Arabidopsis thaliana carbonic anhydrase: cDNA sequence and effect of CO2 on mRNA levels

A full-length cDNA clone encoding carbonic anhydrase was isolated from an Arabidopsis thaliana (Columbia) leaf library. Comparison of the derived amino acid sequence obtained from this clone with those of pea and spinach reveals a considerable degree of identity. The carbonic anhydrase cDNA was used to probe the level of RNA encoding this protein in the leaves of plants grown in elevated CO₂ (660 ppm). We have found that under these conditions the steady-state level of carbonic anhydrase mRNA was increased in comparison with control plants grown in normal atmospheric concentrations of CO₂ (330 ppm). This raises the intruiging possibility that there exists in higher plants a mechanism for perceiving and responding to changes in environmental CO₂ concentrations at the genetic level.     

CO2 exchange characteristics during dark-light transitions in wild-type and mutant Chlamydomonas reinhardii cells

A burst of net CO₂ uptake was observed during the first 3–4 min after the onset of illumination in both wild-type Chlamydomonas reinhardii in which carbonic anhydrase was chemically inhibited with ethoxyzolamide and in a mutant of C. reinhardii (ca-1-12-1C) deficient in carbonic anhydrase activity. The burst was followed by a rapid decrease in the CO₂ uptake rate so that net evolution often occurred. After a 2–3 min period of CO₂ evolution, net CO₂ uptake again increased and ultimately reached a steady-state, positive rate. From [¹⁴CO₂]-tracer studies it was determined that CO₂ fixation proceeded at a nearly linear rate throughout the period of illumination. Thus, prior to reaching a steady state, there was a rapid accumulation of inorganic carbon inside the cells which apparently reached a supercritical concentration and the excess was excreted, causing a subsequent efflux of CO₂. A post illumination burst of net CO₂ efflux was also observed in ethoxyzolamide-inhibited wild type and ca-1 mutant cells, but not in the unihibited wild type. [¹⁴CO₂]-tracer experiments revealed that this burst was the result of a collapse of a large internal inorganic carbon pool at the onset of darkness rather than a photorespiratory post-illumination burst. These results indicate that upon illumination, chemical or genetic inhibition of carbonic anhydrase initially causes an accumulation of excess inroganic carbon in C. reinhardii cells, and that unknown regulatory mechanisms correct for this imbalance by first excreting the excess inorganic carbon and then, after several dampened oscillations, achieving an equilibrium between bicarbonate uptake, bicarbonate dehydration, and CO₂ fixation.     

Carbon Oxysulfide Inhibition of the CO(2)-Concentrating Process of Unicellular Green Algae

Carbonyl sulfide (COS), a substrate for carbonic anhydrase, inhibited alkalization of the medium, O₂ evolution, dissolved inorganic carbon accumulation, and photosynthetic CO₂ fixation at pH 7 or higher by five species of unicellular green algae that had been air-adapted for forming a CO₂-concentrating process. This COS inhibition can be attributed to inhibition of external HCO₃⁻ conversion to CO₂ and OH⁻ by the carbonic anhydrase component of an active CO₂ pump. At a low pH of 5 to 6, COS stimulated O₂ evolution during photosynthesis by algae with low CO₂ in the media without alkalization of the media. This is attributed to some COS hydrolysis by carbonic anhydrase to CO₂. Although COS had less effect on HCO₃⁻ accumulation at pH 9 by a HCO₃⁻ pump in Scenedesmus, COS reduced O₂ evolution probably by inhibiting internal carbonic anhydrases. Because COS is hydrolyzed to CO₂ and H₂S, its inhibition of the CO₂ pump activity and photosynthesis is not accurate, when measured by O₂ evolution, by NaH¹⁴CO₃ accumulation, or by ¹⁴CO₂ fixation.     

