Diurnal change of tartrate dissimilation during the ripening of grapes

l(+)-tartrate-[U-¹⁴C] or sucrose-[U-¹⁴C] was fed into grape berries and ¹⁴CO₂ evolution was determined. ¹⁴CO₂ evolution front l(+)-tartrate-[U-¹⁴C] was slightly higher in mature than immature berries, and that from sucrose-[U-¹⁴C] was higher in immature than mature ones. ¹⁴CO₂ evolution from l(+)-tartrate-[U-¹⁴C] was irregular throughout the day until 2 or 3 weeks after flowering. This stage shifted to regular ¹⁴CO₂ evolution until 6 or 7 weeks after flowering, and the mode of ¹⁴CO₂ evolution showed diurnal variation; higher in the day than at night. Then the stage without variation of ¹⁴CO₂ evolution followed 10 weeks after flowering. These observations indicate that tartrate is not biochemically inert in grape berries, while the amount of ¹⁴CO₂ evolution from sucrose-[U-¹⁴C] was higher at night than in the day through the whole ripening process, except in the early stage.     

Preparation of [U-14C]-labelled glycogen, maltosaccharides, maltose, and D-glucose by photoassimilation of 14CO2 in Anacystis nidulans and selective enzymic degradation.

A procedure is described for the isolation from the phototrophic procaryole Anacystis nidulans of [U-¹⁴C]-labelled glycogen, with high specific radioactivity,formed when NaH¹⁴CO₃ was added to non-dividing cells that continued to photoassimilate CO₂. [U-¹⁴C]-Labelled glycogen was then treated with isoamylase (EC 3.2.1.68), isoamylase plus beta-amylase (EC 3.2.1.2), or glucoamylase (EC 3.2.1.3) to give [U-¹⁴C]-labelled maltosaccharides, maltose-U-¹⁴C, or d-glucose-U-¹⁴C, respectively.     

Conversion of tartrate to malate and monoethyl tartrate in grape leaves

¹⁴CO₂ evolution from l(+)-tartrate-[U-¹⁴C] in grape leaves was observed confirming the dissimilation of tartrate. 30 sec after the administration of l(+)-tartrate-[U-¹⁴C], 3 compounds were found to contain ¹⁴C. Two of them were identified as monethyl tartrate and malate by chromatographic and MS studies. It is suggested that the ¹⁴CO₂ evolved is derived from malate-[U-¹⁴C] which is metabolically formed from l(+)-tartrate-[U-¹⁴C], and that monoethyl tartrate is not an intermediate for the conversion to malate.     

Biodegradation of atrazine in surface soils and subsurface sediments collected from an agricultural research farm

