Effect of CO(2), O(2), and Light on Photosynthesis and Photorespiration in Wheat

Unidirectional O₂ fluxes were measured with ¹⁸O₂ in a whole plant of wheat cultivated in a controlled environment. At 2 or 21% O₂, O₂ uptake was maximum at 60 microliters per liter CO₂. At lower CO₂ concentrations, it was strongly inhibited, as was photosynthetic O₂ evolution. At 2% O₂, there remained a substantial O₂ uptake, even at high CO₂ level; the O₂ evolution was inhibited at CO₂ concentrations under 330 microliters per liter. The O₂ uptake increased linearly with light intensity, starting from the level of dark respiration. No saturation was observed at high light intensities. No significant change in the gas-exchange patterns occurred during a long period of the plant life. An adaptation to low light intensities was observed after 3 hours illumination. These results are interpreted in relation to the functioning of the photosynthetic apparatus and point to a regulation by the electron acceptors and a specific action of CO₂. The behavior of the O₂ uptake and the study of the CO₂ compensation point seem to indicate the persistence of mitochondrial respiration during photosynthesis.     

Photosynthetic o(2) exchange kinetics in isolated soybean cells

Light-dependent O₂ exchange was measured in intact, isolated soybean (Glycine max. var. Williams) cells using isotopically labeled O₂ and a mass spectrometer. The dependence of O₂ exchange on O₂ and CO₂ was investigated at high light in coupled and uncoupled cells. With coupled cells at high O₂, O₂ evolution followed similar kinetics at high and low CO₂. Steady-state rates of O₂ uptake were insignificant at high CO₂, but progressively increased with decreasing CO₂. At low CO₂, steady-state rates of O₂ uptake were 50% to 70% of the maximum CO₂-supported rates of O₂ evolution. These high rates of O₂ uptake exceeded the maximum rate of O₂ reduction determined in uncoupled cells, suggesting the occurrence of another light-induced O₂-uptake process (i.e. photorespiration).

Rates of O₂ exchange in uncoupled cells were half-saturated at 7% to 8% O₂. Initial rates (during induction) of O₂ exchange in uninhibited cells were also half-saturated at 7% to 8% O₂. In contrast, steady-state rates of O₂ evolution and O₂ uptake (at low CO₂) were half-saturated at 18% to 20% O₂. O₂ uptake was significantly suppressed in the presence of nitrate, suggesting that nitrate and/or nitrite can compete with O₂ for photoreductant.

These results suggest that two mechanisms (O₂ reduction and photorespiration) are responsible for the light-dependent O₂ uptake observed in uninhibited cells under CO₂-limiting conditions. The relative contribution of each process to the rate of O₂ uptake appears to be dependent on the O₂ level. At high O₂ concentrations (≥40%), photorespiration is the major O₂-consuming process. At lower (ambient) O₂ concentrations (≤20%), O₂ reduction accounts for a significant portion of the total light-dependent O₂ uptake.

     

Photoinhibition of CO(2)-Dependent O(2) Evolution by Intact Chloroplasts Isolated from Spinach Leaves

