Biosynthesis of piperlongumine

The incorporation of l-[U-¹⁴C]lysine and l-[U-¹⁴C]phenylalanine into piperlongumine has been demonstrated in Piper longum. The subsequent stepwise degradation to methyl-(3,4,5-trimethoxyphenyl)-propanoate and δ-aminovaleric acid revealed that the C₆-C₃ moiety of the alkamide arises from phenylalanine; the heterocyclic ring is biosynthesised from lysine. It has also been shown that dl-[2-¹⁴C]tyrosine and [2-¹⁴C]sodium acetate are poor precursors of piperlongumine.     

Studies on the biosynthesis of coenzyme F420 in methanogenic bacteria

Coenzyme F₄₂₀ is a 8-hydroxy-5-deazaflavin present in methanogenic bacteria. We have investigated whether the pyrimidine ring of the deazaflavin originates from guanine as in flavin biosynthesis, in which the pyrimidine ring of guanine is conserved. For this purpose the incorporation of [2-¹⁴C]guanine and of [8-¹⁴C]guanine into F₄₂₀ by growing cultures of Methanobacterium thermoautotrophicum was studied. Only in the case of [2-¹⁴C]guanine did F₄₂₀ become labeled. The specific radioactivity of the deazaflavin and of guanine isolated from nucleic acids of [2-¹⁴C]guanine grown cells were identical. This finding suggests that the pyrimidine ring of the deazaflavin and of flavins are synthesized by the same pathway.F₄₂₀ did not become labeled when M. thermoautotrophicum was grown in the presence of methyl-[¹⁴C] methionine, [U-¹⁴C]phenylalanine or [U-¹⁴C]tyrosine. This excludes that C-5 of the deazaflavin is derived from the methyl group of methionine and that the benzene ring comes from phenylalanine or tyrosine.     

Incorporation of various putative precursors into cuticular 3,4-dihydroxyphenylacetic acid of adult Tenebrio molitor

Post-emergence levels of 3,4-dihydroxyphenylacetic acid (DOPAC) and ketocatechol were determined in cuticle from adult Tenebrio molitor. Possible pathways for biosynthesis of DOPAC were studied by comparing the incorporation of injected [U-¹⁴C]tyrosine, [7-¹⁴C]dopamine, [7-¹⁴C]DOPA, [7-¹⁴C]tyramine, [U-¹⁴C]p-hydroxyphenylpyruvic acid (p-HPPA) and [ring-³H]p-hydroxyphenylacetic acid (p-HPAA) into cuticular DOPAC during its period of maximal increase 1–3 days after adult emergence. Increased incorporation of [U-¹⁴C]tyrosine between days 0 and 3 suggests rapid de novo biosynthesis of DOPAC from this primary precursor. Of the putative intermediates tested, only p-HPPA had a pattern of incorporation similar to that seen with tyrosine. Since p-HPAA was poorly incorporated into both cuticle and DOPAC, a tentative pathway tyrosine → p-HPPA → 3,4-dihydroxyphenylpyruvic acid → DOPAC is proposed.     

Biosynthesis of the 3-benzylchroman-4-one eucomin in Eucomis bicolor

Feeding experiments have demonstrated the specific incorporation of radioactivity from dl-phenylalanine-[1-¹⁴C], l-phenylalanine-[U-¹⁴C], sodium acetate-[2-¹⁴C] and l-methionine-[methyl-¹⁴C] into the 3-benzylchroman-4-one eucomin in Eucomis bicolor. The labelling patterns indicate that eucomin is biosynthesized by the addition of a carbon atom derived from methionine onto a C₁₅ chalcone-type skeleton. Radioactivity from 2′,4′,4-trihydroxy-6′-methoxychalcone-[methyl-¹⁴C] and 2′,4′-dihydroxy-4,6′-dimethoxychalcone-[6′-methyl-¹⁴C] was incorporated into eucomin, the latter compound being the better precursor, demonstrating the feasibility that 2′-methoxychalcones are biosynthetic precursors of the “homoisoflavonoids”. Possible biosynthetic relationships in this class of compounds are discussed.     

