Effect of CO2 on Colony Development by Bifidobacterium Species

This report investigates the requirement for CO₂ for colony formation by Bifidobacterium species in both anoxic and oxic environments. All tested Bifidobacterium species exhibited difficulty in developing colonies in an atmosphere of 100% N₂ but developed well when 1% CO₂ was present. In the presence of CO₂, the oxygen tolerance of the tested species was not improved. In the absence of CO₂, only B. boum, a microaerophilic species, could develop colonies under an N₂-based 5% O₂ atmosphere, indicating that while CO₂ is not an essential factor for colony development, both CO₂ and O₂ have stimulatory effects on B. boum colony development.     

The Effect of Temperature on the Occurrence of O(2) and CO(2) Insensitive Photosynthesis in Field Grown Plants

The sensitivity of photosynthesis to O₂ and CO₂ was measured in leaves from field grown plants of six species (Phaseolus vulgaris, Capsicum annuum, Lycopersicon esculentum, Scrophularia desertorum, Cardaria draba, and Populus fremontii) from 5°C to 35°C using gas-exchange techniques. In all species but Phaseolus, photosynthesis was insensitive to O₂ in normal air below a species dependent temperature. CO₂ insensitivity occurred under the same conditions that resulted in O₂ insensitivity. A complete loss of O₂ sensitivity occurred up to 22°C in Lycopersicon but only up to 6°C in Scrophularia. In Lycopersicon and Populus, O₂ and CO₂ insensitivity occurred under conditions regularly encountered during the cooler portions of the day. Because O₂ insensitivity is an indicator of feedback limited photosynthesis, these results indicate that feedback limitations can play a role in determining the diurnal carbon gain in the field. At higher partial pressures of CO₂ the temperature at which O₂ insensitivity occurred was higher, indicating that feedback limitations in the field will become more important as the CO₂ concentration in the atmosphere increases.     

Survival of Aspergillus flavus and Fusarium moniliforme in High-Moisture Corn Stored Under Modified Atmospheres

Freshly harvested high-moisture corn with 29.4% moisture and corn remoistened to 19.6% moisture were inoculated with Aspergillus flavus Link ex Fr. and stored for 4 weeks at about 27 C in air (0.03% CO₂, 21% O₂, and 78% N₂) and three modified atmospheres: (i) 99.7% N₂ and 0.3% O₂; (ii) 61.7% CO₂, 8.7% O₂, and 29.6% N₂; and (iii) 13.5% CO₂, 0.5% O₂, and 84.8% N₂. Kernel infections by A. flavus, Fusarium moniliforme (Sheld.) Snyd. et Hans., and other fungi were monitored weekly. The modified-atmosphere treatments delayed deterioration by A. flavus and F. moniliforme, but their growth was not completely stopped. A. flavus survived better in the remoistened than in the freshly harvested corn. F. moniliforme survived in both. A. flavus and F. moniliforme were the dominant fungi in corn removed from the modified atmospheres and exposed to normal air for 1 week.     

Interactive Effects of CO(2) and O(2) in Soil on Root and Top Growth of Barley and Peas

Barley and pea plants were grown under several regimens of different compositions of soil atmosphere, the O₂ concentration varying from 0 to 21% and the CO₂ concentration from 0 to 8%. In absence of CO₂, the effect of O₂ on root length in barley was characterized by equal root lengths within the range of 21 to 7% O₂ and a steep decline between 7 and 0%. In peas, while showing the same general response, the decline occurred between 14 and 7% O₂. Root numbers of the seminal roots of barley decreased already with reduction in O₂ concentration from 21 to 14%. Dry matter production was affected somewhat differently by O₂ and CO₂ concentration. Dry matter production in barley was reduced at 14% O₂ while root length decreased between 7 and 0%. In peas, dry matter production was favored by low CO₂ concentrations except where there was no oxygen. At 21% O₂, increasing CO₂ concentrations did not seem to affect root length up to concentrations of 2% CO₂. At 8% CO₂, root length was decreased. The inter-active effects of CO₂ and O₂ are characterized by a reduced susceptibility to CO₂ at O₂ values below 7%, and a very deleterious effect of 8% CO₂ at 7% O₂.     

