C(4) Pathway Photosynthesis at Low Temperature in Cold-tolerant Atriplex Species

Two species of Atriplex were grown under low temperature (8 C day/6 C night) and high temperature (28 C day/20 C night) regimes. The photosynthetic capacity of these plants was studied as a function of temperature in a leaf gas exchange cuvette. Both species showed substantial photosynthetic capacity between 4 and 10 C and this was not enhanced by growth at low temperatures but rather, was somewhat greater in plants grown at higher temperature. Photosynthetic capacity of low temperature-grown plants at high temperature was greater in Atriplex confertifolia (Torr. and Frem.) S. Watts., a native of cool deserts, than in Atriplex vesicaria (Hew. ex. Benth.) from warmer desert areas. Leaves of both species were also subjected to ¹⁴CO₂ pulse-chase and steady-state feeding experiments under controlled temperature conditions. These experiments revealed that the kinetics of carbon assimilation through the intermediates of the C₄ pathway is not substantially disrupted at low temperature in either species. There was, however, a substantial interchange of label between aspartate and malate at low temperature which was not evident at high temperature. There was also an increase in the pool sizes of the C₄ acids involved in photosynthesis of A. confertifolia. Speculation as to the explanation of these changes and their possible significance in promoting low temperature C₄ photosynthesis in these plants is presented.     

Photorespiratory rates in wheat and maize as determined by o-labeling

A method was devised to quantify short-term photorespiratory rates in terrestrial plants using ¹⁸O-intermediates of the glycolate pathway, specifically glycolate, glycine, and serine. The pathway intermediates were isolated and analyzed on a GC/MS to determine molecular percent ¹⁸O-enrichment. Rates of glycolate synthesis were determined from ¹⁸O-labeling kinetics of the intermediates, derived rate equations, and nonlinear regression techniques. Glycolate synthesis in wheat (Triticum aestivum L.), a C₃ plant, and maize (Zea mays L.), a C₄ plant, was stimulated by high O₂ concentrations and inhibited by high CO₂ concentrations. The synthesis rates were 7.3, 2.1, and 0.7 micromoles per square decimeter per minute under a 21% O₂ and 0.035% CO₂ atmosphere for leaf tissue of wheat, maize seedlings, and 3-month-old maize, respectively. Photorespiratory CO₂ evolution rates were estimated to be 27, 6, and 2%, respectively, of net photosynthesis for the three groups of plants under the above atmosphere. The results from maize tissue support the hypothesis that C₄ plants photorespire, albeit at a reduced rate in comparison to C₃ plants, and that the CO₂/O₂ ratio in the bundle sheath of maize is higher in mature tissue than in seedling tissue. The pool size of the three photorespiratory intermediates remained constant and were unaffected by changes in either CO₂ or O₂ concentrations throughout the 10-minute labeling period. This suggests that photorespiratory metabolism is regulated by other mechanism besides phosphoglycolate synthesis by ribulose-1,5-bisphosphate carboxylase/oxygenase, at least under short-term conditions. Other mechanisms could be alternate modes of synthesis of the intermediates, regulation of some of the enzymes of the photorespiratory pathway, or regulation of carbon flow between organelles involved in photorespiration. The glycolate pool became nearly 100% ¹⁸O-labeled under an atmosphere of 40% O₂. This pool failed to become 100% ¹⁸O-enriched under lower O₂ concentrations.     

