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.     

Metabolic pools associated with monoterpene biosynthesis in higher plants

Partial degradations of (+)-isothujone biosynthesised in Tanacetum vulgare after feeding IPP-[4-¹⁴C], DMAPP-[4-¹⁴C] or 3,3-dimethylacrylate-[Me-¹⁴C], and of geraniol and (+)-pulegone formed in Pelargonium graveolens and Mentha pulegium respectively after uptake of 3,3-dimethylacrylate-[Me-¹⁴C], indicated that none of these metabolites was a direct source of the part of the monoterpene skeleton derived hypothetically from DMAPP. Uptake of glucose-[U¹⁴C] into P. graveolens led, in contrast, to both IPP and DMAPP-derived moieties of geraniol being extensively labelled. Feeding of l-valine-[U-¹⁴C] and l-leucine-[U-¹⁴C] to all three plants resulted in negligible incorporation of tracer into monoterpenes. A soluble enzyme system prepared from foliage of T. vulgare that had been exposed to CO₂-[¹⁴C] for 20 days converted isotopically-normal IPP into GPP with the DMAPP-derived portion containing essentially all (>98%) of the radioactivity present. These observations and those previously obtained from feeding experiments with other [¹⁴C]-labelled precursors on the same plant species are consistent with the occurrence of two metabolic pools of intermediates for monoterpene biosynthesis, one of which is probably protein-bonded.     

Characterization of [14C]apiogalacturonans synthesized in a cell-free system from Lemna minor.

Radioactive polysaccharide was synthesized when uridine 5′-(α-d-[U-¹⁴C]apio-d-furanosyl pyrophosphate) (containing some uridine 5′-(α-d-[U-¹⁴C]xylopyranosyl pyrophosphate)) was incubated with a particulate enzyme preparation from Lemna minor. Characterization experiments established that the product: (i) was insoluble in methanol and water, (ii) contained d-[U-¹⁴C]apiose (75%) and d-[U-¹⁴C]xylose (25%), and (iii) was soluble in 1% ammonium oxalate. The material solubilized by ammonium oxalate (solubilized product): (i) was separated into five fractions by column chromatography with diethylaminoethyl-Sephadex (DEAE-Sephadex), (ii) contained [U-¹⁴C]apiobiose side chains that were removed by hydrolysis at pH 4, and (iii) was degraded by fungal pectinase. Both d-[U-¹⁴C]apiose residues of the [U-¹⁴C]apiobiose side chains were synthesized in vivo since radioactivity was distributed equally between the two residues. The presence of uridine 5′-(α-d-galactopyranosyluronic acid pyrophosphate) during synthesis of radioactive polysaccharide resulted in: (i) an increase in the incorporation of radioactive d-[U-¹⁴C]apiose into solubilized product, (ii) an increase in the ratio of d-[U-¹⁴C]apiose to d-[U-¹⁴C]xylose present in solubilized product, (iii) an increase in the amount of [U-¹⁴C]apiobiose plus d-[U-¹⁴C]apiose released from the solubilized product by hydrolysis at pH 4, and (iv) a tighter binding of the solubilized product to DEAE-Sephadex. These results show that apiogalacturonans similar to or the same as those synthesized by the intact plant were synthesized in the particulate enzyme preparation isolated from L. minor. [¹⁴C]Apiogalacturonans completely free of d-[U-^l4C]xylose were not isolated. The [¹⁴C]apiogalacturonan with the least d-[U-¹⁴C]xylose still had 4.8% of its radioactivity present in d-[U-¹⁴C]xylose. The possibility remains that d-xylose is a normal constituent of the apiogalacturonans of the cell wall of L. minor.     

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.     

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.     

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 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.     

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.     

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.     

