Mineralization of Parathion in the Rice Rhizosphere

We studied ¹⁴CO₂ evolution from ring-labeled [2,6-¹⁴C]parathion (O,O-diethyl-O-p-nitrophenyl phosphorothioate) in the rhizosphere of rice seedlings. The soil samples (nonflooded [60% water-holding capacity] and flooded) were treated first with technical parathion (20 μg/g) and then after 10 days with ring-labeled [¹⁴C]parathion. In unplanted soil, less than 5.5% of the ¹⁴C in the parathion was evolved as ¹⁴CO₂ in 15 days under both flooded and nonflooded conditions. In soil planted with rice, 9.2% of the radiocarbon was evolved as ¹⁴CO₂ under nonflooded conditions, and 22.6% was evolved under flooded conditions. These results suggest that soil planted with rice permits significant ring cleavage, especially under flooded conditions.     

Polymerization of guaiacol by lignin-degrading manganese peroxidase from Bjerkandera adusta in aqueous organic solvents

 Lignin-degrading manganese (II) peroxidase (MnP) purified from the culture of a wood-rotting basidiomycete, Bjerkandera adusta, was used in the polymerization of guaiacol. MnP was found to catalyze polymerization of guaiacol in 50% aqueous acetone, dimethyl formamide, methanol, ethanol, dioxane, acetonitrile, ethylene glycol and methylcellosolve. Maximum yield of polyguaiacol was achieved in 50% aqueous acetone. The weight average molecular weight (M _w) of the polymer was estimated to be 30 300 by gel permeation chromatography. However, matrix-assisted laser desorption ionization time of flight mass spectroscopy (MALDI-TOF-MS) analysis gave a more reliable M _w of 1690. IR, ¹³C-NMR, MALDI-TOF-MS and pyrolysis GC-MS analyses showed the presence of C–C and C–O linkages and quinone structure in polyguaiacol. It was also indicated that polyguaiacol has a methoxy-phenyl group as the terminal moiety. This suggests that polyguaiacol is a branched polymer in which guaiacol units are cross-linked at the phenolic group. Thermal gravimetric and differential scanning calorimetric analyses were also carried out. MnP also catalyzed the polymerization of o-cresol, 2,6-dimethoxyphenol and other phenolic compounds and aromatic amines. M _w of these polymers ranged from around 1000 to 1500. Received: 2 August 1999 / Received revision: 10 December 1999 / Accepted: 4 January 2000     

Thermophilic Anaerobic Biodegradation of [14C]Lignin, [14C]Cellulose, and [14C]Lignocellulose Preparations

Thermophilic (55°C) anaerobic enrichment cultures were incubated with [¹⁴C-lignin]lignocellulose, [¹⁴C-polysaccharide]lignocellulose, and kraft [¹⁴C]lignin prepared from slash pine, Pinus elliottii, and ¹⁴C-labeled preparations of synthetic lignin and purified cellulose. Significant but low percentages (2 to 4%) of synthetic and natural pine lignin were recovered as labeled methane and carbon dioxide during 60-day incubations, whereas much greater percentages (13 to 23%) of kraft lignin were recovered as gaseous end products. Percentages of label recovered from lignin-labeled substrates as dissolved degradation products were approximately equal to percentages recovered as gaseous end products. High-pressure liquid chromatographic analyses of CuO oxidation products of sound and degraded pine lignin indicated that no substantial chemical modifications of the remaining lignin polymer, such as demethoxylation and dearomatization, occurred during biodegradation. The polysaccharide components of pine lignocellulose and purified cellulose were relatively rapidly mineralized to methane and carbon dioxide; 31 to 37% of the pine polysaccharides and 56 to 63% of the purified cellulose were recovered as labeled gaseous end products. An additional 10 to 20% of the polysaccharide substrates was recovered as dissolved degradation products. Overall, these results indicate that elevated temperatures can greatly enhance rates of anaerobic degradation of lignin and lignified substrates to methane and low-molecular-weight aromatic compounds.     