Mechanism of c(4) photosynthesis: the size and composition of the inorganic carbon pool in bundle sheath cells

We sought to characterize the inorganic carbon pool (CO₂ plus HCO₃⁻) formed in the leaves of C₄ plants when C₄ acids derived from CO₂ assimilation in mesophyll cells are decarboxylated in bundle sheath cells. The size and kinetics of labeling of this pool was determined in six species representative of the three metabolic subgroups of C₄ plants. The kinetics of labeling of the inorganic carbon pool of leaves photosynthesizing under steady state conditions in ¹⁴CO₂ closely paralleled those for the C-4 carboxyl of C₄ acids for all species tested. The inorganic carbon pool size, determined from its ¹⁴C content at radioactivity saturation, ranged between 15 and 97 nanomoles per milligram of leaf chlorophyll, giving estimated concentrations in bundle sheath cells of between 160 and 990 micromolar. The size of the pool decreased, together with photosynthesis, as light was reduced from 900 to 95 microeinsteins per square meter per second or as external CO₂ was reduced from 400 to 98 microliters per liter. A model is developed which suggests that the inorganic carbon pool existing in the bundle sheath cells of C₄ plants during steady state photosynthesis will comprise largely of CO₂; that is, CO₂ will only partially equlibrate with bicarbonate. This predominance of CO₂ is believed to be vital for the proper functioning of the C₄ pathway.     

Lacunal gas discharge as a measure of productivity in the seagrasses Zostera capricorni,Cymodocea serrulata and Syringodium isoetifolium

A new method for estimating the rate of photosynthetic fixation of carbon in seagrasses is described. This method, which is sensitive and simple to apply, is based on the close relationship between photosynthetic rate and the volume of gas discharged through the lacunae.During photosynthesis, the gas discharged from the lacunae was composed primarily of oxygen (32.5%) and nitrogen (67.5%). The rate of discharge was proportional to the rate of photosynthesis and hence was a function of light intensity. There was a linear relationship between gases discharged from the lacunae and oxygen released into the water column. Calibration curves were derived relating volume of gases (oxygen and nitrogen) released from the lacunae to total oxygen produced during photosynthesis for three species of seagrasses (Zostera capricorni Aschers., Cymodocea serrulata (R. Br.) Aschers. & Magnus and Syringodium isoetifolium (Aschers.) Dandy). Molar ratios of ¹⁴C fixed to oxygen produced were close to unity (1.008±0.016; n=8) indicating that measurements of lacunal gas released may be used to measure productivity.     

The Effect of Light on the Tricarboxylic Acid Cycle in Green Leaves: III. A Comparison between Some C(3) and C(4) Plants

The chlorophyll-based specific activity of cytochrome oxidase and three exclusively mitochondrial enzymes of the tricarboxylic acid cycle showed little variation between leaves of C₃ and C₄ plants or between mesophyll and bundle sheath cells of Atriplex spongiosa and Sorghum bicolor. However, a large, light-dependent transfer of label from intermediates of the tricarboxylic acid cycle to photosynthetic products was a feature of leaves of C₄ plants. This light-dependent transfer of label was barely detectable in leaves of C₃ plants and in leaves of F₁ and F₃ hybrids of Atriplex rosea (C₄) and Atriplex patula spp hastata (C₃). The light-dependent transfer of label to photosynthetic products in leaves of C₄ plants was inhibited by the tricarboxylic acid cycle inhibitors malonate and fluoroacetate. The requirement for continued tricarboxylic acid cycle activity was also indicated in experiments with specifically labeled succinate-¹⁴C. These experiments, together with the distribution of ¹⁴C in glucose prepared from sucrose-¹⁴C formed during the metabolism of succinate-2,3-¹⁴C, confirmed that the photosynthetic metabolism of malate and aspartate derived from the tricarboxylic acid cycle, and not the refixation of respiratory CO₂, was the main path of carbon from the cycle to photosynthesis.     

