Photosynthetic acclimation to rising atmospheric carbon dioxide concentration

With rising level of CO2 in the atmosphere plants are expected to be exposed to higher concentration of CO2. Since, CO2 is a substrate limiting photosynthesis particularly in C3 plants in the present atmosphere, the impact of elevated CO2 would depend mainly on how photosynthesis acclimates or adjusts to the long term elevated level of CO2. Photosynthetic acclimation is a change in photosynthetic efficiency of leaves due to long term exposure to elevated CO2. This change in photosynthetic efficiency could be a biochemical adjustment that may improve the overall performance of a plant in a high CO2 environment or it could be due to metabolic compulsions as a result of physiological dysfunction. Acclimation has generally become synonymous with the word response, if long term exposure to elevated CO2 decreases the photosynthesis rate (Pn) at a given CO2 level, it is called negative acclimation, if it stimulates Pn at a given CO2 level, it is called positive acclimation. Photosynthetic acclimation is clearly revealed by comparing Pn of ambient and elevated CO2 grown plants at same level of CO2. Species level differences in acclimation to elevated CO2 have been reported. The physiological basis of differential photosynthetic acclimation to elevated CO2 is discussed in relation to the regulation of photosynthesis and photosynthetic carbon partitioning at cellular level.     

13C NMR characterization of an exchange reaction between CO and CO2 catalyzed by carbon monoxide dehydrogenase

Carbon monoxide dehydrogenase (CODH) catalyzes the reversible oxidation of CO to CO2 at a nickel-iron-sulfur cluster (the C-cluster). CO oxidation follows a ping-pong mechanism involving two-electron reduction of the C-cluster followed by electron transfer through an internal electron transfer chain to external electron acceptors. We describe 13C NMR studies demonstrating a CODH-catalyzed steady-state exchange reaction between CO and CO2 in the absence of external electron acceptors. This reaction is characterized by a CODH-dependent broadening of the 13CO NMR resonance; however, the chemical shift of the 13CO resonance is unchanged, indicating that the broadening is in the slow exchange limit of the NMR experiment. The 13CO line broadening occurs with a rate constant (1080 s-1 at 20 degrees C) that is approximately equal to that of CO oxidation. It is concluded that the observed exchange reaction is between 13CO and CODH-bound 13CO2 because 13CO line broadening is pH-independent (unlike steady-state CO oxidation), because it requires a functional C-cluster (but not a functional B-cluster) and because the 13CO2 line width does not broaden. Furthermore, a steady-state isotopic exchange reaction between 12CO and 13CO2 in solution was shown to occur at the same rate as that of CO2 reduction, which is approximately 750-fold slower than the rate of 13CO exchange broadening. The interaction between CODH and the inhibitor cyanide (CN-) was also probed by 13C NMR. A functional C-cluster is not required for 13CN- broadening (unlike for 13CO), and its exchange rate constant is 30-fold faster than that for 13CO. The combined results indicate that the 13CO exchange includes migration of CO to the C-cluster, and CO oxidation to CO2, but not release of CO2 or protons into the solvent. They also provide strong evidence of a CO2 binding site and of an internal proton transfer network in CODH. 13CN- exchange appears to monitor only movement of CN- between solution and its binding to and release from CODH.     

Fetal CO2 kinetics

Knowledge of CO2 kinetics in the fetus is important for the design and interpretation of fetal metabolic studies that use carbon-labelled tracers. To study fetal CO2 kinetics, four fetal sheep were infused at constant rate with NaH14CO3 to simulate a constant rate of fetal 14CO2 production from the metabolism of a 14C-labelled substrate. Uterine and umbilical blood flows, and concentrations of 14CO2 and total CO2 in umbilical arterial and venous blood and in uterine arterial and venous blood were measured. During steady state, the excretion of 14CO2 via the umbilical circulation was 99.6 +/- 1.0 (SEM)% of the NaH14CO3 infusion rate. The irreversible disposal rate of CO2 molecules from the fetal CO2 pool was approximately 5 times greater than the metabolic production of CO2 by the fetus. This evidence demonstrates that measurements of fetal 14CO2 excretion via the umbilical circulation can provide an accurate measurement of fetal 14CO2 production and that the exchange rate of CO2 molecules between placenta and fetal blood is much greater than the net rate of excretion of CO2 molecules from fetus to placenta.     

