Biodegradation of Trichloroacetic Acid in Norway Spruce/Soil System

Trichloroacetic acid (TCA) belongs to secondary atmospheric pollutants affecting the forest health. Distribution of [1,2-¹⁴C]TCA-residues and TCA biodegradation were investigated in 4-year-old nursery-grown trees of Norway spruce [Picea abies (L.) Karst.] in the whole plant/soil system. Radioactivity was monitored in needles, wood, roots and soil as well as in the air. During two weeks of exposure TCA was continuously degraded, especially in the soil. Estimates of radioactivity balance showed loss of radioactivity into the atmosphere in the form of ¹⁴CO₂; unincorporated [1,2-¹⁴C]TCA, chloroform, carbon monoxide and methane were not detected at all. TCA degradation to CO₂ was indicated also in the spruce needles. Moreover, it was found that soil litter contained [1,2-¹⁴C]TCA unavailable to microorganisms.     

Anaerobic C1 Metabolism of the O-Methyl-14C-Labeled Substituent of Vanillate

The O-methyl substituents of aromatic compounds constitute a C₁ growth substrate for a number of taxonomically diverse anaerobic acetogens. In this study, strain TH-001, an O-demethylating obligate anaerobe, was chosen to represent this physiological group, and the carbon flow when cells were grown on O-methyl substituents as a C₁ substrate was determined by ¹⁴C radiotracer techniques. O-[methyl-¹⁴C]vanillate (4-hydroxy-3-methoxy-benzoate) was used as the labeled C₁ substrate. The data showed that for every O-methyl carbon converted to [¹⁴C]acetate, two were oxidized to ¹⁴CO₂. Quantitation of the carbon recovered in the two products, acetate and CO₂, indicated that acetate was formed in part by the fixation of unlabeled CO₂. The specific activity of ¹⁴C in acetate was 70% of that in the O-methyl substrate, suggesting that only one carbon of acetate was derived from the O-methyl group. Thus, it is postulated that the carboxyl carbon of the product acetate is derived from CO₂ and the methyl carbon is derived from the O-methyl substituent of vanillate. The metabolism of O-[methyl-¹⁴C]vanillate by strain TH-001 can be described as follows: 3¹⁴CH₃OC₇H₅O₃ + CO₂ + 4H₂O → ¹⁴CH₃COOH + 2¹⁴CO₂ + 10H⁺ + 10e^- + 3HOC₇H₅O₃.     

Degradation and Fate of Carbon Tetrachloride in Unadapted Methanogenic Granular Sludge

The potential of granular sludge from upflow anaerobic sludge blanket (UASB) reactors for bioremediation of chlorinated pollutants was evaluated by using carbon tetrachloride (CT) as a model compound. Granular sludges cultivated in UASB reactors on methanol, a volatile fatty acid mixture, or sucrose readily degraded CT supplied at a concentration of 1,500 nmol/batch (approximately 10 μM) without any prior exposure to organohalogens. The maximum degradation rate was 1.9 μmol of CT g of volatile suspended solids⁻¹ day⁻¹. The main end products of CT degradation were CO₂ and Cl⁻, and the yields of these end products were 44 and 68%, respectively, of the initial amounts of [¹⁴C]CT and CT-Cl. Lower chlorinated methanes accumulated in minor amounts temporarily. Autoclaved (dead) sludges were capable of degrading CT at rates two- to threefold lower than those for living sludges, indicating that abiotic processes (mediated by cofactors or other sludge components) played an important role in the degradation observed. Reduced components in the autoclaved sludge were vital for CT degradation. A major part (51%) of the CT was converted abiotically to CS₂. The amount of CO₂ produced (23%) was lower and the amount of Cl⁻ produced (86%) was slightly higher with autoclaved sludge than with living sludge. Both living and autoclaved sludges could degrade chloroform. However, only living sludge degraded dichloromethane and methylchloride. These results indicate that reductive dehalogenation, which was mediated better by living sludge than by autoclaved sludge, is only a minor pathway for CT degradation. The main pathway involves substitutive and oxidative dechlorination reactions that lead to the formation of CO₂. Granular sludge, therefore, has outstanding potential for gratuitous dechlorination of CT to safe end products.     