Plasmodium falciparum: microaerophilic requirements in human red blood cells.

The respiratory requirements of Plasmodium falciparum were studied in vitro in continuous cultivation. The cultures were held in petri dishes containing the parasites incubated in different gas mixtures for periods of 72 to 144 hr with daily media changes. Atmospheres were combinations of 0.5 to 21% O₂ mixed with 1 to 5% CO₂ diluted with N₂. Gas concentrations and the pH of media were measured with an $\text{O}{}_2\text{CO}{}_2$ analyzer. Best growth was realized in all cases at 3% O₂ and 1 to 2% CO₂. The culture appeared to be selfperpetuating in O₂ concentrations as low as 0.5% providing the CO₂ was not over 2%. Oxygen concentrations of 21% proved deleterious to growth. The parasite however, failed to grow in the highly reducing atmosphere of anaerobic “Brewer Jars,” suggesting that P. falciparum is an obligate microaerophile.     

Conversion of photosynthetic products in the light in CO2-free O2 and N2 in leaves of Zea mays L. and Phaseolus vulgaris L.

Summary After 10 min illumination of segments of bean (Phaseolus vulgaris L.) or maize (Zea mays L.) leaves in air with ¹⁴CO₂, the atmosphere was changed to CO₂-free O₂ or N₂ and conversion of photosynthetic products in the light was investigated. The experiments have shown that after the ¹⁴CO₂ assimilation period the bean leaves contain the pool of weakly fixed ¹⁴C (WF-¹⁴C) which is converted into stable products during the subsequent period of illumination in CO₂-free N₂. In O₂ atmosphere the WF-¹⁴C pool is initially the main source of CO₂ evolved. The marked decrease in radioactivity of sucrose and starch during illumination of bean leaves in O₂ atmosphere indicates that these compounds were also the source of CO₂ evolved in the light. The total amount of previously fixed ¹⁴C remained almost on the same level during illumination of maize leaves in N₂ as well as in O₂. However, oxygen changed the distribution of ¹⁴C in photosynthetic products, which is suggested to be the consequence of the photorespiration process in maize.Abbreviation WF-¹⁴C weakly fixed ¹⁴C     

Influence of Modified Atmosphere Storage on Aflatoxin Production in High Moisture Corn

Samples of freshly harvested corn and remoistened corn were inoculated with Aspergillus flavus and stored for 4 weeks at about 27 C in air and three modified atmospheres. Aflatoxins and fat acidity were determined weekly. Corn stored in the modified atmospheres did not accumulate over 15 μg of aflatoxin B₁ per kg and 20 μg of total aflatoxins per kg. Corn from the high CO₂ treatment (61.7% CO₂, 8.7% O₂, and 29.6% N₂) was visibly molded at 4 weeks and had a higher fat acidity than the other treatments. In the N₂ (99.7% N₂ and 0.3% O₂) and controlled atmosphere (13.5% CO₂, 0.5% O₂, 84.8% N₂) treatments, a fermentation-like odor was detected. When the corn was removed from the modified atmospheres it deteriorated rapidly and was soon contaminated with aflatoxins.     

Enhancement of photosynthetic CO2 assimilation in the absence of oxygen,as dependent upon species and temperature

Summary The assimilation of CO₂ was enhanced in seven plant species by 44% at 30° in the absence of oxygen, and in three of the species by 85% at 40°. Net assimilation of CO₂ was not significantly greater in the absence of O₂ than it was in air with leaves of three tropical grasses and of one dicotyledonous species, Amaranthus palmeri. For two species in 30°, the enhanced CO₂ assimilation values were similar to those of the tropical grasses and of A. palmeri. The absence of O₂ did not enhance net CO₂ assimilation in maize even in light of low intensity.     

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.     

