Studies of Elodea nuttallii grown under photorespiratory conditions. I. Photosynthetic characteristics

Abstract. The photosynthetic characteristics of Elodea nuttallii grown in wastewater in continuous flow reactors in a greenhouse were investigated. The diurnal changes in dissolved inorganic carbon (DIC), dissolved oxygen (DO) and pH were monitored. Photosynthesis removed both CO₂(aq) and HCO₃^? from the reactors. A stoichiometry of 1.19:1 was observed between HCO₃^? removal during photosynthesis and OH^? production during photosynthesis, consistent with theories regarding direct bicarbonate utilization. In laboratory experiments, the light compensation points (г_PPFD) were similar (31–35μmol m^?2 s^?1) to reported values for other macrophytes; however, the light saturation level was high (1100μmol m^?2 s^?1) and similar to values reported for aerial portions Of heterophyllous macrophytes. The kinetics of photosynthetic oxygen evolution (K_m (CO₂) = 96mmol m^?3; V_max= 133mmol g^?1 Chl h^?1) and the CO₂ compensation point (г= 44cm³ m^?3) suggested an adaptive, low photorespiratory state in response to low carbon concentrations. Photosynthetic V_max values were slightly, but significantly higher (P 0.001) at pH 8.0 compared to pH 4.5. While CO₂ utilization at pH 8 could account for most of the observed phototsynthetic rates, an HCO₃^? component was present, suggesting two separate transport systems for HCO₃^? and CO₂(aq) in E. nuttallii. The activity of RUBISCO (160.3 mmol g^?1 Chl h^?1 was one of the highest reported values for aquatic macrophytes. Compared to RUBISCO, we observed lower activities of the β-carboxylating enzymes phopho enolpyruvate carboyxlase (PEPcase), 24.1 mmol g^?1 Chl h^?1; phosphor enol pyruvate carboxykinase (PEPCKase), 14 mmol g^?1 Chl h^?1. This suggests that the potential light-independent fixation of carbon in E. nuttallii was much less than RUBISCO-dependent fixation. The RUBISCO/PEPcase ratio was 6.6, indicating that E. nuttallii was similar to Myriophyllum sp. in possessing a physiological adaptation to low CO₂ levels which is hypothesized to include carbonic anhydrase (CA) and an active transport system for HCO₃^?. CA levels were surprisingly low in E. nuttallii (14.2 EUmg Chl^?).     

Regulation of the induction of bicarbonate uptake by dissolved CO2 in the marine diatom, Phaeodactylum tricornutum

Physiological properties of photosynthesis were determined in the marine diatom, Phaeodactylum tricornutum UTEX640, during acclimation from 5% CO₂ to air and related to H₂CO₃ dissociation kinetics and equilibria in artificial seawater. The concentration of dissolved inorganic carbon at half maximum rate of photosynthesis (K_0·5[DIC]) value in high CO₂‐grown cells was 1009 mmol m ^{? 3} but was reduced three‐fold by the addition of bovine carbonic anhydrase (CA), whereas in air‐grown cells K_0·5[DIC] was 71 mmol m ^{? 3}, irrespective of the presence of CA. The maximum rate of photosynthesis (P_max) values varied between 300 and 500 μ mol O₂ mg Chl ^{? 1} h ^{? 1} regardless of growth pCO₂. Bicarbonate dehydration kinetics in artificial seawater were re‐examined to evaluate the direct HCO₃ ^? uptake as a substrate for photosynthesis. The uncatalysed CO₂ formation rate in artificial seawater of 31·65°/_oo of salinity at pH 8·2 and 25 °C was found to be 0·6 mmol m ^{? 3} min ^{? 1} at 100 mmol m ^{? 3} DIC, which is 53·5 and 7·3 times slower than the rates of photosynthesis exhibited in air‐ and high CO₂‐grown cells, respectively. These data indicate that even high CO₂‐grown cells of P. tricornutum can take up both CO₂ and HCO₃ ^? as substrates for photosynthesis and HCO₃ ^? use improves dramatically when the cells are grown in air. Detailed time courses were obtained of changes in affinity for DIC during the acclimation of high CO₂‐grown cells to air. The development of high‐affinity photosynthesis started after a 2–5 h lag period, followed by a steady increase over the next 15 h. This acclimation time course is the slowest to be described so far. High CO₂‐grown cells were transferred to controlled DIC conditions, at which the concentrations of each DIC species could be defined, and were allowed to acclimate for more than 36 h. The K_0·5[DIC] values in acclimated cells appeared to be correlated only with [CO_2(aq)] in the medium but not to HCO₃ ^? , CO₃^{2 ?} , total [DIC] or the pH of the medium and indicate that the critical signal regulating the affinity of cells for DIC in the marine diatom, P. tricornutum, is [CO_2(aq)] in the medium.     