The involvement of sucrose,glucose and other metabolites in the synthesis of triterpenes and dopa in the laticifers of Euphorbia lathyris

A quantitative triterpene analysis was made of latex stem tissue of Euphorbia lathyris. Young plants seedlings of E. lathyris were incubated with various labelled precursors. Incorporation into triterpenes was obtained from [2-¹⁴C]mevalonic acid, [1-¹⁴C]acetate, [3-¹⁴C]pyruvate, [U-¹⁴C]sucrose, [U-¹⁴C]glucose, [U-¹⁴C]xylose, [U-¹⁴C]glyoxylate, [2,3-¹⁴C]succinic acid, [1-¹⁴C]glycerol [U-¹⁴C]serine. Both sugars tyrosine appeared to be effective precursors in DOPA synthesis inside the laticifers. Exogenously supplied mevalonic acid was only involved in triterpene synthesis outside the laticifers. GC-RC of triterpenes synthesized from [U-¹⁴C]glucose revealed the origin of these compounds in the latex. The labelled triterpenes obtained after incorporation of the other mentioned labelled precursors were only partly synthesized in the laticifers. For quantitative data on latex triterpene synthesis seedlings were incubated with [U-¹⁴C]sucrose, [U-¹⁴C]glucose, [U-¹⁴C]xylose [1-¹⁴C]acetate in the presence of increasing amounts of unlabelled substrate. From the amount of ¹⁴C incorporated into the triterpenes the amount of substrate directly involved in triterpene synthesis was calculated, as was the absolute triterpene yield. Sucrose showed the highest triterpene yield, equivalent to the daily increase of the triterpene content of growing seedlings. The possible significance of the other precursors in triterpene synthesis in the laticifers is discussed.     

Biosynthesis of the 2-arylbenzofuran phytoalexin vignafuran in Vigna unguiculata

Feeding experiments using l-phenylalanine-[U-¹⁴C], dl-phenylalanine-[1-¹⁴C] and -[2-¹⁴C] together with degradative studies have been used to investigate the biosynthesis of the 2-arylbenzofuran phytoalexin vignafuran in UV-treated seedlings of cowpea (Vigna unguiculata). During the biosynthetic process, C-3 of phenylalanine appears to be lost, and the resulting labelling pattern is consistent with vignafuran being derived from an isoflavonoid precursor, but the phenylalanine-derived aromatic ring becomes the 2-aryl substituent and not part of the benzofuran system. A previously proposed pathway to 2-arylbenzofurans by loss of C-6 from a coumestan is thus excluded. Alternative routes are suggested.     

Metabolism of phenylpropanoids in Hydrangea serrata var. thunbergii and the biosynthesis of phyllodulcin

DL-Phenylalanine-[3-¹⁴C] and cinnamic acid-[3-¹⁴C] were fed to this plant and the label from cinnamic acid was incorporated into gallic acid, phyllodulcin and quercetin. By feeding p- coumaric acid-[U-³H], caffeic acid-[U-³H] and hydrangea glucoside A-[U-³H], it was possible to show that hydroxylation at C-3′in phyllodulcin occurs after the ring closure of dihydroisocoumarin. The biosynthetic pathway of phyllodulcin in this plant is thus: phenylalanine → cinnamic acid → p- coumaric acid → hydrangenol → phyllodulcin.     

Incorporation of shikimate and 4-(2′-carboxyphenyl)-4-oxobutyrate into phylloquinone

The patterns of incorporation of d-[G-¹⁴C]shikimate and variously labelled ¹⁴C-4-(2′-carboxy-phenyl)-4-oxobutyrate into the naphthoquinone nucleus of phylloquinone by maize shoots have been investigated. The results show that (a) the alicyclic ring and C-7 of shikimate give rise to Ring A and either C-1 or C-4, and (b) the phenyl ring, 2′-carboxy and C-4, and C-2 and -3 of 4-(2′-carboxyphenyl)-4-oxobutyrate give rise to Ring A, C-1 and -4 and C-2 and -3. Radioactivity from α-[1-¹⁴C]naphthol, 1,4-[1,4-¹⁴C]naphthoquinone and [Me-¹⁴C]menadione is not incorporated into phylloquinone to any significant extent.     