Contrasting growth response of an N2-fixing and non-fixing forb to elevated CO2: dependence on soil N supply

With the ability to symbiotically fix atmospheric N₂, legumes may lack the N-limitations thought to constrain plant response to elevated concentrations of atmospheric CO₂. The growth and photosynthetic responses of two perennial grassland species were compared to test the hypotheses that (1) the CO₂ response of wild species is limited at low N availability, (2) legumes respond to a greater extent than non-fixing forbs to elevated CO₂, and (3) elevated CO₂ stimulates symbiotic N₂ fixation, resulting in an increased amount of N derived from the atmosphere. This study investigated the effects of atmospheric CO₂ concentration (365 and 700 mol mol^–1) and N addition on whole plant growth and C and N acquisition in an N₂-fixing legume (Lupinus perennis) and a non-fixing forb (Achillea millefolium) in controlled-chamber environments. To evaluate the effects of a wide range of N availability on the CO₂ response, we incorporated six levels of soil N addition starting with native field soil inherently low in N (field soil + 0, 4, 8, 12, 16, or 20 g N m^–2 yr^–1). Whole plant growth, leaf net photosynthetic rates (A), and the proportion of N derived from N₂ fixation were determined in plants grown from seed over one growing season. Both species increased growth with CO₂enrichment, but this response was mediated by N supply only for the non-fixer, Achillea. Its response depended on mineral N supply as growth enhancements under elevated CO₂ increased from 0% in low N soil to +25% at the higher levels of N addition. In contrast, Lupinus plants had 80% greater biomass under elevated CO₂ regardless of N treatment. Although partial photosynthetic acclimation to CO₂ enrichment occurred, both species maintained comparably higher A in elevated compared to ambient CO₂ (+38%). N addition facilitated increased A in Achillea, however, in neither species did additional N availability affect the acclimation response of A to CO₂. Elevated CO₂ increased plant total N yield by 57% in Lupinus but had no effect on Achillea. The increased N in Lupinus came from symbiotic N₂ fixation, which resulted in a 47% greater proportion of N derived from fixation relative to other sources of N. These results suggest that compared to non-fixing forbs, N₂-fixers exhibit positive photosynthetic and growth responses to increased atmospheric CO₂ that are independent of soil N supply. The enhanced amount of N derived from N₂ fixation under elevated CO₂ presumably helps meet the increased N demand in N₂-fixing species. This response may lead to modified roles of N₂-fixers and N₂-fixer/non-fixer species interactions in grassland communities, especially those that are inherently N-poor, under projected rising atmospheric CO₂.     

Photosynthesis of Grass Species Differing in Carbon Dioxide Fixation Pathways: IV. ANALYSIS OF REDUCED OXYGEN RESPONSE IN PANICUM MILIOIDES AND PANICUM SCHENCKII

Reduced photorespiration has been reported in Panicum milioides on the basis of lower CO₂ compensation concentrations than in C₃ species, lower CO₂ evolution in the light, and less response of apparent photosynthesis to O₂ concentration. The lower response to O₂ in P. milioides could be due to reduced O₂ competition with CO₂ for reaction with ribulose 1,5-bisphosphate, to a reduced loss of CO₂, or to an initial fixation of CO₂ by phosphoenolpyruvate carboxylase. Experiments were carried out with Panicum maximum Jacq., a C₄ species having no apparent photorespiration; tall fescue (Festuca arundinacea Schreb.), a C₃ species; P. milioides Nees ex Trin.; and Panicum schenckii Hack. The latter two species are closely related and have low photorespiration rates. CO₂ exchange was measured at five CO₂ concentrations ranging from 0 to 260 microliters per liter at both 2 and 21% O₂. Mesophyll conductance or carboxylation efficiency was estimated by plotting substomatal CO₂ concentrations against apparent photosynthesis. In the C₄ species P. maximum, mesophyll conductance was 0.96 centimeters per second and was unaffected by O₂ concentration. At 21% O₂ mesophyll conductance of tall fescue was decreased 32% below the value at 2% O₂. Decreases in mesophyll conductance at 21% O₂ for P. milioides and P. schenckii were similar to that for tall fescue. On the other hand, loss of CO₂ in CO₂-free air, estimated by extrapolating the CO₂ response curve to zero CO₂, was increased from 1.8 to 6.5 milligrams per square decimeter per hour in tall fescue as O₂ was raised from 2-21%. Loss of CO₂ was less than 1 milligram per square decimeter per hour for P. milioides and P. schenckii and was unaffected by O₂. The results suggest that the reduced O₂ response in P. milioides and P. schenckii is due to a lower loss of CO₂ in the light rather than less inhibition of carboxylation by O₂, since the decrease in carboxylation efficiency at 21% O₂ was similar for P. milioides, P. schenckii, and tall fescue. The inhibition of apparent photosynthesis by 21% O₂ in these three species at low light intensities was similar at 31 to 36% which also indicates similar O₂ effects on carboxylation. Apparent photosynthesis at high light intensity was inhibited less by 21% O₂ in P. milioides (16.8%) and P. schenckii (23.8%) than in tall fescue (28.4%). This lower inhibition in the Panicum species may have been due to a higher degree of recycling of photorespired CO₂ in these species than in tall fescue.     