Metabolism of glycerol-1,2,3-trimethylsuccinate in rat hepatocytes

The metabolism of glycerol-1,2,3-trimethylsuccinate ester was investigated in rat hepatocytes. The ester displayed a greater nutritional value than D-glucose, as a precursor of either CO₂ or glycogen. In terms of ¹⁴CO₂ production, the value calculated from experiments conducted in the presence of 1.9 mM [U-¹⁴C] glycerol-1,2,3-trimethylsuccinate, glycerol-1,2,3-trimethyl[1,4-¹⁴C] succinate and glycerol- 1,2,3-trimethyl[2,3-¹⁴C] succinate represented about 50 times that found in cells incubated with 1.0 mM D-[U-¹⁴C] glucose. For glycogen synthesis, the results found with the ester were approximately 7-8 times higher than those found with the hexose. A further advantage of the ester over D-glucose consisted in the fact that, at increasing concentrations of these nutrients, a maximal metabolic response may be reached at lower levels of glycerol-1,2,3-trimethylsuccinate than D-glucose. By comparison with previous data obtained in the same experimental model, glycerol-1,2,3-trimethylsuccinate was also found to display a higher nutritional value than the dimethyl ester of succinic acid. It is proposed, therefore, that glycerol-1,2,3-trimethylsuccinate could be used to support ATP generation in cells endangered by an imbalance between the rate of synthesis and hydrolysis of this adenine nucleotide.     

Biodegradation of Nitro-Substituted Explosives 2,4,6-Trinitrotoluene, Hexahydro-1,3,5-Trinitro-1,3,5-Triazine, and Octahydro-1,3,5,7-Tetranitro-1,3,5-Tetrazocine by a Phytosymbiotic Methylobacterium sp. Associated with Poplar Tissues (Populus deltoides × nigra DN34)

A pink-pigmented symbiotic bacterium was isolated from hybrid poplar tissues (Populus deltoides × nigra DN34). The bacterium was identified by 16S and 16S-23S intergenic spacer ribosomal DNA analysis as a Methylobacterium sp. (strain BJ001). The isolated bacterium was able to use methanol as the sole source of carbon and energy, which is a specific attribute of the genus Methylobacterium. The bacterium in pure culture was shown to degrade the toxic explosives 2,4,6-trinitrotoluene (TNT), hexahydro-1,3,5-trinitro-1,3,5-triazene (RDX), and octahydro-1,3,5,7-tetranitro-1,3,5-tetrazocine (HMX). [U-ring-¹⁴C]TNT (25 mg liter⁻¹) was fully transformed in less than 10 days. Metabolites included the reduction derivatives amino-dinitrotoluenes and diamino-nitrotoluenes. No significant release of ¹⁴CO₂ was recorded from [¹⁴C]TNT. In addition, the isolated methylotroph was shown to transform [U-¹⁴C]RDX (20 mg liter⁻¹) and [U-¹⁴C]HMX (2.5 mg liter⁻¹) in less than 40 days. After 55 days of incubation, 58.0% of initial [¹⁴C]RDX and 61.4% of initial [¹⁴C]HMX were mineralized into ¹⁴CO₂. The radioactivity remaining in solution accounted for 12.8 and 12.7% of initial [¹⁴C]RDX and [¹⁴C]HMX, respectively. Metabolites detected from RDX transformation included a mononitroso RDX derivative and a polar compound tentatively identified as methylenedinitramine. Since members of the genus Methylobacterium are distributed in a wide diversity of natural environments and are very often associated with plants, Methylobacterium sp. strain BJ001 may be involved in natural attenuation or in situ biodegradation (including phytoremediation) of explosive-contaminated sites.     

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.     

Characterization of particulate D-apiosyl-and D-xylosyltransferase from Lemna minor.

A particulate enzyme preparation capable of catalyzing the transfer of d-[U-¹⁴C]apiose and d-[U-¹⁴C]xylose from uridine 5′-(α-d-[U-¹⁴C]apio-d-furanosyl pyrophosphate) (UDP[U-¹⁴C]Api) and uridine 5′-(α-d-[U-¹⁴C]xylopyranosyl pyrophosphate) (UDP[U-¹⁴C]Xyl) to endogenous acceptor molecules was isolated from Lemna minor. The two enzymes were named UDP-d-apiose:acceptor d-apiosyltransferase and UDP-d-xylose:acceptor d-xylosyltransferase and were associated with particulate material sedimenting between 480 and 34,800g. The rate of d-[U-¹⁴C]apiose or d-[U-¹⁴C]xylose incorporation was proportional to the quantity of enzyme preparation used and was constant with time to 1.5 min. Both enzymes showed a pH optimum of 5.7 in citrate-phosphate buffer. The d-apiosyltransferase has a K_m for UDP[U-¹⁴C]Api of 4.9 μm. Bovine serum albumin and sucrose stimulated the rate of incorporation of both pentoses. Both enzymes rapidly lost activity; with our best conditions, approximately 50% of each enzyme activity was lost in 6 min at 25 °C or in 3 h at 4 °C. Incorporation of d-[U-¹⁴C]apiose was obtained in the absence of added uridine 5′-(α-d-galactopyranosyluronic acid pyrophosphate) (UDPGalUA); however, the addition of UDPGalUA not only almost doubled the rate of incorporation, but also increased the total incorporation of d-[U-^l4C]apiose and extended the proportional range of incorporation at 25 °C from 1.5 to 2 min.     

