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.

     

Photorespiratory phenomena in maize: oxygen uptake, isotope discrimination, and carbon dioxide efflux

Concurrent O₂ evolution, O₂ uptake, and CO₂ uptake by illuminated maize (Zea mays) leaves were measured using ¹³CO₂ and ¹⁸O₂. Considerable O₂ uptake occurred during active photosynthesis. At CO₂ compensation, O₂ uptake increased. Associated with this increase was a decrease in O₂ release such that a stoichiometric exchange of O₂ occurred. The rate of O₂ exchange at CO₂ compensation was directly related to O₂ concentration in the atmosphere at least up to 8% (v/v).     

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 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.     

Carbon Dioxide-Induced Oscillations in Fluorescence and Photosynthesis: Role of Thylakoid Membrane Energization in Regulation of Photosystem II Activity

The response of CO₂ fixation to a sudden increase in ambient CO₂ concentration has been investigated in intact leaf tissue from spinach (Spinacia oleracea) using a dual channel infrared gas analyzer. Simultaneous with these measurements, changes in fluorescence emission associated with a weak, modulated measuring beam were recorded. Application of brief (2-3 seconds) dark intervals enabled estimation of the dark fluorescence level (F_o) under both steady state and transient conditions. The degree of suppression of F_o level fluorescence in the light was strongly correlated with nonphotochemical quenching under all conditions. During CO₂-induced oscillations in photosynthesis under 2% O₂ the changes in nonphotochemical quenching anticipate changes in the rate of uptake of CO₂. At such low levels of O₂ and constant illumination, changes in the relative quantum efficiency of open photosystem II units were estimated as the ratio of the rate of CO₂ uptake and the photochemical quenching coefficient. Under the same conditions the relative quantum efficiency of photosystem II was found to vary inversely with the degree of nonphotochemical quenching. The relationship between changes in the rate of CO₂ uptake: photochemical quenching coefficient and nonphotochemical quenching was altered somewhat when the same experiment was conducted under 20% O₂. The results suggest that electron transport coupled to reduction of O₂ occurs to varying degrees with time during oscillations, especially when ambient O₂ concentrations are high.     

On the nature of the oxygen uptake in the light by Chondrus crispus. Effects of inhibitors,temperature and light intensity

The nature of the different processes of O₂ uptake involved in the light in the red macroalga Chondrus crispus Stackhouse (Rhodophyta, Gigartinales) was investigated. At limiting CO₂, INH (2.5 mM) did not alter the O₂ uptake rate. Glycolate was not excreted and did not accumulate within the cells. KCN reduced the rate of O₂ uptake in the light by 76% at limiting CO₂ and by 43% at saturating CO₂, but caused > 95% inhibition of O₂ evolution. DCMU (5 μM) totally blocked the photosynthetic electron transport chain, but allowed a residual O₂ uptake of 3.0±0.6 μmol O₂ .h^?1.g^?1 FW, irrespective of the CO₂ concentration. In saturating CO₂, a high light intensity pretreatment significantly stimulated the rate of O₂ uptake compared to net O₂ evolution, suggesting the persistence, in the light, of mitochondrial respiration. Irrespective of the CO₂ concentration, the optimum temperature for O₂ evolution was 17°C whereas dark O₂ uptake increased linearly with temperature. In contrast, O₂ uptake in the light showed an optimum at 17°C in limiting CO₂, and 21–25° C in saturating CO₂; its Q₁₀ was 2.4 at limiting CO₂, a value close to that of RuBP oxygenase, and 3.1 at saturating CO₂, a value close to that of dark respiration. It is concluded that: 1) mitochondrial respiration and Mehler reaction are both involved at all CO₂ concentrations, 2) RuBP oxygenase activity cannot account for more than 45%, and Mehler reaction for less than 20%, of the total O₂ uptake observed in the light at limiting CO₂.     