Chloroethene Biodegradation in Sediments at 4°C

Microbial reductive dechlorination of [1,2-¹⁴C]trichloroethene to [¹⁴C]cis-dichloroethene and [¹⁴C]vinyl chloride was observed at 4°C in anoxic microcosms prepared with cold temperature-adapted aquifer and river sediments from Alaska. Microbial anaerobic oxidation of [1,2-¹⁴C]cis-dichloroethene and [1,2-¹⁴C]vinyl chloride to ¹⁴CO₂ also was observed under these conditions.     

Glucose metabolism in anaerobic rice seedlings

More than 80% of the radioactivity from [U-¹⁴C]glucose metabolised by anaerobic rice seedlings or by excised roots or coleoptiles was recovered as ethanol plus CO₂; less than 5% was recovered as water-soluble acidic components. Rates of ¹⁴CO₂ formation from [U-¹⁴C]glucose were similar in roots and coleoptiles in both N₂ and air atmospheres. More ¹⁴CO₂ was formed from [U-¹⁴C]glucose than could be accounted for by ethanolic fermentation, and the specific yields of ¹⁴CO₂ from [6-¹⁴C]glucose and [1-¹⁴C]glucose gave unusually high C-6/C-1 ratios (1.7) in the anaerobic coleoptile. The results may indicate that appreciable pentan synthesis occurs in the anaerobic coleoptile.     

Effect of enriched rhizosphere carbon dioxide on nitrate and ammonium uptake in hydroponically grown tomato plants

Previous reports have indicated positive effects of enriched rhizosphere dissolved inorganic carbon on the growth of salinity-stressed tomato (Lycopersicon esculentum L. Mill. cv. F144) plants. In the present work we tested whether a supply of CO₂ enriched air to the roots of hydroponically grown tomato plants had an effect on nitrogen uptake in these plants. Uptake was followed over periods of 6 to 12 hours and measured as the depletion of nitrogen from the nutrient solution aerated with either ambient or CO₂ enriched air. Enriched rhizosphere CO₂ treatments (5000 μmol mol^-1) increased NO₃ ^- uptake up to 30% at pH 5.8 in hydroponically grown tomato plants compared to control treatments aerated with ambient CO₂ (360 μmol mol^-1). Enriched rhizosphere CO₂ treatments had no effect on NH₃ ⁺ uptake. Acetazolamide, an inhibitor of apoplastic carbonic anhydrase, increased NO₃ ^- uptake in ambient rhizosphere CO₂ treatments, but had no effect on NO₃ ^- uptake in enriched rhizosphere CO₂ treatments. Ethoxyzolamide, an inhibitor of both cytoplasmic and extracellular carbonic anhydrase, decreased NO₃ ^- uptake in ambient rhizosphere CO₂ treatments. In contrast, a CO₂ enriched rhizosphere increased NO₃ ^- uptake with ethoxyzolamide, although not to the same extent as in plants without ethoxyzolamide. It is suggested that a supply of enriched CO₂ to the rhizosphere influenced NO₃ ^- uptake through the formation of increased amounts of HCO₃ ^- in the cytosol. This revised version was published online in June 2006 with corrections to the Cover Date.     

The effect of methionine on the metabolism of serine and glycine in vitamin B-12-deficient rats

The effect of methionine supplementation on glycine and serine metabolism was studied in vitamin B-12-deficient rats which received only 0.2% methionine in the diet. In the perfused liver, incorporation of the C-2 of glycine to the C-3 of serine was increased by addition of methionine to the perfusate. The oxidation of [1-¹⁴C]glycine to ¹⁴CO₂ was however depressed. Unlike methionine, glycine did not have any significant effect on the liver folate coenzyme distribution. Oxidation of [3-¹⁴C]serine to ¹⁴CO₂ both in vivo and in perfused liver was increased by methionine. A major portion of the C-3 radioactivity however was recovered in glucose. Data presented indicate that the rate of oxidation of [2-¹⁴C]histidine to ¹⁴CO₂ is more sensitive indicator of folate deficiency than the rate of oxidation of [3-¹⁴C] serine to ¹⁴CO₂ although both are presumably tetrahydrofolate dependent.     