Effects of elevated CO2 and O3 on N-cycling and N2O emissions: a short-term laboratory assessment

Background and aims

Elevated atmospheric CO₂ (eCO₂) and tropospheric O₃ (eO₃) can alter soil microbial processes, including those underlying N₂O emissions, as an indirect result of changes in plant inputs. In this study, effects of eCO₂ and eO₃ on sources of N₂O in a soybean (Glycine max (L.) Merr.) agroecosystem in Illinois (SoyFACE) were investigated. We hypothesized that increases in available C and anaerobic microhabitat under eCO₂ would stimulate N₂O emissions, with a proportionally larger increase in denitrification derived N₂O (N₂O_D) compared to nitrification plus nitrifier denitrification derived N₂O (N₂O_N+ND). We expected opposite effects under eO₃.

Methods

Isotopically labeled ¹⁵NH ₄ ¹⁴ NO₃ and ¹⁴NH ₄ ¹⁵ NO₃ were used to evaluate mineral N transformations, N₂O_D, and N₂O_N+ND in a 12-day incubation experiment.

Results

We observed minimal effects of eCO₂ and eO₃ on N₂O emissions, movement of ¹⁵?N through mineral N pools, soil moisture content and C availability. Possibly, altered C and N inputs by eCO₂ and eO₃ were small relative to the high soil organic C content and N-inputs via biological N₂-fixation, minimizing potential effects of eCO₂ and eO₃ on N-cycling.

Conclusion

We conclude that eCO₂ and eO₃ did not affect N₂O emissions in the short term. However, it remains to be tested whether N₂O emissions in SoyFACE will be unaltered by eCO₂ and eO₃ on a larger temporal scale under field conditions.     

Photosynthesis in Flaveria brownii A.M. Powell : A C(4)-Like C(3)-C(4) Intermediate

Leaves of Flaveria brownii exhibited slightly higher amounts of oxygen inhibition of photosynthesis than the C₄ species, Flaveria trinervia, but considerably less than the C₃ species, Flaveria cronquistii. The photosynthetic responses to intercellular CO₂, light and leaf temperature were much more C₄-like than C₃-like, although 21% oxygen inhibited the photosynthetic rate, depending on conditions, up to 17% of the photosynthesis rate observed in 2% O₂. The quantum yield for CO₂ uptake in F. brownii was slightly higher than that for the C₄ species F. trinervia in 2% O₂, but not significantly different in 21% O₂. The quantum yield was inhibited 10% in the presence of 21% O₂ in F. brownii, yet no significant inhibition was observed in F. trinervia. An inhibition of 27% was observed for the quantum yield of F. cronquistii in the presence of 21% O₂. The photosynthetic response to very low intercellular CO₂ partial pressures exhibited a unique pattern in F. brownii, with a break in the linear slope observed at intercellular CO₂ partial pressure values between 15 and 20 μbar when analyzed in 21% O₂. No significant break was observed when analyzed in 2% O₂. When taken collectively, the gas-exchange results reported here are consistent with previous biochemical studies that report incomplete intercellular compartmentation of the C₃ and C₄ enzymes in this species, and suggest that F. brownii is an advanced, C₄-like C₃-C₄ intermediate.     

