Effects of Soil Water Content on Biodegradation of Phenanthrene in a Mixture of Organic Contaminants

Phenanthrene biodegradation was investigated at different soil water contents [0.11, 0.22, 0.33, 0.44 g H₂O (g soil)^?1] to determine the effects of water availability on biodegradation rate. A subsurface horizon of Kennebec silty loam soil was used in this study. [9-¹⁴C] phenanthrene was dissolved in a mixture of organic contaminants that consisted of 76% decane, 6% ρ-xylene, 6% phenanthrene, 6% pristane, and 6% naphthalene, and then added to the soil. The highest rate of mineralization, in which 0.23% of the [9-¹⁴C] phenanthrene degraded to ¹⁴CO₂ after 66 days of incubation, was observed at the soil water content of 0.44 g H₂O/g dry soil. Most of the ¹⁴C remained in the soil as the parent compound or as nonextractable compounds by acetonitrile at the highest water content. Concentrations of nonextractable compounds increased with water content, but residual extractable phenanthrene decreased significantly with increasing water content, which presumably indicates that bio-transformation occurred. The mineralization analysis of radiolabeled 9th carbon in phenanthrene underestimated phenanthrene biodegradation. The strong adsorption and low solubility of phenanthrene contributed to the low mineralization of phenanthrene 9th carbon. The other components were subject to higher biological and abiotic dissipation processes with increasing soil water content.     

Nuclear analytical methods for trace element studies in calcified tissues

Various nuclear analytical methods have been developed and applied to determine the elemental composition of calcified tissues (teeth and bones). Fluorine was determined by prompt gamma activation analysis through the¹⁹F(p, α ψ)¹⁶O reaction. Carbon was measured by activation analysis with He-3 ions, and the technique of Proton-Induced X-ray Emission (PIXE) was applied to simultaneously determine Ca, P, and trace elements in well-documented teeth. Dental hard tissues: enamel, dentine, cementum, and their junctions, as well as different parts of the same tissue, were examined separately. Furthermore, using a Proton Microprobe, we measured the surface distribution of F and other elements on and around carious lesions on the enamel. The depth profiles of F, and other elements, were also measured right up to the amelodentin junction.

     

Metabolism of Leucine and Alanine in Growing Rats Fed the Diets with Various Protein to Energy Ratios

In order to clarify the nutritional significance of metabolism of the carbon skeleton of individual amino acids, the metabolic fates of l-leucine-U-¹⁴C and l-alanine-U-¹⁴C were investigated in growing rats fed the diets with various protein calories percents (PC%) at 410 kcal of metabolizable energy.

The incorporation of ¹⁴C into body protein in 12 hr after the injection of leucine-¹⁴C was about 73% of the dose in the 0 and 5 PC% groups, though it decreased with increasing the levels of dietary protein from 10 to 30 PC%. The value of ¹⁴C recovery in body protein almost agreed with the net protein utilization (NPU) determined for the whole egg protein in a similar experimental condition. The ¹⁴C recovery in expired CO₂ and body lipid suggested that the carbon skeleton of leucine is well utilized as an energy source when the dietary carbohydrate is extensively replaced by protein.

While, the incorporation of ¹⁴C into body protein from alanine-¹⁴C was less than about 11% of the dose in all the dietary groups, and the majority of ¹⁴C was recovered in expired CO₂ and body lipid in a remarked contrast to leucine.

A similar pattern in urinary excretion of ¹⁴C was obtained for these amino acids, and the refracted rise of ¹⁴C from 10 PC% may give an indication for minimum protein requirements.     

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.     