Intermediary Metabolism of Organic Matter in the Sediments of a Eutrophic Lake

The rates, products, and controls of the metabolism of fermentation intermediates in the sediments of a eutrophic lake were examined. ¹⁴C-fatty acids were directly injected into sediment subcores for turnover rate measurements. The highest rates of acetate turnover were in surface sediments (0- to 2-cm depth). Methane was the dominant product of acetate metabolism at all depths. Simultaneous measurements of acetate, propionate, and lactate turnover in surface sediments gave turnover rates of 159, 20, and 3 μM/h, respectively. [2-¹⁴C]propionate and [U-¹⁴C]lactate were metabolized to [¹⁴C]acetate, ¹⁴CO₂, and ¹⁴CH₄. [¹⁴C]formate was completely converted to ¹⁴CO₂ in less than 1 min. Inhibition of methanogenesis with chloroform resulted in an immediate accumulation of volatile fatty acids and hydrogen. Hydrogen inhibited the metabolism of C₃-C₅ volatile fatty acids. The rates of fatty acid production were estimated from the rates of fatty acid accumulation in the presence of chloroform or hydrogen. The mean molar rates of production were acetate, 82%; propionate, 13%; butyrates, 2%; and valerates, 3%. A working model for carbon and electron flow is presented which illustrates that fermentation and methanogenesis are the predominate steps in carbon flow and that there is a close interaction between fermentative bacteria, acetogenic hydrogen-producing bacteria, and methanogens.     

Oxidative metabolism of carbon disulphide by the rat. Effect of treatments which modify the liver toxicity of carbon disulphide

The liver toxicity of a standard dose of CS₂ was increased by phenobarbitone pre-treatment and by fasting and decreased by prior administration of a small dose of CS₂; it was less marked in female than in male rats.Rats were given an intraperitoneal dose of ¹⁴CS₂ to study its in vivo conversion to ¹⁴CO₂ under conditions which modify the liver toxicity of CS₂. The radioactive CO₂ exhaled was found to be linearly related to the amount of cytochrome P-450 present in the liver at the time of administering ¹⁴CS₂; it was also found to be related to the severity of the toxic changes caused in the liver, but here the relationship was not linear and was more complex.When liver microsomes were incubated with CS₂, a marked loss of cytochrome P-450 was observed only when NADPH was present. In contrast with the loss of the cytochrome observed with NADPH alone, which is associated with the formation of malonaldehyde, that due to CS₂ still occurred in the presence of EDTA, even though the formation of malonaldehyde was largely prevented.These results are compatible with the hypothesis that CS₂ requires metabolism for its liver toxicity.     

Humic Acids as Electron Acceptors for Anaerobic Microbial Oxidation of Vinyl Chloride and Dichloroethene

Anaerobic oxidation of [1,2-¹⁴C]vinyl chloride and [1,2-¹⁴C]dichloroethene to ¹⁴CO₂ under humic acid-reducing conditions was demonstrated. The results indicate that waterborne contaminants can be oxidized by using humic acid compounds as electron acceptors and suggest that natural aquatic systems have a much larger capacity for contaminant oxidation than previously thought.     