Active uptake of CO2 during photosynthesis in the green alga Eremosphaera viridis is mediated by a CO2-ATPase

Mass spectrometry was used to investigate the uptake of CO₂ in Eremosphaera viridis DeBary. Upon illumination, cells preincubated at pH 7.5 with 100 M dissolved inorganic carbon (DIC) rapidly depleted almost all the free CO₂ from the medium. Rapid equilibrium between HCO ₃ ^- and CO₂ occurred upon addition of bovine carbonic anhydrase (CA) to the medium, showing that CO₂ depletion resulted from a selective uptake of CO₂ rather than an uptake of all inorganic carbon species. Glycolaldehyde (10 mM) completely inhibited CO₂ fixation but had little effect on CO₂ transport. Transfer of glycolaldehyde-treated cells to the dark caused a rapid efflux of CO₂ from the unfixed intracellular DIC pool which was found to be at least threeto sixfold higher in concentration than that of the external medium. These results indicate that E. viridis actively transports CO₂ against a concentration gradient. No external CA was detected in these cells either by potentiometric or mass-spectrometric assay. In the absence of external CA, the rate of photosynthetic O₂ evolution in the pH range 7.5 to 8.0 did not exceed the calculated rate of CO₂ supply, indicating a limited capacity for HCO₂ uptake in these cells. Electrophysiological measurements indicate that CO₂ uptake is electrically silent and thus is not a consequence of H⁺-CO₂ symport activity. Microsomal membranes isolated from Eremosphaera showed ATPase activity which was enhanced by CO₂. These results indicate that active CO₂ uptake is mediated by an ATPase.Abbreviations BTP 1,3-bis[tris(hydroximethyl)-methylamino]-propane - CA carbonic anhydrase - Chl chlorophyll - DIC dissolved inorganic carbon - [¹⁴C]DMO 5,5-dimethyl-[2-¹⁴C]-oxaz-didine-2,4-dione - WA Wilbur-Anderson units This work was supported by grants to B.C. and R.R.L. from the Natural Sciences and Engineering Research Council of Canada. We thank the Department of Biology, Queen's University, Kingston, Ontario for the use of the mass-spectrometer facility. We are indebted to A.G. Miller for his expert advice on operating the mass spectrometer and to Ms. Shahebina Samji for running the Bradford assays.     

Peat CO2 production in a natural and cutover peatland: Implications for restoration

Although studies have shown that peatland drainage andharvesting alter local hydrology, microclimate, and peatcharacteristics, little is known about the effects of these changes onCO₂ production rates. This study examines the differentfactors affecting CO₂ production from natural and cutoverpeatlands. Laboratory peat incubations were performed under aerobic andanaerobic conditions to determine the influence of temperature, soilmoisture, and peat depth on CO₂ production rates from peatsamples taken from: (1) a natural peatland; (2) a 2-yearpost-cutover peatland and; (3) a 7-year post-cutover peatland.CO₂ production rates ranged from 0.21 to 4.87 µmolg^–1 d^–1 under anaerobic conditions,and from 0.37 to 15.69 µmol g^–1d^–1 in the aerobic trials. While no significantdifferences were found between the CO₂ production rates ofthe two cutover sites, the natural site consistently displayed higherproduction values. The natural site was also the only site to exhibitstrong depth dependent trends, thus indicating the importance of theupper peat layer with respect to substrate quality. Higher productionrates were found under aerobic than anaerobic conditions, with thegreatest response to oxygen observed at the natural site. Productionrates increased with both temperature and soil moisture, with maximumproduction rates found at 20 °C and 92% moisture content.Temperature responses were generally greater at the cutover sites, whilesoil moisture had greater effects on the natural site peat.Results of this work agree with previous studies that suggest that itis essential to begin restoration once a cutover peatland is abandoned.Re-wetting a cutover peatland (through restoration practices) isnecessary to prevent an increase in peat temperature and CO₂production since cutover peat has higher Q₁₀ values thannatural peat. A decrease in overall peatland oxidation should reduce thepersistent source of atmospheric CO₂ from cutover peatlandsand the irreversible changes in peat structure that impedeSphagnum re-establishment.     