Carbon Assimilation in Photoheterotrophic Cells of Peanut (Arachis hypogaea L.) Grown in Still Nutrient Medium

The relative transport of photosynthetic and dark carboxylation products in photoheterotrophic cells of Arachis hypogaea L. var. TMV-3 at varied phases of growth were determined. Despite the presence of an equally competent photosynthetic apparatus as determined from ¹⁴CO₂ incorporation rates in the dark and light, pulse-chase experiments revealed little or no change in the radioactivity of the C₃ intermediates but rapid disappearance of label from the dark carbon assimilates (malate and other tricarboxylic acid cycle intermediates) with a simultaneous increase in the aminoacid pool in early log-phase (10 days old) cells. However, significant flow of carbon through the photosynthetic intermediates resulting in the accumulation of sugars occurred in the late log-phase (34 days old) cells. Limitation of exogenous sugar in the nutrient milieu and depletion of reserve carbohydrates stored in starch of the chloroplasts of the cells were considered as the decisive factors in promoting transport of C₃ cycle intermediates through the reductive pentose phosphate pathway in photoheterotrophic cells. The observed drain of radioactivity even from the small amounts of tricarboxylic acid cycle intermediates synthesized during photosynthesis into glutamate indicated that the transport of carbon through the nonautotrophic pathway is not controlled by these factors.     

Mechanism of C4 photosynthesis in Chloris gayana: pool sizes and kinetics of 14CO2 incorporation into 4-carbon and 3-carbon intermediates.

In one group of C₄ species, including Chloris gayana, C₄ acids are decarboxylated via phosphoenolpyruvate carboxykinase to give phosphoenolpyruvate as the initial C₃ product. This paper presents an analysis of the kinetics of labeling of various photosynthetic intermediates in Chloris gayana leaves exposed to ¹⁴CO₂, and the pool sizes of these intermediates, primarily to provide information about the subsequent metabolism of phosphoenolpyruvate. Saturation labeling of the C-4 of aspartate and malate, and the C-1 of 3-phosphoglycerate, indicated photosynthetically active pools of 0.45, 0.22, and 0.95 μol/mg chlorophyll, respectively. For aspartate and 3-phosphoglycerate, the total leaf pools and the photosynthetic pools were of similar size, but the total pool of malate was about 100 times larger than the photosynthetically active pool. From the relative rates of labeling of phosphoenolpyruvate, pyruvate, alanine, and C-1, C-2 plus C-3 of aspartate, during steady-state ¹⁴CO₂ assimilation, relative pool sizes were calculated to be about 10:11:78:100, respectively. Pulse/chase labeling of leaves provided estimates of relative photosynthetic pool sizes in the ratio of about 6:15:90:100, respectively, where aspartate is arbitrarily assigned a value of 100 in both cases. Notably, labeling of alanine was consistent with its derivation from the C-1, C-2 plus C-3 carbons of aspartate, and the alanine pool was at least eight times larger than the phosphoenolpyruvate pool that showed similar labeling kinetics. Results were consistent with the view that at least most of the phosphoenolpyruvate produced by C₄ acid decarboxylation is metabolized via alanine.     

Two photosynthetic mechanisms mediating the low photorespiratory state in submersed aquatic angiosperms

The submersed angiosperms Myriophyllum spicatum L. and Hydrilla verticillata (L.f.) Royal exhibited different photosynthetic pulse-chase labeling patterns. In Hydrilla, over 50% of the ¹⁴C was initially in malate and aspartate, but the fate of the malate depended upon the photorespiratory state of the plant. In low photorespiration Hydrilla, malate label decreased rapidly during an unlabeled chase, whereas labeling of sucrose and starch increased. In contrast, for high photorespiration Hydrilla, malate labeling continued to increase during a 2-hour chase. Thus, malate formation occurs in both photorespiratory states, but reduced photorespiration results when this malate is utilized in the light. Unlike Hydrilla, in low photorespiration Myriophyllum, ¹⁴C incorporation was via the Calvin cycle, and less than 10% was in C₄ acids.

Ethoxyzolamide, a carbonic anhydrase inhibitor and a repressor of the low photorespiratory state, increased the label in glycolate, glycine, and serine of Myriophyllum. Isonicotinic acid hydrazide increased glycine labeling of low photorespiration Myriophyllum from 14 to 25%, and from 12 to 48% with high photorespiration plants. Similar trends were observed with Hydrilla. Increasing O₂ increased the per cent [¹⁴C]glycine and the O₂ inhibition of photosynthesis in Myriophyllum. In low photorespiration Myriophyllum, glycine labeling and O₂ inhibition of photosynthesis were independent of the CO₂ level, but in high photorespiration plants the O₂ inhibition was competitively decreased by CO₂. Thus, in low but not high photorespiration plants, glycine labeling and O₂ inhibition appeared to be uncoupled from the external [O₂]/[CO₂] ratio.

