Carbon assimilation pathways in sulfate reducing bacteria. Formate,carbon dioxide,carbon monoxide,and acetate assimilation by Desulfovibrio baarsii

Desulfovibrio baarsii is a sulfate reducing bacterium, which can grown on formate plus sulfate as sole energy source and formate and CO₂ as sole carbon sources. It is shown by ¹⁴C labelling studies that more than 60% of the cell carbon is derived from CO₂ and the rest from formate. The cells thus grow autotrophically. Labelling studies with [¹⁴C]acetate, ¹⁴CO and [¹⁴C]formate indicate that CO₂ fixation does not proceed via the Calvin cycle. The labelling patterns of alanine, aspartate, glutamate, and glucosamine indicate that acetate (or activated acetic acid) is an early intermediate in formate and CO₂ assimilation; the methyl group of acetate is derived from formate, and the carboxyl group from CO₂ via CO; pyruvate is formed from acetyl-CoA by reductive carboxylation. The capacity to synthesize an acetate unit from two C₁-compounds obviously distinguishes D. baarsii from those Desulfovibrio species, which require acetate as a carbon source in addition to CO₂.     

Autotrophic synthesis of activated acetic acid from two CO2 inMethanobacterium thermoautotrophicum

An in vitro system of autotropic synthesis of activated acetic acid from¹⁴CO₂ inMethanobacterium thermoautotrophicum was developed.

1. A recognized¹⁴CO₂-fixation product in vitro was activated [¹⁴C] acetic acid. It could be trapped enzymatically into citrate and released again as [¹⁴C] acetate by citrate synthase and citrate lyase, respectively.
2. The synthesis of both activated acetic acid and methane from CO₂ proceeded in parallel under a variety of conditions. Both of these processes were stimulated greatly and to the same extent by the addition of methyl coenzyme M to the assay.
3. Various inhibitors of methanogenesis tested also inhibited acetate synthesis, e.g. CH₂Cl₂, CHCl₃, CCl₄, N₂O, and bromoethane sulfonic acid. Cyanide specifically inhibited the synthesis of activated acetic acid, whereas methane formation was unaffected. Cyanide inhibition was relieved by adding CO, whereas the inhibition by the other compounds was not.

The data suggest: The product studied in vitro was acetyl CoA. Its synthesis involves intermediates of CO₂ reduction to methane. In addition, a cyanide-sensitive reaction is required which does not participate in CO₂ reduction to methane.     

Acetate formation from CO and CO2 by cell extracts of Peptostreptococcus productus (strain Marburg)

Cell extracts of Peptostreptococcus productus (strain Marburg) obtained from CO grown cells mediated the synthesis of acetate from CO plus CO₂ at rates of 50 nmol/min × mg of cell protein. ¹⁴CO was specifically incorporated into C₁ of acetate. No label exchange occurred between ¹⁴C₁ of acetyl-CoA and CO, indicating that ¹⁴CO incorporation into acetate was by net synthesis rather than by an exchange reaction. In acetate synthesis from CO plus CO₂ the latter substrate could be replaced to some extent by formate or methyl tetrahydrofolate as the methyl donor. The methyl group of methyl cobalamin was incorporated into acetate ony at very low activities. The cell extracts contained high levels of enzyme activities involved in acetate or cell carbon synthesis from CO₂. The following enzymic activities were detected: CO: methyl viologen oxidoreductase, formate dehydrogenase, formyl tetrahydrofolate synthetase, methenyl tetrahydrofolate cyclohydrolase, methylene tetrahydrofolate dehydrogenase, methylene tetrahydrofolate reductase, phosphate acetyltransferase, acetate kinase, hydrogenase, NADPH: benzyl viologen oxidoreductase, and pyruvate synthase. Some kinetic and other properties were studied.     