The purpose of the present study was to assess atrazine (2-chloro-4-ethylamino-6-isopropylamino-s-triazine) mineralization by indigenous microbial communities and to investigate constraints associated with atrazine biodegradation in environmental samples collected from surface soil and subsurface zones at an agricultural site in Ohio. Atrazine mineralization in soil and sediment samples was monitored as ¹⁴CO₂ evolution in biometers which were amended with ¹⁴C-labeled atrazine. Variables of interest were the position of the label ([U-¹⁴C-ring]-atrazine and [2-¹⁴C-ethyl]-atrazine), incubation temperature (25°C and 10°C), inoculation with a previously characterized atrazine-mineralizing bacterial isolate (M91-3), and the effect of sterilization prior to inoculation. In uninoculated biometers, mineralization rate constants declined with increasing sample depth. First-order mineralization rate constants were somewhat lower for [2-¹⁴C-ethyl]-atrazine when compared to those of [U-¹⁴C-ring]-atrazine. Moreover, the total amount of ¹⁴CO₂ released was less with [2-¹⁴C-ethyl]-atrazine. Mineralization at 10°C was slow and linear. In inoculated biometers, less ¹⁴CO₂ was released in [2-¹⁴C-ethyl]-atrazine experiments as compared with [U-¹⁴C-ring]-atrazine probably as a result of assimilatory incorporation of ¹⁴C into biomass. The mineralization rate constants (k) and overall extents of mineralization (P _max ) were higher in biometers that were not sterilized prior to inoculation, suggesting that the native microbial populations in the sediments were contributing to the overall release of ¹⁴CO₂ from [U-¹⁴C-ring]-atrazine and [2-¹⁴C-ethyl]-atrazine. A positive correlation between k and aqueous phase atrazine concentrations (C _eq ) in the biometers was observed at 25°C, suggesting that sorption of atrazine influenced mineralization rates. The sorption effect on atrazine mineralization was greatly diminished at 10°C. It was concluded that sorption can limit biodegradation rates of weakly-sorbing solutes at high solid-to-solution ratios and at ambient surface temperatures if an active degrading population is present. Under vadose zone and subsurface aquifer conditions, however, low temperatures and the lack of degrading organisms are likely to be primary factors limiting the biodegradation of atrazine.Abbreviations C _eq solution phase atrazine concentration at equilibrium - C _s amount of atrazine sorbed - CLA [2-¹⁴C-ethyl]-atrazine - k first-order mineralization rate constant - K _d sorption coefficient - m slope - P _max maximum amount of CO₂ released - RLA [U-¹⁴C-ring]-atrazine     

Biodegradation of atrazine in surface soils and subsurface sediments collected from an agricultural research farm

The purpose of the present study was to assess atrazine (2-chloro-4-ethylamino-6-isopropylamino-s-triazine) mineralization by indigenous microbial communities and to investigate constraints associated with atrazine biodegradation in environmental samples collected from surface soil and subsurface zones at an agricultural site in Ohio. Atrazine mineralization in soil and sediment samples was monitored as ¹⁴CO₂ evolution in biometers which were amended with ¹⁴C-labeled atrazine. Variables of interest were the position of the label ([U-¹⁴C-ring]-atrazine and [2-¹⁴C-ethyl]-atrazine), incubation temperature (25°C and 10°C), inoculation with a previously characterized atrazine-mineralizing bacterial isolate (M91-3), and the effect of sterilization prior to inoculation. In uninoculated biometers, mineralization rate constants declined with increasing sample depth. First-order mineralization rate constants were somewhat lower for [2-¹⁴C-ethyl]-atrazine when compared to those of [U-¹⁴C-ring]-atrazine. Moreover, the total amount of ¹⁴CO₂ released was less with [2-¹⁴C-ethyl]-atrazine. Mineralization at 10°C was slow and linear. In inoculated biometers, less ¹⁴CO₂ was released in [2-¹⁴C-ethyl]-atrazine experiments as compared with [U-¹⁴C-ring]-atrazine probably as a result of assimilatory incorporation of ¹⁴C into biomass. The mineralization rate constants (k) and overall extents of mineralization (P _max ) were higher in biometers that were not sterilized prior to inoculation, suggesting that the native microbial populations in the sediments were contributing to the overall release of ¹⁴CO₂ from [U-¹⁴C-ring]-atrazine and [2-¹⁴C-ethyl]-atrazine. A positive correlation between k and aqueous phase atrazine concentrations (C _eq ) in the biometers was observed at 25°C, suggesting that sorption of atrazine influenced mineralization rates. The sorption effect on atrazine mineralization was greatly diminished at 10°C. It was concluded that sorption can limit biodegradation rates of weakly-sorbing solutes at high solid-to-solution ratios and at ambient surface temperatures if an active degrading population is present. Under vadose zone and subsurface aquifer conditions, however, low temperatures and the lack of degrading organisms are likely to be primary factors limiting the biodegradation of atrazine.     

Inhibition of glucose utilization for acetylcholine synthesis by cerebrospinal fluid.