The stereochemistry of biosynthesis of decaprenoxanthin in a cell-free system

Intact cells of Flavobacterium dehydrogenans grown on glucose or acetate did not incorporate mevalonic acid-[¹⁴C]. After treatment with lysozyme the protoplasts were lysed by sonication in a dilute medium containing mevalonic acid-[¹⁴C] and the cell-free system produced incorporated label into uncyclized C₄₀, monocyclic C₄₅ and bicyclic C₅₀ carotenoids of which decaprenoxanthin was the most abundant.With mevalonate-[2-¹⁴C,4R-4-³H₁] the ¹⁴C:³H ratios of the carotenoids showed that the hydrogen atoms at C-2 and C-6 of the ring and that at C-3 of the 1-hydroxy, 2-methyl but-2-ene-4-yl residues of decaprenoxanthin were derived from the 4-pro-R hydrogen atom of mevalonic acid.Mevalonate-[2-¹⁴C,2R-2-³H₁] and mevalonate-[2-¹⁴C,2S-2-³H₁] gave ratios which showed that the C-4 hydrogen atoms of decaprenoxanthin were derived from the 2-pro-S hydrogen atom of mevalonic acid.     

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.     

Metabolism of [2-3H]- and [6-3H]-nicotinic acid in intact Nicotiana tabacum plants

Earlier observations of Dawson on the relative incorporation of [2-³H]- and [6-³H]-nicotinic acid into nicotine have been confirmed in intact Nicotiana tabacum plants. All the tritium in the nicotine derived from [2-³H]-nicotinic acid was located at C-2 of the pyridine ring. However the radioactive nicotine derived from [6-³H]-nicotinic acid was not labelled specifically at C-6 with tritium. By carrying out feeding experiments with [6-¹⁴-C, 2-³H]- and [6-¹⁴C, ³H]-nicotinic acids, it was established that there was very little loss of tritium from C-2 and C-6 of nicotinic acid during 5 days of metabolism in the tobacco plant.     

The biosynthesis of the thiazole moiety of thiamine in Salmonella typhimurium

The mechanism of biosynthesis of 4-methyl-5-β-hydroxyethyl thiazole, the thiazole moiety of thiamine was studied in Salmonella typhimurium. Using the adenosine derepression technique the incorporation of various ¹⁴C-labeled precursors was determined. We found that [Me-¹⁴C]methionine, [2-¹⁴C]methionine, [U-¹⁴C]alanine, and [2-¹⁴C]glycine were not incorporated whereas [2-¹⁴C]-tyrosine was incorporated. Degradation of the 4-methyl-5-β-hydroxyethyl thiazole obtained after [2-¹⁴C]tyrosine incorporation revealed that all of the activity was located on carbon-2. These findings are discussed and compared with previous findings concerning 4-methyl-5-β-hydroxyethyl thiazole biosynthesis.     

Biosynthesis of dioscorine : Incorporation of nicotinic acid into the isoquinuclidine moiety

The administration of nicotinic-[2-¹⁴C] acid to Dioscorea hispida plants afforded radioactive dioscorine (1.9% absolute incorporation) and a systematic degradation of the alkaloid indicated that essentially all the activity was located at C-3. Dioscorine derived from nicotinic-[5,6-¹⁴C, ¹³C₂] acid was also labelled. Its proton noise decoupled ¹³C NMR spectrum contained satellites at C-1 and C-7 due to spin-spin coupling of contiguous ¹³C atoms arising from direct incorporation of the labelled nicotinic acid. A biosynthetic scheme representing a novel utilization of nicotinic acid is proposed.     

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.     