Pathways of methanol conversion in a thermophilic anaerobic (55 °C) sludge consortium

The pathway of methanol conversion by a thermophilic anaerobic consortium was elucidated by recording the fate of carbon in the presence and absence of bicarbonate and specific inhibitors. Results indicated that about 50% of methanol was directly converted to methane by the methylotrophic methanogens and 50% via the intermediates H₂/CO₂ and acetate. The deprivation of inorganic carbon species [(HCO₃^–+CO₂)] in a phosphate-buffered system reduced the rate of methanol conversion. This suggests that bicarbonate is required as an electron (H₂) sink and as a co-substrate for the efficient and complete removal of the chemical oxygen demand. Nuclear magnetic resonance spectroscopy was used to investigate the route of methanol conversion to acetate in bicarbonate-sufficient and bicarbonate-depleted environments. The proportions of [1,2-¹³C]acetate, [1-¹³C]acetate and [2-¹³C]acetate were determined. Methanol was preferentially incorporated into the methyl group of acetate, whereas HCO₃^– was the preferred source of the carboxyl group. A small amount of the added H¹³CO₃^– was reduced to form the methyl group of acetate and a small amount of the added ¹³CH₃OH was oxidised and found in the carboxyl group of acetate when ¹³CH₃OH was converted. The recovery of [¹³C]carboxyl groups in acetate from ¹³CH₃OH was enhanced in bicarbonate-deprived medium. The small amount of label incorporated in the carboxyl group of acetate when ¹³CH₃OH was converted in the presence of bromoethanesulfonic acid indicates that methanol can be oxidised to CO₂ prior to acetate formation. These results indicate that methanol is converted through a common pathway (acetyl-CoA), being on the one hand reduced to the methyl group of acetate and on the other hand oxidised to CO₂, with CO₂ being incorporated into the carboxyl group of acetate.     

Mesophilic syntrophic acetate oxidation during methane formation by a triculture at high ammonium concentration

In a mesophilic (37°C) triculture at a high ammonium concentration and pH8, methanogenesis from acetate occurred via syntrophic acetate oxidation. Studies with ¹⁴C-labelled substrates showed that the amount of labelled methane formed from 1-¹⁴C-labelled acetate was equal to that formed from 2-¹⁴C-labelled acetate. Labelled methane was also formed from H¹⁴CO₃ ^-. These results clearly showed that both the methyl and carboxyl groups of acetate were oxidized to CO₂ and that CO₂ was reduced to CH₄ through hydrogenotrophic methanogenesis. During growth of the triculture, a significant isotopic exchange between the carboxyl group of acetate and bicarbonate occurred. As a result, there was a decrease in the specific activity of 1-¹⁴C-acetate, and the production of ¹⁴CO₂ was slightly higher from 1-¹⁴C- than from 2-¹⁴C-acetate. For each mole acetate degraded, 0.94 mol methane was formed; 9.2 mmol acetate was metabolized during the 294 days of incubation.     

Acetate synthesis from 2 CO2 in acetogenic bacteria: is carbon monoxide an intermediate?

Cultures of Acetobacterium woodii and Clostridium thermoaceticum growing on fructose or glucose, respectively, were found to produce small, but significant amounts of carbon monoxide. In the gas phase of the cultures up to 53 ppm CO were determined. The carbon monoxide production was completely inhibited by 1 mM cyanide. Cultures and cell suspensions of both acetogens incorporated ¹⁴CO specifically into the carboxyl group of acetate. This CO fixation into C₁ of acetate was unaffected by cyanide (1 mM). The findings are taken to indicate that CO (in a bound form) is the physiological precursor of the C₁ of acetate in acetate synthesis from CO₂. The cyanide inhibition experiments support the hypothesis that the cyanide-sensitive carbon monoxide dehydrogenase may serve to reduce CO₂ to CO rather than to incorporate the carbonyl into C₁ of acetate.     

Use of Carbon Isotopes to Estimate Incorporation of Added CO(2) by Greenhouse-Grown Tomato Plants

A method is presented which uses the ¹³C and ¹⁴C isotope abundance in CO₂-enriched greenhouse crops to determine the percentage of plant organic carbon derived from artificially added CO₂. In a greenhouse experiment with CO₂ concentrations elevated to 1100 ± 100 microliters per liter during part of the daylight hours and maintained at normal atmospheric concentrations (340 microliters per liter) during the rest of the time, it was shown by ¹⁴C analysis that between 41% and 42% of the carbon in tomato plants (Lycopersicon esculentum var 4884) came from the artificially added CO₂. Similar results were obtained from ¹³C analyses when the CO₂ pressure-dependent isotope separation was taken into account.     