Abstract— Replacement of bicarbonate-Locke incubation medium with feline CSF reduced [¹⁴C]ACh formation from [U-¹⁴C]glucose by rat brain mince approx 30%. CSF was obtained from a cannula leading to the cisterna magna of freely moving cats. The component of CSF responsible for inhibition was characterized as a dialyzable heat-stable organic anion. Choline acetyltransferase activity was not altered by CSF. [¹⁴C]ACh synthesis and ¹⁴CO₂ production from [U-¹⁴C]glucose but not from [2-¹⁴C]-pyruvate were inhibited by CSF, suggesting inhibition in the metabolism of glucose to pyruvate. The anionic fraction of human CSF was as potent as that from feline CSF in inhibiting ¹⁴CO₂ production from [U-¹⁴C]glucose. Brain hexokinase was inhibited by the anionic fraction of feline CSF. The inhibition was non-competitive with respect to glucose and uncompetitive with respect to ATP. It is suggested that inhibition of hexokinase by CSF was responsible at least in part for the inhibition of glucose metabolism which resulted in decreased [¹⁴C]ACh synthesis and ¹⁴CO₂ production.     

Carbohydrate oxidation by leucoplasts from suspension cultures of soybean (Glycine max L.)

The aim of this work was to discover how leucoplasts from suspension cultures of soybean (Glycine max L.) oxidize hexose monophosphates. Leucoplasts were isolated from protoplast lysates on a continuous gradient of Nycodenz with a yield of 28% and an intactness of 80%. Incubation of the leucoplasts with ¹⁴C-labelled substrates led to ¹⁴CO₂ production, that was dependent upon leucoplast intactness, from [U-¹⁴C]glucose 6-phosphate, [U-¹⁴C]glucose 1-phosphate, [U-¹⁴C] fructose 6-phosphate and [U-¹⁴C]glucose+ATP, but not from [U-¹⁴C]fructose-1,6-bisphosphate or [U-¹⁴C]triose phosphate. The yield from [U-¹⁴C]glucose 6-phosphate was at least four times greater than that from any of the other substrates. When [1-¹⁴C]-, [2-¹⁴C]-, [3,4-¹⁴C]-, and [6-¹⁴C]glucose 6-phosphate were supplied to leucoplasts significant ¹⁴CO₂ production that was dependent upon leucoplast intactness was found only for [1-¹⁴C]glucose 6-phosphate. It is argued that soybean cell leucoplasts oxidize glucose 6-phosphate via the oxidative pentose phosphate pathway with very little recycling, and that in these plastids glycolysis to acetyl CoA is negligible.S.A.C. thanks the Science and Engineering Research Council for a research studentship.     

Validation of the design of feeding experiments involving [(14)C]substrates used to monitor metabolic flux in higher plants

The aim of this study was to examine whether flux through the pathways of carbohydrate oxidation is accurately reflected in the pattern of ¹⁴CO₂ release from positionally labelled [¹⁴C]substrates in conventional radiolabel feeding studies. Heterotrophic cell suspension cultures of Arabidopsis thaliana were used for this work. The presence of an alkaline trap to capture metabolically generated ¹⁴CO₂ had no significant effect on the ratio of ¹⁴CO₂ release from specifically labelled [¹⁴C]substrates, or on the metabolism of [U-¹⁴C]glucose by the cells. Although the amount of ¹⁴CO₂ captured in a conventional time-course study was only about half of that released from a sample acidified at an equivalent time point, the ratios of ¹⁴CO₂ released from different positionally labelled [¹⁴C]glucose and [1-¹⁴C]gluconate were the same in untreated and acidified samples. Less than 5% of radioactivity supplied to the growth medium as [¹⁴C]bicarbonate was incorporated into acid-stable compounds, and there was no evidence for appreciable reassimilation of ¹⁴CO₂ generated intracellularly during oxidation of [1-¹⁴C]gluconate by the cells. It is concluded that the ratio of label captured from specifically labelled [¹⁴C]glucose is a valid and convenient measure of the relative rates of oxidation of the different positional carbon atoms within the supplied respiratory substrate. However, it is argued that failure to compensate for the incomplete absorption of ¹⁴CO₂ by an alkaline trap may distort estimates of respiration that rely on an absolute measure of the amount of ¹⁴CO₂ generated by metabolism.     

