Interactions of blue light and inorganic carbon supply in the control of light-saturated photosynthesis in brown algae

Photosynthetic capacities of five species of brown algae in red light were found to be strongly limited by the inorganic carbon supply of natural sea water. Under these conditions, pH 8·2 and dissolved inorganic carbon concentration (DIG) of 2·1 mol m^?3, a short pulse of blue light was found to increase the subsequent rate of photosynthesis in saturating red light. The degree of blue light stimulation varied between species, ranging from an increase of over 200% of the original rate in Colpomenia peregrins to only 10% in Dictyota dichotoma. Increasing the DIG concentration of sea water by bicarbonate addition resulted in carbon saturation of photosynthesis in all five species. Blue light stimulation was greatly reduced at these higher DIG concentrations. The response in Laminaria digitata was examined in more detail by manipulation of pH and DIG to produce solutions with different concentrations of dissolved CO₂. At a CO₂ concentration typical of normal sea water (12·4 mmol m^?3), blue light treatment increased photosynthetic rate by approximately 50%. Blue light stimulation was increased to over 150% at CO₂ concentrations below that of sea water, whereas at concentrations above that of sea water, the effect was diminished. Therefore, the effect of blue light on photosynthetic capacity appears to involve an increase in the rate of supply of carbon dioxide to the plant.     

Influence of carbon supply on the circadian rhythmicity of photosynthesis and its stimulation by blue light in Ectocarpus siliculosus: clues to the mechanism of inorganic carbon acquisition in lower brown algae

Stimulation or light-saturated rates of photosynthesis in Ectocarpus siliculosus (Dillwyn) Lyngb. by blue light was eliminated by increasing dissolved inorganic carbon (DIC) or by lowering pH in natural seawater. The amplitude of the circadian rhythm of photosynthesis was also diminished under these conditions, and the pH compensation points in a closed system were higher in the presence of blue light and during the circadian day. These observations suggest that blue light and the circadian clock regulate the activity of a carbon acquisition system in these plants. The inhibitor of external carbonic anhydrase, acetazolamide, reduced overall rates of photosynthesis by only about 30%, but ethoxyzolamide suppressed the circadian rhythm of photosynthesis almost completely and markedly reduced the duration of responses to blue light pulses. Similar patterns were obtained when photosynthesis was measured in strongly limiting DIC concentrations (0–0.5 mol m^?3). Since blue light stimulated photosynthesis under these conditions of strong carbon limitation, we suggest that blue light activates the release of CO₂ from an internal CO₂ store. We propose a metabolic pathway with similarities to that of CAM plants. Non-photosynthetic fixation leads to the accumulation of a storage metabolite. The circadian clock and blue light control the mobilization of CO₂ at the site of decarboxylation of this metabolite. In the presence of continuous blue light the pathway is proposed to cycle and act as a pump for CO₂ into the chloroplasts. This hypothesis helps to explain a number of previously reported peculiarities of brown algal photosynthesis.     

The induction of inorganic carbon transport and external carbonic anhydrase in Chlamydomonas reinhardtii is regulated by external CO2 concentration

Induction of the carbon concentrating mechanism (CCM) has been investigated during the acclimation of 5% CO₂‐grown Chlamydomonas reinhardtii 2137 mt + cells to well‐defined dissolved inorganic carbon (C_i) limited conditions. The CCM components investigated were active HCO₃^? transport, active CO₂ transport and extracellular carbonic anhydrase (CA_ext) activity. The CA_ext activity increased 10‐fold within 6 h of acclimation to 0·035% CO₂ and there was a further slight increase over the next 18 h. The CA_ext activity also increased substantially after an 8 h lag period during acclimation to air in darkness. Active CO₂ and HCO₃^? uptake by C. reinhardtii cells were induced within 2 h of acclimation to air, but active CO₂ transport was induced prior to active HCO₃^? transport. Similar results were obtained during acclimation to air in darkness. The critical C_i concentrations effecting the induction of active C_i transport and CA_ext activity were determined by allowing cells to acclimate to various inflow CO₂ concentrations in the range 0·035–0·84% at constant pH. The total C_i concentration eliciting the induction and repression of active C_i transport was higher during acclimation at pH 7·5 than at pH 5·5, but the external CO₂ concentration was the same at both pHs of acclimation. The concentration of external CO₂ required for the full induction and repression of C_i transport and CA_ext activity were 10 and 100 μM , respectively. The induction of CA_ext and active C_i transport are not correlated temporally, but are regulated by the same critical CO₂ concentration in the medium.     