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.     

One-carbon metabolism in methanogens: evidence for synthesis of a two-carbon cellular intermediate and unification of catabolism and anabolism in Methanosarcina barkeri

One-carbon metabolic transformations associated with cell carbon synthesis and methanogenesis were analyzed by long- and short-term ¹⁴CH₃OH or ¹⁴CO₂ incorporation studies during growth and by cell suspensions. ¹⁴CH₃OH and ¹⁴CO₂ were equivalently incorporated into the major cellular components (i.e., lipids, proteins, and nucleic acids) during growth on H₂-CO₂-methanol. ¹⁴CH₃OH was selectively incorporated into the C-3 of alanine with decreased amounts fixed in the C-1 and C-2 positions, whereas ¹⁴CO₂ was selectively incorporated into the C₁ moiety with decreasing amounts assimilated into the C-2 and C-3 atoms. Notably, ¹⁴CH₄ and [3-¹⁴C]alanine synthesized from ¹⁴CH₃OH during growth shared a common specific activity distinct from that of CO₂ or methanol. Cell suspensions synthesized acetate and alanine from ¹⁴CO₂. The addition of iodopropane inhibited acetate synthesis but did not decrease the amount of ¹⁴CH₃OH or ¹⁴CO₂ fixed into one-carbon carriers (i.e., methyl coenzyme M or carboxydihydromethanopterin). Carboxydihydromethanopterin was only labeled from ¹⁴CH₃OH in the absence of hydrogen. Cell extracts catalyzed the synthesis of acetate from ¹⁴CO (~1 nmol/min per mg of protein) and an isotopic exchange between CO₂ or CO and the C-1 of pyruvate. Acetate synthesis from ¹⁴CO was stimulated by methyl B₁₂ but not by methyl tetrahydrofolate or methyl coenzyme M. Methyl coenzyme M and coenzyme M were inhibitory to acetate synthesis. Cell extracts contained high levels of phosphotransacetylase (>6 μmol/min per mg of protein) and acetate kinase (>0.14 μmol/min per mg of protein). It was not possible to distinguish between acetate and acetyl coenzyme A as the immediate product of two-carbon synthesis with the methods employed.     

Acetate metabolism inMethanosarcina barkeri

Methanosarcina barkeri was grown by acetate fermentation in complex medium (N₂ gas phase). The molar growth yield was 1.6–1.9 g cells/mol methane formed. Under these conditions 63–82% of the methane produced byMethanosarcina strains was derived from the methyl carbon of acetate, indicating that some methane was derived from other media components. Growth was not demonstrated in complex media lacking acetate or mineral acetate medium containing acetate but lacking H₂/CO₂, methanol, or trypticase and yeast extract. Acetate metabolism byM. barkeri strain MS was further exmined in mineral acetate medium containing H₂/CO₂ and/or methanol, but lacking cysteine. Under these conditions, more methane was derived from the methyl carbon of acetate than from the carboxyl carbon. Methanogenesis from the methyl group increased with increasing acetate concentration. The methyl carbon contributed up to 42% of the methane formed with H₂/CO₂ and up to 5% with methanol. Methanol stimulated the oxidation of the methyl group of acetate to CO₂. The average rates of methane formation from acetate were 1.3 nomol/min ·ml/culture (0.04mg² cell dry weight) in defined media (gas phase H₂/CO₂) and complex media (gas phase N₂). Acetate contributed up to 60% of cell carbon formed under the growth conditions examined. Similar quantities of cell carbon were derived from the methyl and carboxyl carbons of acetate, suggesting incorporation of this compound as a two-carbon unit. Incorporated acetate was not preferentially localized in lipid material, as 70% of the incorporated acetate was found in the wall and protein cell fractions. Acetate catabolism was stimulated by pregrowing of cultures in media containing acetate, while acetate anabolism was not influenced. The results are discussed in terms of the differences between the mechanisms of acetate catabolism and anabolism.Abbreviations CH₃-S-CoM methyl coenzyme M - TCA trichloroacetic acid - CoM coenzyme M (2-mercaptoethane sulfonic acid) - E^o standard potential change (pH 7) - F₄₂₀ Factor 420, a low redox electron carrier - G^o standard free energy change (pH 7) - kJ kilojoules (=0.24 kilocalories) - PBBW Weimer's phosphate-buffered basal medium - X unknown C₁ carrier     