Active CO(2) Transport by the Green Alga Chlamydomonas reinhardtii

Mass spectrometric measurements of dissolved free ¹³CO₂ were used to monitor CO₂ uptake by air grown (low CO₂) cells and protoplasts from the green alga Chlamydomonas reinhardtii. In the presence of 50 micromolar dissolved inorganic carbon and light, protoplasts which had been washed free of external carbonic anhydrase reduced the ¹³CO₂ concentration in the medium to close to zero. Similar results were obtained with low CO₂ cells treated with 50 micromolar acetazolamide. Addition of carbonic anhydrase to protoplasts after the period of rapid CO₂ uptake revealed that the removal of CO₂ from the medium in the light was due to selective and active CO₂ transport rather than uptake of total dissolved inorganic carbon. In the light, low CO₂ cells and protoplasts incubated with carbonic anhydrase took up CO₂ at an apparently low rate which reflected the uptake of total dissolved inorganic carbon. No net CO₂ uptake occurred in the dark. Measurement of chlorophyll a fluorescence yield with low CO₂ cells and washed protoplasts showed that variable fluorescence was mainly influenced by energy quenching which was reciprocally related to photosynthetic activity with its highest value at the CO₂ compensation point. During the linear uptake of CO₂, low CO₂ cells and protoplasts incubated with carbonic anhydrase showed similar rates of net O₂ evolution (102 and 108 micromoles per milligram of chlorophyll per hour, respectively). The rate of net O₂ evolution (83 micromoles per milligram of chlorophyll per hour) with washed protoplasts was 20 to 30% lower during the period of rapid CO₂ uptake and decreased to a still lower value of 46 micromoles per milligram of chlorophyll per hour when most of the free CO₂ had been removed from the medium. The addition of carbonic anhydrase at this point resulted in more than a doubling of the rate of O₂ evolution. These results show low CO₂ cells of Chlamydomonas are able to transport both CO₂ and HCO₃⁻ but CO₂ is preferentially removed from the medium. The external carbonic anhydrase is important in the supply to the cells of free CO₂ from the dehydration of HCO₃⁻.     

CO2 is the first species formed upon CO oxidation by CO dehydrogenase from Pseudomonas carboxydovorans

The active species of CO₂, i.e. CO₂ or HCO ₃ ^- , formed in the CO dehydrogenase reaction was determined using the pure enzyme from the carboxydotrophic bacterium Pseudomonas carboxydovorans. Employing an assay system similar to that used to test for carbonic anhydrase, data were obtained which are quite compatible with those expected if CO₂ is the first species formed. In addition, carbonic anhydrase activity was not detected in P. carboxydovorans.     

Effects of Acetazolamide (Diamox), Ethoxzolamide and High Levels of CO2 on Carbonic Anhydrase, Photosystem Activity, and Oxygen Evolution in Euglena gracilis

Investigations using steady-state culture conditions indicate that carbonic anhydrase activity is correlated to the photosynthetic rate in Euglena in some but not all circumstances. When cultures grown with 5% CO₂ were changed to air growth, the photosynthetic rate was independent of the carbonic anhydrase activity. While experiments using the inhibitor acetazolamide indicated a close correlation between photosynthetic capacity and carbonic anhydrase activity, the inhibitor was found to be nonspecific. Acetazolamide altered photosystem activities directly as measured by the photoreduction of DCPIP in chloroplast preparations, whole-cell fluorescence transients of chlorophyll a, and by whole chain photoelectron flow. Ethoxzolamide, another inhibitor of carbonic anhydrase, was also found to inhibit photosystem activities, i.e., the photoreduction of DCPIP, and in vivo photoelectron flow, at high concentrations. Cells grown in 5% CO₂ were less sensitive to the effects of acetazolamide than cells exposed to air. The rate of electron flow in chloroplasts from cells grown with 5% CO₂ and exposed to 10 mM acetazolamide was 2.5-fold faster than that of chloroplasts from air-grown cells exposed to the same concentration of inhibitor. The whole cell chlorophyll a fluorescence transients of cultures grown with high CO₂ were completely different from those of air-grown cells and also showed fewer effects on exposure to acetazolamide. These results suggest a reevaluation of the hypothesis that carbonic anhydrase activity regulates photosynthesis. It is also apparent that results from air-grown and 5% CO₂-grown cultures cannot be directly compared in such studies.     