12CO2 emission from different metabolic pathways measured in illuminated and darkened C3 and C4 leaves at low,atmospheric and elevated CO2 concentration

The detection of 12CO2 emission from leaves in air containing 13CO2 allows simple and fast determination of the CO2 emitted by different sources, which are separated on the basis of their labelling velocity. This technique was exploited to investigate the controversial effect of CO2 concentration on mitochondrial respiration. The 12CO2 emission was measured in illuminated and darkened leaves of one C4 plant and three C3 plants maintained at low (30-50 ppm), atmospheric (350-400 ppm) and elevated (700-800 ppm) CO2 concentration. In C3 leaves, the 12CO2 emission in the light (Rd) was low at ambient CO2 and was further quenched in elevated CO2, when it was often only 20-30% of the 12CO2 emission in the dark, interpreted as the mitochondrial respiration in the dark (Rn). Rn was also reduced in elevated CO2. At low CO2, Rd was often 70-80% of Rn, and a burst of 12CO2 was observed on darkening leaves of Mentha sativa and Phragmites australis after exposure for 4 min to 13CO2 in the light. The burst was partially removed at low oxygen and was never observed in C4 leaves, suggesting that it may be caused by incomplete labelling of the photorespiratory pool at low CO2. This pool may be low in sclerophyllous leaves, as in Quercus ilex where no burst was observed. Rd was inversely associated with photosynthesis, suggesting that the Rd/Rn ratio reflects the refixation of respiratory CO2 by photosynthesizing leaves rather than the inhibition of mitochondrial respiration in the light, and that CO2 produced by mitochondrial respiration in the light is mostly emitted at low CO2, and mostly refixed at elevated CO2. In the leaves of the C4 species Zea mays, the 12CO2 emission in the light also remained low at low CO2, suggesting efficient CO2 refixation associated with sustained photosynthesis in non-photorespiratory conditions. However, Rn was inhibited in CO2-free air, and the velocity of 12CO2 emission after darkening was inversely associated with the CO2 concentration. The emission may be modulated by the presence of post-illumination CO2 uptake deriving from temporary imbalance between C3 and C4 metabolism. These experiments suggest that this uptake lasts longer at low CO2 and that the imbalance is persistent once it has been generated by exposure to low CO2.     

Rewinding the tape: selection of algae adapted to high CO2 at current and pleistocene levels of CO2

Selective history is thought to constrain the extent and direction of future adaptation by limiting access to genotypes that are advantageous in a novel environment. Populations of Chlamydomonas previously selected at high CO2 were either backselected at ambient levels of CO2, or selected at levels of CO2 that last occurred during glaciation in the Pleistocene. There was no effect of selective history on adaptation to either level of CO2, and the high CO2 phenotypes were evolutionarily reversible such that fitness in ambient CO2 returned to values seen in controls. CO2 uptake affinity improved relative to the ancestor in both ambient and glacial CO2, although wild-type regulation of CO2 uptake, which deteriorated during previous selection at high CO2, was not restored by selection at lower levels of CO2. Trade-offs in both CO2 uptake affinity and growth were seen after selection at any given level of CO2. Adaptation to ambient and glacial-era levels of CO2 produced a range of phenotypes, suggesting that chance rather than selective history contributes to the divergence of replicate populations in this system.     