Terpene Biosynthesis in Cell-free Extracts and Excised Shoots from Wedgwood Iris

Excised shoots and cell-free extracts prepared from Wedgwood iris (Iris hollandica Hoog. “Wedgwood”) shoots metabolized ¹⁴C-labeled mevalonic acid (MVA). By using cell-free extracts, the ¹⁴C from MVA-1-¹⁴C was recovered as ¹⁴CO₂, while that from MVA-2-¹⁴C was recovered as neutral terpenes, acid-hydrolyzable terpenes, or ¹⁴CO₂. Also, under optimal incubation conditions, 12.8 nanomoles R-MVA-2-¹⁴C was incorporated into neutral terpenes per milligram fresh weight per hour. In contrast, excised shoots incorporated only 0.58 nanomoles R-MVA-2-¹⁴C per mg fresh weight per hour. Labeled products identified from the cell-free system were squalene, farnesol, geranylgeraniol, and compounds that are converted to farnesol and geranylgeraniol after alkaline hydrolysis. Squalene and a 4,4-dimethylsterol were identified as products from excised shoots but not the terpene alcohols or the alkaline-hydrolyzable compounds.     

The Mechanism of Acetate and Pyruvate Oxidation by Trypanosoma cruzi

The epimastigote or culture form of Trypanosoma cruzi oxidizes [3-¹⁴C] pyruvate and [2-¹⁴C] acetate to ¹⁴CO₂ without an apparent increase in overall respiration. This oxidation takes place through the tricarboxylic acid cycle as shown by (a) the incorporation of substrate ¹⁴C into cycle intermediates; (b) the earlier liberation of acetate carboxyl carbon as CO₂; and (c) the characteristic intramolecular distribution of pyruvate and acetate carbon atoms in the skeletal carbon of aspartic and glutamic acids. Upon oxidation of [3-¹⁴C] pyruvate and [2-¹⁴C] acetate, two of the products, alanine and glutamic acid, are found to account for more than 50% of incorporated ¹⁴C; labeling of alanine predominates with [3-¹⁴C] pyruvate while labeling of glutamic acid predominates with [2-¹⁴C] acetate. Using [1- or 6-¹⁴C] glucose as substrate, the pattern of ¹⁴C distribution in soluble metabolites closely resembles that obtained with [3-¹⁴C] pyruvate, in accordance with the joint operation of the Embden-Meyerhof pathway and Krebs cycle. The cycle operation depends on electron transport through the mitochondrial respiratory chain, since antimycin A, at a relatively low concentration, inhibits the oxidation of [2-¹⁴C] acetate to ¹⁴CO₂, to the same extent as the parasite respiration. Though functional in T. cruzi epimastigotes, the oxidative role of the Krebs’ cycle is apparently limited by the absence of an efficient oxidative apparatus. The cycle operation does, however, constitute an important source of skeletal carbon for the biosynthesis of amino acids and can contribute to the process of glycogenesis.     

Evidence for arginine as the endogenous precursor of necines in heliotropium

In pyrrolizidine alkaloid-bearing Heliotropium angiospermum and H. indicum shoots exposed, in the light, to ¹⁴C-labeled CO₂ for 44 hours, the incorporation of ¹⁴C into 1,2-epoxy-1-hydroxymethylpyrrolizidine and retronecine amounted to 0.23 and 0.15%, respectively, of the total carbon assimilated. Treatment of the shoots with α-dl-difluoromethylornithine, the specific ornithine decarboxylase inhibitor, at 1 to 2 millimolar had no effect on ¹⁴C incorporation into the necines. In contrast, α-dl-difluoromethylarginine, the specific arginine decarboxylase inhibitor, prevented the incorporation of ¹⁴C into the necines of both species; the inhibitor did not affect the absolute incorporation of ¹⁴C from exogenous [1,4-¹⁴C] putrescine in either species. Thus, arginine is the only apparent endogenous precursor of the putrescine channeled into pyrrolizidines, at least in these two Heliotropium species that exhibited a relatively much higher in vitro activity of arginine decarboxylase than of ornithine decarboxylase. However, within 28 hours after administration, not only exogenous l-[5-¹⁴C]arginine, but also exogenous l-[5-¹⁴C]ornithine exhibited significant incorporation of their label into the necines, incorporation that could be partially prevented by both inhibitors. Neither inhibitor affected the rates of ¹⁴C-labeled CO₂ assimilation, transformation of labeled assimilates into ethanol-insoluble compounds, or the very high degree of conversion of the introduced amino acids into other compounds. Methodology related to alkaloid biosynthetic studies is discussed.     