These data indicate that the low photorespiratory states of Hydrilla and Myriophyllum are mediated by different mechanisms, the former being C₄-like, while the latter resembles that of low CO₂-grown algae. Both may require carbonic anhydrase to enhance the use of inorganic carbon for reducing photorespiration.

     

Photosynthetic Induction in a C(4) Dicot, Flaveria trinervia: II. Metabolism of Products of CO(2) Fixation after Different Illumination Times

The metabolism of fixed ¹⁴CO₂ and the utilization of the C-4 carboxyl of malate and aspartate were examined during photosynthetic induction in Flaveria trinervia, a C₄ dicot of the NADP-malic enzyme subgroup. Pulse/chase experiments indicated that both malate and aspartate appeared to function directly in the C₄ cycle at all times during the induction period (examined after 30 seconds, 5 minutes and 20 minutes illumination). However, the rate of loss of ¹⁴C-label from the C-4 position of malate plus aspartate was relatively slow after 30 seconds of illumination, compared to treatments after 5 or 20 minutes of illumination. Similarly, the appearance of label in other photosynthetic products (e.g. 3-phosphoglycerate, sugar phosphates, alanine) during the chase periods was generally slower after only 30 seconds of leaf illumination, compared to that after 5 of 20 minutes illumination. This may be due to the lower rate of photosynthesis after 30 seconds illumination. The appearance of label in carbons 1→3 of each C₄ acid during the chase periods was relatively slow after either 30 seconds or 5 minutes illumination, while there was a relatively rapid accumulation of label in carbons 1→3 of both C₄ acids after 20 minutes illumination. Thus, while the turnover rate of the ¹⁴C-4 label in both C₄ acids increased only during the first 5 minutes of the induction period, only later during induction is there an increased rate of appearance of label in other carbon atoms of the C₄ acids. The implied source of ¹⁴C for labeling of the 1→3 positions of the C₄ acids is an apparent carbon flux from 3-phosphoglycerate of the reductive pentose phosphate pathway to phosphoenolpyruvate of the C₄ cycle.     

Carbon: freshwater plants

δ¹³C values for freshwater aquatic plant matter varies from ?11 to ?50‰ and is not a clear indicator of photosynthetic pathway as in terrestrial plants. Several factors affect δ¹³C of aquatic plant matter. These include: (1) The δ¹³C signature of the source carbon has been observed to range from +1‰ for HCO₃^? derived from limestone to ?30‰ for CO₂ derived from respiration. (2) Some plants assimilate HCO₃^?, which is –7 to –11‰ less negative than CO₂. (3) C₃, C₄, and CAM photosynthetic pathways are present in aquatic plants. (4) Diffusional resistances are orders of magnitude greater in the aquatic environment than in the aerial environment. The greater viscosity of water acts to reduce mixing of the carbon pool in the boundary layer with that of the bulk solution. In effect, many aquatic plants draw from a finite carbon pool, and as in terrestrial plants growing in a closed system, biochemical discrimination is reduced. In standing water, this factor results in most aquatic plants having a δ¹³C value similar to the source carbon. Using Farquhar's equation and other physiological data, it is possible to use δ¹³C values to evaluate various parameters affecting photosynthesis, such as limitations imposed by CO₂ diffusion and carbon source.     