Metabolism of Radiolabeled β-Guaiacyl Ether-Linked Lignin Dimeric Compounds by Phanerochaete chrysosporium

Phanerochaete chrysosporium metabolized the radiolabeled lignin model compounds [γ-¹⁴C]guaiacylglycerol-β-guaiacyl ether and [4-methoxy-¹⁴C]veratrylglycerol-β-guaiacyl ether (VI) to ¹⁴CO₂ in stationary and in shaking cultures. ¹⁴CO₂ evolution was greater in stationary culture. ¹⁴CO₂ evolution from [γ-¹⁴C]guaiacyl-glycerol-β-guaiacyl ether and [4-methoxy-¹⁴C]veratrylglycerol-β-guaiacyl ether in stationary cultures was two- to threefold greater when 100% O₂ rather than air (21% O₂) was the gas phase above the cultures. ¹⁴CO₂ evolution from the metabolism of the substrates occurred only as the culture entered the stationary phase of growth. The presence of substrate levels of nitrogen in the medium suppressed ¹⁴CO₂ evolution from both substrates in stationary cultures. [¹⁴C]veratryl alcohol and 4-ethoxy-3-methoxybenzyl alcohol were formed as products of the metabolism of VI and 4-ethoxy-3-methoxyphenylglycerol-β-guaiacyl ether, respectively.     

Ligninolytic system of Phanerochaete chrysosporium: Inhibition by o-Phthalate

The degradation rate of [synthetic-¹⁴C]-lignin to ¹⁴CO₂ by Phanerochaete chrysosporium in cultures buffered with 0.01 M 2,2-dimethylsuccinate (DMS) was twice that in 0.01 M o-phthalate-buffered cultures. This difference could be totally accounted for by o-phthalate inhibition of the activity of the ligninolytic system. ¹⁴CO₂ production from ring-, sidechain-, and methoxyl-labeled lignins was inhibited, the degree of inhibition being dependent on o-phthalate concentration. Oxidations of ¹⁴C-glucose, ¹⁴C-acetovanillone, and ¹⁴C-apocynol were not inhibited; thus o-phthalate is not a general inhibitor, and might inhibit activities involved in attack of the lignin polymer. DMS is a suitable buffer for the ligninolytic system. Degradation rates of ring-labeled lignin to ¹⁴CO₂ of 10–15% in 24 h were obtained consistently over the pH range 3.6–4.5, with an optimum near pH 4.0.Non-Standard Abbreviations DMS dimethylsuccinate     

Preparation, Characterization, and Microbial Degradation of Specifically Radiolabeled [14C]Lignocelluloses from Marine and Freshwater Macrophytes

Specifically radiolabeled [¹⁴C-lignin]lignocelluloses were prepared from the aquatic macrophytes Spartina alterniflora, Juncus roemerianus, Rhizophora mangle, and Carex walteriana by using [¹⁴C]phenylalanine, [¹⁴C]tyrosine, and [¹⁴C]cinnamic acid as precursors. Specifically radiolabeled [¹⁴C-polysaccharide]lignocelluloses were prepared by using [¹⁴C]glucose as precursor. The rates of microbial degradation varied among [¹⁴C-lignin]lignocelluloses labeled with different lignin precursors within the same plant species. To determine the causes of these differential rates, [¹⁴C-lignin]lignocelluloses were thoroughly characterized for the distribution of radioactivity in nonlignin contaminants and within the lignin macromolecule. In herbaceous plants, significant amounts (8 to 24%) of radioactivity from [¹⁴C]phenylalanine and [¹⁴C]tyrosine were found associated with protein, although very little (3%) radioactivity from [¹⁴C]cinnamic acid was associated with protein. Microbial degradation of radiolabeled protein resulted in overestimation of lignin degradation rates in lignocelluloses derived from herbaceous aquatic plants. Other differences in degradation rates among [¹⁴C-lignin]lignocelluloses from the same plant species were attributable to differences in the amount of label being associated with ester-linked subunits of peripheral lignin. After acid hydrolysis of [¹⁴C-polysaccharide]lignocelluloses, radioactivity was detected in several sugars, although most of the radioactivity was distributed between glucose and xylose. After 576 h of incubation with salt marsh sediments, 38% of the polysaccharide component and between 6 and 16% of the lignin component (depending on the precursor) of J. roemerianus lignocellulose was mineralized to ¹⁴CO₂; during the same incubation period, 30% of the polysaccharide component and between 12 and 18% of the lignin component of S. alterniflora lignocellulose was mineralized.     

