Glycolate Metabolism and Excretion by Chlamydomonas reinhardtii

The flux of glycolate through the C₂ pathway in Chlamydomonas reinhardtii was estimated after inhibition of the pathway with aminooxyacetate (AOA) or aminoacetonitrile (AAN) by measurement of the accumulation of glycolate and glycine. Cells grown photoautotrophically in air excreted little glycolate except in the presence of 2 mm AOA when they excreted 5 micromoles glycolate per hour per milligram clorophyll. Cells grown on high CO₂ (1-5%) when transferred to air produced three times as much glycolate, with half of the glycolate metabolized and half excreted. The lower amount of glycolate produced by the air-grown cells reflects the presence of a CO₂ concentrating mechanism which raises the internal CO₂ level and decreases the ribulose-1,5-bisP oxygenase reaction for glycolate production. Despite the presence of the CO₂ concentrating mechanism, there was still a significant amount of glycolate produced and metabolized by air-grown Chlamydomonas. The capacity of these cells to metabolize between 5 and 10 micromoles of glycolate per hour per milligram chlorophyll was confirmed by measuring the biphasic uptake of added labeled glycolate. The initial rapid (<10 seconds) phase represented uptake of glycolate; the slow phase represented the metabolism of glycolate. The rates of glycolate metabolism were in agreement with those determined using the C₂-cycle inhibitors during CO₂ fixation.     

Glycolate Metabolism in Low and High CO(2)-Grown Chlorella pyrenoidosa and Pavlova lutheri as Determined by O-Labeling

Photorespiration in Chlorella pyrenoidosa Chick. was assayed by measuring ¹⁸O-labeled intermediates of the glycolate pathway. Glycolate, glycine, serine, and excreted glycolate were isolated and analyzed on a gas chromatograph/mass spectrometer to determine isotopic enrichment. Rates of glycolate synthesis were determined from ¹⁸O-labeling kinetics of the intermediates, pool sizes, derived rate equations, and nonlinear regression techniques. Glycolate synthesis was higher in high CO₂-grown cells than in air-grown cells when both were assayed under the same O₂ and CO₂ concentrations. Synthesis of glycolate, for both types of cells, was stimulated by high O₂ levels and inhibited by high CO₂ levels. Glycolate synthesis in 1.5% CO₂-grown Chlorella, when exposed to a 0.035% CO₂ atmosphere, increased from about 41 to 86 nanomoles per milligram chlorophyll per minute when the O₂ concentration was increased from 21% to 40%. Glycolate synthesis in air-grown cells increased from 2 to 6 nanomoles per milligram chlorophyll per minute under the same gas levels. Synthesis was undetectable when either the O₂ concentration was lowered to 2% or the CO₂ concentration was raised to 1.5%. Glycolate excretion was also sensitive to O₂ and CO₂ concentrations in 1.5% CO₂-grown cells and the glycolate that was excreted was ¹⁸O-labeled. Air-grown cells did not excrete glycolate under any experimental condition. Indirect evidence indicated that glycolate may be excreted as a lactone in Chlorella. Photorespiratory ¹⁸O-labeling kinetics were determined for Pavlova lutheri, which unlike Chlorella and higher plants did not directly synthesize glycine and serine from glycolate. This alga did excrete a significant proportion of newly synthesized glycolate into the media.     

Photorespiratory Properties of Mesophyll Protoplasts of Nicotiana plumbaginifolia