Intact spinach (Spinacia oleracea L.) chloroplasts, when pre-illuminated at 4 millimoles quanta per square meter per second for 8 minutes in a CO₂-free buffer at 21% O₂, showed a decrease (30-70%) in CO₂-dependent O₂ evolution and ¹⁴CO₂ uptake. This photoinhibition was observed only when the O₂ concentration and the quantum fluence rate were higher than 4% and 1 millimole per square meter per second, respectively. There was only a small decrease in the extent of photoinhibition when the CO₂ concentration was increased from 0 to 25 micromolar during the treatment, but photoinhibition was abolished when the CO₂ concentration was increased to 30 micromolar. Addition of small quantities of P-glycerate (40-200 micromolar) or glycerate (160 micromolar) was found to prevent photoinhibition. Other intermediates of the Calvin cycle (fructose-6-P, fructose-1,6-P, ribose-5-P, ribulose-5-P) also prevented photoinhibition to various extents. Oxaloacetate was not effective in preventing photoinhibition in these chloroplasts. The amount of O₂ evolved during treatments with 3-P-glycerate or glycerate was no more than 65% of that measured in the presence of low CO₂ concentrations (9-12 micromolar) which did not prevent photoinhibition. In all cases, the extent to which photoinhibition was prevented by these metabolites was not correlated to the amount of O₂ evolved during the photoinhibitory treatment. It is concluded that in these chloroplasts the prevention of the O₂-dependent photoinhibition of light saturated CO₂ fixation capacity is not linked to the dissipation of excitation energy via the photosynthetic electron transport nor to ATP utilization. The requirement of O₂ for photoinhibition of CO₂ fixation capacity in isolated chloroplasts may be explained by an effect of O₂ in allowing metabolic depletion of Calvin cycle intermediates.     

Kinetics and Apparent K(m) of Oxygen Cycle under Conditions of Limiting Carbon Dioxide Fixation

A mass spectrometer with a membrane inlet was used to monitor light-driven O₂ evolution, O₂ uptake, and CO₂ uptake in suspensions of algae (Scenedesmus obliquus). We observed the following. (a) The rate of O₂ uptake, which, in the presence of iodoacetamide, replaces the uptake of CO₂, showed a distinct plateau (V_max) beyond ~30% O₂ and was half-maximal at ~8% O₂. We concluded that this light-driven O₂ uptake process, which does not involve carbon compounds, is saturated at lower O₂ concentrations than are photorespiration and glycolate formation. (b) In the absence of inhibitor, O₂ evolution was relatively unaffected by the presence or absence of CO₂. During the course of CO₂ depletion, electron flow to CO₂ was replaced by an equivalent flow to O₂. (c) There was a distinct delay between the cessation of CO₂ uptake and the increase in O₂ uptake. We ascribe this delay to the transient utilization of another electron acceptor—possibly bicarbonate or another bound form of CO₂.     

O(2) uptake in the light in chlamydomonas: evidence for persistent mitochondrial respiration

The nature of the process responsible for the stationary O₂ uptake occurring in the light under saturating CO₂ concentration in Chlamydomonas reinhardii has been investigated. For this purpose, a mass spectrometer with a membrane inlet system was used to measure O₂ uptake and evolution in the algal suspension. First, we observed that the O₂ uptake rate was constant (about 0.5 micromoles of O₂ per milligram chlorophyll per minute) during a light to dark transition and was not affected by 3-(3,4-dichlorophenyl)-1,1-dimethylurea. Salicylhydroxamic acid had no effect on O₂ uptake in the dark or in the light, but was found to have the same inhibitory effect either in the dark or in the light when added to cyanide-treated algae. The stimulation of the O₂ uptake rate due to the uncoupling effect of carbonyl cyanide m-chlorophenylhydrazone was about the same in the dark or in the light. From these results, we conclude that mitochondrial respiration is maintained during illumination and therefore is not inhibited by high ATP levels. Another conclusion is that in conditions where photorespiration is absent, no other light-dependent O₂ uptake process occurs. If Mehler reactions are involved, in Chlamydomonas, under conditions where both photosynthetic carbon oxidation and reduction cycles cannot operate (as in cyanide-treated algae), their occurrence in photosynthesizing algae either under saturating CO₂ concentration or at the CO₂ compensation point appears very unlikely. The comparison with the situation previously reported in Scenedesmus (R. J. Radmer and B. Kok 1976 Plant Physiol 58: 336-340) suggests that different O₂ uptake processes might be present in these two algal species.     

