Estimation of Mesophyll Conductance to CO(2) Flux by Three Different Methods

The resistance to diffusion of CO₂ from the intercellular airspaces within the leaf through the mesophyll to the sites of carboxylation during photosynthesis was measured using three different techniques. The three techniques include a method based on discrimination against the heavy stable isotope of carbon, ¹³C, and two modeling methods. The methods rely upon different assumptions, but the estimates of mesophyll conductance were similar with all three methods. The mesophyll conductance of leaves from a number of species was about 1.4 times the stomatal conductance for CO₂ diffusion determined in unstressed plants at high light. The relatively low CO₂ partial pressure inside chloroplasts of plants with a low mesophyll conductance did not lead to enhanced O₂ sensitivity of photosynthesis because the low conductance caused a significant drop in the chloroplast CO₂ partial pressure upon switching to low O₂. We found no correlation between mesophyll conductance and the ratio of internal leaf area to leaf surface area and only a weak correlation between mesophyll conductance and the proportion of leaf volume occupied by air. Mesophyll conductance was independent of CO₂ and O₂ partial pressure during the measurement, indicating that a true physical parameter, independent of biochemical effects, was being measured. No evidence for CO₂-accumulating mechanisms was found. Some plants, notably Citrus aurantium and Simmondsia chinensis, had very low conductances that limit the rate of photosynthesis these plants can attain at atmospheric CO₂ level.     

Theoretical Considerations when Estimating the Mesophyll Conductance to CO(2) Flux by Analysis of the Response of Photosynthesis to CO(2)

The conductance for CO₂ diffusion in the mesophyll of leaves can limit photosynthesis. We have studied two methods for determining the mesophyll conductance to CO₂ diffusion in leaves. We generated an ideal set of photosynthesis rates over a range of partial pressures of CO₂ in the stroma and studied the effect of altering the mesophyll diffusion conductance on the measured response of photosynthesis to intercellular CO₂ partial pressure. We used the ideal data set to test the sensitivity of the two methods to small errors in the parameters used to determine mesophyll conductance. The two methods were also used to determine mesophyll conductance of several leaves using measured rather than ideal data sets. It is concluded that both methods can be used to determine mesophyll conductance and each method has particular strengths. We believe both methods will prove useful in the future.     

Inorganic Carbon Diffusion between C(4) Mesophyll and Bundle Sheath Cells: Direct Bundle Sheath CO(2) Assimilation in Intact Leaves in the Presence of an Inhibitor of the C(4) Pathway

Photosynthesis rates of detached Panicum miliaceum leaves were measured, by either CO₂ assimilation or oxygen evolution, over a wide range of CO₂ concentrations before and after supplying the phosphoenolpyruvate (PEP) carboxylase inhibitor, 3,3-dichloro-2-(dihydroxyphosphinoyl-methyl)-propenoate (DCDP). At a concentration of CO₂ near ambient, net photosynthesis was completely inhibited by DCDP, but could be largely restored by elevating the CO₂ concentration to about 0.8% (v/v) and above. Inhibition of isolated PEP carboxylase by DCDP was not competitive with respect to HCO₃⁻, indicating that the recovery was not due to reversal of enzyme inhibition. The kinetics of ¹⁴C-incorporation from ¹⁴CO₂ into early labeled products indicated that photosynthesis in DCDP-treated P. miliaceum leaves at 1% (v/v) CO₂ occurs predominantly by direct CO₂ fixation by ribulose 1,5-bisphosphate carboxylase. From the photosynthesis rates of DCDP-treated leaves at elevated CO₂ concentrations, permeability coefficients for CO₂ flux into bundle sheath cells were determined for a range of C₄ species. These values (6-21 micromoles per minute per milligram chlorophyll per millimolar, or 0.0016-0.0056 centimeter per second) were found to be about 100-fold lower than published values for mesophyll cells of C₃ plants. These results support the concept that a CO₂ permeability barrier exists to allow the development of high CO₂ concentrations in bundle sheath cells during C₄ photosynthesis.     