The photorespiratory activity of mesophyll protoplasts of Nicotiana plumbaginifolia has been clearly demonstrated by the presence of a Warburg-effect, the occurrence of an important CO₂-sensitive O₂ uptake and the effect of some photorespiratory inhibitors on photosynthetic activity. At a nonsaturating dissolved inorganic carbon (DIC) concentration (0.1 millimolar), we observed that the rate of CO₂ fixation was 60% lower at 50% O₂ compared to that measured at 2% O₂. Using ¹⁸O₂ and mass spectrometry, we measured O₂ exchange as a function of light intensity and of DIC concentration. Oxygen uptake measured at the CO₂ compensation point (47.4 micromoles O₂ per hour per milligram chlorophyll) was three-fold higher than that measured at a saturating CO₂ concentration. Cyanide or iodoacetamide, inhibitors of the Calvin cycle, were found to reduce the O₂ uptake to the same extent as CO₂ saturation. We conclude from these results that the major part of the CO₂-sensitive O₂ uptake is due to photorespiration. Further, we investigated the effect on net photosynthesis of some inhibitors of the glycolate pathway. At CO₂ saturation (10 millimolar DIC), 5 millimolar aminoacetonitrile (AAN), and 1 millimolar aminooxyacetate (AOA) did not cause any significant decrease in net photosynthesis. However, when these two inhibitors were added under a period of active photorespiration (10 minutes at the CO₂ compensation point at 20% O₂), we observed a decrease in the rate of net photosynthesis at 10 millimolar DIC measured afterward (respectively, 18 and 29%). This inhibition did not appear at 2% O₂, but was stronger at 50% O₂ (40% for AAN and 47% for AOA). With 0.05 millimolar butyl 2-hydroxy-3-butynoate (BHB) or 0.5 millimolar l-methionine-dl-sulfoximine (l-MSO), rates of net photosynthesis at 10 millimolar DIC were decreased by 10 to 15%. Additional decreases were observed after a period at the CO₂ compensation point at 20% O₂ (30% for BHB and 20% for l-MSO). From the sites of action of the four inhibitors tested, we suggest the inhibition of photosynthesis occurring after a period of active photorespiration to be due to the toxic accumulation of nonmetabolized phosphoglycolate.     

The Regulation of Photosynthesis in Leaves of Field-Grown Spring Wheat (Triticum aestivum L., cv Albis) at Different Levels of Ozone in Ambient Air

Wheat (Triticum aestivum L. cv Albis) was grown in open-top chambers in the field and fumigated daily with charcoal-filtered air (0.015 microliters per liter O₃), nonfiltered air (0.03 microliters per liter O₃), and air enriched with either 0.07 or 0.10 microliters per liter ozone (seasonal 8 hour/day [9 am-5 pm] mean ozone concentration from June 1 until July 10, 1987). Photosynthetic ¹⁴CO₂ uptake was measured in situ. Net photosynthesis, dark respiration, and CO₂ compensation concentration at 2 and 21% O₂ were measured in the laboratory. Leaf segments were freeze-clamped in situ for the determination of the steady state levels of ribulose 1,5-bisphosphate, 3-phosphoglycerate, triose-phosphate, ATP, ADP, AMP, and activity of ribulose, 1,5-bisphosphate carboxylase/oxygenase. Photosynthesis of flag leaves was highest in filtered air and decreased in response to increasing mean ozone concentration. CO₂ compensation concentration and the ratio of dark respiration to net photosynthesis increased with ozone concentration. The decrease in photosynthesis was associated with a decrease in chlorophyll, soluble protein, ribulose bisphosphate carboxylase/oxygenase activity, ribulose bisphosphate, and adenylates. No decrease was found for triose-phosphate and 3-phosphoglycerate. The ratio of ATP to ADP and of triosephosphate to 3-phosphoglycerate were increased suggesting that photosynthesis was limited by pentose phosphate reductive cycle activity. No limitation occurred due to decreased access of CO₂ to photosynthetic cells since the decrease in stomatal conductance with increasing ozone concentration did not account for the decrease in photosynthesis. Ozonestressed leaves showed an increased degree of activation of ribulose bisphosphate carboxylase/oxygenase and a decreased ratio of ribulose bisphosphate to initial activity of ribulose bisphosphate carboxylase/oxygenase. Nevertheless, it is suggested that photosynthesis in ozone stressed leaves is limited by ribulose bisphosphate carboxylation possibly due to an effect of ozone on the catalysis by ribulose bisphosphate carboxylase/oxygenase.     

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.     