CHLOROPLAST STRUCTURE AND FUNCTION IN CULTURED TOBACCO TISSUE

A comparative study was made of the ability of cultured pith tissue, leaves of buds induced from callus, and mature leaf tissue of Nicotiana tabacum L. ‘Maryland Mammoth’ to fix carbon, as determined by light-induced C¹⁴O₂ incorporation. Photosynthetic ability was then correlated with the fine structure of chloroplasts from these tissues. The light to dark incorporation ratio for C¹⁴O₂ was at least 3 times as great in the leaf tissue as in growing cultured tissue. The chlorophyll content of the leaf tissue was 10 times as great. The carbon fixation pattern of all the tissues, as determined by radioautographs of chromatogramed extracts, was qualitatively the same. The rate of sucrose synthesis differed greatly, since 20% of the total radioactivity of the extracts from mature leaf tissue appeared in sucrose, while only 1.0% was found in sucrose from callus extracts. The incorporation of C¹⁴O₂ into sugars was inhibited in all the tissue by DCMU (3,4-dichlorophenyl,1, 1-dimethylurea). Cultured tissue past the log phase of growth was intermediate between the younger cultured tissue and the leaf tissue in its chlorophyll content and ability to incorporate C¹⁴O₂ in the light. Proplastids from dark-grown callus possessed stroma lamellae, but prolamellar bodies were not observed. The chloroplasts from growing callus were partially differentiated in comparison with chloroplasts from mature leaf tissue, since each granum had only 4-7 lamellae. Chloroplasts from callus past the log phase of growth were indistinguishable from those in mature leaves. This study establishes that the differentiation of chloroplasts in cultured tissue is a function of the growth rate of the tissue. The growth rate and degree of differentiation of the tissue can be regulated, so a well-defined system is available for the experimental study of chloroplast differentiation.     

Losses of14C from roots of pulse-labelled wheat and barley during washing from soil

In crop carbon budget studies losses of root material during storage and washing of samples may cause considerable errors. To correct data from field experiments where rhizosphere C fluxes in wheat and barley were determined by¹⁴C pulse-labelling at different development stages, experiments were performed to quantify losses of¹⁴C from roots during washing. Losses of¹⁴C from wheat roots grown on nutrient solution and stored in different ways, decreased from on average 45% of total¹⁴C content 8 days after labelling to 27% after 21 days. This decrease was probably related to the incorporation of¹⁴C into structural compounds. During washing of oven-dried soil cores of held-grown wheat and barley 3 weeks after labelling, different size classes of losses of¹⁴C from the roots increased substantially with the development stage of the crop at labelling. The 0.3–0.6 mm size class increased from 5% of the¹⁴C in roots > 0.3 mm in young plants to 25% at ripening, and the < 0.3 mm size class increased from 8 to 41% of total¹⁴C content. The latter size class was, however, determined by washing handpicked roots and may therefore partly consist of adhering exudates, mucilages and microorganisms. The effect of development stage on root washing losses was attributed to root senescence which increases the fragility of roots. Thus, especially at the rate development stages root washing losses caused a severe underestimation of the root¹⁴C content. However, with these results the¹⁴C distribution patterns of the field experiments could be adequately corrected.Communication No. 77 of the Dutch Programme on Soil Ecology of Arable Farming Systems.     

Omega oxidation of fatty acids and the pathway of 3-hydroxybutyric acid formation

Pathways followed by the carbons of long chain fatty acids in their conversion to 3-hydroxybutyric acid were traced and the contribution of ω-oxidation to fatty acid oxidation was determined in the cellular environment where ketone body formation occurs. 1-¹⁴C-, 2-¹⁴C-, and ω-¹⁴C-labeled fatty acids were injected into alloxan-induced diabetic rats in ketosis. 3-Hydroxybutyric acid was isolated from their urines and degraded. About 1.2 to 1.4 times as much ¹⁴C was found in carbon 1 as carbon 3 of 3-hydroxybutyric acid when the 1-¹⁴C-labeled fatty acids were injected and in carbon 2 as carbon 4 when the 2-¹⁴C-labeled fatty acids were injected. There was about 4 times as much incorporation into carbon 4 as carbon 2 of 3-hydroxybutyric acid formed from the ω-¹⁴C-labeled fatty acids. This means that 50% or more of the fatty acids were oxidized, so that the terminal two carbons of the fatty acids were converted to acetoacetyl-CoA without acetyl-CoA as an intermediate. Incorporation of ¹⁴C into carbons 1 and 2 of the hydroxybutyric acid reflects the distribution of ¹⁴C in acetyl-CoA. Incorporation into carbon 1 was very small when the ω-¹⁴C-labeled fatty acids were substrate. This means that ω-oxidation of fatty acids makes, at most, a small contribution to the formation of the acetyl-CoA pool from which acetoacetate is derived.     