The active uptake of carbon dioxide by the marine diatoms Phaeodactylum ticornutum and Cyclotella sp.

Mass spectromelry has been used to investigate the uptake of CO₂ by two marine diatoms, Phaeodactylum tricornutum and Cyclotella sp. The time course of CO₂ formation in the dark after addition of 100 mmol m^?3 dissolved inorganic carbon (DIC) to cell suspensions showed that external carbonic anhydrase (CA) was not present in cells of P. tricornutum but was present in Cyclotella sp. In the absence of external CA, or when it was inhibited by 5 mmol m^?3 acetazolamide, cells of both species preincubated with 100 mmol m^?3 DIG rapidly depleted almost all of the free CO₂ (3·2mmol m^?31 at pH7·5) from the suspending medium within seconds of illumination and prior to the onset of steady-state photosynthesis. Addition of bovine CA quickly restored the HCO₃^?–CO₂ equilibrium in the medium, indicating that the initial depletion of CO₂ resulted from the selective uptake of CO₂ rather than uptake of all DIG species. Transfer of cells to the dark caused a rapid increase in the CO₂ concentration in the medium, largely as a result of the efflux of unfixed inorganic carbon from the cells. The measured CO₂ uptake rates for both species accounted for 50% of the total DIG uptake at HCO₃^?–CO₂ equilibrium, indicating that HCOHCO₃^? was also being taken up. These results indicate that both Phaeodactylum tricornutum and Cyclotella sp. have the capacity to transport CO₂ actively against concentration and pH gradients.     

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.     

Active Uptake of CO2 by the Diatom Navicula pelliculosa

Mass spectrometry has been used to investigate the transportof CO₂ in the freshwater diatom Navicula pelliculosa. The timecourseof CO₂ formation in the dark after addition of 100 mmol m^–3dissolved inorganic carbon (DIC) to cell suspensions showedthat no external carbonic anhydrase (CA) was present in thesecells. Upon illumination, cells pre-incubated at pH 75 with100 mmol m^–3 DIC, removed almost all free CO₂ from themedium at an initial rate of 285 µmol CO₂ mg^–1Chl h^–1. Equilibrium between HCO₃^– and CO₂ in themedium occurred rapidly upon addition of bovine CA, showingthat CO₂ depletion resulted from a selective uptake of CO₂ ratherthan an uptake of all inorganic carbon species. However, photosyntheticO₂ evolution rate remained constant after CO₂ had been depletedfrom the medium indicating that photosynthesis is sustainedprimarily by active HCO₃^– uptake. Treatment of cells with2-iodoacetamide (83 mol m^–3) completely inhibited CO₂fixation but had little effect on CO₂ transport since initialrates of CO₂ depletion were about 81% that of untreated cells.Transfer of iodoacetamide-treated cells to the dark caused arapid increase in the CO₂ concentration in the medium largelydue to the efflux of the unfixed intracellular DIC pool whichwas found to be about 194 times the concentration of that inthe external medium. These results indicate that Navicula pelliculosaactively takes up molecular CO₂ against a concentration gradientby a process distinct from HCO₃^– transport. Key words: Dissolved inorganic carbon, carbonic anhydrase, bicarbonate transport, CO₂ transport, mass spectrometry     