Ammonia exchange and photorespiration in chlamydomonas

Two hours after the addition of l-methionine-dl-sulfoximine to the cell suspension, glutamine synthetase activity was inhibited by more than 90% in air-grown Chlamydomonas reinhardii. Cells continued to take up NH₃ from the medium provided that the concentration of dissolved CO₂ was high (equilibrated with 4% CO₂ in air). This NH₃ uptake, about 30% of the control, is discussed in terms of glutamate dehydrogenase activity. Without CO₂, or with a low CO₂ level, a NH₃ excretion was observed, the rate of which depended on the actual concentration of the dissolved CO₂. Experiments with ¹⁵NH₃ demonstrated that no NH₃ uptake was masked by this excretion and inversely that no excretion occurred during the uptake in the conditions where it took place. Furthermore, the NH₃ excretion observed in the absence of CO₂ increased when O₂ concentration rose to 15% and was inhibited when 10 millimolar isonicotinic acid hydrazide was supplied to the algal suspension. Thus, NH₃ excretion in the presence of l-methionine-dl-sulfoximine seems to be related to a photorespiratory process inasmuch as it presents the same properties with regard to the O₂ and the isonicotinic acid hydrazide effects. These results favor the hypothesis that NH₃ produced in the medium originates from the glycine to serine reaction. On the other hand, partial inhibition (50%) of photosynthesis by l-methionine-dl-sulfoximine was attributed to uncoupling between electron transfer and photophosphorylation due to NH₃ accumulation into the cell.     

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.     

Synthesis, Excretion, and Metabolism of Glycolate under Highly Photorespiratory Conditions in Euglena gracilis Z

Glycolate was excreted from the 5% CO₂-grown cells of Euglena gracilis Z when placed in an atmosphere of 100% O₂ under illumination at 20,000 lux. The amount of excreted glycolate reached 30% of the dry weight of the cells during incubation for 12 hours. The content of paramylon, the reserve polysaccharide of E. gracilis, was decreased during the glycolate excretion, and of the depleted paramylon carbon, two-thirds was excreted to the outside of cells and the remaining metabolized to other compounds, both as glycolate. The paramylon carbon entered Calvin cycle probably as triose phosphate or 3-phosphoglycerate, but not as CO₂ after the complete oxidation through the tricarboxylic acid cycle. The glycolate pathway was partially operative and the activity of the pathway was much less than the rate of the synthesis of glycolate in the cells under 100% O₂ and 20,000 lux; this led the cells to excrete glycolate outside the cells. Exogenous glycolate was metabolized only to CO₂ but not to glycine and serine. The physiologic role of the glycolate metabolism and excretion under such conditions is discussed.     

Effects of aminoacetonitrile on net photosynthesis, ribulose-1,5-bisphosphate levels, and glycolate pathway intermediates

The effects of aminoacetonitrile (a competitive inhibitor of glycine oxidation) on net photosynthesis, glycolate pathway intermediates, and ribulose-1,5-bisphosphate (RuBP) levels have been investigated at different O₂ and CO₂ concentrations with soybean (Glycine max)[L] Merr. cv Pioneer 1677) leaf discs floated on 25 millimolar aminoacetonitrile (AAN) for 50 minutes prior to assay.

At 2% O₂ and 200 or 330 microliters per liter CO₂, the inhibitor had no effect on the rate of net photosynthesis and RuBP levels when compared with the control levels. At 11% to 60% O₂, AAN caused a decrease in net photosynthesis in addition to the inhibition by O₂. This extra inhibition ranged from 22% to 59% depending on the O₂ and CO₂ concentrations. The levels of RuBP, however, were 1.3 to 2.7 times higher than in the control plants at the same O₂ concentrations. At 40% O₂ and 200 microliters per liter CO₂, the inhibitor caused a 6-fold increase in glycine and more than 2-fold increase in glyoxylate levels, whereas those of glycolate decreased by approximately one-half.