Kinetics of the Oxyhydrogen Reaction in the Presence and Absence of Carbon Dioxide in Scenedesmus obliquus

The oxyhydrogen reaction in the presence and absence of CO₂ was studied in H₂-adapted Scenedesmus obliquus by monitoring the initial rates of H₂, O₂, and ¹⁴CO₂ uptake and the effect of inhibitors on these rates with gas-sensing electrodes and isotopic techniques. In the presence of 0.02 atmosphere O₂, the pH₂ was varied from 0 to 1 atmosphere. Whereas the rate of O₂ uptake increased by only 30%, the rate of H₂ uptake increased severalfold over the range of pH₂ values. At 0.1 atmosphere H₂ and 0.02 atmosphere O₂, rates for H₂ and O₂ uptake were between 15 and 25 micromoles per milligram chlorophyll per hour. As the pH₂ was changed from 0 to 1 atmosphere, the quotient H₂:O₂ changed from 0 to roughly 2. This change may reflect the competition between H₂ and the endogenous respiratory electron donors. Respiration in the presence of glucose and acetate was also competitive with H₂ uptake. KCN inhibited equally respiration (O₂ uptake in the absence of H₂) and the oxyhydrogen reaction in the presence and absence of CO₂. The uncoupler carbonyl cyanide p-trifluoromethoxyphenylhydrazone accelerated the rate of respiration and the oxyhydrogen reaction to a similar extent. It was concluded that the oxyhydrogen reaction both in the presence and absence of CO₂ has properties in common with components of respiration and photosynthesis. Participation of these two processes in the oxyhydrogen reaction would require a closely linked shuttle between mitochondrion and chloroplast.     

Simultaneous measurement of oscillations in oxygen evolution and chlorophyll a fluorescence in leaf pieces

In spinach (Spinacia oleracea) and barley (Hordeum vulgare) leaves, chlorophyll a fluorescence and O₂ evolution have been measured simultaneously following re-illumination after a dark interval or when steady state photosynthesis has been perturbed by changes in the gas phase. In high CO₂ concentrations, both O₂ and fluorescence can display marked dampening oscillations that are antiparallel but slightly out of phase (a rise or fall in fluorescence anticipating a corresponding fall or rise in O₂ by about 10 to 15 seconds). Infrared gas analysis measurements showed that CO₂ uptake behaved like O₂ evolution both in the period of oscillation (about 1 minute) and in its relation to fluorescence. In the steady state, oscillations were initiated by increases in CO₂ or by increases or decreases in O₂. Oscillations in O₂ or CO₂ did not occur without associated oscillations in fluorescence and the latter were a sensitive indicator of the former. The relationship between such oscillations in photosynthetic carbon assimilation and chlorophyl a fluorescence is discussed in the context of the effect of ATP or NADPH consumption on known quenching mechanisms.     

Photosynthetic oxygen exchange in C4 grasses: the role of oxygen as electron acceptor

C₄ grasses of the NAD‐ME type (Astrebla lappacea, Eleusine coracana, Eragrostis superba, Leptochloa dubia, Panicum coloratum, Panicum decompositum) and the NADP‐ME type (Bothriochloa bladhii, Cenchrus ciliaris, Dichanthium sericeum, Panicum antidotale, Paspalum notatum, Pennisetum alopecuroides, Sorghum bicolor) were used to investigate the role of O₂ as an electron acceptor during C₄ photosynthesis. Mass spectrometric measurements of gross O₂ evolution and uptake were made concurrently with measurements of net CO₂ uptake and chlorophyll fluorescence at different irradiances and leaf temperatures of 30 and 40 °C. In all C₄ grasses gross O₂ uptake increased with increasing irradiance at very high CO₂ partial pressures (pCO₂) and was on average 18% of gross O₂ evolution. Gross O₂ uptake at high irradiance and high pCO₂ was on average 3.8 times greater than gross O₂ uptake in the dark. Furthermore, gross O₂ uptake in the light increased with O₂ concentration at both high CO₂ and the compensation point, whereas gross O₂ uptake in the dark was insensitive to O₂ concentration. This suggests that a significant amount of O₂ uptake may be associated with the Mehler reaction, and that the Mehler reaction varies with irradiance and O₂ concentration. O₂ exchange characteristics at high pCO₂ were similar for NAD‐ME and NADP‐ME species. NAD‐ME species had significantly greater O₂ uptake and evolution at the compensation point particularly at low irradiance compared to NADP‐ME species, which could be related to different rates of photorespiratory O₂ uptake. There was a good correlation between electron transport rates estimated from chlorophyll fluorescence and gross O₂ evolution at high light and high pCO₂.     