Enriched rhizosphere CO2 concentrations can ameliorate the influence of salinity on hydroponically grown tomato plants

Our previous work indicated that salinity caused a shift in the predominant site of nitrate reduction and assimilation from the shoot to the root in tomato plants. In the present work we tested whether an enhanced supply of dissolved inorganic carbon (DIC, CO₂+ HCO₃) to the root solution could increase anaplerotic provision of carbon compounds for the increased nitrogen assimilation in the root of salinity-stressed Lycopersicon esculentum (L.) Mill. cv. F144. The seedlings were grown in hydroponic culture with 0 or 100mM NaCl and aeration of the root solution with either ambient or CO₂-enriched air (5000 μmol mol^?1). The salinity-treated plants accumulated more dry weight and higher total N when the roots were supplied with CO₂-enriched aeration than when aerated with ambient air. Plants grown with salinity and enriched DIC also had higher rates of NO^?₃ uptake and translocated more NO^?₃ and reduced N in the xylem sap than did equivalent plants grown with ambient DIC. Incorporation of DIC was measured by supplying a 1 -h pulse of H¹⁴CO^?₃ to the roots followed by extraction with 80% ethanol. Enriched DIC increased root incorporation of DIC 10-fold in both salinized and non-salinized plants. In salinity-stressed plants, the products of dissolved inorganic ¹⁴C were preferentially diverted into amino acid synthesis to a greater extent than in non-salinized plants in which label was accumulated in organic acids. It was concluded that enriched DIC can increase the supply of N and anaplerotic carbon for amino acid synthesis in roots of salinized plants. Thus enriched DIC could relieve the limitation of carbon supply for ammonium assimilation and thus ameliorate the influence of salinity on NO^?₃ uptake and assimilation as well as on plant growth.     

Enzymatic isolation of cells from aquatic macrophytes

Cells were isolated by enzymic digestion from a number of aquatic macrophytes and their photosynthetic activities were determined. Eichhornia crassipes (Mart.) Solms, Myriophyllum spicatum L. and M. brasiliense Cambess provided photosynthetically-active cells after digestion with commercial pectinase. Cells from emergent leaves of M. brasiliense were approximately 3 times more active than cells from submersed leaves (56.1 vs. 17.4 μmoles CO₂ mg^?2 Chl h^?1). Cells could be isolated from E. crassipes by grinding as well as by digestion, but the former were less active (3.1 vs. 24.2 μmoles CO₂ mg Chl h^?1). Attempts to isolate cells from Hydrilla verticillata (L.f.) Royle or Potamogeton pectinatus L. were not successful.     

Immobilization and characterization of carbonic anhydrase purified from E. coli MO1 and its influence on CO2 sequestration

The present investigation entails the immobilisation and characterisation of Escherichia coli MO1-derived carbonic anhydrase (CA) and its influence on the transformation of CO₂ to CaCO₃. CA was purified from MO1 using a combination of Sephadex G-75 and DEAE cellulose column chromatography, resulting in 4.64-fold purification. The purified CA was immobilised in chitosan-alginate polyelectrolyte complex (C-A PEC) with an immobilisation potential of 94.5 %. Both the immobilised and free forms of the enzyme were most active and stable at pH 8.2 and at 37 °C. The K _m and V _max of the immobilised enzyme were found to be 19.12 mM and 416.66 μmol min^?1 mg^?1, respectively; whereas, the K _m and V _max of free enzyme were 18.26 mM and 434.78 μmol min^?1 mg^?1, respectively. The presence of metal ions such as Cu²⁺, Fe²⁺, and Mg²⁺ stimulated the enzyme activity. Immobilised CA showed higher storage stability and maintained its catalytic efficiency after repeated operational cycles. Furthermore, both forms of the enzyme were tested for targeted application of the carbonation reaction to convert CO₂ to CaCO₃. The amounts of CaCO₃ precipitated over free and immobilised CA were 267 and 253 mg/mg of enzyme, respectively. The results of this study show that immobilised CA in chitosan-alginate beads can be useful for CO₂ sequestration by the biomimetic route.     