The decrease in net photosynthesis observed with AAN is not the result of the depletion of the RuBP pool due to the lack of recycling of carbon from the glycolate pathway to the Calvin cycle. The higher levels of RuBP caused by AAN in photorespiratory conditions, suggest that RuBP carboxylase was inhibited. Glyoxylate could be a possible candidate for the inhibition of the enzyme but what is known so far about its inhibitory properties in vitro may not fit the existing in vivo conditions. An alternative explanation for the inhibition is proposed.

     

EXCRETION OF GLYCOLATE BY A SPECIES OF CHLORELLA (CHLOROPHYCEAE)1

The claim that Chlorella sp. (CCAP 211/8p), sometimes referred to as C. fusca, Shihira and Krauss, does not excrete glycolate has been reexamined. Chlorella sp. grown on 5% CO₂in air, excreted glycolate when incubated in light in 10 mM bicarbonate. Excretion ceased 30–60 min after transfer of the cells to air and no excretion could be detected with air-grown cells or with cells grown on 5% CO₂in media buffered at pH 8.0. Incubation with 10 mM isonicotinyl hydrazide, a glycolate pathway inhibitor, caused excretion in air-grown cells and stimulated excretion in CO₂-grown cells indicating that both the rate of glycolate synthesis and metabolism is higher in CO₂grown cells than in air-grown cells. Enhanced glycolate synthesis and excretion in CO₂-grown cells is correlated with law photosynthetic rate in 10 mM bicarbonate, and the photosynthetic rate of these cells doubles over a period of 2–2.5 h after initial transfer from high CO₂to bicarbonate. This correlation of photosynthetic induction with cessation of glycolate excretion is similar to that reported in a bluegreen alga and thought to occur in other green algae. These results indicate that glycolate excretion and its regulation in this species of Chlorella is not different from that in other algae.     

Short-Term and Long-Term Responses of Crassulacean Acid Metabolism Plants to Elevated CO(2)

For the leaf succulent Agave deserti and the stem succulent Ferocactus acanthodes, increasing the ambient CO₂ level from 350 microliters per liter to 650 microliters per liter immediately increased daytime net CO₂ uptake about 30% while leaving nighttime net CO₂ uptake of these Crassulacean acid metabolism (CAM) plants approximately unchanged. A similar enhancement of about 30% was found in dry weight gain over 1 year when the plants were grown at 650 microliters CO₂ per liter compared with 350 microliters per liter. Based on these results plus those at 500 microliters per liter, net CO₂ uptake over 24-hour periods and dry weight productivity of these two CAM succulents is predicted to increase an average of about 1% for each 10 microliters per liter rise in ambient CO₂ level up to 650 microliters per liter.     

Effects of CO(2)-Enrichment and of Aminoacetonitrile on Growth and Photosynthesis of Photoautotrophic Calli of Nicotiana plumbaginifolia

Photoautotrophic calli of Nicotiana plumbaginifolia were grown for 3 weeks under two CO₂ concentrations (500 and 20,000 microliters of CO₂ per liter). Calli cultured at high CO₂ exhibited a two-fold higher rate of growth. At CO₂ test levels, these calli were characterized by a lower net photosynthetic capacity than calli cultured at low CO₂. This diminution due to CO₂ adaptation could be ascribed to a 170% stimulation of dark respiration, a 40% decrease in total ribulose-1,5-bisphosphate carboxylase (Rubisco) activity, and also to a feedback inhibition of photosynthesis: high CO₂ grown calli contained about 5.5-fold more sucrose and three-fold less orthophosphate (Pi) than low CO₂ grown calli. Whether the decrease in Rubisco activity is related to the accumulation of sucrose and to the Pi limitation is discussed. Both calli exhibited a Warburg-effect showing the existence of active photorespiration at low CO₂. In calli grown at low CO₂ with 5 millimolar aminoacetonitrile (AAN), an inhibitor of the glycolate pathway, fresh weight decreased by 25% and chlorophyll content by 40%, dark respiration increased by 50% and net CO₂ uptake decreased by about 60% at 340 microliters of CO₂ per liter and 35% at 10,000 microliters of CO₂ per liter. In these calli, glutamine and glutamate contents were half of control calli. In contrast, AAN did not provoke any noticeable effect in calli grown at high CO₂. In photoautotrophic calli, the inhibition of the glycolate pathway by AAN results in severe perturbations in glutamate metabolism and in chlorophyll biosynthesis.     