Anaerobic Biodegradation of the Lignin and Polysaccharide Components of Lignocellulose and Synthetic Lignin by Sediment Microflora

Specifically radiolabeled [¹⁴C-lignin]lignocelluloses and [¹⁴C-polysaccharide]lignocelluloses were prepared from a variety of marine and freshwater wetland plants including a grass, a sedge, a rush, and a hardwood. These [¹⁴C]lignocellulose preparations and synthetic [¹⁴C]lignin were incubated anaerobically with anoxic sediments collected from a salt marsh, a freshwater marsh, and a mangrove swamp. During long-term incubations lasting up to 300 days, the lignin and polysaccharide components of the lignocelluloses were slowly degraded anaerobically to ¹⁴CO₂ and ¹⁴CH₄. Lignocelluloses derived from herbaceous plants were degraded more rapidly than lignocellulose derived from the hardwood. After 294 days, 16.9% of the lignin component and 30.0% of the polysaccharide component of lignocellulose derived from the grass used (Spartina alterniflora) were degraded to gaseous end products. In contrast, after 246 days, only 1.5% of the lignin component and 4.1% of the polysaccharide component of lignocellulose derived from the hardwood used (Rhizophora mangle) were degraded to gaseous end products. Synthetic [¹⁴C]lignin was degraded anaerobically faster than the lignin component of the hardwood lignocellulose; after 276 days, 3.7% of the synthetic lignin was degraded to gaseous end products. Contrary to previous reports, these results demonstrate that lignin and lignified plant tissues are biodegradable in the absence of oxygen. Although lignocelluloses are recalcitrant to anaerobic biodegradation, rates of degradation measured in aquatic sediments are significant and have important implications for the biospheric cycling of carbon from these abundant biopolymers.     

Determination of sialidase activities in HeLa cells using gangliosides specifically labeled in N-acetylneuraminic acid.

Radioactive gangliosides, N-[¹⁴C]-acetylneuraminylgalactosylglucosylceramide ([¹⁴C]G_M3) and N- [¹⁴C]-acetylneuraminylgalactosyl-N-acetylgalactosaminyl- [N-acetylneuraminyl]-galactosylglucosylceramide ([¹⁴C]G_D1a), were synthesized from CMP-[¹⁴C]sialic acid and the appropriate precursor glycolipid using specific sialyltransferase activities. These compounds were isolated and used as substrates to assay sialidase activity in HeLa cells. Although sodium butyrate added to the culture medium increased G_M3 biosynthesis in HeLa cells, sialidase activity, as well as that of other glycohydrolases, was the same in control and butyrate-treated HeLa cells. The same sialidase activity appeared to hydrolyze both [¹⁴C]G_M3 and [¹⁴C]G_D1a, but not fetuin; the enzyme had a pH optimum of 5.0 and a K_m of 75 μm for the ganglioside substrates. Although the cells contained a high sialidase activity (4–7 nmol/mg of protein/h) and could bind exogenously added [¹⁴C]G_M3, no “ecto”-sialidase activity would be detected in intact cells under conditions where a close to physiological pH is maintained. The results indicate that ganglioside sialidase is not involved directly in the morphological and biochemical differentiation induced in HeLa cells by exposure to sodium butyrate.     

Isolation of a Bacterium Capable of Degrading Peanut Hull Lignin

Thirty-seven bacterial strains capable of degrading peanut hull lignin were isolated by using four types of lignin preparations and hot-water-extracted peanut hulls. One of the isolates, tentatively identified as Arthrobacter sp., was capable of utilizing all four lignin preparations as well as extracted peanut hulls as a sole source of carbon. The bacterium was also capable of degrading specifically labeled [¹⁴C]lignin-labeled lignocellulose and [¹⁴C]cellulose-labeled lignocellulose from the cordgrass Spartina alterniflora and could also degrade [¹⁴C]Kraft lignin from slash pine. After 10 days of incubation with [¹⁴C]cellulose-labeled lignocellulose or [¹⁴C]lignin-labeled lignocellulose from S. alterniflora, the bacterium mineralized 6.5% of the polysaccharide component and 2.9% of the lignin component.     