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.     

Inhibition of inorganic carbon transport by oxygen in a high CO2-requiring mutant (E1) of Anacystis nidulans R2

The effect of O₂ on inorganic carbon (C_i) transport was studied with a high CO₂-requiring mutant (E₁) of Anacystis nidulans R₂. Oxygen (above 2%) inhibited C_i transport by 15–35|X% at CO₂ concentrations above 200 μl/l, but had no apparent effect at low, limiting CO₂ concentration. The action spectra for C_i transport measured in the presence or absence of 20% O₂ showed two peaks around 684 and 625 nm, corresponding to chlorophyll a and phycocyanin absorption, respectively. The difference between these two spectra (anaerobic minus aerobic) showed one peak around 625 nm, which indicates that a linear electron transport from water to O₂ is involved in the O₂ inhibition of C_i transport. Dithiothreitol could overcome the inhibition by O₂. The results suggested that the O₂ inhibition is a result of inactivation of the C_i-transporting system.     

Relationship between Respiration and Photosynthesis in Guard Cell and Mesophyll Cell Protoplasts of Commelina communis L

A mass spectrometric method combining ¹⁶O/¹⁸O and ¹²C/¹³C isotopes was used to quantify the unidirectional fluxes of O₂ and CO₂ during a dark to light transition for guard cell protoplasts and mesophyll cell protoplasts of Commelina communis L. In darkness, O₂ uptake and CO₂ evolution were similar on a protein basis. Under light, guard cell protoplasts evolved O₂ (61 micromoles of O₂ per milligram of chlorophyll per hour) almost at the same rate as mesophyll cell protoplasts (73 micromoles of O₂ per milligram of chlorophyll per hour). However, carbon assimilation was totally different. In contrast with mesophyll cell protoplasts, guard cell protoplasts were able to fix CO₂ in darkness at a rate of 27 micromoles of CO₂ per milligram of chlorophyll per hour, which was increased by 50% in light. At the onset of light, a delay observed for guard cell protoplasts between O₂ evolution and CO₂ fixation and a time lag before the rate of saturation suggested a carbon metabolism based on phosphoenolpyruvate carboxylase activity. Under light, CO₂ evolution by guard cell protoplasts was sharply decreased (37%), while O₂ uptake was slowly inhibited (14%). A control of mitochondrial activity by guard cell chloroplasts under light via redox equivalents and ATP transfer in the cytosol is discussed. From this study on protoplasts, we conclude that the energy produced at the chloroplast level under light is not totally used for CO₂ assimilation and may be dissipated for other purposes such as ion uptake.     

Light-Dependent Oxygen Uptake, Glycolate, and Ammonia Release in l-Methionine Sulfoximine-Treated Chlamydomonas

Glycolate and ammonia excretion plus oxygen exchanges were measured in the light in l-methionine-dl-sulfoximine treated air-grown Chlamydomonas reinhardii. At saturating CO₂ (between 600 and 700 microliters per liter CO₂) neither glycolate nor ammonia were excreted, whereas at the CO₂ compensation concentration (<10 microliters per liter CO₂) treated algae excreted both glycolate and ammonia at rates of 37 and 59 nanomoles per minute per milligram chlorophyll, respectively. From the excretion values we calculate the amount of O₂ consumed through the glycolate pathway. The calculated value was not significantly different from the component of O₂ uptake sensitive to CO₂ obtained from the difference between O₂ uptake of the CO₂ compensation point and at saturating CO₂. This component was about 40% of stationary O₂ uptake measured at the CO₂ compensation point. From these data we conclude that glyoxylate decarboxylation in air-grown Chlamydomonas represents a minor pathway of metabolism even in conditions where amino donors are deficient and that processes other than glycolate pathway are responsible for the O₂ uptake insensitive to CO₂.     