Evidence for Cyclic Photophosphorylation during CO(2) Fixation in Intact Chloroplasts: Studies with Antimycin A, Nitrite, and Oxaloacetate

This study examines the effect of antimycin A and nitrite on ¹⁴CO₂ fixation in intact chloroplasts isolated from spinach (Spinacia oleracea L.) leaves. Antimycin A (2 micromolar) strongly inhibited CO₂ fixation but did not appear to inhibit or uncouple linear electron transport in intact chloroplasts. The addition of small quantities (40-100 micromolar) of nitrite or oxaloacetate, but not NH₄Cl, in the presence of antimycin A restored photosynthesis. Antimycin A inhibition, and the subsequent restoration of photosynthetic activities by nitrite or oxaloacetate, was observed over a wide range of CO₂ concentration, light intensity, and temperature. High O₂ concentration (up to 240 micromolar) did not appear to influence the extent of the inhibition by antimycin A, nor the subsequent restoration of photosynthetic activity by nitrite or oxaloacetate. Studies of O₂ exchanges during photosynthesis in cells and chloroplasts indicated that 2 micromolar antimycin A stimulated O₂ uptake by about 25% while net O₂ evolution was inhibited by 76%. O₂ uptake in chloroplasts in the presence of 2 micromolar antimycin A was 67% of total O₂ evolution. These results suggest that only a small proportion of the O₂ uptake measured was directly linked to ATP generation. The above evidence indicates that cyclic photophosphorylation is the predominant energy-balancing reaction during photosynthesis in intact chloroplasts. On the other hand, pseudocyclic O₂ uptake appears to play only a minimal role.     

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

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

Nitrate-dependent o(2) evolution in intact leaves

Evolution of O₂ by illuminated intact detached leaves from barley (Hordeum vulgare L. cv Athos) and pea (Pisum sativum L. cv Lincoln) in a CO₂-saturating atmosphere was enhanced when KNO₃ (1-2.5 millimolar) had been previously supplied through the transpiration stream. The extra O₂ evolution observed after feeding KNO₃ increased with the light intensity, being maximal at near saturating photon flux densities and resulting in no changes in the initial slope of the O₂ versus light-intensity curve. No stimulation of O₂ evolution was otherwise observed after feeding KCl or NH₄Cl. The data indicate that nitrate assimilation uses photosynthetically generated reductant and stimulates the rate of non-cyclic electron flow by acting as a second electron-accepting assimilatory process in addition to CO₂ fixation.     

Photorespiration in Air and High CO(2)-Grown Chlorella pyrenoidosa

Oxygen inhibition of photosynthesis and CO₂ evolution during photorespiration were compared in high CO₂-grown and air-grown Chlorella pyrenoidosa, using the artificial leaf technique at pH 5.0. High CO₂ cells, in contrast to air-grown cells, exhibited a marked inhibition of photosynthesis by O₂, which appeared to be competitive and similar in magnitude to that in higher C₃ plants. With increasing time after transfer to air, the photosynthetic rate in high CO₂ cells increased while the O₂ effect declined. Photorespiration, measured as the difference between ¹⁴CO₂ and ¹²CO₂ uptake, was much greater and sensitive to O₂ in high CO₂ cells. Some CO₂ evolution was also present in air-grown algae; however, it did not appear to be sensitive to O₂. True photosynthesis was not affected by O₂ in either case. The data indicate that the difference between high CO₂ and air-grown algae could be attributed to the magnitude of CO₂ evolution. This conclusion is discussed with reference to the oxygenase reaction and the control of photorespiration in algae.     