An aluminoborate cluster [AlB12O14(OH)12]: Synthesis and structure of [C5H6N][AlB12O14(OH)12]

A new aluminoborate, [C₅H₆N][AlB₁₂O₁₄(OH)₁₂], has been hydrothermally synthesized at 200 °C. The single-crystal diffraction study reveals that it crystallizes in space group C2/c. It consists of aluminoborate clusters [AlB₁₂O₁₄(OH)₁₂]⁻ and counterions [C₅H₆N]⁺. The aluminoborate cluster contains an Al(OH)₆ octahedron as a core that is capped by two raft-like polyborate units [B₆O₇(OH)₆]. These clusters are further interlinked by extensive hydrogen bonding to form a three-dimensional (3D) network, containing large channels along the b-axis, in which the [C₅H₆N]⁺ cations are located.     

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.     

New Insights into the Ligninolytic Capability of a Wood Decay Ascomycete

Wood-grown cultures of Daldinia concentrica oxidized a permethylated β-¹⁴C-labeled synthetic lignin to ¹⁴CO₂ and also cleaved a permethylated α-¹³C-labeled synthetic lignin to give C_α-C_β cleavage products that were detected by ¹³C nuclear magnetic resonance spectrometry. Therefore, this ascomycete resembles white-rot basidiomycetes in attacking the recalcitrant nonphenolic structures that predominate in lignin.     

Synthesis of carbon-11-labeled casimiroin analogues as new potential PET agents for imaging of quinone reductase 2 and aromatase expression in breast cancer

Carbon-11-labeled casimiroin analogues were first designed and synthesized as new potential PET agents for imaging of quinone reductase (QR) 2 and aromatase expression in breast cancer. [¹¹C]casimiroin (6-[¹¹C]methoxy-9-methyl-[1,3]dioxolo[4,5-h]quinolin-8(9H)-one, [¹¹C]11) and its carbon-11-labeled analogues 5,6,8-trimethoxy-1-[¹¹C]methyl-4-methylquinolin-2(1H)-one ([¹¹C]17), 8-methoxy-1-[¹¹C]methyl-4-methylquinolin-2(1H)-one ([¹¹C]21a), 6,8-dimethoxy-1-[¹¹C]methyl-4-methylquinolin-2(1H)-one ([¹¹C]21b), and 5,8-dimethoxy-1-[¹¹C]methyl-4-methylquinolin-2(1H)-one ([¹¹C]21c), were prepared from their corresponding precursors with [¹¹C]methyl triflate ([¹¹C]CH₃OTf) under basic conditions (NaH) through either O- or N-[¹¹C]methylation and isolated by semi-preparative HPLC method in 40-50% radiochemical yields decay corrected to end of bombardment (EOB), based on [¹¹C]CO₂, and 111-185 GBq/μmol specific activity at the end of synthesis (EOS).     

Structure and Biosynthesis of Cuticular Lipids: Hydroxylation of Palmitic Acid and Decarboxylation of C(28), C(30), and C(32) Acids in Vicia faba Flowers