Energy metabolism in hypoxic astrocytes: Protective mechanism of fructose-1,6-bisphosphate

The protective effects of fructose-1,6-biphosphate (FBP) during hypoxia/ischemia are thought to result from uptake and utilization of FBP as a substrate for glycolysis or from stimulation of glucose metabolism. To test these hypotheses, we measumed CO₂ and lactate production from [6-¹⁴C]glucose, [1-¹⁴C]glucose, and [U-¹⁴C]FBP in normoxic and hypoxic cultured astrocytes with and without FBP present. FBP had little effect on CO₂ production by glycolysis, but increased CO₂ production by the pentose phosphate pathway. Labeled FBP produced very small amounts of CO₂. Lactate production from [1-, and 6-¹⁴C]glucose increased similarly during hypoxic hypoxia; the increase was independent of added FBP. Labeled lactate from [U-¹⁴C]FBP was minimal. We conclude that exogenous FBP is not used by astrocytes as a substrate for glycolysis and that FBP alters glucose metabolism.     

Effect of 2-deoxy-d-Glucose on Aminoacids Metabolism in Rats’ Cerebral Cortex Slices

We studied the effect of different concentrations of 2-deoxy-d-glucose on the l-[U-¹⁴C]leucine, l-[1-¹⁴C]leucine and [1-¹⁴C]glycine metabolism in slices of cerebral cortex of 10-day-old rats. 2-deoxy-d-glucose since 0.5 mM concentration has inhibited significantly the protein synthesis from l-[U-¹⁴C]leucine and from [1-¹⁴C]glycine in relation to the medium containing only Krebs Ringer bicarbonate. Potassium 8.0 mM in incubation medium did not stimulate the protein synthesis compared to the medium containing 2.7 mM, and at 50 mM diminishes more than 2.5 times the protein synthesis compared to the other concentration. Only at the concentration of 5.0 mM, 2-deoxy-d-glucose inhibited the CO₂ production and lipid synthesis from l-[U-¹⁴C] leucine. This compound did not inhibit either CO₂ production, or lipid synthesis from [1-¹⁴C]glycine. Lactate at 10 mM and glucose 5.0 mM did not revert the inhibitory effect of 2-deoxy-d-glucose on the protein synthesis from l-[U-¹⁴C]leucine. 2-deoxy-d-glucose at 2.0 mM did not show any effect either on CO₂ production, or on lipid synthesis from l-[U-¹⁴C]lactate 10 mM and glucose 5.0 mM.     