Carbon Dioxide and Light Responses of Photosynthesis in Cowpea and Pigeonpea during Water Deficit and Recovery

Greenhouse-grown pigeonpea (Cajanus cajan, [L.] Millsp.; cultivar UW-10) and cowpea (Vigna unguiculata, [L.] Walp.; cultivar California No. 5) were well-watered (control) or subjected to low water potential by withholding water to compare their modes of adaptation to water-limited conditions. Leaf CO₂ exchange rate (CER), leaf diffusive conductance to CO₂ (g_l), and CO₂ concentration in the leaf intercellular air space (C_i) were determined at various CO₂ concentrations and photon flux densities (PFD) of photosynthetically active radiation (400 to 700 nanometer). In cowpea, g_l declined to less than 15% of controls and total water potential (ψ_w) at midafternoon declined to −0.8 megapascal after 5 days of withholding water, whereas g_l in pigeonpea was about 40% of controls even though midafternoon ψ_w was −1.9 megapascal. After 8 days of withholding water, ψ_w at midafternoon declined to −0.9 and −2.4 megapascals in cowpea and pigeonpea, respectively. The solute component of water potential (ψ_s) decreased substantially less in cowpea than pigeonpea. Photosynthetic CER at saturation photon flux density (PFD) and ambient external CO₂ concentration (360 microliters per liter) on day 5 of withholding decreased by 83 and 55% in cowpea and pigeonpea, respectively. When measured at external, CO₂ concentration in bulk air of 360 microliters per liter, the CER of cowpea had fully recovered to control levels 3 days after rewatering; however, at 970 microliters per liter the PFD-saturated CERs of both species were substantially lower than in controls, indicating residual impairment. In stressed plants of both species the CER responses to C_i from 250 to 600 microliters per liter indicated that a substantial nonstomatal inhibition of CER had occurred. Although the sensitivity of g_l to water limitation in cowpea suggested a dehydration avoidance response, parallel measurements of CER at various C_i and PFD indicated that photosynthetic activity of cowpea mesophyll was substantially inhibited by the water-limited treatment.     

Oxygen exchange in leaves in the light

Photosynthetic O₂ production and photorespiratory O₂ uptake were measured using isotopic techniques, in the C₃ species Hirschfeldia incana Lowe., Helianthus annuus L., and Phaseolus vulgaris L. At high CO₂ and normal O₂, O₂ production increased linearly with light intensity. At low O₂ or low CO₂, O₂ production was suppressed, indicating that increased concentrations of both O₂ and CO₂ can stimulate O₂ production. At the CO₂ compensation point, O₂ uptake equaled O₂ production over a wide range of O₂ concentrations. O₂ uptake increased with light intensity and O₂ concentration. At low light intensities, O₂ uptake was suppressed by increased CO₂ concentrations so that O₂ uptake at 1,000 microliters per liter CO₂ was 28 to 35% of the uptake at the CO₂ compensation point. At high light intensities, O₂ uptake was stimulated by low concentrations of CO₂ and suppressed by higher concentrations of CO₂. O₂ uptake at high light intensity and 1000 microliters per liter CO₂ was 75% or more of the rate of O₂ uptake at the compensation point. The response of O₂ uptake to light intensity extrapolated to zero in darkness, suggesting that O₂ uptake via dark respiration may be suppressed in the light. The response of O₂ uptake to O₂ concentration saturated at about 30% O₂ in high light and at a lower O₂ concentration in low light. O₂ uptake was also observed with the C₄ plant Amaranthus edulis; the rate of uptake at the CO₂ compensation point was 20% of that observed at the same light intensity with the C₃ species, and this rate was not influenced by the CO₂ concentration. The results are discussed and interpreted in terms of the ribulose-1,5-bisphosphate oxygenase reaction, the associated metabolism of the photorespiratory pathway, and direct photosynthetic reduction of O₂.     