Metabolism of homoacetogens

Homoacetogenic bacteria are strictly anaerobic microorganisms that catalyze the formation of acetate from C₁ units in their energy metabolism. Most of these organisms are able to grow at the expense of hydrogen plus CO₂ as the sole energy source. Hydrogen then serves as the electron donor for CO₂ reduction to acetate. The methyl group of acetate is formed from CO₂ via formate and reduced C₁ intermediates bound to tetrahydrofolate. The carboxyl group is derived from carbon monoxide, which is synthesized from CO₂ by carbon monoxide dehydrogenase. The latter enzyme also catalyzes the formation of acetyl-CoA from the methyl group plus CO. Acetyl-CoA is then converted either to acetate in the catabolism or to cell carbon in the anabolism of the bacteria. The homoacetogens are very versatile anaerobes, which convert a variety of different substrates to acetate as the major end product.     

The use of acetic acid as a source of carbon by cultured Chondrus crispus (Gigartinales,Rhodophyta) stackhouse

When growing seaweeds in tanks, pH and carbon source supply have to be controlled in order to maximize photosynthesis. pH can be controlled either by adding various inorganic acids which requires the extra addition of carbon, or by combining pH control and carbon source with for instance CO₂ or an organic acid such as acetic acid (CH₃COOH). We have found comparable productivity of Chondrus using CO₂ or CH₃COOH in tank culture with an increase in production of 25.0 and 27.5%, respectively, over the control. Laboratory experiments showed that acetic acid enabled us to maintain a steady state total inorganic carbon in the medium, the algae displaying an active photosynthesis. Experiments using labelled acetic acid CH₃-¹⁴COOH showed that the acid molecule or at least the -¹⁴COOH group is taken up by Chondrus although the mechanism was not elucidated. Preliminary extractions with hot ethanol showed that 67.9% of the label was solubilized from labelled tissue. Few counts were found in the carrageenans (< 1 %) and between 25.6 and 45.1% were found in the cellulosic residues. Acetic acid is suggested as an interesting means of regulating the pH and adding carbon in macrophyte culture.     

Dark metabolism of carbon monoxide in lettuce leaf discs

In the dark, leaf tissue of crisphead lettuce (Lactuca sativa L.) metabolized ¹⁴CO to ¹⁴CO₂ and acid-stable products. Tissue incubated at 2.5°C for 3.5 hours and 48 hours converted about 1% and 17%, respectively, of the applied ¹⁴CO to ¹⁴CO₂, and incorporated about 0.04% and 0.6% of the ¹⁴C in acid-stable products. Examination of soluble acid-stable products from ¹⁴CO and ¹⁴CO₂-treated leaf tissue revealed that the labeling patterns of both treatments were identical during the 3.5-hour and the 48-hour incubation periods. Malate, citrate, and aspartate together comprised 70% or more of the soluble radioactivity from both treatments. Incorporation of radioactivity from CO into soluble acid-stable products during a 3-hour incubation period at 2.5°C was inhibited 90% by adding 3% nonradioactive CO₂. These results indicate that in head lettuce in the dark ¹⁴CO is metabolized primarily to ¹⁴CO₂ which is the precursor of acid-stable products. In leaf discs at 2.5°C, the apparent K_m for CO oxidation to CO₂ was 5.3 microliters per liter and the V_max was 9.7 nanoliters per gram per hour. The mitochondrial fraction of the leaf homogenate was the most active fraction to oxidize CO to CO₂, and this activity was heat-labile and cyanide-sensitive.     