A CO2-Flux Mechanism Operating via pH-Polarity in Hydrilla Verticillata Leaves With C3 and C4 Photosynthesis

The aquatic angiosperm Hydrilla verticillata lacks Kranz anatomy, but has an inducible, C₄-based, CO₂ concentrating mechanism (CCM) that concentrates CO₂ in the chloroplasts. Both C₃ and C₄ Hydrilla leaves showed light-dependent pH polarity that was suppressed by high dissolved inorganic carbon (DIC). At low DIC (0.25 mol m⁻³), pH values in the unstirred water layer on the abaxial and adaxial sides of the leaf were 4.2 and10.3, respectively. Abaxial apoplastic acidification served as a CO₂ flux mechanism (CFM), making HCO₃ ⁻ available for photosynthesis by conversion to CO₂. DIC at 10 mol m⁻³ completely suppressed acidification and alkalization. The data, along with previous results, indicated that inhibition was specific to DIC, and not a buffer effect. Acidification and alkalization did not necessarily show 1:1 stoichiometry; their kinetics for the apolar induction phase differed, and alkalization was less inhibited by 2.5 mol m⁻³ DIC. At low irradiance (50 μmol photons m⁻² s⁻¹), where CCM activity in C₄ leaves is minimized, both leaf types had similar DIC inhibition of pH polarity. However, as irradiance increased, DIC inhibition of C₃ leaves decreased. In C₄ leaves the CFM and CCM seemed to compete for photosynthetic ATP and/or reducing power. The CFM may require less, as at low irradiance it still operated maximally, if [DIC] was low. Iodoacetamide (IA), which inhibits CO₂ fixation in Hydrilla, also suppressed acidification and alkalization, especially in C₄ leaves. IA does not inhibit the C₄ CCM, which suggests that the CFM and CCM can operate independently. It has been hypothesized that irradiance and DIC regulate pH polarity by altering the chloroplastic [DIC], which effects the chloroplast redox state and subsequently redox regulation of a plasma-membrane H⁺-ATPase. The results lend partial support to a down-regulatory role for high chloroplastic [DIC], but do not exclude other sites of DIC action. IA inhibition of pH polarity seems inconsistent with the chloroplast NADPH/NADP⁺ ratio being the redox transducer. The possibility that malate and oxaloacetate shuttling plays a role in CFM regulation requires further investigation. This revised version was published online in June 2006 with corrections to the Cover Date.     

Measurement of the photorespiratory activity of the submerged aquatic plant Myriophyllum spicatum L.

Abstract The CO₂ compensation concentrations (points) of leaves of the submerged vascular aquatic plant Myriophyllum spicatum L. were determined in a closed aqueous system at pH 7.0 by a gas chromatographic technique and over the range 10–30deg;C were found to range from 36 to 46 cm³m^?3 in medium equilibrated with 21% O₂ (0.03 kgm^?3), and 25 to 35 cm³m^?3 in medium equilibrated with 2% O₂ (0.03 kgm^?3). The rates of true (TPS) and apparent (APS) photosynthesis of leaves were measured in medium equilibrated with 21% O₂ and buffered at pH 7.0, at subsaturating concentrations (12.8–18.8 mmol m^?3) of dissolved inorganic carbor. (DIC) containing H¹⁴CO₃, by determining the initial rates of uptake by the leaves of DIC and ¹⁴C-activity from the medium. The rate of photorespiration, the difference between TPS and APS, was 7.0–13.3% of TPS over the range of 10–25°C and rose to 29% of TPS at 35°C. The magnitude of the compensation point of this plant is therefore similar to, but is much less O₂-sensitive than, those of C₃ plants, and the photorespiratory rate, at DIC concentrations near the CO₂ compensation point, is very low compared to that of C₃ plants.     