Estimation of Bundle Sheath Cell Conductance in C4 Species and O2 Insensitivity of Photosynthesis

Low conductance to CO2 of bundle sheath cells is required in C4 photosynthesis to maintain high [CO2] at the site of ribulose-1,5-bisphosphate carboxylase/oxygenase (Rubisco). Elevated [CO2] allows high CO2 assimilation rates by this enzyme and prevents Rubisco oxygenase activity and O2 inhibition of carboxylation. Bundle sheath conductance to CO2 was estimated by chemically inhibiting phosphoenolpyruvate carboxylase and calculating the slope of the linear response of leaf CO2 uptake to [CO2]. The inhibitor 3,3-dichloro-2-dihydroxyphosphinoylmethyl-2-propenoate was supplied to detached leaves of Panicum maximum, Panicum miliaceum, and Sorghum bicolor at 4 mM. Uptake of CO2 was measured at 210 mL L-1 O2 over the CO2 concentration range of 0.34 to 28 mL L-1. Without the inhibitor, CO2 uptake increased steeply at low [CO2] and saturated at about 1 mL L-1. After inhibition, CO2 uptake was a linear function of [CO2] over much of the range tested. The slope of this CO2 response, taken as bundle sheath conductance, was 2.35, 1.96, and 1.13 mmol m-2 s-1 for P. maximum, P. miliaceum, and S. bicolor, respectively, on a leaf area basis. Conductance based on bundle sheath area was 0.76, 0.93, and 0.54 mmol m-2 s-1, respectively. Uptake of CO2 by leaves of P. maximum supplied with the inhibitor was not affected by reduction of [O2] from 210 to 20 mL L-1 over the range of [CO2] used. Because [CO2] in bundle sheath cells of inhibited leaves is likely to be much lower than ambient, the lack of O2 sensitivity of CO2 uptake cannot be ascribed to lack of O2 reaction with ribulose bisphosphate and is probably due to the low conductance of bundle sheath cells, especially at low ambient [CO2]. The likely result of reducing [O2] from 210 to 20 mL L-1 is to stimulate carboxylation of ribulose bisphosphate, thus further reducing [CO2] in bundle sheath cells and increasing CO2 diffusion to these cells from the mesophyll. However, the increase in diffusion is greatly limited by low conductance of the bundle sheath cell walls. Calculations based on estimated bundle sheath conductance show that changes in bundle sheath [CO2] of 0.085 to 0.5 mL L-1, which might be associated with reduced [O2], would have a negligible effect on CO2 uptake.     

Mechanisms underlying CO2 diffusion in leaves

Plants provide an excellent system to study CO(2) diffusion because, under light saturated conditions, photosynthesis is limited by CO(2) availability. Recent findings indicate that CO(2) diffusion in leaves can be variable in a short time range. Mesophyll CO(2) conductance could change independently from stomata movement or CO(2) fixing reactions and it was suggested that, beside others, the membranes are mesophyll CO(2) conductance limiting components. Specific aquaporins as membrane intrinsic pore proteins are considered to have a function in the modification of membrane CO(2) conductivity. Because of conflicting data, the mechanism of membrane CO(2) diffusion in plants and animals is a matter of a controversy vivid debate in the scientific community. On one hand, data from biophysics are in favor of CO(2) diffusion limiting mechanisms completely independent from membrane structure and membrane components. On the other, there is increasing evidence from physiology that a change in membrane composition has an effect on CO(2) diffusion.     

Temperature, oxygen, and salt-sensing neurons in C. elegans are carbon dioxide sensors that control avoidance behavior

Homeostatic control of body fluid CO(2) is essential in animals but is poorly understood. C.?elegans relies on diffusion for gas exchange and avoids environments with elevated CO(2). We show that C.?elegans temperature, O(2), and salt-sensing neurons are also CO(2) sensors mediating CO(2) avoidance. AFD thermosensors respond to increasing CO(2) by a fall and then rise in Ca(2+) and show a Ca(2+) spike when CO(2) decreases. BAG O(2) sensors and ASE salt sensors are both activated by CO(2) and remain tonically active while high CO(2) persists. CO(2)-evoked Ca(2+) responses in AFD and BAG neurons require cGMP-gated ion channels. Atypical soluble guanylate cyclases mediating O(2) responses also contribute to BAG CO(2) responses. AFD and BAG neurons together stimulate turning when CO(2) rises and inhibit turning when CO(2) falls. Our results show that C.?elegans senses CO(2) using functionally diverse sensory neurons acting homeostatically to minimize exposure to elevated CO(2).     