CO(2) and O(2) Exchange in Two Mosses, Hypnum cupressiforme and Dicranum scoparium

Photosynthetic CO₂ and O₂ exchange was studied in two moss species, Hypnum cupressiforme Hedw. and Dicranum scoparium Hedw. Most experiments were made during steady state of photosynthesis, using ¹⁸O₂ to trace O₂ uptake. In standard experimental conditions (photoperiod 12 h, 135 micromoles photons per square meter per second, 18°C, 330 microliters per liter CO₂, 21% O₂) the net photosynthetic rate was around 40 micromoles CO₂ per gram dry weight per hour in H. cupressiforme and 50 micromoles CO₂ per gram dry weight per hour in D. scoparium. The CO₂ compensation point lay between 45 and 55 microliters per liter CO₂ and the enhancement of net photosynthesis by 3% O₂versus 21% O₂ was 40 to 45%. The ratio of O₂ uptake to net photosynthesis was 0.8 to 0.9 irrespective of the light intensity. The response of net photosynthesis to CO₂ showed a high apparent K_m (CO₂) even in nonsaturating light. On the other hand, O₂ uptake in standard conditions was not far from saturation. It could be enhanced by only 25% by increasing the O₂ concentration (saturating level as low as 30% O₂), and by 65% by decreasing the CO₂ concentration to the compensation point. Although O₂ is a competitive inhibitor of CO₂ uptake it could not replace CO₂ completely as an electron acceptor, and electron flow, expressed as gross O₂ production, was inhibited by both high O₂ and low CO₂ levels. At high CO₂, O₂ uptake was 70% lower than the maximum at the CO₂ compensation point. The remaining activity (30%) can be attributed to dark respiration and the Mehler reaction.     

Effect of O2 and CO2 on net CO2 exchange in a high-CO2-requiring mutant of Chlamydomonas reinhardtii during dark-light-dark transitions

Net CO₂ exchange was monitored through a dark-light-dark transition, under 2% and 21% O₂ in the presence and absence of CO₂, in Chlamydomonas reinhardtii wild type and the high-CO₂-requiring mutant ca-1-12-1C. Upon illumination at 350 l/l CO₂, ca-1-12-1C cell exhibited a large decrease in net CO₂ uptake following an initial surge of CO₂ uptake. Net CO₂ uptake subsequently attained a steady-state rate substantially lower than the maximum. A large, O₂-enchanced post-illumination burst of CO₂ efflux was observed after a 10-min illumination period, corresponding to a minimum in the net CO₂ uptake rate. A smaller, but O₂-insensitive post-illumination burst was observed following a 30-min illumination period, when net CO₂ uptake was at a steady-state rate. These post-illumination bursts appeared to reflect the release of an intracellular pool of inorganic carbon, which was much larger following the initial surge of net CO₂ uptake than during the subsequent steady-state CO₂ uptake period.With the mutant in CO₂-free gas, O₂-stimulated, net CO₂ efflux was observed in the light, and a small, O₂-dependent post-illumination burst was observed. With wild-type cells no CO₂ efflux was observed in the light in CO₂-free gas under either 2% or 21% O₂, but a small, O₂-dependent post-illumination burst was observed. These results were interpreted as indicating that photorespiratory rates were similar in the mutant and wild-type cells in the absence of CO₂, but that the wild-type cells were better able to scavenge the photorespiratory CO₂.     

Estimation of Photorespiration Based on the Initial Rate of Postillumination CO(2) Release: II. Effects of O(2), CO(2), and Temperature

An open system associated with an infrared gas analyzer was employed to study transients in CO₂ exchange generated upon darkening preilluminated leaf discs of tobacco (Nicotiana tabacum vars John Williams Broadleaf and Havana Seed). An empirical formula presented previously enabled prediction of the analyzer response under nonsteady state conditions as a function of time and of the leaf CO₂ exchange rate. A computer was used to evaluate parameters of the leaf CO₂ release rate to provide an estimate of the initial rate of postillumination CO₂ evolution and to produce maximal agreement between predicted and observed analyzer responses. In 21% O₂, the decline in rate of CO₂ evolution upon darkening followed first order kinetics. Initial rates of CO₂ evolution following darkening were relatively independent of the prior ambient CO₂ concentrations. However, rates of photorespiration expressed as a fraction of net photosynthesis declined rapidly with increasing external CO₂ concentration at 21% O₂. Under normal atmospheric conditions, photorespiration was 45 to 50% of the net CO₂ fixation rate at 32°C and high irradiance. The rapid initial CO₂ evolution observed upon darkening at 21% O₂ was absent in 3% O₂. Rates of photorespiration under normal atmospheric concentrations of CO₂ and O₂ as measured by the postillumination burst were highly dependent upon temperature (observed activation energy = 30.1 kilocalories per mole). The results are discussed with respect to previously published estimates of photorespiration in C₃ leaf tissue.     

