in the above incubation mixture. The rate of conversion of [U¹⁴C]glucose to CO₂ was decreased 20% by leucine at 1 mm and 30–50% by 3-OHB at 1 or 5 mm but not by leucine at 0.1 mm . The effects of 3-OHB and of leucine (1 mm ) were not additive. The effects of leucine were similar in the fed and fasted rats. The rate of conversion of [U-¹⁴C]leucine or [l-^,4C]leucine to ¹⁴CO₂ at 0.1 mm and 1.0 mm was increased by glucose (35%) in the fed or fasted rats. Ketone bodies in the absence of glucose had no effect on leucine oxidation. However, the stimulatory effect of glucose on the rate of conversion of leucine to CO₂ was inhibited by 3-OHB at 5 mm . These results suggest that (a) leucine in increased concentrations (1 mm ) may reduce glucose oxidation by brain cortex while itself becoming an oxidative fuel for brain, and (b) leucine oxidation by brain may be influenced by the prevailing glucose and ketone concentrations.     

Inorganic Carbon Source for Photosynthesis in the Seagrass Thalassia hemprichii (Ehrenb.) Aschers

Photosynthetic carbon uptake of the tropical seagrass Thalassia hemprichii (Ehrenb.) Aschers was studied by several methods. Photosynthesis in buffered seawater in media in the range of pH 6 to pH 9 showed an exponentially increasing rate with decreasing pH, thus indicating that free CO₂ was a photosynthetic substrate. However, these experiments were unable to determine whether photosynthesis at alkaline pH also contained some component due to HCO₃⁻ uptake. This aspect was further investigated by studying photosynthetic rates in a number of media of varying pH (7.8-8.61) and total inorganic carbon (0.75-13.17 millimolar). In these media, photosynthetic rate was correlated with free CO₂ concentration and was independent of the HCO₃⁻ concentration in the medium. Short time-course experiments were conducted during equilibration of free CO₂ and HCO₃⁻ after injection of ¹⁴C labeled solution at acid or alkaline pH. High initial photosynthetic rates were observed when acidic solutions (largely free CO₂) were used but not with alkaline solutions. The concentration of free CO₂ was found to be a limiting factor for photosynthesis in this plant.     

THE EFFECT OF pH ON GROWTH, PROTEIN SYNTHESIS, AND LIPID-RICH PARTICLES OF CULTURED MAMMALIAN CELLS

A simple procedure has been established for controlling and measuring the pH of media in which the bicarbonate-carbonic acid system is the predominant buffer. The HCO^-₃ concentration was maintained at 22.5 mM and the H₂CO₃ concentration was varied by equilibrating the media with 0.5 to 40 per cent CO₂ in air. The curve relating extracellular pH to 3 day cell growth was similar for glass-attached HeLa and Chang liver cells. Maximum growth occurred over a pH range of 7.38 to 7.87. Cell growth declined precipitously on the alkaline side and more gradually on the acid side of the optimal pH range. Comparable pH growth curves were also obtained with newly isolated cells from rat liver and skeletal muscle. It was shown that the effect of pH on growth was independent of the CO₂ concentration and that the essential nutrients in the medium were stable over the pH range studied. Although alkalosis depressed the 3 day cell population, cells exposed to a pH of 8.0 to 8.2 grew at the maximal rate for the first 12 to 24 hours. Growth then ceased abruptly and the cells entered a steady state with respect to net protein synthesis. This was followed by cytoplasmic retraction and cell death. Increasing the concentrations of calcium or magnesium in the medium failed to prevent the effects of alkalosis. Moreover, the increase in CO^-₃ concentration of the media and the concomitant decrease in Ca⁺⁺ ion concentration that occur at high pH were eliminated as determining factors in the growth failure and death. While acidosis had a less pronounced effect on the 3 day cell population, its effect on the growth rate was immediate. The increase in cell generation time was proportional to the H⁺ ion concentration. In each of the cell lines studied, acidosis was accompanied by a striking increase in the number of cytoplasmic perinuclear granules. These granules which stain supravitally with Janus green are extracted from fixed cells with lipid solvents. They maintain their identity in cell homogenates and may be isolated from the other subcellular structures by differential centrifugation; at 100,000 g they form a distinct layer at the top of the supernatant fraction. On the basis of their physical and chemical properties, these granules have been called lipid-rich particles. The accumulation of lipid-rich particles in acidosis was independent of the growth rate and the CO₂ concentration.     