Elevated CO2 influences the expression of floral-initiation genes in Arabidopsis thaliana

Atmospheric CO(2) concentration ([CO(2)]) is rising on a global scale and is known to affect flowering time. Elevated [CO(2)] may be as influential as temperature in determining future changes in plant developmental timing, but little is known about the molecular mechanisms that control altered flowering times at elevated [CO(2)]. Using Arabidopsis thaliana, the expression patterns were compared of floral-initiation genes between a genotype that was selected for high fitness at elevated [CO(2)] and a nonselected control genotype. The selected genotype exhibits pronounced delays in flowering time when grown at elevated [CO(2)], whereas the control genotype is unaffected by elevated [CO(2)]. Thus, this comparison provides an evolutionarily relevant system for gaining insight into the responses of plants to future increases in [CO(2)]. Evidence is provided that elevated [CO(2)] influences the expression of floral-initiation genes. In addition, it is shown that delayed flowering at elevated [CO(2)] is associated with sustained expression of the floral repressor gene, FLOWERING LOCUS C (FLC), in an elevated CO(2)-adapted genotype. Understanding the mechanisms that account for changes in plant developmental timing at elevated [CO(2)] is critical for predicting the responses of plants to a high-CO(2) world of the near future.     

Formation of carbon monoxide from CO2 and H2 by Methanobacterium thermoautotrophicum

Cell suspensions of Methanobacterium thermoautotrophicum were found to reduce CO2 with H2 to CO at a maximal rate of 100 nmol X min-1 X mg protein-1. Half-maximal rates were obtained at a H2 and a CO2 concentration in the gas phase of 10% and 30%, respectively. The CO concentration in the gas phase surpassed the equilibrium concentration by a factor of more than 15 which indicates that CO2 reduction with H2 to CO was energy-driven. This was substantiated by the observation that the cells only formed CO when they also generated methane and that CO formation was completely inhibited by uncouplers. CO formation by cell suspensions and by growing cells was inhibited by cyanide. Neither methane formation nor the electrochemical proton potential were affected by this inhibitor. Cyanide was shown to inactivate specifically the carbon monoxide dehydrogenase present in M. thermoautotrophicum. It is therefore concluded that reduction of CO2 to CO is catalyzed by this enzyme. CO production by growing cells was 5-10-times slower than by resting cells. This is explained by effective CO assimilation in growing cells; when CO assimilation was inhibited by propyl iodide the rate of CO production immediately increased more than tenfold.     

Specification of adaxial and abaxial stomata, epidermal structure and photosynthesis to CO2 enrichment in maize leaves

Acclimation to CO2 enrichment was studied in maize plants grown to maturity in either 350 or 700 microl l-1 CO2. Plants grown with CO2 enrichment were significantly taller than those grown at 350 microl l-1 CO2 but they had the same number of leaves. High CO2 concentration led to a marked decrease in whole leaf chlorophyll and protein. The ratio of stomata on the adaxial and abaxial leaf surfaces was similar in all growth conditions, but the stomatal index was considerably increased in plants grown at 700 microl l-1 CO2. Doubling the atmospheric CO2 content altered epidermal cell size leading to fewer, much larger cells on both leaf surfaces. The photosynthesis and transpiration rates were always higher on the abaxial surface than the adaxial surface. CO2 uptake rates increased as atmospheric CO2 was increased up to the growth concentrations on both leaf surfaces. Above these values, CO2 uptake on the abaxial surface was either stable or increased as CO2 concentration increased. In marked contrast, CO2 uptake rates on the adaxial surface were progressively inhibited at concentrations above the growth CO2 value, whether light was supplied directly to this or the abaxial surface. These results show that maize leaves adjust their stomatal densities through changes in epidermal cell numbers rather than stomatal numbers. Moreover, the CO2-response curve of photosynthesis on the adaxial surface is specifically determined by growth CO2 abundance and tracks transpiration. Conversely, photosynthesis on the abaxial surface is largely independent of CO2 concentration and rather independent of stomatal function.     