Photosynthetic studies with mesophyll protoplasts from Notonia grandiflora, a crassulacean acid metabolism plant

A method is described for rapid enzymatic isolation of mesophyll protoplasts and cells from the crassulacean acid metabolism (CAM) plant Notonia grandiflora DC. The mesophyll protoplasts exhibited high rates of ¹⁴CO₂ fixation both in the light (45 μmol of CO₂ fixed mg^?1 Chl h^?1) and in the dark (20 μmol of CO₂ fixed mg^?1 Chl h^?1). The protoplasts also showed O₂ evolution (40 μmol of O₂ evolved mg^?1 Chl h^?1) without added bicarbonate. Exogenously added bicarbonate had no stimulating effect on the O₂ evolution. Analyses of early photosynthetic products in the light showed the formation of both C₃ and C₄ acids. Aspartate was found to be a predominant photosynthate.     

Evidence that inducible C4-type photosynthesis is a chloroplastic CO2-concentrating mechanism in Hydrilla, a submersed monocot

Hydrilla verticillata (L.f.) Royle exhibits an inducible C₄-type photosynthetic cycle, but lacks Kranz anatomy. Leaves in the C₄-type state (but not C₃-type) contained up to 5-fold higher internal dissolved inorganic carbon (DIC) concentrations than the medium, indicating that they possessed a CO₂-concentrating mechanism (CCM). Several lines of evidence indicated that the chloroplast was the likely site of CO₂ generation. From C₄-type leaf [DIC] measurements, the estimated chloroplastic free [CO₂] was 400 mmol m^?3. This gave a calculated 2% O₂ inhibition of photosynthesis, which was identical to the measured value, and provided independent evidence that the estimated [CO₂] was close to the true value. A homogeneous distribution of DIC in the C₄-type leaf could not account for such a high [CO₂], or the resultant low O₂ inhibition. For C₃-type leaves the estimated chloroplastic [CO₂] was only 7 mmol m^?3, which gave high, and similar, calculated and measured O₂ inhibition values of 22 and 26%, respectively. The CCM did not appear to be located at the plasma membrane, as it operated at low and high pH, indicating that it was independent of use of HCO₃^? from the medium. Also, both C₃^? and C₄-type Hydrilla leaves showed pH polarity in the light, with abaxial and adaxial boundary layer values of about pH 4·0 and 10·5, respectively. Thus, pH polarity was not a direct component of the CCM, though it probably improved access to HCO₃. Additionally, iodoacetamide and methyl viologen greatly reduced abaxial acidification, but not the steady-state CCM. Inhibitor studies suggested that the CCM required photosynthetically generated ATP, but Calvin cycle activity was not essential. Both leaf types accumulated DIC in the dark by an ATP-requiring process, possibly respiration, and C₄-type leaves fixed CO₂ at 11·8% of the light rate. The operation of a CCM to minimize photorespiration, and the ability to recapture respiratory CO₂ at night, would conserve DIC in a densely vegetated lake environment where daytime [CO₂] is severely limiting, while [O₂] and temperatures are high.     

Physiological variables determined under laboratory conditions may explain the bloom of Aphanizomenon ovalisporum in Lake Kinneret

Response of Aphanizomenon ovalisporum to certain environmental parameters was studied to gain a better understanding of the conditions which may have stimulated its autumnal bloom in Lake Kinneret. Optimal temperature for A. ovalisporum growth was 26–30?°C, resulting in growth rates of 0.2–0.3?day^?1, similar to those observed in the lake. Maximal rate of CO₂ fixation (assimilation numbers of 6–8?μg?C?μg^?1?Chl?h^?1) was obtained at low irradiances (I _k of 40–100?μmol?photons?m^?2?s^?1), 200?μM Pi and low N:Pi ratios. Growth was strongly affected by phosphorus availability, reaching a maximum at Pi concentrations above 40?μM. The high demand for phosphorus was indicated by an increase in alkaline phosphatase activity. The relative abundance of Pi in the cells increased by 4-fold in Pi-rich compared with Pi-limited cultures. Uptake of Pi was faster in Pi-depleted compared with Pi-sufficient cells. Maximal photosynthetic rates and K_1/2(HCO₃ ^?) were 140–220?μmol?O₂?mg^?1?Chl?h^?1 and 10–24?μM, respectively. At pH 7.0 the K _1/2(CO₂) was 2.2 and fell to 0.04?μM at pH 9.0. These data indicated that A. ovalisporum is a HCO₃ ^? user, and can explain its high photosynthetic rates during the bloom, under high pH and low dissolved CO₂ conditions. Na⁺ concentrations of about 5?mM were essential for A. ovalisporum growth at high pH approaching values in the lake.     