Drought tolerance of photosynthetic electron transport under CO2‐enriched and normal air in cereal species

The quantum yield of photosynthetic electron transport (ΦPSII), evaluated by means of chlorophyll (Chl) fluorescence analysis, has proven to be a useful screening test for drought tolerance in durum wheat (Triticum durum Desf.). To explore the potential of this parameter further in detecting drought-tolerant genotypes, three cereal species were studied; ΦPSII measurements were carried out under two different gas mixtures, at three points of the induction curve (to obtain the maximal ΦPSII and both the transient and steady-state actual ΦPSII), and at three different water stress levels (moderate, severe and drastic). The species investigated were durum and bread wheat (Triticum aestivum L.) and barley (Hordeum vulgare L.); two cultivars per species, characterized by different levels of drought tolerance, were tested. The two gas mixtures used were normal air (21% O₂, 0.035% CO₂ in N₂) to monitor the whole photosynthetic process under physiological conditions, and CO₂ enriched-low O₂ air (1% O₂, 5% CO₂ in N₂) to monitor ΦPSII reduction under stress mainly related to Calvin cycle activity. When ΦPSII related to both assimilatory and non-assimilatory metabolism was evaluated, the cultivar differences observed under normal Air were more representative of the agronomic performance upon drought stress than under high CO₂-low O₂ air. Maximal ΦPSII showed no difference among either cultivars, gas mixtures or stress levels, the efficiency of excitation capture being highly resistant to drought. The ΦPSII evaluated during the transient yielded predictable values in respect of drought tolerance for durum wheat and barley cultivars, highlighting the key role of regulatory processes such as the Mehler peroxidase reaction and possibly also cyclic electron transport, in preventing overreduction under stress. The results clearly show that when Chl fluorescence analysis is used as a parameter in plant breeding, different experimental conditions should be used depending on the physiological mechanism that is bred or selected for.     

Effect of Temperature, CO(2) Concentration, and Light Intensity on Oxygen Inhibition of Photosynthesis in Wheat Leaves

The effect of 21% O₂ and 3% O₂ on the CO₂ exchange of detached wheat leaves was measured in a closed system with an infrared carbon dioxide analyzer. Temperature was varied between 2° and 43°, CO₂ concentration between 0.000% and 0.050% and light intensity between 40 ft-c and 1000 ft-c. In most conditions, the apparent rate of photosynthesis was inhibited in 21% O₂ compared to 3% O₂. The degree of inhibition increased with increasing temperature and decreasing CO₂ concentration. Light intensity did not alter the effect of O₂ except at light intensities or CO₂ concentrations near the compensation point. At high CO₂ concentrations and low temperature, O₂ inhibition of apparent photosynthesis was absent. At 3% O₂, wheat resembled tropical grasses in possessing a high rate of photosynthesis, a temperature optimum for photosynthesis above 30°, and a CO₂ compensation point of less than 0.0005% CO₂. The effect of O₂ on apparent photosynthesis could be ascribed to a combination of stimulation of CO₂ production during photosynthesis, and inhibition of photosynthesis itself.     

Response of the Endophytic Diazotroph Gluconacetobacter diazotrophicus on Solid Media to Changes in Atmospheric Partial O2 Pressure

Gluconacetobacter diazotrophicus is an N₂-fixing endophyte isolated from sugarcane. G. diazotrophicus was grown on solid medium at atmospheric partial O₂ pressures (pO₂) of 10, 20, and 30 kPa for 5 to 6 days. Using a flowthrough gas exchange system, nitrogenase activity and respiration rate were then measured at a range of atmospheric pO₂ (5 to 60 kPa). Nitrogenase activity was measured by H₂ evolution in N₂-O₂ and in Ar-O₂, and respiration rate was measured by CO₂ evolution in N₂-O₂. To validate the use of H₂ production as an assay for nitrogenase activity, a non-N₂-fixing (Nif⁻) mutant of G. diazotrophicus was tested and found to have a low rate of uptake hydrogenase (Hup⁺) activity (0.016± 0.009 μmol of H₂ 10¹⁰ cells⁻¹ h⁻¹) when incubated in an atmosphere enriched in H₂. However, Hup⁺ activity was not detectable under the normal assay conditions used in our experiments. G. diazotrophicus fixed nitrogen at all atmospheric pO₂ tested. However, when the assay atmospheric pO₂ was below the level at which the colonies had been grown, nitrogenase activity was decreased. Optimal atmospheric pO₂ for nitrogenase activity was 0 to 20 kPa above the pO₂ at which the bacteria had been grown. As atmospheric pO₂ was increased in 10-kPa steps to the highest levels (40 to 60 kPa), nitrogenase activity decreased in a stepwise manner. Despite the decrease in nitrogenase activity as atmospheric pO₂ was increased, respiration rate increased marginally. A large single-step increase in atmospheric pO₂ from 20 to 60 kPa caused a rapid 84% decrease in nitrogenase activity. However, upon returning to 20 kPa of O₂, 80% of nitrogenase activity was recovered within 10 min, indicating a “switch-off/switch-on” O₂ protection mechanism of nitrogenase activity. Our study demonstrates that colonies of G. diazotrophicus can fix N₂ at a wide range of atmospheric pO₂ and can adapt to maintain nitrogenase activity in response to both long-term and short-term changes in atmospheric pO₂.     