Effects of Elevated CO2 and High Temperature on Single Leaf and Canopy Photosynthesis of Rice

The increase of atmospheric CO2 concentration is indisputable. In such condition, photosynthetic response of leaf is relatively well studied, while the comparison of that between single leaf and whole canopy is less emphasized. The stimulation of elevated CO2 on canopy photosynthesis may be different from that on single leaf level. In this study, leaf and canopy photosynthesis of rice ( Oryza sativa L. ) were studied throughout the growing season. High CO2 and temperature had a synergetic stimulation on single leaf photosynthetic rate until grain filling. Photosynthesis of leaf was stimulated by high CO2, although the stimulation was decreased by higher temperature at grain filling stage. On the other hand, the simulation of elevated CO2 on canopy photosynthesis leveled off with time. Stimulation at canopy level disappeared by grain filling stage in beth temperature treatments. Green leaf area index was not significantly affected by CO2 at maturity, but greater in plants grown at higher temperature. Leaf nitrogen content decreased with the increase of CO2 concentration although it was not statistically significant at maturity. Canopy respiration rate increased at flowering stage indicating higher carbon loss. Shading effect caused by leaf development reached maximum at flowering stage. The CO2 stimulation on photosynthesis was greater in single leaf than in canopy. Since enhanced CO2 significantly increased biomass of rice stems and panicles, increase in canopy respiration caused diminishment of CO2 stimulation in canopy net photosynthesis, keaf nitrogen in the canopy level decreased with CO2 concentration and may eventually hasten CO2 stimulation on canopy photosynthesis. Early senescence of canopy leaves in high CO2 is also a possible cause.     

北京海淀公园绿地二氧化碳通量

作为城市生态系统的重要组成部分,城市绿地有着释氧固碳、降温增湿、吸收有毒有害气体、降尘、减噪等多种生态功能。在对北京海淀公园2006年5月到2007年3月的CO2通量观测数据进行质量评价、数据剔除和插补的基础上,通过与温度、太阳辐射等气象数据的相关性分析,定量研究了海淀公园绿地CO2通量的日变化、年变化以及影响因子。结果表明,海淀公园绿地日CO2通量在一年内具有明显的季节变化,植物生长季3—10月份以吸收CO2为主,11月至翌年2月份以释放CO2为主;年净生态系统生产力(NEP)为8.7554 tCO2/hm2a,反映了海淀公园绿地具有较强的固碳能力。     

Entry and exit pathways of CO2 in rat liver mitochondria respiring in a bicarbonate buffer system

The dynamics and pathways of CO2 movements across the membranes of mitochondria respiring in vitro in a CO2/HCO-3 buffer at concentrations close to that in intact rat tissues were continuously monitored with a gas-permeable CO2-sensitive electrode. O2 uptake and pH changes were monitored simultaneously. Factors affecting CO2 entry were examined under conditions in which CO2 uptake was coupled to electrophoretic influx of K+ (in the presence of valinomycin) or Ca2+. The role of mitochondrial carbonic anhydrase (EC 4.2.1.1) in CO2 entry was evaluated by comparison of CO2 uptake by rat liver mitochondria, which possess carbonic anhydrase, versus rat heart mitochondria, which lack carbonic anhydrase. Such studies showed that matrix carbonic anhydrase activity is essential for rapid net uptake of CO2 with K+ or Ca2+. Studies with acetazolamide (Diamox), a potent inhibitor of carbonic anhydrase, confirmed the requirement of matrix carbonic anhydrase for net CO2 uptake. It was shown that at pH 7.2 the major species leaving respiring mitochondria is dissolved CO2, rather than HCO-3 or H2CO3 suggested by earlier reports. Efflux of endogenous CO2/HCO-3 is significantly inhibited by inhibitors of the dicarboxylate and tricarboxylate transport systems of the rat liver inner membrane. The possibility that these anion carriers mediate outward transport of HCO-3 is discussed.     

Effect of CO2 on the fermentation capacities of the acetogen Peptostreptococcus productus U-1.