The influence of enriched rhizosphere CO2 on N uptake and metabolism in wild-type and NR-deficient barley plants

Positive influences of high concentrations of dissolved inorganic carbon (DIC) in the growth medium of salinity-stressed plants are associated with carbon assimilation through phosphoenolpyruvate carboxylase (PEPc) activity in roots; and also in salinity-stressed tomato plants, enriched CO₂ in the rhizosphere increases NO^?₃uptake. In the present study, wild-type and nitrate reductase-deficient plants of barley (Hordeum vulgare L. cv. Steptoe) were used to determine whether the influence of enriched CO₂ on NO^?₃ uptake and metabolism is dependent on the activity of nitrate reductase (NR) in the plant. Plants grown in NH₄⁺and aerated with ambient air, were transferred to either NO₃^? or NH₄⁺ solutions and aerated with air containing between 0 and 6 500 μmol mol^?1 CO₂. Nitrogen uptake and tissue concentrations of NO₃^? and NH₄⁺ were measured as well as activities of NR and PEPc. The uptake of NO^?₃ by the wild-type was increased by increasing CO₂. This was associated with increased in vitro NR activity, but increased uptake of NO₃^? was found also in the NR-deficient genotype when exposed to high CO₂ concentrations; so that the influence of CO₂ on NO₃^? uptake was independent of the reduction of NO₃^? and assimilation into amino acids. The increase in uptake of NO₃^? in wild-type plants with enriched CO₂ was the same at pH 7 as at pH 5, indicating that the relative abundance of HCO₃^? or CO₂ in the medium did not influence NO₃^? uptake. Uptake of NH₄⁺ was decreased by enriched CO₂ in a pH (5 or 7) independent fashion. Thus NO₃^? and NH⁺₄ uptakes are influenced by the CO₂ component of DIC independently of anaplerotic carbon provision for amino acid synthesis, and CO₂ may directly affect the uptake of NO₃^? and NH₄⁺ in ways unrelated to the NR activity in the tissue.     

Photoautotrophic potato cells: Transition from heterotrophic to autotrophic growth

Cells of potato (Solanum tuberosum L.) were obtained which were capable of photoautotrophic growth in liquid suspension culture under a photon flux density of 90–110 μmol m^?2 s^?1 PAR and in an atmosphere enriched with 2% CO₂. These photoautotrophic cells contained between 100 to 200 μg Chl (g fresh weight)^?1 and fixed CO₂ at a maximum rate of 16 μmol CO₂ (g fresh weight)^?1h^?1. In order to obtain cells capable of photoautotrophic growth it was necessary to adapt highly chlorophyllous heterotrophic cells (>50 μg Chl (g fresh weight)^?1) for growth in medium with 2.5 g sucrose 1^?1 (photomixotrophic cells). The photomixotropic cells had a Chl content of ca 100 μg Chl (g fresh weight)^?1 and were capable of photosynthetic activity which allowed them to survive after sugars had been depleted from the medium. It was from the photomixotrophic cells that cells capable of photoautotrophic growth were obtained. Heterotrophic cells initially established in liquid medium with 25 g sucrose I^?1 from chlorophyllous callus contained about 50 to 150 μg Chl (g fresh weight)^?1. However, after 5 to 10 passages the Chl content decreased to a maximum of 15 μg Chl (g fresh weight)^?1. These cells could not be adapted to photomixotrophic or photoautotrophic growth. These cells also were not able to regain Chl or initiate high rates of CO₂ fixation during the stationary phase of growth as did photomixotrophic cells or chlorophyllous heterotrophic cells. The loss of Chl exhibited by the cells during adaption to heterotrophic growth could be attributed at least in part to unbalanced growth (when cell division and growth exceeds Chl accumulation). Sucrose appeared to have an inhibitory effect directly on photosynthesis independent of Chl accumulation.     