Titles of related papers in other sections

Culture of Trypanosoma cruzi (Tulahuen strain) in the presence of ethidium bromide (1–20 μg/ml) resulted in dyskinetoplasty and inhibition of growth, to an extent depending on the dye concentration and the medium composition. The ethidium bromide-induced dyskinetoplasty caused a decrease of (a) the cytochrome content of epimastigotes (a,a₃ and b species); (b) the rate of respiration (endogenous or supported by D-glucose); and (c) the rate of production of ¹⁴CO₂ from [2-¹⁴C]acetate and [1-¹⁴C]glucose. [2-¹⁴C]Acetate oxidation to ¹⁴CO₂ was affected by dyskinetoplasty more than [1-¹⁴C]glucose oxidation, particularly at the exponential growth phase. With dyskinetoplastic epimastigotes, diminution of ¹⁴CO₂ production from [2-¹⁴C]acetate largely exceeded that of oxygen uptake, while with [1-¹⁴C]glucose, ¹⁴CO₂production and respiration were affected to about the same extent. Dyskinetoplasty also decreased the incorporation of [2-¹⁴C]acetate carbon into intermediates of the tricarboxylic acid cycle and related amino acids, and modified the distribution pattern of ¹⁴C in accordance with the decrease of respiration. Reduction of cytochrome content of epimastigotes by restriction of heme compounds during growth decreased ¹⁴CO₂ production from [2-¹⁴C]acetate, like the ethidium-induced dyskinetoplasty. The same occurred after inhibition of electron transfer by antimycin and cyanide, though to a much more significant extent, thus confirming the functional association of electron transport at the mitochondrial cytochrome system of T. cruzi and the enzymatic reactions of the tricarboxylic acid cycle.     

Influence of carbon availability on the production of NO, N2O, N2 and CO2 by soil cores during anaerobic incubation

Net productions of permanent soil atmosphere gases (N₂, CO₂, O₂) and temporary gases (N₂O, NO) were monitored in soil cores using a non-interfering, fully automated measuring technique allowing highly time resolved measurements over prolonged periods. The influence of changes in available organic carbon on CO₂, N₂O, NO and N₂ production was studied by changing the soil carbon content through aerobic preincubations of different length, up to 21 days.The aerobic preincubation caused an increase in NO₃ ^- concentration and a decrease in available carbon content. Available carbon content dominated both CO₂ and total N gas (N₂+N₂O+NO) production during anaerobiosis. Both CO₂ and total N gas production rates decreased with increasing length of the previous aerobic preincubation, this in spite of the higher initial NO₃ ^- concentration.Total denitrification rates were closely related to the anaerobic CO₂ production rates. No relation was found between water soluble carbon content and total denitrification. The N₂O/N₂ ratio could be explained by an interaction of carbon availability, NO₃ ^- concentration and enzyme status. Net N₂O consumption was monitored. The balance between cumulative total N gas production and NO₃ ^- consumption varied according to the different treatments. Cumulative N₂O production exceeded cumulative N₂ production for 0 up to 5 days.     

Catabolism of 5-Aminolevulinic Acid to CO(2) by Etiolated Barley Leaves

The in vivo oxidation of the C₄ and C₅ of 5-aminolevulinic acid (ALA) to CO₂ has been studied in etiolated barley (Hordeum vulgare L. var. Larker) leaves in darkness. The rate of ¹⁴CO₂ evolution from leaves fed [4-¹⁴C]ALA is strongly inhibited by aminooxyacetate, anaerobiosis, and malonate. The rate of ¹⁴CO₂ evolution from leaves fed [5-¹⁴C]ALA is also inhibited by these treatments but to a lesser extent. These results suggest that (a) one step in ALA catabolism is a transamination reaction and (b) the C₄ is oxidized to CO₂ via the tricarboxylic acid cycle to a greater extent than is the C₅.     