GLUCOSE AND AMINO ACID METABOLISM IN OCTOPUS OPTIC AND VERTICAL LOBES IN VITRO

(1) The metabolism of glucose and amino acids in vitro was compared in the rat cerebral cortex and the optic and vertical lobes of the octopus brain. (2) Specific activities and pool sizes of the five amino acids, glutamate, aspartate, glutamine, alanine and γ-aminobutyric acid (GABA), were determined in octopus and rat brain slices after 2 hr incubation with 10 mm -[U-¹⁴C]glucose, 10 mm -L-[U-¹⁴C]glutamate, and 10mm -^L-[U-¹⁴C]glutamate with added 10 mM-glucose. Amino acid pool sizes were similar in rat and octopus brain, with the exception of alanine, which was higher in the octopus. Generally specific activities were from four- to 20-fold higher in rat brain. With [U-¹⁴C]glucose as substrate, specific activities of GABA and glutamate were highest in rat; those of alanine and glutamine highest in octopus brain. With ^L-[U-¹⁴C]glutamate the specific activities of GABA and aspartate were highest in rat, that of aspartate highest and GABA lowest in octopus. The addition of glucose to ^L-[U-¹⁴C]glutamate as substrate had little effect on the specific activities of any of the amino acids. (3) The uptake of some amino acids was determined by incubation with [U-¹⁴C]amino acids for 2 hr, and ¹⁴CO₂ formation was also measured. The amount of label taken up by octopus was uniformly 20-25 per cent of that found for rat brain. The amount of ¹⁴CO₂, however, differed according to the amino acid. Four times as much ¹⁴CO₂ was generated from alanine by octopus optic lobe and twice as much by the vertical lobe than rat cortex, but from glutamate, only 24 per cent in the optic and 15 per cent in the vertical lobe. No ¹⁴CO₂ was generated from [U-¹⁴C]GABA in the octopus, by contrast with the rat. (4) Activity of some of the enzymes involved in amino acid metabolism was determined in homogenates of rat cortex and octopus optic and vertical lobes, with and without activation by Triton X-100. Enzymic activities in the octopus, with the exception of alanine aminotransferase, were lower than in the rat, and glutamate decarboxylase could not be detected in octopus brain, in the absence of detergent.     

THE METABOLISM OF LEUCINE BY DEVELOPING RAT BRAIN: EFFECT OF LEUCINE AND 2-OXO-4-METHYLVALERATE ON LIPID SYNTHESIS FROM GLUCOSE AND KETONE BODIES

Abstract— The oxidation of l -[U-¹⁴C]leucine and l -[l-¹⁴C]leucine at varying concentrations from 0.1 to 5mM to CO₂ and the incorporation into cerebral lipids and proteins by brain slices from 1-week old rats were markedly stimulated by glucose. Although the addition of S mM-dl -3-hydroxybutyrate had no effect on the metabolism of [U-¹⁴C]leucine by brain slices from suckling rats, the stimulatory effects of glucose on the metabolism of l -[U-¹⁴C]leucine were markedly reduced in the presence of dl -3-hydroxybutyrate. The stimulatory effect of glucose on leucine oxidation was, however, not observed in adult rat brain. Furthermore, the incorporation of leucine-carbon into cerebral lipids and proteins was also very low in the adult brain. The incorporation of l -[U-¹⁴C]leucine into cerebral lipids by cortex slices was higher during the first 2 postnatal weeks, which then declined to the adult level. During this time span, the oxidation of l -[U-¹⁴C]leucine to CO₂ remained relatively unchanged. The incorporation in vivo of D-3-hydroxy[3-¹⁴C]butyrate into cerebral lipids was markedly decreased by acute hyperleucinemia induced by injecting leucine into 9-day old rats. In in vitro experiments, 5 mM-leucine had no effect on the oxidation of [U-¹⁴C]glucose to CO₂ or its incorporation into lipids by brain slices from 1-week old rats. However, 5 mM-leucine inhibited the oxidation of d -3-hydroxy-[3-¹⁴C]butyrate, [3-¹⁴C]acetoacetate and [1-¹⁴C]acetate to CO₂ by brain slices, but their incorporation into cerebral lipids was not affected by leucine. In contrast 2-oxo-4-methylvalerate, a deaminated metabolite of leucine, markedly inhibited both the oxidation to CO₂ and the incorporation into lipids of labelled glucose, ketone bodies and acetate by cortex slices from 1-week old rats. These findings suggest that the reduction in the incorporation in vivo of d -3-hydroxy[3-¹⁴C]butyrate into cerebral lipids in rats injected with leucine is most likely caused by 2-oxo-4-methylvalerate formed from leucine. Since the concentrations of leucine and 2-oxo-4-methylvalerate in plasma of untreated patients with maple-syrup urine disease are markedly elevated, our findings are compatible with the possibility that an alteration in the metabolism of glucose and ketone bodies in the brain may contribute to the pathophysiology of this disease.     