Some characteristics of photosynthetic inorganic carbon uptake of a marine macrophytic red alga

Abstract Some characteristics of photosynthetic inorganic carbon uptake by Palmaria palmata, a marine red macroalga, have been measured under physiological conditions in artificial seawater. The apparent affinity of thallus for CO₂ [K_1/2(CO₂)] at pH 8.0 and 15°C was 21.4±3.0mmol m^?3 CO₂ under air, and 25.7±70mmol m^?3 CO₂ under N₂. The corresponding values of V_max were 2.98 ± 0.42 and 3.65±0.87 mmol O₂ evolved g Chr^?1 s^?l. The apparent K_m(CO₂) of isolated ribulose bisphosphate carboxylase was determined at pH 8.0 and 30 °C to be 30.2 mmol m^?3 CO₂, and the corresponding value of V_max was 19.67 μniol CO₂ g protein^?1 s^?1. The CO₂ compensation points of the thallus were measured in artificial seawater at pH 8.0 under air and N₂, using a gas-chromatographic method. The values were relatively low, rising from 10 cm³ m^?3 at 15°C, to 35 cm³ m^?3 at 25°C, but were not affected by the O₂ concentration. The lack of an effect of O₂ on photosynthesis and on compensation point indicates that there is little photorespiratory CO₂ loss in this macroalga. The high affinity of the thallus for CO₂, and the low CO₂ compensation concentrations, are consistent with the occurrence of bicarbonate uptake in this alga.     

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% CO₂ was markedly stimulated (647 ± 50%) at pH 8.0 by the addition of low concentrations of NaCl (concentration required for half-maximal response, K_½, = 18 micromolar). Studies with KCl and Na₂SO₄ 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 CO₂, 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 CO₂ or HCO₃⁻ use (K_½^CO₂ determination; isotopic disequilibrium; and consideration of HCO₃⁻ dehydration rate) were consistent with CO₂ use by the cells, but HCO₃⁻ use could not be ruled out. Isotopic disequilibrium studies showed that CO₂ use was stimulated by Na⁺. Cells grown on 5% CO₂ 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 O₂ evolution during the initial and most rapid period of DIC accumulation suggested that the required energy was obtained from cyclic photophosphorylation.     

Photosynthetic inorganic carbon uptake and accumulation in two marine diatoms

Some physiological characteristics of photosynthetic inorganic carbon uptake have been examined in the marine diatoms Phaeodactylum tricornutum and Cyclotella sp. Both species demonstrated a high affinity for inorganic carbon in photosynthesis at pH7.5, having K_1/2(CO₂) in the range 1.0 to 4.0mmol m^?3 and O_2? and temperature-insensitive CO₂ compensation concentrations in the range 10.8 to 17.6 cm³ m^?3. Intracellular accumulation of inorganic carbon was found to occur in the light; at an external pH of 7.5 the concentration in P. tricornutum was twice, and that in Cyclotella 3.5 times, the concentration in the suspending medium. Carbonic anhydrase (CA) was detected in intact Cyclotella cells but not in P. tricornutum, although internal CA was detected in both species. The rates of photosynthesis at pH 8.0 of P. tricornutum cells and Cyclotella cells treated with 0.1 mol m^?3 acetazolamide, a CA inhibitor, were 1.5- to 5-fold the rate of CO₂ supply, indicating that both species have the capacity to take up HCO₃^? as a source of substrate for photosynthesis. No Na⁺ dependence for HCO₃^? could be detected in either species. These results indicate that these two marine diatoms have the capacity to accumulate inorganic carbon in the light as a consequence, in part, of the active uptake of bicarbonate.     