Metabolic changes during substrate shifts in continuous cultures of the yeast Candida boidinii variant 60

Summary Substrate shift experiments in chemostat cultures with either methanol or glucose as carbon source were performed with the yeast Candida boidinii variant 60. At low dilution rates of 0.064 h^–1 the culture may be easily shifted from methanol to glucose medium and back again to methanol. From these experiments it can be seen that glucose does not give rise to any catabolite inhibition of alcohol oxidase. Alcohol oxidase and formaldehyde dehydrogenase seem to be regulated by a repression-derepression mechanism, as small basal activities of both these enzymes can still be measured during growth on glucose. On the other hand, formate dehydrogenase activity is completely absent in the presence of glucose. This kind of regulation seems to favor the smooth switch from growth on glucose to methanol metabolism.With methanol or glucose, growth yields (Y_S) of 0.3 and 0.35, respectively may be obtained, and oxygen consumption (Q_{O 2}) is much higher in methanol cultures than in glucose-grown cells. Accordingly, the RQ values during growth on methanol decrease to about 0.5. Based on the yield coefficient of 0.3, it is possible to calculate that 38% of the methanol consumed must be incorporated into biomass, whereas 62% of the methanol is oxidized to CO₂. The corresponding RQ of 0.56 could not be experimentally ascertained.The activities of three mitochondrial enzymes were found to be higher in methanol-grown cells than in cells from glucose cultures. The low activites of enzymes for the phosphogluconate route in methanol-grown cells indicates that a cyclic oxidation of formaldehyde via hexose phosphate to CO₂ cannot be of great importance for methanol metabolism.List of Symbols D 1/h Dilution rate - 1/h Specific growth rate - Q_{CO 2} mmol/g·h Specific CO₂ production rate - Q_{O 2} mmol/g·h Specific O₂ comsumption rate - Q_S g/g·h Specific substrate consumption rate - RQ ./. Respiratory quotient (Q_{CO 2}/Q_{O 2}) - S_O g/l Substrate concentration in the feeding medium - $#x0073;$#x0304 g/l Substrate concentration in the fermentor - $#x0078;$#x0304 g/l Biomass in the fermentor - Y_{O 2} g/mmol O₂ Biomass yield on oxygen - Y_S g/g Biomass yield on carbon source     

Autotrophe Gewebekulturen von Ruta graveolens und deren 14CO2-Markierungsprodukte

Summary It is possible to obtain autotrophic callus cultures by inhibiting cell respiration. During a first passage of four weeks the cultures synthesized chlorophyll on an agar-medium with a minimum of organic substances such as sugar, amino acids and vitamins. In the second passage these cultures were kept on the same medium but were aerated with a mixture of 99% N₂ and 1% CO₂. In the third and last passage the medium contained only mineral substances and the same mixture of N₂ and CO₂ was used for aeration. This pure mineral medium was supplemented with the Hoagland's solution.These autotrophic callus cultures were grown for about two years under these conditions and showed a growth quotient of ten.Three different groups of tissues were taken for the ¹⁴CO₂-fixation. The first group was grown for four weeks on a heterotrophic medium and aerated with O₂. This is the socalled respirating group. The second and third group were both aerated with the mixture of N₂/CO₂ but they were grown on different mediums. One of these groups was grown on a heterotrophic medium for four weeks: these are heterotrophic photosynthesizing tissues. The third group was grown on a pure mineral medium, and these are the autotrophic photosynthesizing callus tissues.Respirating tissues are different from photosynthesizing cultures in respect to the quantity of light-induced CO₂-fixation.The thin-layer chromatograms reveal the difference between heterotrophic and autotrophic tissues. In the light dependent ¹⁴CO₂-incorporation the difference is in the amounts of the labelled amino acids glycine and serine. In the dark dependent incorporation the difference is found in the amount of the labelled amino acid aspartic acid. The more autotrophic these tissues are, the higher the level of the CO₂-fixation in these amino acids is.

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Mit Hilfe der Deutschen Forschungsgemeinschaft.     