Arginine Metabolism in Developing Soybean Cotyledons: III. Utilization

Tracerkinetic experiments were performed using l-[guanidino-¹⁴C]arginine, l-[U-¹⁴C]arginine, l-[ureido-¹⁴C]citrulline, and l-[1-¹⁴C]ornithine to investigate arginine utilization in developing cotyledons of Glycine max (L.) Merrill. Excised cotyledons were injected with carrier-free ¹⁴C compounds and incubated in sealed vials containing a CO₂ trap. The free and protein amino acids were analyzed using high performance liquid chromatography and arginine-specific enzyme-linked assays. After 4 hours, 75% and 90% of the ¹⁴C metabolized from [guanidino-¹⁴C]arginine and [U-¹⁴C]arginine, respectively, was in protein arginine. The net protein arginine accumulation rate, calculated from the depletion of nitrogenous solutes in the cotyledon during incubation, was 17 nanomoles per cotyledon per hour. The data indicated that arginine was also catabolized by the arginase-urease reactions at a rate of 5.5 nanomoles per cotyledon per hour. Between 2 and 4 hours ¹⁴CO₂ was also evolved from carbons other than C-6 of arginine at a rate of 11.0 nanomoles per cotyledon per hour. It is suggested that this extra ¹⁴CO₂ was evolved during the catabolism of ornithine-derived glutamate; ¹⁴C-ornithine was a product of the arginase reaction. A model for the estimated fluxes associated with arginine utilization in developing soybean cotyledons is presented.     

Ontogenetic Study of the Effects of Energetic Nutrients on Amino Acid Metabolism of Rat Cerebral Cortex

We studied the effect of various energetic nutrients on metabolism of l-[U-¹⁴C]leucine and [1–¹⁴C]glycine in cerebral cortex of rats at different ages. At gestational age, glucose and lactate stimulated protein synthesis from l-[U-¹⁴C]leucine and [1–¹⁴C]glycine and from l-[U-¹⁴C]leucine, respectively; glucose, -OH-butyrate and lactate stimulated lipid synthesis from l-[U-¹⁴C]leucine. At 10 days of age, glucose, mannose, and fructose stimulated protein synthesis, and glucose and mannose stimulated oxidation to CO₂ as well as lipid synthesis from l-[U-¹⁴C]leucine. In adult rats, glucose, mannose, and fructose stimulated protein synthesis from l-[U-¹⁴C]leucine and [1–¹⁴C]glycine; glutamine also markedly decreased the oxidation of l-[U-¹⁴C]leucine and [1–¹⁴C]glycine in 10–day-old and adult rats.     

Interrelations between sulfate-reducing and methane-producing bacteria in bottom deposits of a fresh-water lake. III. Experiments with 14C-labeled substrates

An ecological substrate relationship between sulfate-reducing and methane-producing bacteria in mud of Lake Vechten has been studied in experiments using ¹⁴C-labeled acetate and lactate as substrates. Fluoroacetate strongly inhibited the formation of ¹⁴CO₂ from [U-¹⁴C]-acetate and β-fluorolactate gave an inhibition of similar magnitude of the breakdown of [U-¹⁴C]-l-lactate to ¹⁴CO₂ thus confirming earlier results on the specific action of these inhibitors. The turnover-rate constant of l-lactate was 2.37 hr^-1 and the average l-lactate pool size was 12.2 μg per gram of wet mud, giving a turnover rate of 28.9 μg of lactate/gram of mud per hr. The turnover-rate constant of acetate was 0.35 hr^-1 and the average pool size was 5.7 μg per gram of wet mud, giving a rate of disappearance of 1.99 μg of acetate/gram of mud per hr. Estimations of the acetate turnover rate based upon the formation of ¹⁴CO₂ from [U-¹⁴C]-acetate or [1-¹⁴C]-acetate yielded figures of the same magnitude (range 0.45 to 1.74). These and other results suggest that only a portion of the lactate dissimilated is turned over through the acetate pool. The ratio of ¹⁴CO₂/¹⁴CH₄ produced from [U-¹⁴C]-acetate by mud was 1.32; indicating that 0.862 moles of CH₄ and 1.138 moles of CO₂ are formed per mole of acetate. From the rate of disappearance of acetate (0.027 μmoles/gram wet mud per hr) and the rate of methane production (0.034 μmoles/gram wet mud per hr), it may be concluded that acetate is an important precursor of methanogenesis in mud (approximately 70%). A substrate relationship between the two groups of bacteria is likely since ¹⁴CH₄ was formed from [U-¹⁴C]-l-lactate.     