Role of Photorespiration and Cyclic Electron Transport in C<Subscript>4</Subscript> Photosynthesis Evolution in the C<Subscript>3</Subscript>–C<Subscript>4</Subscript> Intermediate Species <Emphasis Type="Italic">Sedobassia sedoides</Emphasis>

Plants from two Sedobassia sedoides (Pall.) Aschers populations (Makan and Valitovo) (Chenopodiaceae) with C₂ photosynthesis (precursor of C₄ photosynthesis in phylogenesis) and photorespiratory CO₂-concentrating mechanism were studied. Genetic polymorphism and isotope discrimination (δ¹³С) levels of the plants were determined under natural conditions, and their morpho-physiological parameters such as fresh and dry biomass of the above ground parts of plants, functioning of photosystem I (PSI) and photosystem II (PSII), intensity of net photosynthesis (A), transpiration (E), photorespiration and water use efficiency (WUE) of plants were calculated under control and salinine conditions (0 and 200 mM NaCl). Results of the population-genetic analysis showed that the Makan population is polymorphic (plastic) and the Valitovo population is monomorphic (narrowly specialized). There were no significant differences between the populations based on δ¹³С values or growth parameters, PSII, A, E and WUE under control conditions. Under saline conditions, dry biomass accumulation decreased in the Makan population by 15% and by more than 2- fold in the Valitovo population. Population differences were revealed in terms of photorespiration intensity and P700 oxidation kinetics under control and saline conditions. Under control conditions, Makan plants were characterized by a higher photorespiration intensity, which decreased by 2-fold under saline conditions to the photorespiration level of Valitovo plants. Cyclic electron transport activity was minimal in the control Makan plants, and it increased by almost 2-fold under saline conditions to the level of that in Valitovo plants under control and saline conditions. Under control conditions, photosynthesis in Makan plants can be specified as the proto-Kranz type (transitional type from C₃ to C₂) and that in Valitovo plants can be specified as the C₂ type (C₄ photosynthesis with photorespiratory CO₂-concentrating mechanism), based on their photorespiration level and cyclic electron transport activity. Under saline conditions, Makan plants exhibited features of C₂ photosynthesis. Intraspecific functional differences of photosynthesis were revealed in different populations of intermediate C₃–C₄ plant species S. sedoides which reflect the initial stages of formation of a photorespiratory CO₂-concentrating mechanism during C₄ photosynthesis evolution, accompanied by decrease in salt tolerance.     

Oxygen effects on photosynthesis and C metabolism in desert plants

The effect of 1% and 21% O₂ upon ¹⁴CO₂ assimilation by desert plants exposed for 10 to 90 seconds has been studied. The plants studied can be divided into three groups with respect to O₂. The C₃ plants display the usual Warburg effect. No changes could be observed in the intensity of photosynthesis as a function of O₂ content in another group of plants (showing signs of Crassulacean acid metabolism). In still another group of plants (C₄ plants) the stimulating effect of O₂ on photosynthesis could be detected. In C₃ plants, O₂ inhibits the processing of carbon through the Calvin cycle intermediates. The involvement of carbon in the glycolate pathway fails to explain completely the inhibiting effect of O₂ on photosynthesis. It is assumed that O₂ inhibits the enzymes of the Calvin cycle. In C₄ plants O₂ stimulates the incorporation of ¹⁴C into malate and aspartate. The incorporation of ¹⁴C into the intermediates of the Calvin cycle in C₄ plants is inhibited much like that in typical C₃ plants.     

Fractionation of the stable isotopes of inorganic carbon by seagrasses

The δ¹³C values for seagrasses collected along the Texas Gulf Coast range from −10.9 to −11.4‰. These values are similar to the δ¹³C values of terrestrial C₄ plants, but seagrasses lack bundle sheath cells which are important in determining the δ¹³C values of C₄ plants. This work attempts to explain the reason the δ¹³C values of seagrasses resemble the δ¹³C values of C₄ plants.     