Isolation of cDNA clones of genes induced upon transfer of Chlamydomonas reinhardtii cells to low CO2

Unicellular algae grow well under limiting CO₂ conditions, aided by a carbon concentrating mechanism (CCM). In C. reinhardtii, this mechanism is inducible and is present only in cells grown under low CO₂ conditions. We constructed a cDNA library from cells adapting to low CO₂, and screened the library for cDNAs specific to low CO₂-adapting cells. Six classes of low CO₂-inducible clones were identified. One class of clone, reported here, represents a novel gene associated with adaptation of cells to air. A second class of clones corresponds to the air-inducible periplasmic carbonic anhydrase I (CAH1). These clones represent genes that respond to the level of CO₂ in the environment.     

Endogenously produced CO2 induces stationary phase in tetrahymena cultures

Media concentration of total soluble CO₂ increases with culture age of Tetrahymena pyriformis. CO₂ is a weak acid and is capable of acidifying intracellular pH (pHi). Changes in pHi have been demonstrated to affect cell metabolism and growth in many systems. For these reasons, we investigated whether the concentrations of CO₂ produced in vitro were sufficient to affect cell proliferation and pHi in Tetrahymena. In this study, we used DMO to mimic the weak acid properties of CO₂. DMO is freely permeable to membranes in its uncharged form and has a pKa similar to that of CO₂/HCO. In addition, it has the advantages of being metabolically inert and non-volatile. At concentrations similar to endogenously produced CO₂, DMO acidifies pHi and arrests culture growth. In addition, procedures are described which decrease the media CO₂ concentrations in both growing and non-growing cultures. These conditions lead to increased maximum culture density at stationary phase. The data indicate that, under our conditions, accumulation of CO₂ in the culture leads to cessation of growth, probably through elimination of transmembrane pH gradients, which are necessary for regulation of metabolism and growth.     

A method for the study of CO2 exchanges in in vitro cultured Vitis rupestris plantlets

A CO₂ assay circuit adapted to in vitro culture was designed to investigate CO₂ exchanges in test tube-grown Vitis rupestris plantlets. The CO₂ concentration of the air in culture tubes was measured by injection of samples in the open circuit. It was observed under the culture conditions used that the CO₂ content stabilized during the light phase at 3 times the CO₂ compensation point.Measurements of dark respiration under closed circuit conditions at every two-hour interval during the night did not reveal any limiting by lack of the substrate under mixotrophic culture conditions. A mathematical model of the influence of ambient CO₂ concentration on net CO₂ uptake rates under closed circuit conditions was devised and used to compare net photosynthesis at different lighting levels. Measurement of CO₂ evolution into CO₂-free air under open circuit conditions revealed a post-illumination burst characteristic of photorespiration which increased with the temperature.     

Effect of CO2, CO2 and Diamox on photosynthesis and photorespiration in Chlamydomonas reinhardtii (green alga) and Anacystis nidulans (Cyanobacterium, blue-green alga)

Photorespiration by Chlamydomonas reinhardtii and Anacystis nidulans was measured as the oxygen inhibition of CO₂ uptake and the CO₂ compensation points. Net photosynthesis was oxygen dependent in Chlamydomonas grown in 5% CO₂, but CO₂ insensitive in cultures bubbled with air. Anacystis, even when cultured in 5% CO₂, exhibited an CO₂ insensitive net photosynthesis. The CO₂ compensation point of Chlamydomonas grown in cultures bubbled with air and Anacystis grown in 5% CO₂ enriched air, were reached shortly after the measurement was begun and the values were very low, less than 10 μl CO₂ 1^?1; while Chlamydomonas grown in 5% CO₂ enriched air for 4 days showed a high, but temporary CO₂ compensation point (60 μl CO₂ 1^?1). After a two hour adaptation in low CO₂, a stable, low CO₂ compensation point was reached. It seems that photorespiration can only be detected by the methods used in this study when the algae are cultured in high CO₂, but a mechanism exists which blocks photorespiration when the green algae are adapted to low CO₂ concentrations. When Chlamydomonas was treated with Diamox, an inhibitor of carbonic anhydrase, after cultivation in low CO₂ (air), the cells behaved as if they had been grown in high CO₂. They showed an oxygen sensitive net photosynthesis and a high CO₂ compensation point. This indicates that carbonic anhydrase plays an important role in the regulation of a measurable photorespiration in Chlamydomonas. The results are discussed in relation to previous observations of photorespiration measured by enzyme assay, metabolic products and gas exchange properties.     