Steady-state stomatal responses of C3 and C4 species to blue light fraction: Interactions with CO2 concentration

Blue light induced stomatal opening has been studied by applying a short pulse (~5 to 60 s) of blue light to a background of saturating photosynthetic red photons, but little is known about steady-state stomatal responses. Here we report stomatal responses to blue light at high and low CO₂ concentrations. Steady-state stomatal conductance (g_s) of C₃ plants increased asymptotically with increasing blue light to a maximum at 20% blue (120 μmol m⁻² s⁻¹). This response was consistent from 200 to 800 μmol mol⁻¹ atmospheric CO₂ (C_a). In contrast, blue light induced only a transient stomatal opening (~5 min) in C₄ species above a C_a of 400 μmol mol⁻¹. Steady-state g_s of C₄ plants generally decreased with increasing blue intensity. The net photosynthetic rate of all species decreased above 20% blue because blue photons have lower quantum yield (moles carbon fixed per mole photons absorbed) than red photons. Our findings indicate that photosynthesis, rather than a blue light signal, plays a dominant role in stomatal regulation in C₄ species. Additionally, we found that blue light affected only stomata on the illuminated side of the leaf. Contrary to widely held belief, the blue light-induced stomatal opening minimally enhanced photosynthesis and consistently decreased water use efficiency.     

The effect of light quality on the induction of efficient photosynthesis under low CO2 conditions in Chlamydomonas reinhardtii and Chlorella pyrenoidosa

The effect of blue and red light on the adaptation to low CO₂ conditions was studied in high-CO₂ grown cultures of Chlorella Pyrenoidosa (82T) and Chlamydomonas reinhardtii(137⁺) by measuring O₂ exchange under various inorganic carbon (Cⁱ) concentrations. At equal photosynthetic photon flux density (PPFD), blue light was more favourable for adaptation in both species, compared to red light. The difference in photosynthetic oxygen evolution between cells adapted to low C_iunder blue and red light was more pronounced when oxygen evolution was measured under low C_i compared to high C_i conditions. The effect of light quality on adaptation remained for several hours. The different effects caused by blue and red light was observed in C. pyrenoidosa over a wide range of PPFD with increasing differences at increasing PPFD. The maximal difference was obtained at a PPFD above 1 500 μmol m^?2s^?1. We found no difference in the extracellular carbonic anhydrase activity between blue- and red light adapted cells. The light quality effect recorded under C_i-limiting conditions in C. reinhardtii cells adapted to air, was only 37% less when instead of pure blue light red light containing 12.5% of blue light (similar PPFD as blue light) was used during adaptation to low carbon. This indicates that in addition to affecting photosynthesis, blue light affected a sensory system involved in algal adaptation to low C_i conditions. Since the affinity for C_i of C. Pyrenoidosa and C. reinhardtii cells adapted to air under blue light was higher than that of cells adapted under red light, we suggest that induction of some component(s) of the C_i accumulating mechanism is regulated by the light quality.     

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.     

Influence of carbon supply on the stimulation of light-saturated photosynthesis by blue light in Laminaria saccharina: implications for the mechanism of carbon acquisition in higher brown algae