Overview of the physiological ecology of carbon metabolism in seagrasses

The small but diverse group of angiosperms known as seagrasses form submersed meadow communities that are among the most productive on earth. Seagrasses are frequently light-limited and, despite access to carbon-rich seawaters, they may also sustain periodic internal carbon limitation. They have been regarded as C3 plants, but many species appear to be C3–C4 intermediates and/or have various carbon-concentrating mechanisms to aid the Rubisco enzyme in carbon acquisition. Photorespiration can occur as a C loss process that may protect photosynthetic electron transport during periods of low CO₂ availability and high light intensity. Seagrasses can also become photoinhibited in high light (generally>1000 μE m⁻² s⁻¹) as a protective mechanism that allows excessive light energy to be dissipated as heat. Many photosynthesis–irradiance curves have been developed to assess light levels needed for seagrass growth. However, most available data (e.g. compensation irradiance I_c) do not account for belowground tissue respiration and, thus, are of limited use in assessing the whole-plant carbon balance across light gradients. Caution is recommended in use of I_k (saturating irradiance for photosynthesis), since seagrass photosynthesis commonly increases under higher light intensities than I_k; and in estimating seagrass productivity from H_sat (duration of daily light period when light equals or exceeds I_k) which varies considerably among species and sites, and which fails to account for light-limited photosynthesis at light levels less than I_k. The dominant storage carbohydrate in seagrasses is sucrose (primarily stored in rhizomes), which generally forms more than 90% of the total soluble carbohydrate pool. Seagrasses with high I_c levels (suggesting lower efficiency in C acquisition) have relatively low levels of leaf carbohydrates. Sucrose-P synthase (SPS, involved in sucrose synthesis) activity increases with leaf age, consistent with leaf maturation from carbon sink to source. Unlike terrestrial plants, SPS apparently is not light-activated, and is positively influenced by increasing temperature and salinity. This response may indicate an osmotic adjustment in marine angiosperms, analogous to increased SPS activity as a cryoprotectant response in terrestrial non-halophytic plants. Sucrose synthase (SS, involved in sucrose metabolism and degradation in sink tissues) of both above- and belowground tissues decreases with tissue age. In belowground tissues, SS activity increases under low oxygen availability and with increasing temperatures, likely indicating increased metabolic carbohydrate demand. Respiration in seagrasses is primarily influenced by temperature and, in belowground tissues, by oxygen availability. Aboveground tissues (involved in C assimilation and other energy-costly processes) generally have higher respiration rates than belowground (mostly storage) tissues. Respiration rates increase with increasing temperature (in excess of 40°C) and increasing water-column nitrate enrichment (Z. marina), which may help to supply the energy and carbon needed to assimilate and reduce nitrate. Seagrasses translocate oxygen from photosynthesizing leaves to belowground tissues for aerobic respiration. During darkness or extended periods of low light, belowground tissues can sustain extended anerobiosis. Documented alternate fermentation pathways have yielded high alanine, a metabolic ‘strategy’ that would depress production of the more toxic product ethanol, while conserving carbon skeletons and assimilated nitrogen. In comparison to the wealth of information available for terrestrial plants, little is known about the physiological ecology of seagrasses in carbon acquisition and metabolism. Many aspects of their carbon metabolism — controls by interactive environmental factors; and the role of carbon metabolism in salt tolerance, growth under resource-limited conditions, and survival through periods of dormancy — remain to be resolved as directions in future research. Such research will strengthen the understanding needed to improve management and protection of these environmentally important marine angiosperms.     

Changes in Levels of Intermediates of the C(4) Cycle and Reductive Pentose Phosphate Pathway during Induction of Photosynthesis in Maize Leaves

Changes in the level of metabolites of the C₄ cycle and reductive pentose phosphate (RPP) pathway were measured simultaneously with induction of photosynthesis in maize (Zea mays L.) to evaluate what may limit carbon assimilation during induction in a C₄ plant.