Further studies on the photosynthesis of carrot tissue cultures

The influence of kinetin and sucrose on the photosynthetic activity of carrot (Daucus carota) tissue cultures in relation to growth was investigated. The results showed that light contributes heavily to the growth of tissue cultures measured in terms of fresh and dry weight and cell division activity. In light, the fresh weight, dry weight, and number of cells per explant were about or more than doubled. This indicated that after the development of chloroplasts, carrot tissue cultures can grow autotrophically at least as far as energy and carbon are concerned. Kinetin was shown to have an important role in developing the photosynthetic apparatus and photosynthetic activity of tissue cultures as manifested by the increase of chlorophyll content (60%), Hill activity (about 3-fold), and ¹⁴C-fixation from NaH¹⁴CO₃ (about 20%). On the other hand, the presence of sucrose in the medium reduced the chlorophyll content by about 30% and ¹⁴C-fixation from NaH¹⁴CO₃ in the soluble fraction by about 60%. A possible correlation between the influence of kinetin on sugar uptake and the effect of kinetin on ¹⁴C-fixation from NaH¹⁴CO₃ was discussed.     

Inorganic carbon fixation and metabolism in maize roots as affected by nitrate and ammonium nutrition

The effects of NO^?₃ and NH⁺₄ nutrition on the rates of dark incorporation of inorganic carbon by roots of hydroponically grown Zea mays L. cv. 712 and on the metabolic products of this incorporation, were determined in plants supplied with NaH¹⁴CO₃ in the nutrient solution. The shoots and roots of the plants supplied with NaH¹⁴CO₃ in the root medium for 30 min were extracted with 80%; (v/v) ethanol and fractionated into soluble and insoluble fractions. The soluble fraction was further separated into the neutral, organic acid, amino acid and non-polar fractions. The amino acid fraction was then analyzed to determine quantities and the ¹⁴C content of its individual components. The rates of dark incorporation of inorganic carbon calculated from H¹⁴CO^?₃ fixation and attributable to the activity of phosphoenolpyuvate carboxylase (EC 4.1.1.31), were 5-fold higher in ammonium-fed plants than in nitrate-fed plants after a 30-min pulse of ¹⁴C. This activity forms a small, but significant component of the carbon budget of the root. The proportion of ¹⁴C located in the shoots was also significantly higher in ammonium-fed plants than in nitrate-fed plants, indicating more rapid translocation of the products of dark fixation to the shoots in plants receiving NH⁺/sp₄ nutrition. Ammonium-fed plants favoured incorporation of ¹⁴C into amino acids, while nitrate-fed plants allocated relatively more ¹⁴C into organic acids. The amino acid composition was also dependent on the type of nitrogen supplied, and asparagine was found to accumulate in ammonium-fed plants. The ¹⁴C labelling of the amino acids was consistent with the diversion of ¹⁴C-oxaloacetate derived from carboxlyation of phosphoenolpyruvate into the formation of both asparatate and glutamate. The results support the conclusion that inorganic carbon fixation in the roots of maize plants provides an important anaplerotic source of carbon for NH⁺₄ assimilation.     

Effect of translocation-hindering procedures on source leaf photosynthesis in cucumber

Three treatments which altered translocation rate were applied to cucumber plants: Girdling of source leaf petiole; removal of all aerial sinks; removal of all source leaves except one. Two different effects were observed, one short-term (during the initial 6 hours), and one long-term (detected after several days).