Influence of pH on Terminal Carbon Metabolism in Anoxic Sediments from a Mildly Acidic Lake

The carbon and electron flow pathways and the bacterial populations responsible for transformation of H₂-CO₂, formate, methanol, methylamine, acetate, glycine, ethanol, and lactate were examined in sediments collected from Knaack Lake, Wis. The sediments were 60% organic matter (pH 6.2) and did not display detectable sulfate-reducing activity, but they contained the following average concentration (in micromoles per liter of sediment) of metabolites and end products: sulfide, 10; methane, 1,540; CO₂, 3,950; formate, 25; acetate, 157; ethanol, 174; and lactate, 138. Methane was produced predominately from acetate, and only 4% of the total CH₄ was derived from CO₂. Methanogenesis was limited by low environmental temperature and sulfide levels and more importantly by low pH. Increasing in vitro pH to neutral values enhanced total methane production rates and the percentage of CO₂ transformed to methane but did not alter the amount of ¹⁴CO₂ produced from [2-¹⁴C]acetate (~24%). Analysis of both carbon transformation parameters with ¹⁴C-labeled tracers and bacterial trophic group enumerations indicated that methanogenesis from acetate and both heterolactic- and acetic acid-producing fermentations were important to the anaerobic digestion process.     

Fermentative Metabolism of Chlamydomonas reinhardii: III. Photoassimilation of Acetate

The anaerobic photodissimilation of acetate by Chlamydomonas reinhardii F-60 adapted to a hydrogen metabolism was studied utilizing manometric and isotopic techniques. The rate of photoanaerobic (N₂) acetate uptake was approximately 20 μmoles per milligram chlorophyll per hour or one-half that of the photoaerobic (air) rate. Under N₂, cells produced 1.7 moles H₂ and 0.8 mole CO₂ per mole of acetate consumed. Gas production and acetate uptake were inhibited by monofluoroacetic acid (MFA), 3-(3′,4′-dichlorophenyl)-1,1-dimethylurea (DCMU) and by H₂. Acetate uptake was inhibited about 50% by 5% H₂ (95% N₂). H₂ in the presence of MFA or DCMU stimulated acetate uptake and the result was interpreted to indicate a transition from oxidative to reductive metabolism. Carbon-14 from both [1-¹⁴C]- and [2-¹⁴C]acetate was incorporated under N₂ or H₂ into CO₂, lipids, and carbohydrates. The methyl carbon of acetate accumulated principally (75-80%) in the lipid and carbohydrate fractions, whereas the carboxyl carbon contributed isotope primarily to CO₂ (56%) in N₂. The presence of H₂ caused a decrease in carbon lost from the cell as CO₂ and a greater proportion of the acetate was incorporated into lipid. The results support the occurrence of anaerobic and light-dependent citric acid and glyoxylate cycles which affect the conversion of acetate to CO₂ and H₂ prior to its conversion to cellular material.     

Biomethanation: Anaerobic fermentation of CO2, H2 and CO to methane

Studies to examine the microbial fermentation of coal gasification products (CO₂, H₂ and CO) to methane have been done with a mixed culture of anaerobic bacteria selected from an anaerobic sewage digestor. The specific rate of methane production at 37°C reached 25 mmol/g cell hr. The stoichiometry for methane production was 4 mmol H₂/mol CO₂. Cell recycle was used to increase the cell concentration from 2.5 to 8.3 g/liter; the volumetric rate of methane production ran from 1.3 to 4 liter/liter hr. The biogasification was also examined at elevated pressure (450 psi) and temperature to facilitate interfacing with a coal gasifier. At 60°C, the specific rate of methane production reached 50 mmol/g cell hr. Carbon monoxide utilization by the mixed culture of anaerobes and by a Rhodopseudomonas species was examined. Both cultures are able to carry out the shift conversion of CO and water to CO₂ and hydrogen.     