The Effect of Various Carbonate Sources on the Survival of Escherichia coli in Dairy Cattle Manure

Manure slurries (n = 3) prepared from the feces and urine of lactating dairy cattle (1 part urine, 2.2 parts feces, and 6.8 parts distilled water) had an initial pH of 8.6 ± 0.1; dissolved carbonate concentrations of 48 ± 4 mm, and Escherichia coli counts of 5.9 ± 0.7 logs per ml slurry. The pH of untreated slurries declined to pH 7.0 ± 0.1 by the 10th day of incubation, and the E. coli count increased approximately 10-fold (P < 0.05). When slurries were treated with Na₂CO₃, K₂CO₃, NaHCO₃ or Na₂CO₃·NaHCO₃ (0 to 16 g/kg slurry), the dissolved carbonates increased in a linear fashion, but only Na₂CO₃ and K₂CO₃ (8 g/kg or greater) or Na₂CO₃·NaHCO₃ (16 g/kg) ensured an alkaline pH. Even relatively low concentrations of Na₂CO₃ or K₂CO₃ (8 or 12 g/kg) caused a decrease in E. coli viability (P < 0.05), and E. coli could not be detected if 16 g/kg was added (day 5 or 10 of incubation). Na₂CO₃·NaHCO₃ also caused a decrease in E. coli viability, (P < 0.05), but some E. coli (approximately 10⁴ cells per g) were detected on day 10 even if the concentration was 16 g/kg. NaHCO₃ did not prevent the decrease in pH or cause a decrease in E. coli numbers (P > 0.05). Calculations based on the Henderson-Hasselbalch equation (pH and dissolved carbonates) indicated that little E. coli killing was noted until the dissolved carbonate anion concentrations (CO₃ ⁻²) were greater than 1 mm, but bicarbonate anion (HCO₃ ⁻) concentrations as high as 180 mm did not affect E. coli viability. These results are consistent with the idea that carbonate anion has antimicrobial properties and can kill E. coli in dairy cattle manure. Received: 20 December 2000 / Accepted: 7 February 2001     

The physiological response of marine diatoms to ocean acidification: differential roles of seawater pCO2 and pH

Although increasing the pCO₂ for diatoms will presumably down‐regulate the CO₂‐concentrating mechanism (CCM) to save energy for growth, different species have been reported to respond differently to ocean acidification (OA). To better understand their growth responses to OA, we acclimated the diatoms Thalassiosira pseudonana, Phaeodactylum tricornutum, and Chaetoceros muelleri to ambient (pCO₂ 400 μatm, pH 8.1), carbonated (pCO₂ 800 μatm, pH 8.1), acidified (pCO₂ 400 μatm, pH 7.8), and OA (pCO₂ 800 μatm, pH 7.8) conditions and investigated how seawater pCO₂ and pH affect their CCMs, photosynthesis, and respiration both individually and jointly. In all three diatoms, carbonation down‐regulated the CCMs, while acidification increased both the photosynthetic carbon fixation rate and the fraction of CO₂ as the inorganic carbon source. The positive OA effect on photosynthetic carbon fixation was more pronounced in C. muelleri, which had a relatively lower photosynthetic affinity for CO₂, than in either T. pseudonana or P. tricornutum. In response to OA, T. pseudonana increased respiration for active disposal of H⁺ to maintain its intracellular pH, whereas P. tricornutum and C. muelleri retained their respiration rate but lowered the intracellular pH to maintain the cross‐membrane electrochemical gradient for H⁺ efflux. As the net result of changes in photosynthesis and respiration, growth enhancement to OA of the three diatoms followed the order of C. muelleri > P. tricornutum > T. pseudonana. This study demonstrates that elucidating the separate and joint impacts of increased pCO₂ and decreased pH aids the mechanistic understanding of OA effects on diatoms in the future, acidified oceans.     