The fermentative capacities of the acetogenic bacterium Peptostreptococcus productus U-1 (ATCC 35244) were examined. Although acetate was formed from all the substrates tested, additional products were produced in response to CO2 limitation. Under CO2-limited conditions, fructose-dependent growth yielded high levels of lactate as a reduced end product; lactate was also produced under CO2-enriched conditions when fructose concentrations were elevated. In the absence of supplemental CO2, xylose-dependent growth yielded lactate and succinate as major reduced end products. Although supplemental CO2 and acetogenesis stimulated cell yields on fructose, xylose-dependent cell yields were decreased in response to CO2 and acetogenesis. In contrast, glycerol-dependent growth yielded high levels of ethanol in the absence of supplemental CO2, and pyruvate was subject to only acetogenic utilization independent of CO2. CO2 pulsing during the growth of CO2-limited fructose cultures stopped lactate synthesis immediately, indicating that CO2-limited cells were nonetheless metabolically poised to respond quickly to exogenous CO2. Resting cells that were cultivated at the expense of fructose without supplemental CO2 readily consumed fructose in the absence of exogenous CO2 and formed only lactate. Although the specific activity of lactate dehydrogenase was not appreciably influenced by supplemental C02 during cultivation, cells cultivated on fructose under CO2-enriched conditions displayed minimal capacities to consume fructose in the absence of exogenous CO2. These results demonstrate that the utilization of alternative fermentations for the conservation of energy and growth of P. productus U-1 is augmented by the relative availability of CO2 and growth substrate.     

Perception of breath components by the tropical bont tick,Amblyomma variegatum Fabricius (Ixodidae)

Wall-pore olfactory sensilla located in the capsule of Haller's organ on the tarsus of Amblyomma variegatum ticks bear cells responding to vertebrate breath: one of these sensilla contains a CO2-excited receptor and a second sensillum has a CO2-inhibited receptor. Each of these antagonistic CO2-receptors, which display typical phasic-tonic responses, monitors a different CO2-concentration range. The CO2-inhibited receptor is very sensitive to small concentration changes between 0 and ca. 0.2%, but variations of 0.01% around ambient (ca. 0.04%) induce the strongest frequency modulation of this receptor. An increase of just 0.001-0.002% (10-20 ppm) above a zero CO2-level already inhibits this receptor. By contrast, the CO2-excited receptor is not so sensitive to small CO2 shifts around ambient, but best monitors changes in CO2 concentrations above 0.1%. This receptor is characterized by a steep dose-response curve and a fast inactivation even at high CO2-concentrations (greater than 2%). In a wind-tunnel, Amblyomma variegatum is activated from the resting state and attracted by CO2 concentrations of 0.04 to ca. 1%, which corresponds to the sensitivity range of its CO2-receptors. The task of perceiving the whole concentration range to which this tick is attracted would thus appear to be divided between two receptors, one sensitive to small changes around ambient and the other sensitive to the higher concentrations normally encountered when approaching a vertebrate host.     

Carbon monoxide actuates O(2)-limited heme degradation in the rat brain

The biochemical paradigm for carbon monoxide (CO) is driven by the century-old Warburg hypothesis: CO alters O(2)-dependent functions by binding heme proteins in competitive relation to 1/oxygen partial pressure (PO(2)). High PO(2) thus hastens CO elimination and toxicity resolution, but with more O(2), CO-exposed tissues paradoxically experience less oxidative stress. To help resolve this paradox we tested the Warburg hypothesis using a highly sensitive gas-reduction method to track CO uptake and elimination in brain, heart, and skeletal muscle in situ during and after exogenous CO administration. We found that CO administration does increase tissue CO concentration, but not in strict relation to 1/PO(2). Tissue gas uptake and elimination lag behind blood CO as predicted, but 1/PO(2) vs. [CO] fails even at hyperbaric PO(2). Mechanistically, we established in the brain that cytosol heme concentration increases 10-fold after CO exposure, which sustains intracellular CO content by providing substrate for heme oxygenase (HO) activated after hypoxia when O(2) is resupplied to cells rich in reduced pyridine nucleotides. We further demonstrate by analysis of CO production rates that this heme stress is not due to HO inhibition and that heme accumulation is facilitated by low brain PO(2). The latter becomes rate limiting for HO activity even at physiological PO(2), and the heme stress leads to doubling of brain HO-1 protein. We thus reveal novel biochemical actions of both CO and O(2) that must be accounted for when evaluating oxidative stress and biological signaling by these gases.     