Studies on the biosynthesis of phenols in fungi. Production of 4-methoxytoluquinol, epoxysuccinic acid and a diacetylenic alcohol by surface cultures of Lentinus degener I.M.I. 110525

1. 4-Methoxytoluquinol was secreted into the medium by surface cultures of the basidiomycete Lentinus degener Kalchbr. (approx. 100mg./l. of medium). In addition, epoxysuccinic acid (150–200mg.) and a long-chain diacetylenic alcohol (3mg.) were also secreted. Epoxysuccinic acid has previously been found in the culture medium of some Fungi Imperfecti. These metabolites were all synthesized during the early phase of growth but maximum production occurred some time later. 2. Supplementation of the medium with cycloheximide or 8-azaguanine inhibited the production of epoxysuccinic acid. 3. Sodium [1-¹⁴C]acetate and 6-methyl[¹⁴C]salicylic acid were not incorporated into 4-methoxytoluquinol, but [U-¹⁴C]tyrosine and [Me-¹⁴C]methionine were incorporated to the extent of 0·55 and 4·75% respectively (minimum values). Degradation studies established that the aromatic ring and C-methyl group were derived from the ring and β-carbon atom of tyrosine; the O-methyl group alone was formed from methionine.     

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     

The incorporation of ornithine-[2,3-13C2] into nicotine and nornicotine established by NMR

dl-Ornithine-[2,3-¹³C₂] was synthesized from acetate-[1-¹³C] and ethyl acetamidocyanoacetate-[2-¹³C]. This labelled material was mixed with dl-ornithine-[5-¹⁴C] and fed to Nicotiana glutinosa plants by the wick method. After 10 days the plants were harvested affording radioactive nicotine and nornicotine (0.14% and 0.051% specific incorporations, respectively). Even at these low specific incorporations an examination of their ¹³C NMR spectra established the incorporation of ornithine symmetrically into the pyrrolidine rings of these alkaloids. Satellites were observable at the signals due to C-2′, 3′, 4′ and 5′ positions, arising by the presence of contiguous carbons at C-2′, 3′ and C-4′, 5′.     

Substrate utilization for energy production and lipid synthesis in oligodendrocyte-enriched cultures prepared from rat brain

The metabolism of oligodendrocytes has been studied using cultures of oligodendrocyte-enriched glial cells isolated from cerebra of 5–8-day old rats. Cultures containing 60–80% oligodendrocytes were incubated for 16h with [3-¹⁴C]acetoacetate, d-[3-¹⁴C]3-hydroxybutyrate, [U-¹⁴C]glucose, l-[U-¹⁴C]glutamine and [1-¹⁴C]pyruvate or [2-¹⁴C]pyruvate in the presence or absence of other oxidizable substrates. Labelled CO₂ was collected as an index of oxidative metabolism and the incorporation of label into total lipids, fatty acids and cholesterol was used as an index of the de novo synthesis of lipids. Glucose, acetoacetate, D-3-hydroxybutyrate, pyruvate and l-lactate were measured to determine substrate utilization and product formation under various conditions. Our results indicate that glucose is rapidly converted to lactate and is a relatively poor substrate for oxidative metabolism and lipid synthesis. Ketone bodies were used as an energy source and as precursors for the synthesis of fatty acids and cholesterol. Preferential incorporation of acetoacetate into cholesterol was not observed. Exogenous pyruvate was incorporated into both the glycerol skeleton of complex lipids and into cholesterol and fatty acids. l-Glutamine appeared to be an important substrate for the energy metabolism of these cells.     

Biosynthesis of p-hydroxybenzoic acid in poplar lignin

Biosynthetic pathways to p-hydroxybenzoic acid in polar lignin were examined by tracer experiments. High incorporation of radioactivity to the acid was observed when shikimic acid-[1-¹⁴C], phenylalanine-[3-¹⁴C], trans-cinnamic acid-[3-¹⁴C], p-coumaric acid-[3-¹⁴C] and p-hydroxybenzoic acid-[COOH-¹⁴C] were administered, while incorporation was low from shikimic acid-[COOH-¹⁴C], phenylalanine-[1-¹⁴C], phenylalanine-[2-¹⁴C], tyrosine-[3-¹⁴C], benzoic acid-[COOH-¹⁴C], sodium acetate-[1-¹⁴C] and d-glucose-[U-¹⁴C]. Thus p-hydroxybenzoic acid in poplar lignin is formed mainly via the pathway: shikimic acid → phenylalanine → trans-cinnamic acid → p-coumaric acid → p-hydroxybenzoic acid.