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.     

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 BIOSYNTHESIS OF CHOLESTEROL AND OTHER STEROLS BY BRAIN TISSUE: DISTRIBUTION IN SUBCELLULAR FRACTIONS AS A FUNCTION OF TIME AFTER INJECTION OF [2-14C]MEVALONIC ACID, SODIUM [2-14C]ACETATE AND [U-14C]GLUCOSE INTO 15-DAY-OLD RATS

The distribution of [¹⁴C]-labelled material into subcellular fractions of 15-day-old rat brain was studied at 2 and 24 h following intraperitoneal and intracerebral injection of [2-¹⁴C]sodium acetate, [U-¹⁴C]glucose and [2-¹⁴C]mevalonic acid respectively. The total quantity of labelled isoprenoids in the brain was, except for glucose, greater when the precursor was administered intracerebrally. The intraperitoneal route was more advantageous in the case of [U-¹⁴C]glucose. The subcellular distribution of both labelled total isoprenoid material and sterol was distinct for each labelled precursor. Intracerebrally injected [U-¹⁴C]glucose at both time periods studied suggested no dominance of labelling in any fraction. After intraperitoneal injection of [U-¹⁴C]glucose the microsomes were more prominently labelled. Both methods of administration of sodium [2-¹⁴C]acetate resulted in heavy labelling of the myelin fraction after 24 h. The total labelled isoprenoids resided mainly in the microsomes 24 h after injection of [2-¹⁴C]mevalonic acid. Labelled sterol was found to be localized more in the myelin and microsomal fractions for all three precursors than was the labelled total isoprenoids. Depending on the type of experiment to be conducted, each of these precursors can give different results, which must be interpreted accordingly.     

Glutamic Acid metabolism and the photorespiratory nitrogen cycle in wheat leaves: metabolic consequences of elevated ammonia concentrations and of blocking ammonia assimilation

The effects of methionine sulfoximine and ammonium chloride on [¹⁴C] glutamate metabolism in excised leaves of Triticum aestivum were investigated. Glutamine was the principal product derived from [U¹⁴C]glutamate in the light and in the absence of inhibitor or NH₄Cl. Other amino acids, organic acids, sugars, sugar phosphates, and CO₂ became slightly radioactive. Ammonium chloride (10 mm) increased formation of [¹⁴C] glutamine, aspartate, citrate, and malate but decreased incorporation into 2-oxoglutarate, alanine, and ¹⁴CO₂. Methionine sulfoximine (1 mm) suppressed glutamine synthesis, caused NH₃ to accumulate, increased metabolism of the added radioactive glutamate, decreased tissue levels of glutamate, and decreased incorporation of radioactivity into other amino acids. Methionine sulfoximine also caused most of the ¹⁴C from [U-¹⁴C]glutamate to be incorporated into malate and succinate, whereas most of the ¹⁴C from [1-¹⁴C]glutamate was metabolized to CO₂ and sugar phosphates. Thus, formation of radioactive organic acids in the presence of methionine sulfoximine does not take place indirectly through “dark” fixation of CO₂ released by degradation of glutamate when ammonia assimilation is blocked. When illuminated leaves supplied with [U-¹⁴C] glutamate without inhibitor or NH₄Cl were transferred to darkness, there was increased metabolism of the glutamate to glutamine, aspartate, succinate, malate, and ¹⁴CO₂. Darkening had little effect on the labeling pattern in leaves treated with methionine sulfoximine.     

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.     

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