In saturating irradiances of red light, photosynthesis of Laminaria saccharina (L.) Lamouroux was stimulated by low irradiances of continuous blue light only when the supply of dissolved inorganic carbon (DIC) was limiting. The degree of this stimulation was inversely proportional to the logarithm of the concentration of free CO₂, whether this was adjusted by varying the total DIC or the pH at a given DIC concentration. The final pH reached in a closed system was higher in blue light than in red light. Both acetazolamide and ethoxyzolamide suppressed the responses to blue light almost completely, but reduced photosynthesis in red light by only 30%. Buffering the pH of the seawater also suppressed the stimulation of photosynthesis by blue light without affecting the photosynthetic rate in red light. The transient stimulation of O₂ evolution by a blue light pulse was not accompanied by a corresponding increase in CO₂ consumption. These observations could be explained if, in analogy to the mechanism proposed for Ectocarpus (Schmid, Mills & Dring 1996, Plant Cell and Environment 19,373–382, this issue, accompanying paper), photosynthesis was supported by a blue-light-activated release of CO₂ from an internal store. We suggest that the store is located in the vacuoles of the cortical tissue of the blades. The main photosynthetic tissue, however, is in the overlying meristoderm, and blue-light-activated mobilization of the store could stimulate O₂ evolution only if periplasmic carbonic anhydrase was available to facilitate CO₂ uptake from the cortex.     

Photoautotrophic nutrient utilization and limitation during semi‐continuous growth of Synechocystis sp. PCC6803

Microbial photosynthesis presents a valuable opportunity to capture abundant light energy to produce renewable bioenergy and biomaterials. To understand the factors that control the productivity of photosynthetic microorganisms, we conducted a series of semi‐continuous experiments using bench‐scale photobioreactor (PBR) systems, the cyanobacterium Synechocystis PCC6803 (PCC6803), and light conditions imitating actual day–night light irradiance (LI). Our results demonstrate that using normal BG‐11 medium resulted in severe phosphate (P_i) limitation for continuous operation. Mitigation of P_i‐limitation, by augmenting the P_i content of BG‐11, allowed higher biomass productivity; however, once P_i‐limitation was alleviated, limitation by inorganic carbon (C_i) or LI occurred. C_i‐limitation was detected by a low total C_i concentration (<5 mg C/L) and high and fluctuating pH. C_i‐limitation was relieved by delivering more CO₂, which led to a stable pH in the range of 7–9 and at least 5 mg/L of C_i in HCO. LI limitation, evidenced by an average LI <14 W/m² for PCC6803, was induced by a high biomass concentration of 1,300 mg/L. Thus, this work provides quantitative tools of stoichiometry and kinetics to evaluate limitation on PBRs. Biotechnol. Bioeng. 2010;106: 553–563. © 2010 Wiley Periodicals, Inc.     

Detection of a variable intracellular acid‐labile carbon pool in Thalassiosira weissflogii (Heterokontophyta) and Emiliania huxleyi (Haptophyta) in response to changes in the seawater carbon system

Accumulation of an intracellular pool of carbon (C_i pool) is one strategy by which marine algae overcome the low abundance of dissolved CO₂ (CO_2(aq)) in modern seawater. To identify the environmental conditions under which algae accumulate an acid‐labile C_i pool, we applied a ¹⁴C pulse‐chase method, used originally in dinoflagellates, to two new classes of algae, coccolithophorids and diatoms. This method measures the carbon accumulation inside the cells without altering the medium carbon chemistry or culture cell density. We found that the diatom Thalassiosira weissflogii [(Grunow) G. Fryxell & Hasle] and a calcifying strain of the coccolithophorid Emiliania huxleyi [(Lohmann) W. W. Hay & H. P. Mohler] develop significant acid‐labile C_i pools. Ci pools are measureable in cells cultured in media with 2–30 µmol l^?1 CO_2(aq), corresponding to a medium pH of 8.6–7.9. The absolute C_i pool was greater for the larger celled diatoms. For both algal classes, the C_i pool became a negligible contributor to photosynthesis once CO_2(aq) exceeded 30 µmol l^?1. Combining the ¹⁴C pulse‐chase method and ¹⁴C disequilibrium method enabled us to assess whether E. huxleyi and T. weissflogii exhibited thresholds for foregoing accumulation of DIC or reduced the reliance on bicarbonate uptake with increasing CO_2(aq). We showed that the C_i pool decreases with higher CO₂:HCO₃^? uptake rates.     