Photosynthetic Capacities and Growth Characteristics of Nicotiana tabacum (cv. Xanthi) Cell Suspension Cultures

Photoheterotrophic growth of cell suspensions of Nicotiana tabacum L. (cv. Xanthi) in organic culture medium enriched in sucrose (30 g per liter) showed a classical sigmoid growth curve. The cells developed functional chloroplast structures during the exponential growth phase, when their chlorophyll content increased steadily. A limited drop (30%) in the chlorophyll amount and structural changes of the plastids (starch accumulation) were observed during the lag phase. The measurements of photosynthetic capacities (O₂ evolution and CO₂ fixation) during the growth cycle revealed changes in the photosynthetic ratio (O₂/CO₂), which was near 1 during the lag and stationary phases and near 2 during exponential growth. During exponential growth there was also a rapid NO₃^? uptake. Analysis of label distribution among the products of ¹⁴CO₂ fixation showed that both CO₂ assimilation pathways, linked to the ribulose-biphosphate carboxylase (the autotrophic pathway) and to phosphoenolpyruvate carboxylase (the non-autotrophic pathway) were operative with an important increase of the capacity of the latter during the exponential growth phase. Maximum rate of oxygen evolution, either endogenous or with p-benzoquinone as Hill reagent, as well as the increased CO₂ Fixation capacity via the non-autotrophic pathway during the exponential phase were concomitant with a high cyanide inhibited O₂ uptake.     

Carbon Oxysulfide Inhibition of the CO(2)-Concentrating Process of Unicellular Green Algae

Carbonyl sulfide (COS), a substrate for carbonic anhydrase, inhibited alkalization of the medium, O₂ evolution, dissolved inorganic carbon accumulation, and photosynthetic CO₂ fixation at pH 7 or higher by five species of unicellular green algae that had been air-adapted for forming a CO₂-concentrating process. This COS inhibition can be attributed to inhibition of external HCO₃⁻ conversion to CO₂ and OH⁻ by the carbonic anhydrase component of an active CO₂ pump. At a low pH of 5 to 6, COS stimulated O₂ evolution during photosynthesis by algae with low CO₂ in the media without alkalization of the media. This is attributed to some COS hydrolysis by carbonic anhydrase to CO₂. Although COS had less effect on HCO₃⁻ accumulation at pH 9 by a HCO₃⁻ pump in Scenedesmus, COS reduced O₂ evolution probably by inhibiting internal carbonic anhydrases. Because COS is hydrolyzed to CO₂ and H₂S, its inhibition of the CO₂ pump activity and photosynthesis is not accurate, when measured by O₂ evolution, by NaH¹⁴CO₃ accumulation, or by ¹⁴CO₂ fixation.     

Effects of slowly permeating osmotica on metabolism of vacuolated and nonvacuolated tissues

Vacuolated and nonvacuolated root tissues of Zea mays were exposed to low water potentials by addition of mannitol or glycerol. Temporary increases were observed for O₂ uptake, but CO₂ evolution remained steady. This increase in O₂ uptake ceased after 15 minutes. Further treatment induced decreases in respiration, with similar reductions in O₂ uptake and CO₂ evolution.     