In vitro substrate utilization for lipid synthesis in liver explants from hyperthyroid chickens

• 1.1. Indian River male broiler chickens growing from 7 to 28 days of age were fed diets containing 12, 18, 24 and 30% protein + 0 or 1 mg triiodothyronine (T₃)/kg of diet to study energetic costs of lipogenesis and the use of various substrates for in vitro lipogenesis.
• 2.2. De novo lipid and CO₂ production were determined in the presence of [1-¹⁴C]pyruvate, [2-¹⁴q]pyruvate, [3-¹⁴C]pyruvate, [2-¹⁴C]acetate and [U-¹⁴C]alanine.
• 3.3. Oxygen consumption was determined in mitochondrial preparations to estimate the energetic costs in expiants synthesizing lipid.
• 4.4. Radiolabeled CO₂ derived from [1-¹⁴C]pyruvate was used as an estimate of coenzyme A availability in liver expiants. Lipids derived from [2-¹⁴C]pyruvate, [2-¹⁴C]acetate and [U-¹⁴C]alanine estimate relative substrate efficiency.
• 5.5. Labeled CO₂ production from [1-¹⁴C]pyruvate was greatest in that group fed a 12% protein diet and least in the group fed a 30% protein diet.
• 6.6. In addition, T₃ increased CO₂ production from [1-¹⁴C]pyruvate.
• 7.7. The production of ¹⁴CO₂ from the second carbon of pyruvate or acetate was increased by T₃.
• 8.8. The low-protein diet (12% protein) increased (P <0.05) lipogenesis.
• 9.9. Adding T₃ to the diets decreased carbon flux into lipid from all substrates, but increased CO₂ production from all substrates without changing stage 3 and 4 respiration rates in mitochondrial preparations.
• 10.10. These observations imply that coenzyme A availability may have regulated de novo lipogenesis in the present study.
• 11.11. It was also concluded that previously noted effects of T₃ on intermediary metabolism may involve metabolic pathways that do not involve changes in mitochondrial function.

     

Isotopic studies of carbohydrate metabolism during basidiospore germination in Schizophyllum commune

Summary The metabolism and fate of specifically labeled glucose-¹⁴C were compared to mannitol-l-¹⁴C and arabitol-l-¹⁴C during basidiospore germination of Schizophyllum commune on glucose-asparagine minimal broth. Glucose-l-¹⁴C metabolism led to more ¹⁴CO₂ evolution than glucose-6-¹⁴C in spores and the former activity increased upon germination. Liberation of ¹⁴CO₂ from glucose-3,4-¹⁴C increased at 8 h to 12 h of germination and exceeded the amount of radioactive ¹⁴CO₂ released from glucose-1-¹⁴C. The ¹⁴CO₂ released from glucose-2-¹⁴C increased continually during germination while only minor changes in ¹⁴CO₂ evolution occurred with glucose-6-¹⁴C. Unlabeled ethanol (0.25 M) inhibited ¹⁴CO₂ evolution with glucose-3,4-¹⁴C and ungerminated spores and this inhibition disappeared upon germination.More ¹⁴CO₂ was evolved from labeled glucose during germination and less radioactivity became associated with cellular material. Of the latter, alcohol-soluble extracts of spores or germlings contained mainly radioactive trehalose, less mannitol and little or no labeled arabitol, and this decreased upon germination. Germlings also converted more radioactive glucose-¹⁴C into KOH-insoluble material and KOH-soluble components. Spores or germlings converted arabitol-1-¹⁴C primarily into trehalose and this was not the case for mannitol-1-¹⁴C.     