Simple oscillations in photosynthesis of higher plants

Illumination of leaves of Vicia faba L. provoked oscillations in the rates of CO₂ uptake and O₂ evolution. The oscillations were marked under anaerobic conditions, but were absent at 20% O₂. The minimum CO₂ concentration required for the appearance of oscillations was 600 μl · l^?1. The higher the CO₂ concentration, the stronger the oscillations. The effect of CO₂ concentration was saturated at 1000 μl CO₂ · l^?1. The period of the oscillations was 5–6 min at a light intensity of 80 nE · cm^?2 · s^?1 and became longer on lowering of the intensity. No oscillations appeared at intensities below 12 nE · cm^?2 · s^?1. Oscillations could also be generated by increasing the CO₂ concentration in the atmosphere during strong illumination under anaerobic conditions. The chlorophyl a fluorescence yield showed oscillations, similar in shape and frequency to those of photosynthesis, after such an environmental change. Oscillations were also observed in photosynthesis of other C₃ plants, Lycopersicon esulentum Mill and Glycine max Merrill, under the same conditions as those required for V. faba, but were absent for the C₄ plants, Zea mays and Amaranthus retroflexus L.     

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.     

The CO2 permeability of the plasma membrane of Chlamydomonas reinhardtii: mass-spectrometric 18O-exchange measurements from 13C18O2 in suspensions of carbonic anhydrase-loaded plasma-membrane vesicles

The unicellular green alga Chlamydomonas reinhardtii possesses a CO₂-concentrating mechanism. In order to measure the CO₂ permeability coefficients of the plasma membranes (PMs), carbonic anhydrase (CA) loaded vesicles were isolated from C. reinhardtii grown either in air enriched with 50 mL CO₂ · L?1} (high-C_i cells) or in ambient air (350 μL CO₂ · L?1}; low-C_i cells). Marker-enzyme measurements indicated less than 1% contamination with thylakoid and mitochondrial membranes, and that more than 90% of the PMs from high and low-C_i cells were orientated right-side-out. The PMs appeared to be sealed as judged from the ability of vesicles to accumulate [¹⁴C]acetate along a proton gradient for at least 10 min. Carbonic anhydrase-loaded PMs from high and low-C_i cells of C. reinhardtii were used to measure the exchange of ¹⁸O between doubly labelled CO₂ (¹³C¹⁸O₂) and H₂O in stirred suspensions by mass spectrometry. Analysis of the kinetics of the ¹⁸O depletion from ¹³C¹⁸O₂ in the external medium provides a powerful tool to study CO₂ diffusion across the PM to the active site of CA which catalyses ¹⁸O exchange only inside the vesicles but not in the external medium (Silverman et al., 1976, J Biol Chem 251: 4428–4435). The activity of CA within loaded PM vesicles was sufficient to speed-up the ¹⁸O loss to H₂O to 45360–128800 times the uncatalysed rate, depending on the efficiency of CA-loading and PM isolation. From the ¹⁸O-depletion kinetics performed at pH 7.3 and 7.8, CO₂ permeability coefficients of 0.76 and 1.49·10?3} cm·s?1}, respectively, were calculated for high C_i cells. The corresponding values for low-C_i cells were 1.21 and 1.8·10?3} cm·s?1}. The implications of the similar and rather high CO₂ permeability coefficients (low CO₂ resistance) in high and low-C_i cells for the CO_i-concentrating mechanism of C. reinhardtii are discussed.     

Inorganic carbon transport across cell compartments of the halotolerant alga Dunaliella salina