Glycine,Serine, and Leucine Metabolism in Different Regions of Rat Central Nervous System

We have investigated the glycine, serine and leucine metabolism in slices of various rat brain regions of 14-day-old or adult rats, using [1-¹⁴C]glycine, [2-¹⁴C]glycine, L-[3-¹⁴C]serine and L-[U-¹⁴C]leucine. We showed that the [1-¹⁴C]glycine oxidation to CO₂ in all regions studied occurs almost exclusively through its cleavage system (GCS) in brains of both 14-day-old and adults rats. In 14-day-old rats, the highest oxidation of [1-¹⁴C]glycine was in cerebellum and the lowest in medulla oblongata. In these animals, the L-[U-¹⁴C]leucine oxidation was lower than the [1-¹⁴C]glycine oxidation, except in medulla oblongata where both oxidations were the same. Serine was the amino acid that showed lowest oxidation to CO₂ in all structure studied. In adult rats brains, the highest oxidation of [1-¹⁴C]glycine was in cerebral cortex and the lowest in medulla oblongata. We have not seen difference in the lipid synthesis from both glycine labeled, neither in 14-day-old rats nor in adult ones, indicating that the lipids formed from glycine were not neutral. Lipid synthesis from serine was significantly high than lipid synthesis and from all other amino acids studied in all studied structures. Protein synthesis from L-[U-¹⁴C]leucine was significantly higher than that from glycine in all regions and ages studied.     

INTERACTION OF LEUCINE, GLUCOSE, AND KETONE METABOLISM IN RAT BRAIN IN VITRO

Brain cortex slices from fed, 48 h and 120 h fasted rats were incubated and ¹⁴CO₂ was measured from (a) [U-¹⁴C]glucose (5 mm ) either alone or in the presence of l -lcucine (0.1 or 1 mm ), and (b) [U-¹⁴C]leucine or [l-¹⁴C]leucine at 0.1 or 1 mm with or without glucose (5 mm ). In other experiments, sodium dl -3-hydroxybutyrate (3-OHB) or acetoacetate (AcAc) at 1 or 5 mm were added in the above incubation mixture. The rate of conversion of [U¹⁴C]glucose to CO₂ was decreased 20% by leucine at 1 mm and 30–50% by 3-OHB at 1 or 5 mm but not by leucine at 0.1 mm . The effects of 3-OHB and of leucine (1 mm ) were not additive. The effects of leucine were similar in the fed and fasted rats. The rate of conversion of [U-¹⁴C]leucine or [l-^,4C]leucine to ¹⁴CO₂ at 0.1 mm and 1.0 mm was increased by glucose (35%) in the fed or fasted rats. Ketone bodies in the absence of glucose had no effect on leucine oxidation. However, the stimulatory effect of glucose on the rate of conversion of leucine to CO₂ was inhibited by 3-OHB at 5 mm . These results suggest that (a) leucine in increased concentrations (1 mm ) may reduce glucose oxidation by brain cortex while itself becoming an oxidative fuel for brain, and (b) leucine oxidation by brain may be influenced by the prevailing glucose and ketone concentrations.     