ACQUISITION OF INORGANIC CARBON BY THE MARINE HAPTOPHYTE ISOCHRYSIS GALBANA (PRYMNESIOPHYCEAE)1

Inorganic carbon acquisition has been investigated in the marine haptophyte Isochrysis galbana. External carbonic anhydrase (CA) was present in air‐grown (0.034% CO₂) cells but completely repressed in high (3%) CO₂‐grown cells. External CA was not inhibited by 1.0 mM acetazolamide. The capacity of cells to take up bicarbonate was examined by comparing the rate of photosynthetic O₂ evolution with the calculated rate of spontaneous CO₂ supply; at pH 8.2 the rates of O₂ evolution exceeded the CO₂ supply rate 14‐fold, indicating that this alga was able to take up HCO₃ ^? . Monitoring CO₂ concentrations by mass spectrometry showed that suspensions of high CO₂‐grown cells caused a rapid drop in the extracellular CO₂ in the light and addition of bovine CA raised the CO₂ concentration by restoring the HCO₃ ^? ‐CO₂ equilibrium, indicating that cells were maintaining the CO₂ in the medium below its equilibrium value during photosynthesis. A rapid increase in extracellular CO₂ concentration occurred on darkening the cells, indicating that the cells had accumulated an internal pool of unfixed inorganic carbon. Active CO₂ uptake was blocked by the photosynthetic electron transport inhibitor 3‐(3′,4′‐dichlorphenyl)‐1,1‐dimethylurea, indicating that CO₂ transport was supported by photosynthetic reactions. These results demonstrate that this species has the capacity to take up HCO₃ ^? and CO₂ actively as sources of substrate for photosynthesis and that inorganic carbon transport is not repressed by growth on high CO₂, although external CA expression is regulated by CO₂ concentration.     

Chlorella vulgaris (Chlorellaceae) does not secrete autoinhibitors at high cell densities

Filtrates (conditioned medium) from high-density Chlorella vulgaris cultures in photobioreactors were obtained and tested for autoinhibitory activity under different conditions. Exponentially growing cells were inoculated at low initial cell concentration (2 × 10⁵ cells/ml) in 90% conditioned medium (CM) supplemented with 10% fresh medium (FM) at low (atmospheric) CO₂ levels. The time sequence of DNA histograms of cells in CM cultures showed that there is an accumulation of cells with two and four DNA equivalents in the culture over a period of time, signifying a blockage of cells at the division stage of the cell cycle. Examination of the chemical composition of CM showed the presence of high concentrations (> 10 mM) of bicarbonate. Adding similar bicarbonate concentrations to FM were found to have similar effects as CM cultures, causing blockage of cell division, though the intensity of the blocking effect was lower. The bicarbonate-free CM did not show any cell cycle modulating or inhibitory activity. The growth of cells cultivated at high (5%) CO₂ levels in 90% CM supplemented with 10% FM was comparable to 10% FM cultures, indicating nutrient limitation in 90% CM culture. When the 90% CM culture was supplemented with 100% nutrients, the growth rate and final cell concentration was similar to 100% FM culture. Based on these results we conclude that C. vulgaris does not secrete any autoinhibitor(s) or cell cycle modulating compound(s) under the conditions from which the CM was obtained.     

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.     