Oxygen inhibition of photosynthesis and stimulation of photorespiration in soybean leaf cells

The occurrence of photorespiration in soybean (Glycine max [L.] Merr.) leaf cells was demonstrated by the presence of an O₂-dependent CO₂ compensation concentration, a nonlinear time course for photosynthetic ¹⁴CO₂ uptake at low CO₂ and high O₂ concentrations, and an O₂ stimulation of glycine and serine synthesis which was reversed by high CO₂ concentration. The compensation concentration was a linear function of O₂ concentration and increased as temperature increased. At atmospheric CO₂ concentration, 21% O₂ inhibited photosynthesis at 25 C by 27%. Oxygen inhibition of photosynthesis was competitive with respect to CO₂ and increased with increasing temperature. The Km (CO₂) of photosynthesis was also temperature-dependent, increasing from 12 μm CO₂ at 15 C to 38 μm at 35 C. In contrast, the Ki (O₂) was similar at all temperatures. Oxygen inhibition of photosynthesis was independent of irradiance except at 10 mm bicarbonate and 100% O₂, where inhibition decreased with increasing irradiance up to the point of light saturation of photosynthesis. Concomitant with increasing O₂ inhibition of photosynthesis was an increased incorporation of carbon into glycine and serine, intermediates of the photorespiratory pathway, and a decreased incorporation into starch. The effects of CO₂ and O₂ concentration and temperature on soybean cell photosynthesis and photorespiration provide further evidence that these processes are regulated by the kinetic properties of ribulose-1,5-diphosphate carboxylase with respect to CO₂ and O₂.     

The occurrence of glycolate dehydrogenase and glycolate oxidase in green plants: an evolutionary survey

Homogenates of various lower land plants, aquatic angiosperms, and green algae were assayed for glycolate oxidase, a peroxisomal enzyme present in green leaves of higher plants, and for glycolate dehydrogenase, a functionally analogous enzyme characteristic of certain green algae. Green tissues of all lower land plants examined (including mosses, liverworts, ferns, and fern allies), as well as three freshwater aquatic angiosperms, contained an enzyme resembling glycolate oxidase, in that it oxidized l- but not d-lactate in addition to glycolate, and was insensitive to 2 mm cyanide. Many of the green algae (including Chlorella vulgaris, previously claimed to have glycolate oxidase) contained an enzyme resembling glycolate dehydrogenase, in that it oxidized d- but not l-lactate, and was inhibited by 2 mm cyanide. Other green algae had activity characteristic of glycolate oxidase and, accordingly, showed a substantial glycolate-dependent O₂ uptake. It is pointed out that this distribution pattern of glycolate oxidase and glycolate dehydrogenase among the green plants may have phylogenetic significance.     

Gas Exchange Characteristics of the Submerged Aquatic Crassulacean Acid Metabolism Plant, Isoetes howellii

The submerged aquatic plant Isoetes howellii Engelmann possesses Crassulacean acid metabolism (CAM) comparable to that known from terrestrial CAM plants. Infrared gas analysis of submerged leaves showed Isoetes was capable of net CO₂ uptake in both light and dark. CO₂ uptake rates were a function of CO₂ levels in the medium. At 2,500 microliters CO₂ per liter (gas phase, equivalent to 1.79 milligrams per liter aqueous phase), Isoetes leaves showed continuous uptake in both the light and dark. At this CO₂ level, photosynthetic rates were light saturated at about 10% full sunlight and were about 3-fold greater than dark CO₂ uptake rates. In the dark, CO₂ uptake rates were also a function of length of time in the night period. Measurements of dark CO₂ uptake showed that, at both 2,500 and 500 microliters CO₂ per liter, rates declined during the night period. At the higher CO₂ level, dark CO₂ uptake rates at 0600 h were 75% less than at 1800 h. At 500 microliters CO₂ per liter, net CO₂ uptake in the dark at 1800 h was replaced by net CO₂ evolution in the dark at 0600 h. At both CO₂ levels, the overnight decline in net CO₂ uptake was marked by periodic bursts of accelerated CO₂ uptake. CO₂ uptake in the light was similar at 1% and 21% O₂, and this held for leaves intact as well as leaves split longitudinally. Estimating the contribution of light versus dark CO₂ uptake to the total carbon gain is complicated by the diurnal flux in CO₂ availability under field conditions.     