Proton-motive-force-driven formation of CO from CO2 and H2 in methanogenic bacteria

Cell suspensions of methanogenic bacteria (Methanosarcina barkeri, Methanospirillum hungatei, Methano-brevibacter arboriphilus, and Methanobacterium thermoautotrophicum) were found to form CO from CO2 and H2 according to the reaction: CO2 + H2----CO + H2O; delta G0 = +20 kJ/mol. Up to 15,000 ppm CO in the gas phase were reached which is significantly higher than the equilibrium concentration calculated from delta G0 (95 ppm under the experimental conditions). This indicated that CO2 reduction with H2 to CO is energy-driven and indeed the cells only generated CO when forming CH4. The coupling of the two reactions was studied in more detail with acetate-grown cells of M. barkeri using methanogenic substrates. The effects of the protonophore tetrachlorosalicylanilide (TCS) and of the proton-translocating ATPase inhibitor N,N'-dicyclohexylcarbodiimide (cHxN)2C were determined. TCS completely inhibited CO formation from CO2 and H2 without affecting methanogenesis from CH3OH and H2. In the presence of the protonophore the proton motive force delta p and the intracellular ATP concentration were very low. (cHxN)2C, which partially inhibited methanogenesis from CH3OH and H2, had no effect on CO2 reduction to CO. In the presence of (cHxN)2C delta p was high and the intracellular ATP content was low. These findings suggest that the endergonic formation of CO from CO2 and H2 is coupled to the exergonic formation of CH4 from CH3OH and H2 via the proton motive force and not via ATP. CO formation was not stimulated by the addition of sodium ions.     

大气CO2浓度和温度升高对水稻叶片及群体光合作用的影响

大气ＣＯ２浓度升高对植物光合作用的影响研究多集中在单叶水平,在高ＣＯ２及高温下对植物单叶及群体光合进行比较的研究少有报道,而群体水平的研究则是预测生态系统反应所不可缺少的。采用田间开顶式培养室研究了大气ＣＯ２浓度和温度升高对水稻（ＯｒｙｚａｓａｔｉｖａＬ．）叶片及群体光合作用的影响。发现ＣＯ２浓度和温度对水稻叶片光合作用有协同促进作用,而对群体光合作用的促进则随时间的推移而减弱;单叶光合受到的促进作用大于群体光合;叶面积指数只在营养生长期受到促进,冠层叶片含氮量受ＣＯ２影响降低。群体呼吸（包括茎杆）增加及冠层叶片早衰可能是后期ＣＯ２对群体光合促进作用下降的原因。     

CO2 Uptake and Electron Transport Rates in Wild-Type and a Starchless Mutant of Nicotiana sylvestris (The Role and Regulation of Starch Synthesis at Saturating CO2 Concentrations)

CO2 uptake rate, chlorophyll fluorescence, and 830-nm absorbance were measured in wild-type (wt) Nicotiana sylvestris (Speg. et Comes) and starchless mutant NS 458 leaves at different light intensities and CO2 concentrations. Initial slopes of the relationships between CO2 uptake and light and CO2 were similar, but the maximum rate at CO2 and light saturation was only 30% in the mutant compared with the wt. O2 enhancement of photosynthesis at CO2 and light saturation was relatively much greater in the mutant than in the wt. In 21% O2, the electron transport rate (ETR) calculated from fluorescence peaked near the beginning of the CO2 saturation of photosynthesis. With the further increase of CO2 concentration ETR remained nearly constant or declined a little in the wt but drastically declined in the mutant. Absorbance measurements at 830 nm indicated photosystem I acceptor side reduction in both plants at saturating CO2 and light. Assimilatory charge (postillumination CO2 uptake) measurements indicated trapping of chloroplast inorganic phosphate, supposedly in hexose phosphates, in the mutant. It is concluded that starch synthesis gradually substitutes for photorespiration as electron acceptor with increasing CO2 concentration in the wt but not in the mutant. It is suggested that starch synthesis is co-controlled by the activity of the chloroplast fructose bisphosphatase.