Effect of CO(2) Concentration on Glycine and Serine Formation during Photorespiration

Amount and products of photosynthesis during 10 minutes were measured at different ¹⁴CO₂ concentrations in air. With tobacco (Nicotiana tabacum L. cv. Maryland Mammoth) leaves the percentage of ¹⁴C in glycine plus serine was highest (42%) at 0.005% CO₂, and decreased with increasing CO₂ concentration to 7% of the total at 1% CO₂ in air. However, above 0.03% CO₂ the total amount of ¹⁴C incorporated into the glycine and serine pool was about constant. At 0.005% or 0.03% CO₂ the percentage and amount of ¹⁴C in sucrose was small but increased greatly at higher CO₂ levels as sucrose accumulated as an end product. Relatively similar data were obtained with sugar beet (Beta vulgaris L. cv. US H20) leaves. The results suggest that photorespiration at high CO₂ concentration is not inhibited but that CO₂ loss from it becomes less significant.     

Degree of C(4) Photosynthesis in C(4) and C(3)-C(4)Flaveria Species and Their Hybrids : I. CO(2) Assimilation and Metabolism and Activities of Phosphoenolpyruvate Carboxylase and NADP-Malic Enzyme

The degree of C₄ photosynthesis was assessed in four hybrids among C₄, C₄-like, and C₃-C₄ species in the genus Flaveria using ¹⁴C labeling, CO₂ exchange, ¹³C discrimination, and C₄ enzyme activities. The hybrids incorporated from 57 to 88% of the ¹⁴C assimilated in a 10-s exposure into C₄ acids compared with 26% for the C₃-C₄ species Flaveria linearis, 91% for the C₄ species Flaveria trinervia, and 87% for the C₄-like Flaveria brownii. Those plants with high percentages of ¹⁴C initially fixed into C₄ acids also metabolized the C₄ acids quickly, and the percentage of ¹⁴C in 3-phosphoglyceric acid plus sugar phosphates increased for at least a 30-s exposure to ¹²CO₂. This indicated a high degree of coordination between the carbon accumulation and reduction phases of the C₄ and C₃ cycles. Synthesis and metabolism of C₄ acids by the species and their hybrids were highly and linearly correlated with discrimination against ¹³C. The relationship of ¹³C discrimination or ¹⁴C metabolism to O₂ inhibition of photosynthesis was curvilinear, changing more rapidly at C₄-like values of ¹⁴C metabolism and ¹³C discrimination. Incorporation of initial ¹⁴C into C₄ acids showed a biphasic increase with increased activities of phosphoenolpyruvate carboxylase and NADP-malic enzyme (steep at low activities), but turnover of C₄ acids was linearly related to NADP-malic enzyme activity. Several other traits were closely related to the in vitro activity of NADP-malic enzyme but not phosphoenolpyruvate carboxylase. The data indicate that the hybrids have variable degrees of C₄ photosynthesis but that the carbon accumulation and reduction portions of the C₄ and C₃ cycles are well coordinated.     

Intercellular Diffusion Limits to CO(2) Uptake in Leaves : Studies in Air and Helox

We studied plants of five species with hypostomatous leaves, and six with amphistomatous leaves, to determine the extent to which gaseous diffusion of CO₂ among the mesophyll cells limits photosynthetic carbon assimilation. In helox (air with nitrogen replaced by helium), the diffusivities of CO₂ and water vapor are 2.3 times higher than in air. For fixed estimated CO₂ pressure at the evaporating surfaces of the leaf (pⁱ), assimilation rates in helox ranged up to 27% higher than in air for the hypostomatous leaves, and up to 7% higher in the amphistomatous ones. Thus, intercellular diffusion must be considered as one of the processes limiting photosynthesis, especially for hypostomatous leaves. A corollary is that CO₂ pressure should not be treated as uniform through the mesophyll in many leaves. To analyze our helox data, we had to reformulate the usual gas-exchange equation used to estimate CO₂ pressure at the evaporating surfaces of the leaf; the new equation is applicable to any gas mixture for which the diffusivities of CO₂ and H₂O are known. Finally, we describe a diffusion-biochemistry model for CO₂ assimilation that demonstrates the plausibility of our experimental results.     

13CO2/12CO2 exchange fluxes in a clamp‐on leaf cuvette: disentangling artefacts and flux components