UPTAKE OF INORGANIC CARBON BY CLADOPHORA GLOMERATA (CHLOROPHYTA) FROM THE BALTIC SEA1

Carbon uptake in the green macroalga Cladophora glomerata (L.) Kütz. from the brackish Baltic Sea was studied by recording changes in pH, alkalinity, and inorganic carbon concentration of the seawater medium during photosynthesis. The use of specific inhibitors identified three uptake mechanisms: 1) dehydration of HCO₃ ^? into CO₂ by periplasmic carbonic anhydrase, followed by diffusion of CO₂ into the cell; 2) direct uptake of HCO₃ ^? via a 4,4′‐diisothiocyanato‐stilbene‐2,2′‐disulfonate‐sensitive mechanism; and 3) uptake of inorganic carbon by the involvement of a vanadate‐sensitive P‐type H ⁺ ‐ATPase (proton pump). A decrease in the alkalinity of the seawater medium during carbon uptake, except when treated with vanadate, indicated a net uptake of the ionic species contributing to alkalinity (i.e. HCO₃ ^? , CO₃^{2 ?} , and OH ^? ) from the medium, where OH ^? influx is equivalent to H ⁺ efflux. This would suggest that the proton pump is involved in HCO₃ ^? transport. We also show that the proton pump can be induced by carbon limitation. The inducibility of carbon uptake in C. glomerata may partly explain why this species is so successful in the upper littoral zone of the Baltic Sea. Usually, carbon limitation is not a problem in the upper littoral of the sea. However, it may occur frequently within dense Cladophora belts with high photosynthetic rates that create high pH and low carbon concentrations in the alga's microenvironment.     

KINETICS OF THE SODIUM-DEPENDENT TRANSPORT OF GAMMA-AMINOBUTYRIC ACID BY SYNAPTOSOMES

The kinetics of transport of gamma-aminobutyric acid [2,3-³H] by synaptosomes from rat brain was studied by means of a rapid filtration technique. The rate of uptake was proportional to the protein concentration over the range 0.05—0.2 mg of synaptosomal protein per ml. Although apparent allosteric kinetics were observed with sodium, transport followed simple saturation kinetics with respect to GABA and no heterotropic, cooperative effects of GABA on sodium on kinetics were observed. A minimum of three interacting sodium sites is suggested the basis of Hill plots of the sodium data. Both the apparent K_m and V_max for GABA were functions of the sodium ion concentration but the effect of sodium was considerably greater on V_max than on the apparent K_m The V_max for GABA was 1.1 ± 0.5 nmol.min^?1 mg^?1 of protein at 95 mm sodium and decreased to 12 per Cent of this value at 19 mm sodium. The apparent K^m for GABA increased from 4.0 ± 1.0 μm at 95 mm sodium to 8.4 ± 2.0 μm at 19 mm sodium. Potassium was a noncompetitive inhibitor with respect to GABA and did not affect the apparent cooperativity observed with sodium. These findings are discussed in terms of models of GABA transport.     

PHOTOSYNTHETIC UTILIZATION OF INORGANIC CARBON IN THE ECONOMIC BROWN ALGA,HIZIKIA FUSIFORME (SARGASSACEAE) FROM THE SOUTH CHINA SEA1

The mechanism of inorganic carbon (C_i) acquisition by the economic brown macroalga, Hizikia fusiforme (Harv.) Okamura (Sargassaceae), was investigated to characterize its photosynthetic physiology. Both intracellular and extracellular carbonic anhydrase (CA) were detected, with the external CA activity accounting for about 5% of the total. Hizikia fusiforme showed higher rates of photosynthetic oxygen evolution at alkaline pH than those theoretically derived from the rates of uncatalyzed CO₂ production from bicarbonate and exhibited a high pH compensation point (pH 9.66). The external CA inhibitor, acetazolamide, significantly depressed the photosynthetic oxygen evolution, whereas the anion‐exchanger inhibitor 4,4′‐diisothiocyano‐stilbene‐2,2′‐disulfonate had no inhibitory effect on it, implying the alga was capable of using HCO₃^? as a source of C_i for its photosynthesis via the mediation of the external CA. CO₂ concentrations in the culture media affected its photosynthetic properties. A high level of CO₂ (10,000 ppmv) resulted in a decrease in the external CA activity; however, a low CO₂ level (20 ppmv) led to no changes in the external CA activity but raised the intracellular CA activity. Parallel to the reduction in the external CA activity at the high CO₂ was a reduction in the photosynthetic CO₂ affinity. Decreased activity of the external CA in the high CO₂ grown samples led to reduced sensitiveness of photosynthesis to the addition of acetazolamide at alkaline pH. It was clearly indicated that H. fusiforme, which showed CO₂‐limited photosynthesis with the half‐saturating concentration of C_i exceeding that of seawater, did not operate active HCO₃^? uptake but used it via the extracellular CA for its photosynthetic carbon fixation.