Light-dependent bicarbonate uptake and CO2 efflux in the marine microalga Nannochloropsis gaditana

 Inorganic carbon (Ci) uptake and efflux has been investigated in the marine microalga Nannochloropsis gaditana Lubian by monitoring CO₂ fluxes in cell suspensions using mass spectrometry. Addition of H¹³CO₃ ⁻ to cell suspensions in the dark caused a transient increase in the CO₂ concentration in the medium far in excess of the equilibrium CO₂ concentration. The magnitude of this release was dependent on the length of time the cells had been kept in the dark. Once equilibrium between the Ci species had been achieved, a CO₂ efflux was observed after saturating light intensity was applied to the cells. External carbonic anhydrase (CA) was not detected nor does this species demonstrate a capacity to take up CO₂ by active transport. Photosynthetic O₂ evolution and the release CO₂ in the dark depend on HCO₃ ⁻ uptake since both were inhibited by the anion exchange inhibitor, 4,4′-diisothiocyanatostilbene-2,2′-disulfonic acid (DIDS). The bicarbonate uptake mechanism requires light but can also continue for short periods in the dark. Ethoxyzolamide, a CA inhibitor, markedly inhibited CO₂ efflux in the dark, indicating that CO₂ efflux was dependent upon the intracellular dehydration of HCO₃ ⁻. These results indicate that Nannochloropsis possesses a bicarbonate uptake system which causes the accumulation of high intracellular Ci levels and an internal CA which maintains the equilibrium between CO₂ and HCO₃ ⁻ and thus causes a subsequent release of CO₂ to the external medium. Received: 20 September 1999 / Accepted: 25 October 1999     

INDUCIBLE MECHANISMS FOR HCO3– UTILIZATION AND REPRESSION OF PHOTORESPIRATION IN PROTOPLASTS AND THALLI OF THREE SPECIES OF ULVA (CHLOROPHYTA)1

Thalli of Ulva reticulata Forskaal, Ulva rigida C. Ag., and Ulva pulchra Jaasund were incubated at different concentrations of dissolved CO₂. Incubation at a high CO₂ concentration resulted in decreased oxygen evolution rate and lower affinity for inorganic carbon at high pH conditions, i.e. the ability to use HCO₃^– as a carbon source was reduced. This effect was reversible, and plants regained this HCO₃^– uptake capacity when transferred to air concentrations of CO₂. The phytosynthetic oxygen evolution rate of plants grown at high CO₂ concentration was reduced by high O₂ concentrations, whereas thalli and protoplasts from cultures grown at air concentration were not affected. This is interpreted as a deactivation of the carbon-concentrating mechanism during conditions of high CO₂ resulting in high photorespiration when plants are exposed to high O₂ concentrations. Protoplasts were not affected by high O₂ to the same extent and were not able to utilize HCO₃^– from the medium. The algae were able to grow at very low CO₂ concentrations, but growth was suppressed when an inhibitor of external carbonic anhydrase was present. Assay of carbonic anhydrase activities showed that external and internal CA activities were lower in plants grown at a high CO₂ concentration compared to plants grown at a low concentration of CO₂. Possible mechanisms for HCO₃^– utilization in these Ulva species are discussed.     

Photosynthetic Carbon Metabolism in Photoautotrophic Cell Suspension Cultures Grown at Low and High CO(2)

Photosynthetic carbon metabolism was characterized in four photoautotrophic cell suspension cultures. There was no apparent difference between two soybean (Glycine max) and one cotton (Gossypium hirsutum) cell line which required 5% CO₂ for growth, and a unique cotton cell line that grows at ambient CO₂ (660 microliters per liter). Photosynthetic characteristics in all four lines were more like C₃ mesophyll leaf cells than the cell suspension cultures previously studied. The pattern of ¹⁴C-labeling reflected the high ratio of ribulosebisphosphate carboxylase to phosphoenolpyruvate carboxylase activity and showed that CO₂ fixation occurred primarily by the C₃ pathway. Photorespiration occurred at 330 microliters per liter CO₂, 21% O₂ as indicated by the synthesis of high levels of ¹⁴C-labeled glycine and serine in a pulse-chase experiment and by oxygen inhibition of CO₂ fixation. Short-term CO₂ fixation in the presence and absence of carbonic anhydrase showed CO₂, not HCO₃⁻, to be the main source of inorganic carbon taken up by the low CO₂-requiring cotton cells. The cells did not have a CO₂-concentrating mechanism as indicated by silicone oil centrifugation experiments. Carbonic anhydrase was absent in the low CO₂-requiring cotton cells, present in the high CO₂-requiring soybean cell lines, and absent in other high CO₂ cell lines examined. Thus, the presence of carbonic anhydrase is not an essential requirement for photoautotrophy in cell suspension cultures which grow at either high or low CO₂ concentrations.     