Recycling of carbon in the oxidative pentose phosphate pathway in non-photosynthetic plastids

Recycling of carbon in the oxidative pentose phosphate pathway (OPPP) of intact pea root plastids has been studied. The synthesis of dihydroxyacetone phosphate (DHAP) and evolution of CO₂ was followed in relation to nitrite reduction. A close coupling was observed between all three measured fluxes which were linear for up to 60 min and dependent upon the integrity of the plastids. However, the quantitative relationship between 1-¹⁴CO₂ evolution from glucose 6-phosphate and nitrite reduction varied with available hexose phosphate concentration. When 10 mM glucose 6-phosphate was supplied to intact plastids a stoichiometry of 1.35 was observed between ¹⁴CO₂ evolution and nitrite reduction. As exogenous glucose 6-phosphate was decreased this value fell, becoming 0.47 in the presence of 0.2 mM glucose 6-phosphate, indicative of considerable recycling of carbon. This conclusion was reinforced when using [2-¹⁴C]glucose-6-phosphate. The measured release of 2-¹⁴CO₂ was consistent with the data for 1-¹⁴CO₂, suggesting complete recycling of carbon in the OPPP. Ribose 5-phosphate was also able to support nitrite reduction and DHAP production. A stoichiometry of 2 NO ₂ ^? reduced: 1 DHAP synthesised was observed at concentrations of 1 mM ribose 5-phosphate or less. At concentrations of ribose 5-phosphate greater than 1 mM this stoichiometry was lost as a result of enhanced DHAP synthesis without further increase in nitrite reduction. It is suggested that this decoupling from nitrite reduction is a function of excess substrate entering directly into the non-oxidative reactions of the OPPP, and may be useful when the demand for OPPP products is not linked to the demand for reductant. The significance of recycling in the OPPP is discussed in relation to the coordination of nitrate assimilation with carbohydrate oxidation in roots and with the utilisation of carbohydrate by other pathways within plastids.     

Carbon balance and water use efficiency of frequently cut Lolium perenne L. swards at elevated carbon dioxide

The impact of doubled atmospheric [CO₂] on the carbon balance of regularly cut Lolium perenne L. swards was studied for two years under semi-field conditions in the Wageningen Rhizolab. CO₂ and H₂O vapour exchange rates of the swards were measured continuously for two years in transparent enclosures. The light utilization efficiencies of the swards ranged between 1.5 g CO₂ MJ^–1 global radiation (high light, ambient [CO₂]) and 2.8 g CO₂ MJ^–1 (low light, doubled [CO₂]). The above-ground net primary productivity (NPP) in the enclosures was greater by 29% in 1994 and 43% in 1995 in the doubled [CO₂] treatments, but only 20% and 25% more carbon was recovered in the periodical cuts. Thus, NPP increased significantly more than did the harvested above-ground biomass. The positive [CO₂] effect on net carbon assimilation is therefore associated with a preferential allocation of extra carbon to the roots and soil. In addition to higher canopy photosynthesis and leaf elongation rates, a small part of the positive [CO₂] effects on NPP could be attributed to a decrease of the specific respiration of the shoots. On a canopy basis however, respiration was equal or slightly higher at doubled [CO₂] due to the higher amount of standing biomass. Comparison of NPP and carbon recovered in different harvests showed that allocation to roots and soil was highest in spring, it was low in early summer and increased again in late summer and autumn. The total gross amount of carbon partitioned to the roots and soil during the two year period was 57% more at doubled [CO₂]. The total amount of carbon that was sequestered in the soil after subtraction of the respiratory losses was 458 g m^–2 and 779 g m^–2 in the ambient and doubled [CO₂] treatments, respectively. The average water use efficiency (WUE) of the swards was increased by a factor 1.5 at doubled [CO₂]. Both WUE and its positive interaction with [CO₂] varied between years and were positively correlated with global irradiance. At doubled [CO₂], the higher WUE was fully compensated for by a higher leaf area index. Therefore, total transpiration on a canopy basis was equal for the ambient and the doubled [CO₂] concentrations in both years.