Intracellular concentrations and metabolism of carbon compounds in tobacco callus cultures: effects of light and auxin

Callus cultures derived from pith tissue of Nicotiana tabacum were grown on two media either under continuous illumination or in complete darkness. The first medium limited greening ability of callus grown in the light (3 milligrams per liter naphthalene acetic acid, 0.3 milligram per liter 2-isopentenylaminopurine, Murashige and Skoog salts, and 2% sucrose). The second medium encouraged chlorophyll synthesis (greening) though not shoot formation (0.3 milligram per liter naphthalene acetic acid; 0.3 milligrans per liter 2-isopentylaminopurine). To measure intracellular concentrations, calli were grown for 15 days on these standard media containing [U-¹⁴C]sucrose. The dry weight proportions of the calli (as a fraction of fresh weight) and many metabolite concentrations nearly doubled in light-grown cells compared to dark-grown cells and increased 30 to 40% on low-auxin media relative to high-auxin media. Glutamine concentrations (from 4 to 26 millimolar) were very high, probably due to the NH₃ content of the media. Proline concentrations were 20-fold higher in calli grown on low-auxin media in the light (green cells), possibly a stress response to high osmotic potentials in these cells. To analyze sucrose metabolism, callus cells were allowed to take up 0.2% (weight per volume) [U-¹⁴C]sucrose for up to 90 minutes. In callus tissues and in pith sections from stems of tobacco plants, sucrose was primarily metabolized through invertase activity, producing equal amounts of labeled glucose and fructose. Respiration of ¹⁴CO₂ followed the labeling patterns of tricarboxylic acid cycle intermediates. Photorespiration activity was low.     

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.     

Rates of Microbial Metabolism in Deep Coastal Plain Aquifers

Rates of microbial metabolism in deep anaerobic aquifers of the Atlantic coastal plain of South Carolina were investigated by both microbiological and geochemical techniques. Rates of [2-¹⁴C]acetate and [U-¹⁴C]glucose oxidation as well as geochemical evidence indicated that metabolic rates were faster in the sandy sediments composing the aquifers than in the clayey sediments of the confining layers. In the sandy aquifer sediments, estimates of the rates of CO₂ production (millimoles of CO₂ per liter per year) based on the oxidation of [2-¹⁴C] acetate were 9.4 × 10⁻³ to 2.4 × 10⁻¹ for the Black Creek aquifer, 1.1 × 10⁻² for the Middendorf aquifer, and <7 × 10⁻⁵ for the Cape Fear aquifer. These estimates were at least 2 orders of magnitude lower than previously published estimates that were based on the accumulation of CO₂ in laboratory incubations of similar deep subsurface sediments. In contrast, geochemical modeling of groundwater chemistry changes along aquifer flowpaths gave rate estimates that ranged from 10⁻⁴ to 10⁻⁶ mmol of CO₂ per liter per year. The age of these sediments (ca. 80 million years) and their organic carbon content suggest that average rates of CO₂ production could have been no more than 10⁻⁴ mmol per liter per year. Thus, laboratory incubations may greatly overestimate the in situ rates of microbial metabolism in deep subsurface environments. This has important implications for the use of laboratory incubations in attempts to estimate biorestoration capacities of deep aquifers. The rate estimates from geochemical modeling indicate that deep aquifers are among the most oligotrophic aquatic environments in which there is ongoing microbial metabolism.     

Short-Term Effects of CO(2) on Gas Exchange of Leaves of Bigtooth Aspen (Populus grandidentata) in the Field

The short term effects of increased levels of CO₂ on gas exchange of leaves of bigtooth aspen (Populus grandidentata Michx.) were studied at the University of Michigan Biological Station, Pellston, MI. Leaf gas exchange was measured in situ in the upper half of the canopy, 12 to 14 meters above ground. In 1900 microliters per liter CO₂, maximum CO₂ exchange rate (CER) in saturating light was increased by 151% relative to CER in 320 microliters per liter CO₂. The temperature optimum for CER shifted from 25°C in 320 microliters per liter CO₂ to 37°C in 1900 microliters per liter CO₂. In saturating light, increasing CO₂ level over the range 60 to 1900 microliters per liter increased CER, decreased stomatal conductance, and increased leaf water use efficiency. The initial slope of the CO₂ response curve of CER was not significantly different at 20 and 30°C leaf temperatures, although the slope did decline significantly during leaf senescence. In 1900 microliters per liter CO₂, CER increased with increasing light. The light saturation point and maximum CER were higher in 30°C than in 20°C, although there was little effect of temperature in low light. The experimental results are consistent with patterns seen in laboratory studies of other C₃ species and define the parameters required by some models of aspen CER in the field.