Analysis of the Relative Increase in Photosynthetic O2 Uptake When Photosynthesis in Grapevine Leaves Is Inhibited following Low Night Temperatures and/or Water Stress

We found similarities between the effects of low night temperatures (5°C–10°C) and slowly imposed water stress on photosynthesis in grapevine (Vitis vinifera L.) leaves. Exposure of plants growing outdoors to successive chilling nights caused light- and CO₂-saturated photosynthetic O₂ evolution to decline to zero within 5 d. Plants recovered after four warm nights. These photosynthetic responses were confirmed in potted plants, even when roots were heated. The inhibitory effects of chilling were greater after a period of illumination, probably because transpiration induced higher water deficit. Stomatal closure only accounted for part of the inhibition of photosynthesis. Fluorescence measurements showed no evidence of photoinhibition, but nonphotochemical quenching increased in stressed plants. The most characteristic response to both stresses was an increase in the ratio of electron transport to net O₂ evolution, even at high external CO₂ concentrations. Oxygen isotope exchange revealed that this imbalance was due to increased O₂ uptake, which probably has two components: photorespiration and the Mehler reaction. Chilling- and drought-induced water stress enhanced both O₂ uptake processes, and both processes maintained relatively high rates of electron flow as CO₂ exchange approached zero in stressed leaves. Presumably, high electron transport associated with O₂ uptake processes also maintained a high ΔpH, thus affording photoprotection.     

Deconvolution of the three components of the photoacoustic signal by curve fitting and the relationship of CO2 uptake to proton fluxes

The photoacoustic response of the photosynthetic apparatus to a short light pulse consists of three components: heat evolution, O₂ evolution and CO₂ uptake. Recent attempts of deconvoluting the individual components by curve-fitting by means of model curves [Kolbowski et al. (1990) Photosynth Res 25: 309–316] suffered from the fact that the model curve for CO₂ uptake changed its curve shape with CO₂ concentration. Here, it is shown that good fits can be obtained if a stretching factor is incorporated into the fitting routine which adjusts the shape of the uptake model curve. The relationship between CO₂ uptake und H⁺ transport across the thylakoid membrane was investigated by experiments in different CO₂ concentrations from 0 to 7%. It was found that under limiting conditions (7% CO₂) the flux ratio CO₂: O₂ was close to 4. This was compared with the value expected from the stoichiometries of the linear electron transport chain.     

Salt-Induced Metabolic Changes in Dunaliella salina

An increase of medium NaCl concentration induces Dunaliella cells to evolve O₂ photosynthetically even in the absence of CO₂. This NaCl-induced O₂ evolution may reflect the induced conversion of reserve carbohydrate to glycerol. The quantum yield for the NaCl-induced O₂ evolution, in the absence of CO₂, is 1.5-fold higher than that obtained for CO₂ fixation. Since the synthesis of glycerol from reserve carbohydrate in the absence of CO₂ requires only 0.5 ATP/NADPH, whereas photosynthesis requires at least 1.3 ATP/NADPH, it is concluded that the ATP/2e⁻ ratio coupled to NADP reduction in Dunaliella is lower than required for CO₂ fixation.     