A CO2-enriched atmosphere improves in vitro growth of Brazilian ginseng [Pfaffia glomerata (Spreng.) Pedersen]

The aim of the present study was to evaluate the effects of forced ventilation and CO₂ enrichment (360 or 720 μmol mol^?1 CO₂) on the in vitro growth and development of Pfaffia glomerata, an endangered medicinal species, under photomixotrophic or photoautotrophic conditions. P. glomerata nodal segments showed substantial differences in growth, relative water content and water loss from leaves, photosynthetic pigments, stomatal density, and leaf anatomical characteristics under these different treatments. CO₂ enrichment led to increased photosynthetic pigments and reduced stomatal density of in vitro cultivated P. glomerata. A lack of sucrose in the culture medium increased 20-hydroxyecdysone levels, but the increase in CO₂ levels did not further elevate the accumulation of 20-hydroxyecdysone. All growth increased in a CO₂-enriched atmosphere. In addition, CO₂ enrichment, with or without sucrose, gave a lower relative water loss from leaves. This finding indicates that either a photoautotrophic or photomixotrophic system in a CO₂-enriched atmosphere may be suitable for large-scale propagation of this species.     

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.

     

Effect of oxygen on photosynthesis by spinach leaf protoplasts

The photosynthetic CO₂ fixation by spinach leaf (Spinacia oleracea L. var. Kyoho) protoplasts was inhibited by substituting an atmosphere of N₂ with one of either air (21% O₂) or 100% O₂. The inhibitory effect of 100% O₂ was greater than that of air. The mode of inhibition by 100% O₂ and air was competitive with respect to CO₂; Ki(O₂) value was 0.32 mM at pH 7 and 0.28 mM at pH 8.5 The labeling patterns of compounds in protoplasts exposed to ¹⁴CO₂ in light after transferring them from N₂ to O₂ atmospheres were examined. There was no detectable ¹⁴CO₂ incorporation into glycolate under anaerobic and O₂ atmospheres; a more marked labeling of glycine occurred under an oxidative environment compared to that under the anaerobic condition, presumably because of a rapid transformation of glycolate to glycine in the protoplasts.     

Effect of several MAP compositions on the microbiological and sensory properties of Graviera cheese

The shelf life of Graviera cheese, a full fat cheese produced in Heraklion (Crete Greece), was investigated. Graviera cheese was stored at 4 °C for up to 90 days in polyamide packages under three different modified atmosphere compositions. Control cheeses were packaged in air whereas MAP mixtures were MAP₁: 40% CO₂/55% N₂/5% O₂, MAP₂: 60% CO₂/40% N₂ and MAP₃: 50% CO₂/50% N₂. Sampling of product was carried out every 10 days to investigate its sensory quality and microbiological characteristics. Ten trained panelists participated in the sensory panel to evaluate the cheeses for external appearance (color, texture), taste, and flavor in a scale from 1 to 10 (1 very poor, 10 very good). The microbiological analysis revealed that there were no colonies of Staphylococcus aureus and Listeria monocytogenes whereas both Escherichia coli and Total Viable Counts (TVC) increased strongly in control samples but were inhibited under all MAP compositions.