Quantitation of the O(2)-Dependent, CO(2)-Reversible Component of the Postillumination CO(2) Exchange Transient in Tobacco and Maize Leaves

The postillumination transient of CO₂ exchange and its relation to photorespiration has been examined in leaf discs from tobacco (Nicotiana tabacum) and maize (Zea mays). Studies of the transients observed by infrared gas analysis at 1, 21, and 43% O₂ in an open system were extended using the nonsteady state model described previously (Peterson and Ferrandino 1984 Plant Physiol 76: 976-978). Cumulative CO₂ exchange equivalents (i.e. nanomoles CO₂) versus time were derived from the analyzer responses of individual transients. In tobacco (C₃), subtraction of the time course of cumulative CO₂ exchange under photorespiratory conditions (21 or 43% O₂) from that obtained under nonphotorespiratory conditions (1% O₂) revealed the presence of an O₂-dependent and CO₂-reversible component within the first 60 seconds following darkening. This component was absent in maize (C₄) and at low external O₂:CO₂ ratios (i.e. <100) in tobacco. The size of the component in tobacco increased with net photosynthesis as irradiance was increased and was positively associated with inhibition of net photosynthesis by O₂. This relatively simple and rapid method of analysis of the transient is introduced to eliminate some uncertainties associated with estimation of photorespiration based on the maximal rate of postillumination CO₂ evolution. This method also provides a useful and complementary tool for detecting variation in photorespiration.     

O(2)-insensitive photosynthesis in c(3) plants : its occurrence and a possible explanation

Leaves of C₃ plants which exhibit a normal O₂ inhibition of CO₂ fixation at less than saturating light intensity were found to exhibit O₂-insensitive photosynthesis at high light. This behavior was observed in Phaseolus vulgaris L., Xanthium strumarium L., and Scrophularia desertorum (Shaw.) Munz. O₂-insensitive photosynthesis has been reported in nine other C₃ species and usually occurred when the intercellular CO₂ pressure was about double the normal pressure. A lack of O₂ inhibition of photosynthesis was always accompanied by a failure of increased CO₂ pressure to stimulate photosynthesis to the expected degree. O₂-insensitive photosynthesis also occurred after plants had been water stressed. Under such conditions, however, photosynthesis became O₂ and CO₂ insensitive at physiological CO₂ pressures. Postillumination CO₂ exchange kinetics showed that O₂ and CO₂ insensitivity was not the result of elimination of photorespiration.

It is proposed that O₂ and CO₂ insensitivity occurs when the concentration of phosphate in the chloroplast stroma cannot be both high enough to allow photophosphorylation and low enough to allow starch and sucrose synthesis at the rates required by the rest of the photosynthetic component processes. Under these conditions, the energy diverted to photorespiration does not adversely affect the potential for CO₂ assimilation.

     

Simultaneous Transport of CO(2) and HCO(3) by the Cyanobacterium Synechococcus UTEX 625

A mass spectrometer was used to simultaneously follow the time course of photosynthetic O₂ evolution and CO₂ depletion of the medium by cells of the cyanobacterium Synechococcus leopoliensis UTEX 625. Analysis of the data indicated that both CO₂ and HCO₃⁻ were simultaneously and continuously transported by the cells as a source of substrate for photosynthesis. Initiation of HCO₃⁻ transport by Na⁺ addition had no effect on ongoing CO₂ transport. This result is interpreted to indicate that the CO₂ and HCO₃⁻ transport systems are separate and distinctly different transport systems. Measurement of CO₂-dependent photosynthesis indicated that CO₂ uptake involved active transport and that diffusion played only a minor role in CO₂ acquisition in cyanobacteria.     