After 20 minutes in the dark, there was an immediate rise in photosynthesis during the first 30 seconds of illumination, followed by a gradual rise approaching steady-state rate after 20 minutes of illumination. Among metabolites of the C₄ cycle, there was a net increase in the level of C₃ compounds (the sum of pyruvate, alanine, and phosphoenolpyruvate) during the first 30 seconds of illumination, while there was a net decrease in the level of C₄ acids (malate plus aspartate). The total level of metabolites of the C₄ cycle underwent a sharp increase during this period. At the same time, there was a sharp rise in the level of intermediates of the RPP pathway (ribulose-1,5-bis-phosphate, 3-phosphoglycerate, dihydroxyacetonephosphate, and fructose-1,6-bisphosphate) during the first minute of illumination. The net increase of carbon among intermediates of the C₄ cycle and RPP pathway was far above that of carbon input from CO₂ fixation, and the increase in intermediates of the RPP pathway could not be accounted for by decarboxylation of C₄ acids, suggesting that an endogenous source of carbon supplies the cycles. After 3 minutes of illumination there was a gradual rise in the levels of intermediates of the C₄ cycle and in the total level of metabolites measured in the RPP pathway. This rise in metabolite levels occurs as photosynthesis gradually increases and may be required for carbon assimilation to reach maximum rates in C₄ plants. This latter stage of inductive autocatalysis through the RPP pathway may contribute to the final buildup of these intermediates.

     

Productivity and respiration of three seagrass species from the gulf of Aqaba (Jordan) and some related factors

Net productivity and rates of respiration of the seagrasses Halodule uninervis (Forsk.) Aschers., Halophila ovalis (R. Brown) Hooker fil. and Halophila stipulacea (Forsk.) Aschers., from Aqaba (Jordan) are presented in this paper. The effect of some physical and chemical parameters on the productivity of H. stipulacea is discussed in some detail. Of the three species, H. stipulacea is considered a shade plant since it is photoinhibited at light intensities near 100 Wm^?2 and has a productivity/respiration ratio of 1.8 at 30 m depth.     

Effect of nitrate limitation on the photosynthetically active pools of aspartate and malate in maize, a NADP malic enzyme C4 plant

After two weeks of moderate N restriction, growth of 3-week-old Zea mays L. plants was less than half that of the control and aspartate and malate levels in the leaves were severely suppressed (45 and 65% decrease, respectively). Since in NADP malic enzyme type C₄ plants, such as maize, malate and aspartate are intermediates in the C₄ photosynthetic pathway, the operation of the latter was investigated. Moderate nitrogen deficiency had only a small effect on the rate of photosynthesis (20% decrease) measured under 1000 umol m^?2 s^?1 irradiance. ¹⁴CO₂ pulse-¹²CO₂ chase experiments combined with measurements of in vitro photosynthetic enzyme activities demonstrated the operation of a typical C⁴ photosynthetic pathway in N-restricted plants. The turnover rates of malate and aspartate molecules involved in the C₄ cycle were determined by the loss of label in the carbon 4 moiety of these molecules during the chase period. It is shown that N restriction did not alter the turnover of malate but greatly accelerated that of aspartate. The amounts of malate and aspartate moving through photosynthetically active pools were estimated using a kinetic model. For malate, the size of this pool appeared to be only slightly diminished whereas for aspartate the size of the corresponding pool decreased by a factor of 3. It is proposed that under moderate NO₃^? deficiency, despite deviations in malate metabolism leading to a pronounced decrease in the size of its cellular pool, a large amount of malate remained in the operation of the C₄ pathway. By contrast, the participation of aspartate in the operation of the C₄ pathway was greatly reduced.     