The inorganic carbon (C_i) accumulation and the intracellular location of carbonic anhydrase (CA, EC 4.2.1.1) in the halotolerant unicellular alga Dunaliella salina have been investigated. The rate of HCO₃ -dependent O₂ evolution was determined by growth conditions. Algae grown under high CO₂ conditions (5% CO₂ in air, v/v; high C_i cells) had a very low affinity for HCO₃^? at pH 7.0 and 8.2, whereas algae grown under low CO₂ conditions (0.03% CO₂ in air; low C_i cells) showed a high affinity for HCO₃^? at both pH values and were sensitive to Dextran-bound sulfonamide (DBS), an inhibitor of extracellular CA. The photosynthetic rate or HCO₄^? dependent O₂ evolution was always higher at pH 7.0 than at pH 8.2. Ethoxyzolamide (EZ), an inhibitor of total (extacellular plus intracellular) CA activity, strongly inhibited photosynthesis at both pH values. During adaptation from high to low CO₂ conditions CA activity increased in chloroplasts in a process dependent on the novo protein synthesis. Carbonic anhydrase activity was found in the supernatant and pellet fractions of chloroplast homogenates. The rate of photosynthesis of chloroplasts from low C_i cells was higher at pH 7.0 than at pH 8.2. The alkalinization of the growth medium, which took place only in the presence of C_i, was partially inhibited by DBS and completely by EZ. We suggest that in D. salina CO₂ is the general form of C_i transported across the plasma membrane and the chloroplast envelope and that bicarbonate enters the cell mainly, although not entirely, by an ‘indirect’ mechanism after dehydration to CO₂.     

EXOGENOUS SOURCES OF INORGANIC CARBON FOR PHOTOSYNTHESIS BY MARINE MACROALGAE1

Thirty-five species of marine macroalgae were tested for their ability to remove inorganic carbon from seawater using the pH-drift technique. Six of these species, all Rhodophyta, were unable to use HCO₃^–. The remaining species exhibited a range in ability to use HCO₃^– and deplete inorganic carbon (C_τ); the three most effective species, all Chlorophyta, raised the pH to over 10.50, depleted the concentration of CO₂ effectively to zero, and depleted the concentration of C_τ to less than 50% of that at air-equilibrium. In contrast, the six species restricted to CO₂ did not raise the pH above 9.0 at a CO₂ concentration of about 1.5 μmol · L^-1 and depleted the concentration of C_τ to about 80% of that at air-equilibrium. Ability to raise pH and deplete C_τ was linked to the habitat in which the species grew. Five of the six species which lack the ability to use HCO₃^– grow subtidally in relatively low light beneath a canopy of larger Phaeophyta. None of these species grow in rockpools where carbon-depletion may occur. Species from rockpools were all effective at removing inorganic carbon. Competition for C_τ may be one of the factors that determines species composition in rockpools. There was a species-specific difference between the calculated concentration of C_τ at the end of a pH-drift experiment and that measured directly. Most, but not all, species with the ability to generate high pH-values showed a lower than calculated final concentration of C_τ consistent with precipitation of CaCO₃. A number of Rhodophyta with no, or a limited, ability to use HCO₃^– showed the opposite response, with final concentrations of C_τ exceeding that calculated from the pH. Calculations based on the maximum gross rate of production of CO₂ from HCO₃^– in the absence of external carbonic anhydrase confirmed the results of the pH-drift experiments by demonstrating HCO₃^– -use in Monostroma fuscum (Post et Rupr.) Wittr. And Ulva lactuca L. and the lack of this ability in Lomentaria articulate (Huds.) Lyngb. Rates of net photosynthesis at air-equilibrium were greater than 95% of those at 2.3 mmol C_τ· L^-1 for many of the species which were able to use HCO₃^–, but on average only 72% for the six species restricted to CO₂.     

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.     

Photosynthesis, Photorespiration and Respiration of Detached Spruce Twigs as Influenced by Oxygen Concentration and Light Intensity

The effects of oxygen concentration and light intensity on the rates of apparent photosynthesis, true photosynthesis, photorespiration and dark respiration of detached spruce twigs were determined by means of an infra-red carbon dioxide analyzer (IRCA). A closed circuit system IRCA was filled with either 1 per cent of oxygen in nitrogen, air (21 % O₂) or pure oxygen (100 % O₂). Two light intensities 30 × 10³ erg · cm ^?2· s^?1 and 120 × 10³ erg · cm^?2· s^?1 were applied. It has been found that the inhibitory effect of high concentration of oxygen on the apparent photosynthesis was mainly a result of a stimulation of the rate of CO₂ production in light (photorespiration). In the atmosphere of 100 % O₂, photorespiration accounts for 66–80 per cent of total CO₂ uptake (true photosynthesis). Owing to a strong acceleration of photorespiration by high oxygen concentrations, the rate of true photosynthesis calculated as the sum of apparent photosynthesis and photorespiration was by several times less inhibited by oxygen than the rate of apparent photosynthesis. The rates of dark respiration were essentially unaffected by the oxygen concentrations used in the experiments. An increase in the intensity of light from 30 × 10³ erg · cm^?3· s^?1 to 120 · 10³ erg · cm^?2· s^?1 enhanced the rate of photorespiration in the atmospheres of 21 and 100 % oxygen but not in 1 % O₂. The rate of apparent photosynthesis, however, was little affected by light intensity in an atmosphere of 1 % oxygen.     