Specificity factor of Rubisco: estimation in intact leaves by carboxylation at different CO2/O2 ratios

The specificity factor of Rubisco (S _f) was estimated in intact leaves from the carboxylation of ribulose-1,5-bisphosphate (RuBP) at various CO₂/O₂ ratios. As oxygenation is calculated by the difference of the ¹⁴CO₂ uptake by RuBP in the absence and presence of oxygen, it is important to choose the optimum CO₂/O₂ ratios. At high CO₂ concentration (1,000 cm³ m^?3 and higher) oxygenation consumes less than 50% RuBP but the difference of concentrations of CO₂ at cell walls (C _w) and at the carboxylation centers (C _c) is 2?C5% and the influence of mesophyll resistance (r _md) is of minor importance. To accumulate large endogenous pool of RuBP, the leaves were preilluminated in the CO₂- and O₂-free gas environments for 8 to 10 s. Thereafter the light was switched off and the leaves were flushed with the gas containing different concentrations of ¹⁴CO₂ and O₂. The specificity factor of Rubisco was calculated from the amount of the tracer taken up under different ¹⁴CO₂/O₂ ratios by the exhaustion of the RuBP pool. Application of ¹⁴CO₂ allowed us to discriminate between the CO₂ uptake and the concurrent respiratory CO₂ release which proceeded at the expense of unlabelled intermediates.     

Effect of Oxygen on Photosynthesis, Photorespiration and Respiration in Detached Leaves. II. Corn and other Monocotyledons

The effect of O₂ on the CO₂ exchange of detached leaves of corn (Zea mays), wheat (Triticum vulgare), oats (Avena sativa), barley (Hordeum vulgare), timothy (Phleum pratense) and cat-tail (Typha angustifolia) was measured with a Clark oxygen electrode and infrared carbon dioxide analysers in both open and closed systems.

Corn leaves did not produce CO₂ in the light at any O₂ concentration, as was shown by the zero CO₂ compensation point and the absence of a CO₂ burst in the first minute of darkness. The rate of photosynthesis was inhibited by O₂ and the inhibition was not completely reversible. On the other hand, the steady rate of respiration after a few minutes in the dark was not affected by O₂.

These results were interpreted as indicating the absence of any measurable respiration during photosynthesis. Twelve different varieties of corn studied all responded to O₂ in the same way.

The other 5 monocotyledons studied did produce CO₂ in the light. Moreover, the CO₂ compensation point increased linearly with O₂ indicating a stimulation of photorespiration.

The implications of the lack of photorespiration in studies of primary productivity are discussed.

     

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.     

In situ estimation of net CO2 assimilation, photosynthetic electron flow and photorespiration in Turkey oak (Q. cerris L.) leaves: diurnal cycles under different levels of water supply

Diurnal time courses of net CO₂ assimilation rates, stomatal conductance and light-driven electron fluxes were measured in situ on attached leaves of 30-year-old Turkey oak trees (Quercus cerris L.) under natural summer conditions in central Italy. Combined measurements of gas exchange and chlorophyll a fluorescence under low O₂ concentrations allowed the demonstration of a linear relationship between the photochemical efficiency of PSII (fluorescence measurements) and the apparent quantum yield of gross photosynthesis (gas exchange). This relationship was used under normal O₂ to compute total light-driven electron fluxes, and to partition them into fractions used for RuBP carboxylation or RuBP oxygenation. This procedure also yielded an indirect estimate of the rate of photorespiration in vivo. The time courses of light-driven electron flow, net CO₂ assimilation and photorespiration paralleled that of photosynthetic photon flux density, with important afternoon deviations as soon as a severe drought stress occurred, whereas photochemical efficiency and maximal fluorescence underwent large but reversible diurnal decreases. The latter observation indicated the occurrence of a large non-photochemical energy dissipation at PSII. We estimated that less than 60% of the total photosynthetic electron flow was used for carbon assimilation at midday, while about 40% was devoted to photorespiration. The rate of carbon loss by photorespiration (R₁) reached mean levels of 56% of net assimilation rates. The potential application of this technique to analysis of the relative contributions of thermal de-excitation at PSII and photorespiratory carbon recycling in the protection of photosynthesis against stress effects is discussed.