Compensation point and isotopic characteristics of c(3)/c(4) intermediates and hybrids in panicum

Leaf CO₂ compensation points and stable hydrogen, oxygen and carbon isotope ratios were determined for Panicum species including C₃/C₄ intermediate photosynthesis plants, hybrids between C₃/C₄ intermediates and C₃ plants, C₃ and C₄ plants in the Panicum genus as well as several other C₃ and C₄ plants. C₃ plants had the highest compensation points, followed by hybrids, C₃/C₄ intermediates, and C₄ plants. δ¹³C values of cellulose nitrate and saponifiable lipids from C₄ plants were about 10‰ higher than those observed for cellulose nitrate and saponifiable lipids of C₃/C₄ intermediates, hybrids, and C₃ plants. Oxygen isotope ratios of cellulose as well as those of leaf water were similar for all plants. There was substantial variability in the δD values of cellulose nitrate among the plants studied. In contrast, such variability was not observed in δD values of water distilled from the leaves, nor in the δD values of the saponifiable lipids. Variability in δD values of cellulose nitrate from C₃/C₄ intermediates, hybrids, C₃, and C₄ plants is due to fractionations occurring during biochemical reactions specific to leaf carbohydrate metabolism.     

CAM photosynthesis in submerged aquatic plants

Crassulacean acid metabolism (CAM) is a CO₂-concentrating mechanism selected in response to aridity in terrestrial habitats, and, in aquatic environments, to ambient limitations of carbon. Evidence is reviewed for its presence in five genera of aquatic vascular plants, includingIsoëtes, Sagittaria, Vallisneria, Crassula, andLittorella. Initially, aquatic CAM was considered by some to be an oxymoron, but some aquatic species have been studied in sufficient detail to say definitively that they possess CAM photosynthesis. CO₂-concentrating mechanisms in photosynthetic organs require a barrier to leakage; e.g., terrestrial C₄ plants have suberized bundle sheath cells and terrestrial CAM plants high stomatal resistance. In aquatic CAM plants the primary barrier to CO₂ leakage is the extremely high difrusional resistance of water. This, coupled with the sink provided by extensive intercellular gas space, generates daytime CO₂(pi) comparable to terrestrial CAM plants. CAM contributes to the carbon budget by both net carbon gain and carbon recycling, and the magnitude of each is environmentally influenced. Aquatic CAM plants inhabit sites where photosynthesis is potentially limited by carbon. Many occupy moderately fertile shallow temporary pools that experience extreme diel fluctuations in carbon availability. CAM plants are able to take advantage of elevated nighttime CO2 levels in these habitats. This gives them a competitive advantage over non-CAM species that are carbon starved during the day and an advantage over species that expend energy in membrane transport of bicarbonate. Some aquatic CAM plants are distributed in highly infertile lakes, where extreme carbon limitation and light are important selective factors. Compilation of reports on diel changes in titratable acidity and malate show 69 out of 180 species have significant overnight accumulation, although evidence is presented discounting CAM in some. It is concluded that similar proportions of the aquatic and terrestrial floras have evolved CAM photosynthesis. AquaticIsoëtes (Lycophyta) represent the oldest lineage of CAM plants and cladistic analysis supports an origin for CAM in seasonal wetlands, from which it has radiated into oligotrophic lakes and into terrestrial habitats. Temperate Zone terrestrial species share many characteristics with amphibious ancestors, which in their temporary terrestrial stage, produce functional stomata and switch from CAM to C₃. Many lacustrineIsoëtes have retained the phenotypic plasticity of amphibious species and can adapt to an aerial environment by development of stomata and switching to C₃. However, in some neotropical alpine species, adaptations to the lacustrine environment are genetically fixed and these constitutive species fail to produce stomata or loose CAM when artificially maintained in an aerial environment. It is hypothesized that neotropical lacustrine species may be more ancient in origin and have given rise to terrestrial species, which have retained most of the characteristics of their aquatic ancestry, including astomatous leaves, CAM and sediment-based carbon nutrition.     

Inhibition of seagrass photosynthesis by ultraviolet-B radiation

Effects of ultraviolet-B radiation on the photosynthesis of seagrasses (Halophila engelmanni Aschers, Halodule wrightii Aschers, and Syringodium filiforme Kütz) were examined. The intrinsic tolerance of each seagrass to ultraviolet-B, the presence and effectiveness of photorepair mechanisms to ultraviolet-B-induced photosynthetic inhibition, and the role of epiphytic growth as a shield from ultraviolet-B were investigated.