Absorption characteristics and kinetics of CO2 capture into N-methyldiethanolamine aqueous solution catalyzed by the immobilized carbonic anhydrase

Abstract

Carbonic anhydrase (CA) is the most effective CO₂ hydratase catalyst, but the poor storage stability and repeatability of CA limit its development. Therefore, CA was immobilized on the epoxy magnetic composite microspheres to enhance the CO₂ absorption into N-methyldiethanolamine (MDEA) aqueous solution in this work. In the presence of immobilized CA, the CO₂ absorption rate of MDEA solution (10?wt%) (0.63?mmol·min^?1) was greatly improved by almost 40%, and their reaction equilibrium time was shortened from 150?min to 90?min compared with that into MDEA solution. The results indicated that the absorption of CO₂ into MDEA solution had been significantly enhanced by using CA. After the 7th reuse recycle, the activity of the immobilized CA was still closed to its initial value at 313.15?K. Moreover, enzyme catalytic kinetics of immobilized CA was investigated using the p-nitrophenyl acetate (p-NPA) as substrate. The values of Michaelis–Menten constant (K_m) and the maximum velocity (V_max) of the immobilized CA were calculated to be 27.61?mmol/L and 20.14?×?10^?3?mmol·min^?1·mL^?1, respectively. Besides, the kinetics of CO₂ reaction into MDEA with or without CA were also compared. The results showed that CO₂ absorption into CA/MDEA aqueous solution obeyed the pseudo first order regime and the second order kinetics rate constant (k₂) was calculated to be 929?m³·kmol^?1·s^?1, which was twice higher than that of MDEA aqueous solution without immobilized CA (k₂=414 m³·kmol^?1·s^?1) at 313.15?K.     

Studies of Elodea nuttallii grown under photorespiratory conditions. II. Evidence for bicarbonate active transport

Abstract. Elodea nuttallii was grown under greenhouse conditions in domestic wastewater in an aquatic treatment system under conditions conducive to photorespiration. Initial research on the photosynthetic characteristics of E. nuttallii suggest that the submergent macrophyte possessed a carbon concentrating mechanism. Isotopic disequilibria H¹⁴CO₃-uptake studies (5-80s) were used to assess the bicarbonate active-transport capabilities in E. nuttallii leaves. Using a range of substrate concentrations (50-50200mmol m^?3), the accumulation of label (mmol g^?1 Chl) over time due to transport was found initially to exceed accumulation due to fixation until steady state rates were observed. Internal steady state pools of dissolved inorganic carbon (DIC) ranged from 40 to 80 mol m^?3. The concentration factor (CF: the ratio of internal cyroplasmic (DIC] to external medium [DIC]) decreased from 800 to 114 as external bicarbonate concentrations were increased. Inhibition of transport by uncouplers (2,4-dinitrophenol (DNP), carbonyl cyanide-m-chlorophenylhydrazone (CCCP)); ATPase inhibitors (dicylcohexocarbodiamide (DCCD), phloridzin, arsenate); electron transport inhibitors (DCMU, Antimycin A), and carbonic anhydrase inhibitors (ethoxyzolamide, acetazolamide) suggest that bicarbonate transport required (1) a proton motive force, (2) a functional ATPase, (3) a chloroplast carbon sink, and possibly (4) a CA-like moiety associated with the transport protein. While plasmalemmasomes were not observed, the plasmalemma was vesiculated and acid and alkaline banding was observed when leaves were incubated under light in the presence of bicarbonate. These data are consistent with the operation of a bicarbonate-cation symport which concentrates substrate against a concentration gradient at the expense of metabolic energy. The presence of an active transport system for bicarbonate ensures that internal carbon concentrations are high when carbon dioxide, is scarce and bicarbonate is the only carbon species available in aquatic treatment systems during photorespiratory conditions. Therefore, E. nuttallii is particularly well suited for use in these systems.