No overall stimulation of soil respiration under mature deciduous forest trees after 7 years of CO2 enrichment

The anthropogenic rise in atmospheric CO₂ is expected to impact carbon (C) fluxes not only at ecosystem level but also at the global scale by altering C cycle processes in soils. At the Swiss Canopy Crane (SCC), we examined how 7 years of free air CO₂ enrichment (FACE) affected soil CO₂ dynamics in a ca. 100‐year‐old mixed deciduous forest. The use of ¹³C‐depleted CO₂ for canopy enrichment allowed us to trace the flow of recently fixed C. In the 7th year of growth at ～550 ppm CO₂, soil respiratory CO₂ consisted of 39% labelled C. During the growing season, soil air CO₂ concentration was significantly enhanced under CO₂‐exposed trees. However, elevated CO₂ failed to stimulate cumulative soil respiration (R_s) over the growing season. We found periodic reductions as well as increases in instantaneous rates of R_s in response to elevated CO₂, depending on soil temperature and soil volumetric water content (VWC; significant three‐way interaction). During wet periods, soil water savings under CO₂‐enriched trees led to excessive VWC (>45%) that suppressed R_s. Elevated CO₂ stimulated R_s only when VWC was ≤40% and concurrent soil temperature was high (>15 °C). Seasonal Q₁₀ estimates of R_s were significantly lower under elevated (Q₁₀=3.30) compared with ambient CO₂ (Q₁₀=3.97). However, this effect disappeared when three consecutive sampling dates of extremely high VWC were disregarded. This suggests that elevated CO₂ affected Q₁₀ mainly indirectly through changes in VWC. Fine root respiration did not differ significantly between treatments but soil microbial biomass (C_mic) increased by 14% under elevated CO₂ (marginally significant). Our findings do not indicate enhanced soil C emissions in such stands under future atmospheric CO₂. It remains to be shown whether C losses via leaching of dissolved organic or inorganic C (DOC, DIC) help to balance the C budget in this forest.     

Chlorophyll a Fluorescence Predicts Total Photosynthetic Electron Flow to CO(2) or NO(3)/NO(2) under Transient Conditions

A model which predicts total photosynthetic electron flow from a linear regression of the relationship between corrected steady-state quantum yield and nonphotochemical quenching (E Weis, JA Berry [1987] Biochem Biophys Acta 894: 198-208) was formulated for N-limited cells of the green alga Selenastrum minutum. Unlike other models based on net CO₂ fixation, our model is based on total photosynthetic electron flow measured as gross O₂ evolution. This allowed for the prediction of total photosynthetic electron flow from water to both CO₂ fixation and NO₃⁻/NO₂⁻ reduction. The linear regression equation predicting electron flow is of the form: J = I · Q_q[0.4777-0.3282 Q_NP] (where J = gross photosynthetic electron flow, I = incident PAR, Q_q = photochemical quenching, Q_NP = nonphotochemical quenching). During steady-state photosynthesis, over a range of irradiance, the model predicted a photosynthetic light saturation curve which was well correlated with that observed. Although developed under steady-state conditions, the model was tested during nonsteady-state photosynthesis induced by transient nitrogen assimilation. The model predicted transient rates of gross O₂ evolution which were in excellent agreement with the rates observed under a variety of conditions regardless of whether CO₂ or NO₃⁻/NO₂⁻ served as the physiological electron acceptor. The fluorescence transients resulting from ammonium and nitrate assimilation are discussed with respect to metabolic demands for reductant and ATP.