Short-Term Effects of CO(2) on Gas Exchange of Leaves of Bigtooth Aspen (Populus grandidentata) in the Field

The short term effects of increased levels of CO₂ on gas exchange of leaves of bigtooth aspen (Populus grandidentata Michx.) were studied at the University of Michigan Biological Station, Pellston, MI. Leaf gas exchange was measured in situ in the upper half of the canopy, 12 to 14 meters above ground. In 1900 microliters per liter CO₂, maximum CO₂ exchange rate (CER) in saturating light was increased by 151% relative to CER in 320 microliters per liter CO₂. The temperature optimum for CER shifted from 25°C in 320 microliters per liter CO₂ to 37°C in 1900 microliters per liter CO₂. In saturating light, increasing CO₂ level over the range 60 to 1900 microliters per liter increased CER, decreased stomatal conductance, and increased leaf water use efficiency. The initial slope of the CO₂ response curve of CER was not significantly different at 20 and 30°C leaf temperatures, although the slope did decline significantly during leaf senescence. In 1900 microliters per liter CO₂, CER increased with increasing light. The light saturation point and maximum CER were higher in 30°C than in 20°C, although there was little effect of temperature in low light. The experimental results are consistent with patterns seen in laboratory studies of other C₃ species and define the parameters required by some models of aspen CER in the field.     

Measurement of carbon dioxide compensation points of freshwater algae

A technique is described for the measurement of total dissolved inorganic carbon by acid release as CO₂ followed by its conversion to methane and detection by flame ionization in a modified gas chromatograph. This method was used to determine the dissolved inorganic carbon concentration reached at compensation point when algae were allowed to photosynthesize in a closed system in a buffer at known pH, and the CO₂ compensation point was calculated from this concentration. The CO₂ compensation points of 16 freshwater algae were measured at acid and alkaline pH in air-saturated medium: at acid pH the CO₂ compensation points ranged from 4.8 to 41.5 microliters per liter while at alkaline pH they ranged from 0.2 to 7.2 microliters per liter. Removal of O₂ from the medium caused a slight lowering of compensation point at acid pH but had little effect at alkaline pH. These low, O₂-insensitive compensation points are characteristic of C₄ plants. It is suggested that these low CO₂ compensation points are maintained by an active bicarbonate uptake by algae especially at alkaline pH.     

Glycolate Formation and Excretion by Chlorella pyrenoidosa and Netrium digitus

Conditions are described whereby suspensions of Chlorella pyrenoidosa and Netrium digitus photosynthetically biosynthesize and excrete glycolate continuously in high yields. Aminooxyacetic acid, an inhibitor of pyridoxal phosphate-linked enzymes, increased the excretion of glycolate approximately 4-fold in 1 hour (8 millimolar) and 20-fold in 4 hours (40 millimolar) in the presence of 0.2% CO₂ in air. The amount of glycolate excreted in the presence of aminooxyacetate and an atmosphere of 0.2% CO₂ in air equaled or exceeded the amount excreted in 0.2% CO₂ in O₂ minus aminooxyacetate. CO₂ and light were required for glycolate excretion. Aminooxyacetate also stimulated photosynthetic glycolate excretion in an atmosphere of 0.2% CO₂ in nitrogen or helium, although the stimulation was not as great as when air or O₂ was present.

The excreted glycolate was converted to H₂ and CO₂ by the combined action of glycolic oxidase and the formic hydrogenlyase complex found in Escherichia coli in total conversion yields of 80%.