The short-term effect was observed exclusively in girdled leaves and involved a reduction in ¹⁴CO₂ fixation rate paralleled by an increase in stomatal resistance. The effects were maximal after 3 hours with subsequent recovery. Stomatal closure apparently resulted from the 5 to 10% water deficit temporarily detected in girdled leaves which probably induced the observed temporary increases in abscisic acid content. Kinetin counteracted the effects of girdling.

The long-term effect was detected 3 days after girdling and 3 to 5 days after sink manipulation. An increase or decrease in ¹⁴CO₂ fixation rate was observed when the sink-source ratio was increased or decreased respectively, accompanied by a respective decrease or increase in starch content. Changes in the relative amount of ¹⁴CO₂ incorporated into various photosynthetic products were also observed. Stomatal closure was not involved, and the decrease in CO₂ fixation was not counteracted by kinetin.

     

The Role of Glycerol and Inorganic Ions in Osmoregulatory Responses of the Euryhaline Flagellate Chlamydomonas pulsatilla Wollenweber

The green euryhaline flagellate Chlamydomonas pulsatilla Wollenweber, isolated from a coastal marine environment, was grown exponentially over the salinity range of 10 to 200% artificial seawater (ASW). The cellular volume and aqueous space of the alga, measured by [¹⁴C] mannitol and ³H₂O tracer analyses of centrifuged cell pellets, ranged between 2.3 and 3.1 picoliters and between 1.5 and 2.1 picoliters, respectively. The nonaqueous space determined in those analyses (28-35%) was consistent with the cell composition of the alga. The glycerol content of the alga increased almost linearly with increasing salinity; its contribution to intracellular osmolality at 200% ASW was about 57%. The contribution of amino acids and soluble carbohydrates to the cell osmotic balance was small. Intracellular ion concentrations determined by analyzing centrifuged cell pellets of known [¹⁴C]mannitol space by atomic absorption spectrophotometry, and by neutron activation analyses of washed cells were similar. At 10% ASW, potassium and magnesium were the major cations, and chloride and phosphate were the major anions. The sodium and chloride content of the alga increased with increasing salinity; at 200% ASW the intracellular concentration of both sodium and chloride was about 400 millimolar. The intracellular osmolality (π_int) matched closely the external osmolality (π_ext) over the entire salinity range except at 10% ASW where π_int exceeded π_ext by 120 to 270 milliosmoles per kilogram H₂O.     

Detection of acetyl coenzyme A as an early CO2 assimilation intermediate in Methanobacterium

The pivotal role of acetyl coenzyme A in CO₂ assimilation by autotrophic methanogenic bacteria has been demonstrated by pulse-labelling of growing Methanobacterium thermoautotrophicum with ¹⁴CO₂. After very short incubation with ¹⁴CO₂ (1.5 s) approximately 1% of label incorporated into the soluble cell fraction was contained in acetyl coenzyme A. The percentage distribution of ¹⁴C within acetyl CoA markedly decreased with time, which is indicative for acetyl CoA being an immediate ¹⁴CO₂ fixation product. Label in the acetate molecule first appeared in the carboxyl carbon, but the methyl carbon became equally labelled within only 10 s. The acetyl CoA was compared with authentic material by various criterions and its cellular concentration was determined to be 52 M. This small cellular pool size of acetyl CoA as compared to e.g. alanine (6.4 mM) provides an explanation for the observed labelling kinetics. The data are fully consistent with autotrophic carbon assimilation via a total synthesis of acetyl coenzyme A from 2 CO₂.Dedicated to Professor Dr. Gerhart Drews on occasion of his 60th birthday     

Metabolism of [5-h]proline by barley leaves and its use in measuring the effects of water stress on proline oxidation