CO(2) and O(2) Exchanges in the CAM Plant Ananas comosus (L.) Merr: Determination of Total and Malate-Decorboxylation-Dependent CO(2)-Assimilation Rates; Study of Light O(2)-Uptake

Photosynthesis and light O₂-uptake of the aerial portion of the CAM plant Ananas comosus (L.) merr. were studied by CO₂ and O₂ gas exchange measurements. The amount of CO₂ which was fixed during a complete day-night cycle was equal to the amount of total net O₂ evolved. This finding justifies the assumption that in each time interval of the light period, the difference between the rates of net O₂-evolution and of net light atmospheric CO₂-uptake give the rates of malate-decarboxylation-dependent CO₂ assimilation. Based upon this hypothesis, the following photosynthetic characteristics were observed: (a) From the onset of the light to midphase IV of CAM, the photosynthetic quotient (net O₂ evolved/net CO₂ fixed) was higher than 1. This indicates that malate-decarboxylation supplied CO₂ for the photosynthetic carbon reduction cycle during this period. (b) In phase III and early phase IV, the rate of CO₂ assimilation deduced from net O₂-evolution was 3 times higher than the maximum rate of atmospheric CO₂-fixation during phase IV. A conceivable explanation for this stimulation of photosynthesis is that the intracellular CO₂-concentration was high because of malate decarboxylation. (c) During the final hours of the light period, the photosynthetic quotient decreased below 1. This may be the result of CO₂-fixation by phosphoenolpyruvate-carboxylase activity and malate accumulation. Based upon this hypothesis, the gas exchange data indicates that at least 50% of the CO₂ fixed during the last hour of the light period was stored as malate. Light O₂-uptake determined with ¹⁸O₂ showed two remarkable characteristics: from the onset of the light until midphase IV the rate of O₂-uptake increased progressively; during the following part of the light period, the rate of O₂-uptake was 3.5 times higher than the maximum rate of CO₂-uptake. When malate decarboxylation was reduced or suppressed after a night in a CO₂-free atmosphere or in continuous illumination, the rate of O₂-uptake was higher than in the control. This supports the hypothesis that the low rate of O₂-uptake in the first part of the light period is due to the inhibition of photorespiration by increased intracellular CO₂ concentration because of malate decarboxylation. In view of the law of gas diffusion and the kinetic properties of the ribulose-1,5-bisphosphate carboxylase/oxygenase, O₂ and CO₂ gas exchange suggest that at the end of the light period the intracellular CO₂ concentration was very low. We propose that the high ratio of O₂-uptake/CO₂-fixation is principally caused by the stimulation of photorespiration during this period.     

Effect of Photon Fluence Rate on Oxygen Evolution and Uptake by Chlamydomonas reinhardtii Suspensions Grown in Ambient and CO(2)-Enriched Air

A closed system consisting of an assimilation chamber furnished with a membrane inlet from the liquid phase connected to a mass spectrometer was used to measure O₂ evolution and uptake by Chlamydomonas reinhardtii cells grown in ambient (0.034% CO₂) or CO₂-enriched (5% CO₂) air. At pH = 6.9, 28°C and concentrations of dissolved inorganic carbon (DIC) saturating for photosynthesis, O₂ uptake in the light (U_o) equaled O₂ production (E_o) at the light compensation point (15 micromoles photons per square meter per second). E_o and U_o increased with increasing photon fluence rate (PFR) but were not rate saturated at 600 micromoles photons per square meter per second, while net O₂ exchange reached a saturation level near 500 micromoles photons per square meter per second which was nearly the same for both, CO₂-grown and air-grown cells. Comparison of the U_o/E_o ratios between air-grown and CO₂-grown C. reinhardtii showed higher values for air-grown cells at light intensities higher than light compensation. For both, air-grown and CO₂-grown algae the rates of mitochondrial O₂ uptake in the dark measured immediately before and 5 minutes after illumination were much lower than U_o at PFR saturating for net photosynthesis. We conclude that noncyclic electron flow from water to NADP⁺ and pseudocyclic electron flow via photosystem I to O₂ both significantly contribute to O₂ exchange in the light. In contrast, mitochondrial respiration and photosynthetic carbon oxidation cycle are regarded as minor O₂ consuming reactions in the light in both, air-grown and CO₂-grown cells. It is suggested that the “extra” O₂ uptake by air-grown algae provides ATP required for the energy dependent CO₂/HCO₃⁻ concentrating mechanism known to be present in these cells.