Leaks and isotopic disequilibria represent potential errors and artefacts during combined measurements of gas exchange and carbon isotope discrimination (Δ). This paper presents new protocols to quantify, minimize, and correct such phenomena. We performed experiments with gradients of CO₂ concentration (up to ±250 μmol mol^?1) and δ¹³C_CO2 (34‰), between a clamp‐on leaf cuvette (LI‐6400) and surrounding air, to assess (1) leak coefficients for CO₂, ¹²CO₂, and ¹³CO₂ with the empty cuvette and with intact leaves of Holcus lanatus (C₃) or Sorghum bicolor (C₄) in the cuvette; and (2) isotopic disequilibria between net photosynthesis and dark respiration in light. Leak coefficients were virtually identical for ¹²CO₂ and ¹³CO₂, but ～8 times higher with leaves in the cuvette. Leaks generated errors on Δ up to 6‰ for H. lanatus and 2‰ for S. bicolor in full light; isotopic disequilibria produced similar variation of Δ. Leak errors in Δ in darkness were much larger due to small biological : leak flux ratios. Leak artefacts were fully corrected with leak coefficients determined on the same leaves as Δ measurements. Analysis of isotopic disequilibria enabled partitioning of net photosynthesis and dark respiration, and indicated inhibitions of dark respiration in full light (H. lanatus: 14%, S. bicolor: 58%).     

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.     

Analysis of Stomatal and Nonstomatal Components in the Environmental Control of CO(2) Exchange in Leaves of Welwitschia mirabilis

In well-watered plants of Welwitschia mirabilis, grown in the glass-house under high irradiance conditions, net CO₂ assimilation was almost exclusively observed during the daytime. The plants exhibited a very low potential for Crassulacean acid metabolism, which usually resulted in reduced rates of net CO₂ loss for several hours during the night. In leaves exposed to the diurnal changes in temperature and humidity typical of the natural habitats, CO₂ assimilation rates in the light were markedly depressed under conditions resembling those occurring during midday, when leaf temperatures and the leaf-air vapor pressure differences were high (36°C and 50 millibars bar⁻¹, respectively). Studies on the relationship between CO₂ assimilation rate and intercellular CO₂ partial pressure at various temperatures and humidities showed that this decrease in CO₂ assimilation was largely due to stomatal closure. The increase in the limitation of photosynthesis by CO₂ diffusion, which is associated with the strong decline in stomatal conductance in Welwitschia exposed to midday conditions, may significantly contribute to the higher ¹³C content of Welwitschia compared to the majority of C₃ species.     

Discrimination Against 13CO2 in Leaves,Pod Walls,and Seeds of Water-stressed Chickpea

The rate of photosynthesis (P _N) in leaves and pods as well as carbon isotope content in leaves, pod walls, and seeds was measured in well-watered (WW) and water-stressed (WS) chickpea plants. The P _N, on an area basis, was negligible in pods compared to leaves and was reduced by water stress (by 26%) only in leaves. WS pod walls and seeds discriminated less against ¹³CO₂ than did the controls. This response was not observed for leaves as is usually the case. Pod walls and seeds discriminated less against ¹³CO₂ than did leaves in both WW and WS plants. Measurement of carbon isotope composition in pods may be a more sensitive tool for assessing the impact of water stress on long-term assimilation than is the instantaneous measurement of gas exchange rates.     

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.     

Use of sediment CO2 by submersed rooted plants

Background and Aims

Submersed plants have different strategies to overcome inorganic carbon limitation. It is generally assumed that only small rosette species (isoetids) are able to utilize the high sediment CO₂ availability. The present study examined to what extent five species of submersed freshwater plants with different morphology and growth characteristics (Lobelia dortmanna, Lilaeopsis macloviana, Ludwigia repens, Vallisneria americana and Hydrocotyle verticillata) are able to support photosynthesis supplied by uptake of CO₂ from the sediment.

Methods

Gross photosynthesis was measured in two-compartment split chambers with low inorganic carbon availability in leaf compartments and variable CO₂ availability (0 to >8 mmol L⁻¹) in root compartments. Photosynthetic rates based on root-supplied CO₂ were compared with maximum rates obtained at saturating leaf CO₂ availability, and ¹⁴C experiments were conducted for two species to localize bottlenecks for utilization of sediment CO₂.

Key Results

All species except Hydrocotyle were able to use sediment CO₂, however, with variable efficiency, and with the isoetid, Lobelia, as clearly the most effective and the elodeid, Ludwigia, as the least efficient. At a water column CO₂ concentration in equilibrium with air, Lobelia, Lilaeopsis and Vallisneria covered >75% of their CO₂ requirements by sediment uptake, and sediment CO₂ contributed substantially to photosynthesis at water CO₂ concentrations up to 1000 µmol L⁻¹. For all species except Ludwigia, the shoot to root ratio on an areal basis was the single factor best explaining variability in the importance of sediment CO₂. For Ludwigia, diffusion barriers limited uptake or transport from roots to stems and transport from stems to leaves.