The objective of these experiments was to determine the fate of tritium from the 5 position of proline and to assess the validity of its loss to H₂O as a measure of proline oxidation. When [5-³H]proline was fed to barley (Hordeum vulgare) leaves, tritium was recovered in H₂O and metabolites such as glutamate, glutamine, organic acids, aspartate, asparagine, and γ-aminobutyrate. Collectively these metabolites, which are oxidation products of proline, accounted for 8% of the ³H recovered after 5 hours. In spite of the amount recovered in metabolites, the rates of proline oxidation estimated by measuring ³H₂O recovery from [5-³H]proline were only slightly lower than rates estimated by incorporation of ¹⁴C into oxidized products and loss of ¹⁴C from total proline. Therefore, ³H₂O recovery from [5-³H]proline is useful in assessing the effects of stress on proline metabolism.

Water stress inhibited proline oxidation, as reported previously. In addition, a reconversion of proline oxidation products to proline occurred in stressed leaves. This observation probably indicates a breakdown in cellular compartmentation of proline synthesis and proline oxidation.

     

Fixation of O(2) during Photorespiration: Kinetic and Steady-State Studies of the Photorespiratory Carbon Oxidation Cycle with Intact Leaves and Isolated Chloroplasts of C(3) Plants

Mass spectrometric techniques were used to trace the incorporation of [¹⁸O]oxygen into metabolites of the photorespiratory pathway. Glycolate, glycine, and serine extracted from leaves of the C₃ plants, Spinacia oleracea L., Atriplex hastata, and Helianthus annuus which had been exposed to [¹⁸O]oxygen at the CO₂ compensation point were heavily labeled with ¹⁸O. In each case one, and only one of the carboxyl oxygens was labeled. The abundance of ¹⁸O in this oxygen of glycolate reached 50 to 70% of that of the oxygen provided after only 5 to 10 seconds exposure to [¹⁸O]oxygen. Glycine and serine attained the same final enrichment after 40 and 180 seconds, respectively. This confirms that glycine and serine are synthesized from glycolate.

The labeling of photorespiratory intermediates in intact leaves reached a mean of 59% of that of the oxygen provided in the feedings. This indicates that at least 59% of the glycolate photorespired is synthesized with the fixation of molecular oxygen. This estimate is certainly conservative owing to the dilution of labeled oxygen at the site of glycolate synthesis by photosynthetic oxygen. We examined the yield of ¹⁸O in glycolate synthesized in vitro by isolated intact spinach chloroplasts in a system which permitted direct sampling of the isotopic composition of the oxygen at the site of synthesis. The isotopic enrichment of glycolate from such experiments was 90 to 95% of that of the oxygen present during the incubation.

The carboxyl oxygens of 3-phosphoglycerate also became labeled with ¹⁸O in 20- and 40-minute feedings with [¹⁸O]oxygen to intact leaves at the CO₂ compensation point. Control experiments indicated that this label was probably due to direct synthesis of 3-phosphoglycerate from glycolate during photorespiration. The mean enrichment of 3-phosphoglycerate was 14 ± 4% of that of glycine or serine, its precursors of the photorespiratory pathway, in 10 separate feeding experiments. It is argued that this constant dilution of label indicates a constant stoichiometric balance between photorespiratory and photosynthetic sources of 3-phosphoglycerate at the CO₂ compensation point.

Oxygen uptake sufficient to account for about half of the rate of ¹⁸O fixation into glycine in the intact leaves was observed with intact spinach chloroplasts. Oxygen uptake and production by intact leaves at the CO₂ compensation point indicate about 1.9 oxygen exchanged per glycolate photorespired. The fixation of molecular oxygen into glycolate plus the peroxisomal oxidation of glycolate to glyoxylate and the mitochondrial conversion of glycine to serine can account for up to 1.75 oxygen taken up per glycolate.

These studies provide new evidence which supports the current formulation of the pathway of photorespiration and its relation to photosynthetic metabolism. The experiments described also suggest new approaches using stable isotope techniques to study the rate of photorespiration and the balance between photorespiration and photosynthesis in vivo.