Glucose handling by hepatocytes from obese Zucker rats

Hepatocytes isolated from obese Zucker rats showed a significantly higher rate of both [U-¹⁴C]glucose and [U-¹⁴C]lactate incorporation into [¹⁴C]lipid than those from their lean counterparts. This was associated with a marked increase in the lipogenic rate measured by the incorporation of³H₂O into the cell esterified fatty acids. Although there were no changes in the incorporation of the tracer into either [¹⁴C]glycogen or¹⁴CO₂, the [¹⁴C] total uptake was significantly higher in the obese animals. The high rate of [¹⁴C]lipid synthesis from glucose was observed both at 15 and 30 mM substrate concentrations and was linked to an enhanced uptake of the tracer into the cell as measured using the decarboxilation of [1-¹⁴C]glucose in the presence of phenazine methosulphate. The presence of insulin in the incubation medium had no effect on the uptake of glucose by the liver cells. However, the large uptake of glucose by the hepatocytes from the obese animals was not related to an enhanced rate of transport as measured using 3-O-methyl[U-¹⁴C]glucose. The activity of glucose-6-phosphate dehydrogenase together with a higher [1-¹⁴C]glucose/[U-¹⁴C]glucose descarboxylation ratio indicate a predominant very active pentose phosphate pathway which may be responsible for the enhanced glucose uptake observed in the hepatocytes from the obese animals.     

The input and fate of new C in two forest soils under elevated CO2

The aim of this study was to estimate (i) the influence of different soil types on the net input of new C into soils under CO₂ enrichment and (ii) the stability and fate of these new C inputs in soils. We exposed young beech–spruce model ecosystems on an acidic loam and calcareous sand for 4 years to elevated CO₂. The added CO₂ was depleted in ¹³C, allowing to trace new C inputs in the plant–soil system. We measured CO₂‐derived new C in soil C pools fractionated into particle sizes and monitored respiration as well as leaching of this new C during incubation for 1 year. Soil type played a crucial role in the partitioning of C. The net input of new C into soils under elevated CO₂ was about 75% greater in the acidic loam than in the calcareous sand, despite a 100% and a 45% greater above‐ and below‐ground biomass on the calcareous sand. This was most likely caused by a higher turnover of C in the calcareous sand as indicated by 30% higher losses of new C from the calcareous sand than from the acidic loam during incubation. Therefore, soil properties determining stabilization of soil C were apparently more important for the accumulation of C in soils than tree productivity. Soil fractionation revealed that about 60% of the CO₂‐derived new soil C was incorporated into sand fractions. Low natural ¹³C abundance and wide C/N ratios show that sand fractions comprise little decomposed organic matter. Consistently, incubation indicated that new soil C was preferentially respired as CO₂. During the first month, evolved CO₂ consisted to 40–55% of new C, whereas the fraction of new C in bulk soil C was 15–23% only. Leaching of DOC accounted for 8–23% of the total losses of new soil C. The overall effects of CO₂ enrichment on soil C were small in both soils, although tree growth increased significantly on the calcareous sand. Our results suggest that the potential of soils for C sequestration is limited, because only a small fraction of new C inputs into soils will become long‐term soil C.     

GLUCOSE AND AMINO ACID METABOLISM IN SOME INVERTEBRATE NERVOUS SYSTEMS

(1) The in vitro metabolism of [U-¹⁴C]glucose and [U-¹⁴C]glutamate was compared in snail, octopus and locust ganglia, and in rat cerebral cortex. (2) The metabolic patterns are quantitatively similar. The major labelled metabolites formed from glucose or glutamate by rat cortex and the invertebrate systems were CO₂, aspartate, glutamate, glutamine and alanine. γ-Aminobutyric acid (GABA) was formed in substantial amounts only by locust and rat. (3) A much larger proportion of labelled glucose and glutamate was converted to alanine by the invertebrates compared with rat cortex, although ¹⁴CO₂ production was lower. (4) The effect of glucose in reducing aspartate formation and stimulating glutamine formation from [U-¹⁴C]glutamate in mammalian cortex was observed in the locust but not in the molluscs. (5) Labelled citric acid cycle intermediates were formed in substantial quantities from glucose and glutamate only by snail and locust.