Conclusions

Submersed plants other than isoetids can utilize sediment CO₂, and small and medium sized elodeids with high root to shoot area in particular may benefit substantially from uptake of sediment CO₂ in low alkaline lakes.Key words: Submersed rooted plants, CO₂ uptake, sediment CO₂, Lobelia dortmanna, Lilaeopsis macloviana, Ludwigia repens, Vallisneria americana, Hydrocotyle verticillata     

Effect of carbon dioxide and temperature on photosynthetic CO2 uptake and photorespiratory CO2 evolution in sunflower leaves

Using an open gas-exchange system, apparent photosynthesis, true photosynthesis (TPS), photorespiration (PR) and dark respiration of sunflower (Helianthus annuus L.) leaves were determined at three temperatures and between 50 and 400 l/l external CO₂. The ratio of PR/TPS and the solubility ratio of O₂/CO₂ in the intercellular spaces both decreased with increasing CO₂. The rate of PR was not affected by the CO₂ concentration in the leaves and was independent of the solubility ratio of oxygen and CO₂ in the leaf cell. At photosynthesis-limiting concentrations of CO₂, the ratio of PR/TPS significantly increased from 18 to 30°C and the rate of PR increased from 4.3 mg CO₂ dm^-2 h^-1 at 18°C to 8.6 mg CO₂ dm^-2 h^-1 at 30°C. The specific activity of photorespired CO₂ was CO₂-dependent but temperature-independent, and the carbon traversing the glycolate pathway appeared to be derived both from recently fixed assimilate and from older reserve materials. It is concluded that PR as a percentage of TPS is affected by the concentrations of O₂ and CO₂ around the photosynthesizing cells, but the rate of PR may also be controlled by other factors.Abbreviations APS apparent photosynthesis (net CO₂ uptake) - PR photorespiration (CO₂ evolution in light) - RuBP ribulose-1,5-bisphosphate - TPS true photosynthesis (true CO₂ uptake)     

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.     

TRANSPORT OF CARBON AMONG CONNECTED RAMETS OF EICHHORNIA CRASSIPES (PONTEDERIACEAE) AT NORMAL AND HIGH LEVELS OF CO2

The floating, stoloniferous plant, Eichhornia crassipes, has high rates of productivity and rapidly invades new sites. Because the transport of carbon among connected ramets is known to increase the growth of clonal plants, we asked whether there is intraclonal carbon transport in E. crassipes. Because net photosynthesis of E. crassipes is significantly higher at high levels of atmospheric CO₂, we also asked if high CO₂ can change patterns of carbon transport in ways that might modify clonal growth. We exposed individual ramets within groups of connected ramets to ¹⁴CO₂ for 15–45 min and measured the distribution of ¹⁴C in the group after 4 days of growth at 350, 700, 1,400, or 2,800 μ1 1^−-1 CO₂. At 350 μ1 1^−-1 CO₂, a parent ramet exported approximately 10% of the ¹⁴C that it assimilated to its first rooted offspring ramet. The offspring exported a similar percentage of the ^l4C it assimilated toward the parent; two-thirds of this ¹⁴C was retained by the parent, and one-third moved into new offspring of the parent. In all ramets, imported carbon moved into leaves as well as roots. At the higher levels of CO₂, the percentage of assimilated carbon exported from a parent ramet to the leaf blades of its first offspring was lower by half. High CO₂ had little other effect on carbon transport. E. crassipes maintains bidirectional transport of carbon between ramets even under uniform and favorable environmental conditions and when external CO₂ levels are very high.     

The effect of oxygen on 14CO2 fixation in mesophyll cells isolated from Digitaria sanguinalis (L.) Scop. leaves

Mesophyll cells were isolated from fully-expanded leaves of $\text{Digitaria sanguinalis}$ (L.) Scop. by a combined maceration-filtration technique. In the presence of pyruvate, photosynthetic ¹⁴CO₂ uptake in the isolated cells was not inhibited by atomospheric levels of oxygen. In contrast, superatmospheric levels of oxygen substantially inhibited the light-dependent fixation of ¹⁴CO₂. These oxygen effects are similar to those observed with intact C4 leaves and suggest that the lack of inhibition of C4 photosynthesis by atmospheric levels of oxygen results from the relative oxygen-insensitivity of the phosphopyruvate carboxylase-CO₂ pump in the mesophyll.     