     

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.     

Metabolism of Serine in Growing Rats and Chicks at Various Dietary Protein Levels

The metabolic fate of the carbon skeleton of l-serine-U-¹⁴C has been investigated, in vivo and in vitro, in growing rats and chicks fed the diets with various protein calories percents (PC%) at 410 kcal of metabolizable energy.

The incorporation of ¹⁴C into body protein at 12 hr after the injection of serine-¹⁴C was about 49% of the injected dose in rats fed the 10 or 15 PC % diet, though the value was reduced in rats fed lower and higher protein diets. The ¹⁴CO₂ production was smaller in rats fed the 10 and 15 PC% diet, and it showed an inverse pattern to that of the ¹⁴C incorporation into body protein. Urinary excretion of ¹⁴C was higher in rats fed 10 and higher PC% diets, whose growth rate and net body protein retention were maximum.

In contrast to the case of rats, the incorporation of ¹⁴C into body protein of chicks at 6 hr after the injection was rather reduced in the 15 PC% group. The proportion of ¹⁴C excreted as uric acid was remarkably increased above the 10 PC% group, and about 19% of the injected dose was recovered in the 50 PC% group.

The catabolic rate of serine in the liver slices of rats and chicks was increased by high protein diets.

These results support the concept that the nutritional significance of metabolism of the carbon skeleton of serine in growing rats and chicks is different from each other, especially at high protein diets.     

Effect of Fusicoccin on Dark CO(2) Fixation by Vicia faba Guard Cell Protoplasts

When Vicia faba guard cell protoplasts were treated with fusicoccin, dark ¹⁴CO₂ fixation rates increased by as much as 8-fold. Rate increase was saturated with less than 1 micromolar fusicoccin. Even after 6 minutes of dark ¹⁴CO₂ fixation, more than 95% of the incorporated radioactivity was in stable products derived from carboxylation of phosphoenolpyruvate (about 50% and 30% in malate and aspartate, respectively). The relative distribution of ¹⁴C among products and in the C-4 position of malate (initially more than 90% of [¹⁴C]malate) was independent of fusicoccin concentration. After incubation in the dark, malate content was higher in protoplasts treated with fusicoccin. A positive correlation was observed between the amounts of ¹⁴CO₂ fixed and malate content.

It was concluded that (a) fusicoccin causes an increase in the rate of dark ¹⁴CO₂ fixation without alteration of the relative fluxes through pathways by which it is metabolized, (b) fusicoccin causes an increase in malate synthesis, and (c) dark ¹⁴CO₂ fixation and malate synthesis are mediated by phosphoenolpyruvate carboxylase.

     

Method for measuring microbial degradation and mineralization of14C-labeled chitin obtained from the blue crab,Callinectes sapidus

A method for measuring microbial degradation and mineralization of radiolabeled native chitin is described.¹⁴C-labeled chitin was synthesized in vivo by injecting shed blue crabs (Callinectes sapidus) with N-acetyl-D-[1-¹⁴C]-glucosamine and allowing for its incorporation into the exoskeleton. The cuticle had a total organic carbon content of 0.48 mg C mg^–1 with a specific radioactivity of 6,356 CPM mg^–1. Glucosamine, i.e., chitin content as determined colorimetrically, was 22% (w/w). Microbial degradation and mineralization rates were assessed in batch culture using¹⁴C-chitin as substrate and York River water as inoculum. Replicate flasks were sampled daily for enumeration of chitinoclastic bacteria and the radiolabel recovered as particulate¹⁴C-chitin or¹⁴CO₂. The amount of¹⁴CO₂ generated was directly proportional to the loss of particulate¹⁴C-chitin, with 96% of the added label recovered as the sum of both phases. The maximum rate of mineralization was 207 mg day^–1 g^–1 seeded¹⁴C-chitin at 20°C. Highest chitinoclastic bacterial counts corresponded to the period of maximum rate of chitinolysis. It is suggested that the rate of chitin mineralization is limited by exoenzymatic depolymerization and not by chitin concentration.VIMS Contribution no. 1215.     