Utilization of inorganic carbon in the edible cyanobacterium Ge-Xian-Mi (Nostoc) and its role in alleviating photo-inhibition

The present work investigated the inorganic carbon (C_i) uptake, fluorescence quenching and photo‐inhibition of the edible cyanobacterium Ge‐Xian‐Mi (Nostoc) to obtain an insight into the role of CO₂ concentrating mechanism (CCM) operation in alleviating photo‐inhibition. Ge‐Xian‐Mi used HCO₃^– in addition to CO₂ for its photosynthesis and oxygen evolution was greater than the theoretical rates of CO₂ production derived from uncatalysed dehydration of HCO₃^–. Multiple transporters for CO₂ and HCO₃^– operated in air‐grown Ge‐Xian‐Mi. Na⁺‐dependent HCO₃^– transport was the primary mode of active C_i uptake and contributed 53–62% of net photosynthetic activity at 250 µmol L^?1 KHCO₃ and pH 8.0. However, the CO₂‐uptake systems and Na⁺‐independent HCO₃^– transport played minor roles in Ge‐Xian‐Mi and supported, respectively, 39 and 8% of net photosynthetic activity. The steady‐state fluorescence decreased and the photochemical quenching increased in response to the transport‐mediated accumulation of intracellular C_i. Inorganic carbon transport was a major factor in facilitating quenching during the initial stage and the initial rate of fluorescence quenching in the presence of iodoacetamide, an inhibitor of CO₂ fixation, was 88% of control. Both the initial rate and extent of fluorescence quenching increased with increasing external dissolved inorganic carbon (DIC) and saturated at higher than 200 µmol L^?1 HCO₃^–. The operation of the CCM in Ge‐Xian‐Mi served as a means of diminishing photodynamic damage by dissipating excess light energy and higher external DIC in the range of 100–10000 µmol L^?1 KHCO₃ was associated with more severe photo‐inhibition under strong irradiance.     

Quantification of the rate of CO2 formation in the periplasmic space of microalgae during photosynthesis. A comparison of whole-cell rate constants for CO2 and HCO3– uptake among three species of the green alga Chlorella

As previously described, the absolute rate of photosynthesis due to a limited concentration of dissolved inorganic carbon at alkaline pH, where the rate of CO₂ formation is strictly limited, plotted as a function of chlorophyll (Chl) concentration, will take the form of a rectangular hyperbola combined with a linear rate directly proportional to [Chl], which are, respectively, due to the contribution of CO₂ and HCO₃^– to photosynthesis. This model represents that the mathematical asymptote of absolute rate of photosynthesis versus cell density is described by the whole-cell rate constant for HCO₃^– uptake and the maximum rate of CO₂ formation in the extracellular space. This means that any trace modification of the CO₂ formation rate outside the cell will alter the photosynthetic rate and should be detectable experimentally. In air-grown Chlorella ellipsoidea and C. kessleri and in high CO₂-grown C. saccharophila, the graph of the absolute rate of photosynthesis against [Chl] clearly followed the mathematical model described above and the actual CO₂ formation rates outside the cells were not significantly different from the calculated rates. It also indicated that the whole-cell rate constants for CO₂ and HCO₃^– uptake in air-grown C. ellipsoidea and C. saccharophila were similar at ≈ 300 and 2·0 mm³μg^–1 Chl min^–1, respectively, whereas those in air-grown C. kessleri were ≈ 550 and 15 mm³μg^–1 Chl min^–1. These results indicate that no acidification of the periplasmic space occurs, and there is no trace activity of external carbonic anhydrase in these microalgae.     