Carbon isotope fractionation in plants

Plants with the C₃, C₄, and crassulacean acid metabolism (CAM) photosynthetic pathways show characteristically different discriminations against ¹³C during photosynthesis. For each photosynthetic type, no more than slight variations are observed within or among species. CAM plants show large variations in isotope fractionation with temperature, but other plants do not. Different plant organs, subcellular fractions and metabolises can show widely varying isotopic compositions. The isotopic composition of respired carbon is often different from that of plant carbon, but it is not currently possible to describe this effect in detail. The principal components which will affect the overall isotope discrimination during photosynthesis are diffusion of CO₂, interconversion of CO₂ and HCO^?₃, incorporation of CO₂ by phosphoenolpyruvate carboxylase or ribulose bisphosphate carboxylase, and respiration. Theisotope fractionations associated with these processes are summarized. Mathematical models are presented which permit prediction of the overall isotope discrimination in terms of these components. These models also permit a correlation of isotope fractionations with internal CO₂ concentrations. Analysis of existing data in terms of these models reveals that CO₂ incorporation in C₃ plants is limited principally by ribulose bisphosphate carboxylase, but CO₂ diffusion also contributes. In C₄ plants, carbon fixation is principally limited by the rate of CO₂ diffusion into the leaf. There is probably a small fractionation in C₄ plants due to ribulose bisphosphate carboxylase.     

Inhibition of Dark CO(2) Fixation and Photosynthesis in Leaf Discs of Corn Susceptible to the Host-specific Toxin Produced by Helminthosporium maydis, Race T

The host-specific toxin produced by Helminthosporium maydis, race T, causes 50% inhibition of dark fixation of ¹⁴CO₂ by leaf discs of susceptible (Texas male sterile) corn when it is diluted to approximately 1/10,000 of the volume of the original fungus culture filtrate. Dilutions of 1/10 or less are required for equivalent inhibition of discs prepared from resistant (N) corn. Root growth and photosynthesis were considerably less sensitive (dilution values 1/3000 and 1/1200, respectively), as was leakage of ¹⁴C induced by toxin from preloaded discs. Based on literature values for dilutions causing ion leakage or inhibition of mitochondrial oxidation, toxin dilutions several orders of magnitude greater bring about inhibition of dark CO₂ fixation. Preincubation of discs in light increased sensitivity of dark fixation to toxin and an effect of light on symptom development was shown. Phosphoenolypruvate carboxylase activity in extracts of roots or leaves was not affected by toxin nor was the enzyme level altered in excised leaves treated with toxin. Inhibition of dark fixation of CO₂ provides a bioassaay for race T toxin which is both reliable and rapid.     

Photosynthesis of Lipids from CO(2) in Spinacia oleracea

Young expanding spinach leaves exposed to ¹⁴CO₂ under physiological conditions for up to 20 minutes assimilated CO₂ into lipids at a mean rate of 7.6 micromoles per milligram chlorophyll per hour following a lag period of 5 minutes. Label entered into all parts of the lipid molecule and only 28% of the ¹⁴C fixed into lipids was found in the fatty acid moieties, i.e. fatty acids were synthesized from CO₂in vivo at a mean rate of 2.1 micromoles per milligram chlorophyll per hour. Intact spinach chloroplasts isolated from these leaves incorporated H¹⁴CO₃ into fatty acids at a maximal rate of 0.6 micromole per milligram chlorophyll per hour, but were unable to synthesize either the polar moieties of their lipids or polyunsaturated fatty acids. Since isolated chloroplasts will only synthesize fatty acids at rates similar to the one obtained with intact leaves in vivo if acetate is used as a precursor, it is suggested that acetate derived from leaf mitochondria is the physiological fatty acid precursor.     

Catabolism of 5-Aminolevulinic Acid to CO(2) by Etiolated Barley Leaves

The in vivo oxidation of the C₄ and C₅ of 5-aminolevulinic acid (ALA) to CO₂ has been studied in etiolated barley (Hordeum vulgare L. var. Larker) leaves in darkness. The rate of ¹⁴CO₂ evolution from leaves fed [4-¹⁴C]ALA is strongly inhibited by aminooxyacetate, anaerobiosis, and malonate. The rate of ¹⁴CO₂ evolution from leaves fed [5-¹⁴C]ALA is also inhibited by these treatments but to a lesser extent. These results suggest that (a) one step in ALA catabolism is a transamination reaction and (b) the C₄ is oxidized to CO₂ via the tricarboxylic acid cycle to a greater extent than is the C₅.