Combined effects of chronic ozone and elevated CO2 on Rubisco activity and leaf components in soybean Glycine max

Content and activity of Rubisco and concentrations of leaf nitrogen, chlorophyll and total non-structural carbohydrates (TNC) were determined at regular intervals during the 1993 and 1994 growing seasons to understand the effects and interactions of [O3] and elevated [CO2] on biochemical limitations to photosynthesis during ontogeny. Soybean (Glycine max var. Essex) was grown in open-top field chambers in either charcoal-filtered air (CF, 20 nmol mol^-1) or non-filtered air supplemented with 1.5 x ambient [O3] (c. 80 nmol mol^-1) at ambient (AA, 360 mol mol^-1) or elevated [CO2] (700 mol mol^-1). Sampling period significantly affected all the variables examined. Changes included a decrease in the activity and content of Rubisco during seed maturation, and increased nitrogen (N), leaf mass per unit area (LMA) and total non-structural carbohydrates (TNC, including starch and sucrose) through the reproductive phases. Ontogenetic changes were most rapid in O2-treated plants. At ambient [CO2], O3 decreased initial activity (14-64% per unit leaf area and 14-29% per unit Rubisco) and content of Rubisco (9-53%), and N content per unit leaf area. Ozone decreased LMA by 17-28% of plants in CF-AA at the end of the growing season because of a 24-41% decrease in starch and a 59-80% decrease in sucrose. In general, elevated CO2], in CF or O3-fumigated air, reduced the initial activity of Rubisco and activation state while having little effect on Rubisco content, N and the chlorophyll content, per unit leaf area. Elevated CO2 decreased Rubisco activity by 14-34% per unit leaf area and 15-25% per unit Rubisco content of plants in grown CF-AA, nd increases LMA by 27-74% of the leaf mass per unit area in CF-AA because of a 23-148% increase in starch. However, the data suggest that, at elevated [CO2], increases in starch and sucrose are not directly responsible for the deactivation of Rubisco. Also, there was little evidence of an adjustment of Rubisco activity in response to starch and sucrose metabolism. Significant interactions between elevated [CO2] and [O3] on all variables examined generally resulted in alleviation or amelioration of the O3 effects at elevated CO2. These data provide further support to the idea that elevated atmospheric CO2 will reduce or prevent damage from pollutant O3.     

Bacterial metabolism of algal extracellular carbon

Measurements of microbial utilization of extracellular organic carbon (EOC) released by phytoplankton commonly consider only EOC fractions subject to rapid uptake. Questions remain whether other EOC fractions are metabolized, what portion is labile, and with what assimilation efficiency this carbon substrate is utilized. ¹⁴C-EOC was prepared by incubation of the natural mixed planktonic community from an oligotrophic lake with H¹⁴CO₃ in the light. ¹⁴C-EOC which was not rapidly removed by heterotrophs remained in solution and was isolated by filtration. This residual EOC was inoculated with lake microheterotrophs in laboratory microcosms, and utilization kinetics were determined through long-term assays of cumulative ¹⁴CO₂ production. Time-courses for ¹⁴CO₂ production were consistent for all assays and were well described by a deterministic mixed-order degradation model. On twelve sampling occasions, from 29% to 76% of residual ¹⁴C-EOC was labile to further metabolism by lake heterotrophs. First-order rate constants for EOC utilization showed a mode of 0.05 to 0.15 per day. From 33% to 78% of gross ¹⁴C-EOC uptake was respired (mean 50%), indicating appreciable return of algal EOC to the pelagic food web as microbial biomass.Contribution No. 596, W. K. Kellogg Biological Station, Michigan State University.