INORGANIC CARBON LIMITATION OF PHOTOSYNTHESIS IN ULVA ROTUNDATA (CHLOROPHYTA)1

A computerized oxygen electrode Astern was used to make rapid and accurate measurements of photosynthetic light and dissolved inorganic carbon (DIC) response cures with a macroalga. Ulva rotundata Blid. was grown in an outdoor, continuous flow system in seawater under sunlight or 9% of sunlight at Beaufort, North Carolina. The light compensation points in the shade- and sun-grown plants, measured in seawater, were at photon flux densities (PFDs) of 16 and 27 μmol. Photons·m^?2·s^?1, respectively but the quantum yield of O₂ evolution was not significantly different. Rates of photosynthesis in seawater per unit area of thallus under saturating light and rates of dark respiration were about 1.5-fold higher in sun- than in shade-grown plants. The concentration of DIC in seawater (approximately 2 mM) limited photosynthesis at absorbed PFDs above 60–70 μmol photons·m^?2·s^?1 Addition of 20 mM inorganic carbon had no effect on quantum yield but caused about a 1.5-fold increase in the light-saturated photosynthetic rate in both shade- and sun-grown Ulva. The effect of DIC supplementation was greatest in plants grown in October and least in plants grown in June. The light- and DIC-saturated rate of photosynthesis in seawater was similar to the maximum rate obtained by exposing Ulva to 10% CO₂, in the gas phase. The carbon isotope values (δ¹³C, reflecting the ¹³C/¹²C ratio compared to a standard) of Ulva grown in the same seawater supply were dependent on light and agitation. Samples from Beaufort Inlet were more negative (δ¹³C value, ?20.03‰) than those grown in bright light with agitation (δ¹³C value, ?17.78‰ outdoors; ?17.23‰ indoors), which may indicate DIC supply limited carbon uptake in seawater.     

Destructive hydrogen peroxide production in Eucheuma denticulatum (Rhodophyta) during stress caused by elevated pH,high light intensities and competition with other species

Growth of Eucheuma denticulatum was studied in the field and in laboratory experiments. Field co-cultivation of E. denticulatum with the green alga Ulva reticulata or the seagrass Thalassia sp. reduced daily growth rate (DGR) of a Tanzanian and a Philippine strain of E. denticulatum by 10–100% and 10–55%, respectively, depending upon the type of water current: a unidirectional water current produced the best growth. Laboratory co-cultivation of a Tanzanian strain of E. denticulatum with U. reticulata also reduced DGR (to 8% of the control) and nitrate-nitrogen uptake rate (to <30% of the control) of E. denticulatum and, moreover, it increased epiphytism of a red filamentous alga on E. denticulatum. E. denticulatum monoculture at pH 8·6 ± 0·5 or at photosynthetic photon flux densities (PPFDs) higher than its growth optimum (350 ± 50 μmol photons m^-2 s^-1) also increased epiphytism. The lack of a competitive mechanism for inorganic carbon uptake in Eucheuma may have contributed to its reduced growth during co-cultivation. During co-cultivation, elevated pH regimes (pH > 8·5) were created around the Eucheuma thalli as a result of photosynthesis, thus decreasing the concentration of CO₂ in the seawater to values around 1 μmM. As Eucheuma depends mainly on the CO₂ in the seawater for its growth, a higher pH can cause CO₂ limitation by decreasing CO₂ concentration. Hydrogen peroxide (H₂O₂) production from the Tanzanian strain was also determined by luminol-dependent chemiluminescence. H₂O₂ production was found to increase with increased pH and PPFD (probably as a result of oxidative stress). Preincubation of plants with catalase for 5 min before addition of luminol prevented chemiluminescence, confirming H₂O₂ as the substrate of the luminol reaction. We suggest that the inefficiency of E. denticulatum in HCO^- ₃ utilisation contributes to its poor growth during field coexistence with seagrasses or Ulva sp. and that carbon deficiency induces H₂O₂ production in E. denticulatum.