The structure and composition of the cutin monomers from the flower petals of Vicia faba were determined by hydrogenolysis (LiAlH₄) or deuterolysis (LiAlD₄) followed by thin layer chromatography and combined gas-liquid chromatography and mass spectrometry. The major components were 10, 16-dihydroxyhexadecanoic acid (79.8%), 9, 16-dihydroxyhexadecanoic acid (4.2%), 16-hydroxyhexadecanoic acid (4.2%), 18-hydroxyoctadecanoic acid (1.6%), and hexadecanoic acid (2.4%). These results show that flower petal cutin is very similar to leaf cutin of V. faba. Developing petals readily incorporated exogenous [1-¹⁴C]palmitic acid into cutin. Direct conversion of the exogeneous acid into 16-hydroxyhexadecanoic acid, 10, 16-dihydroxy-, and 9, 16-dihydroxyhexadecanoic acid was demonstrated by radio gas-liquid chromatography of their chemical degradation products. About 1% of the exogenous [1-¹⁴C]palmitic acid was incorporated into C₂₇, C₂₉, and C₃₁n-alkanes, which were identified by combined gas-liquid chromatography and mass spectrometry as the major components of the hydrocarbons of V. faba flowers. The radioactivity distribution among these three alkanes (C₂₇, 15%; C₂₉, 48%; C₃₁, 38%) was similar to the per cent composition of the alkanes (C₂₇, 12%; C₂₉, 43%; C₃₁, 44%). [1-¹⁴C]Stearic acid was also incorporated into C₂₇, C₂₉, and C₃₁n-alkanes in good yield (3%). Trichloroacetate, which has been postulated to be an inhibitor of fatty acid elongation, inhibited the conversion of [1-¹⁴C]stearic acid to alkanes, and the inhibition was greatest for the longer alkanes. Developing flower petals also incorporated exogenous C₂₈, C₃₀, and C₃₂ acids into alkanes in 0.5% to 5% yields. [G-³H]n-octacosanoic acid (C₂₈) was incorporated into C₂₇, C₂₉, and C₃₁n-alkanes. [G-³H]n-triacontanoic acid (C₃₀) was incorporated mainly into C₂₉ and C₃₁ alkanes, whereas [9, 10, 11-³H]n-dotriacontanoic acid (C₃₂) was converted mainly to C₃₁ alkane. Trichloroacetate inhibited the conversion of the exogenous acids into alkanes with carbon chains longer than the exogenous acid, and at the same time increased the amount of the direct decarboxylation product formed. These results clearly demonstrate direct decarboxylation as well as elongation and decarboxylation of exogenous fatty acids, and thus constitute the most direct evidence thus far obtained for an elongation-decarboxylation mechanism for the biosynthesis of alkanes.     

In vivo biosynthesis of -linolenic acid in plants

[1-¹⁴C]acetate was readily incorporated into unsaturated fatty acids by leaf slices of spinach, barley and whole cells of $\text{Chlorella}\text{pyrenoidosa}$ and $\text{Candida}\text{bogoriensis}$. In these systems the [¹⁴C] label in newly synthesized oleate and linoleate was approximately equally distributed in the C_1–9 and the C_10–18 fragments obtained by reductive ozonolysis of these acids, whereas in a-linolenic acid over 90% of the total [¹⁴C] was localized in the C_1–9 fragment. While [1-¹⁴C]oleic acid was converted by whole cells of $\text{Chlorella}$ to [1-¹⁴C]linoleic and [1-¹⁴C]linolenic acids, [U-¹⁴C]oleic acid yielded [U-¹⁴C]linoleic acid but a-linolenic acid was labeled only in the carboxyl terminal carbon atoms. When spinach leaf slices were supplied with carboxyl labeled octanoic, decanoic, dodecanoic, tetradecanoic and octadecanoic acids, only the first three acids were converted to a-linolenic acids while the last two acids were ineffective. Thus we suggest that (a) linoleic acid is not the precursor of a-linolenic acid and (b) 12:3(3, 6, 9) is the earliest permissible trienoic acid which is then elongated to a-linolenic acid.     

Effects of pH on Lignin and Cellulose Degradation by Streptomyces viridosporus

Lignocellulose degradation by Streptomyces viridosporus results in the oxidative depolymerization of lignin and the production of a water-soluble lignin polymer, acid-precipitable polymeric lignin (APPL). The effects of the culture pH on lignin and cellulose metabolism and APPL production by S. viridosporus are reported. Dry, ground, hot-water-extracted corn (Zea mays) lignocellulose was autoclaved in 1-liter reagent bottles (5 g per bottle) and inoculated with 50-ml volumes of S. viridosporus cells suspended in buffers of specific pH (pH 6.0 to 9.2 at 0.4 pH unit intervals). Four replicates of inoculated cultures and of uninoculated controls at each pH were incubated as solid-state fermentations at 37°C. After 6 weeks of incubation the percent loss of lignocellulose, lignin, and carbohydrate and the amount of APPL produced were determined for each replicate. Optimal lignocellulose degradation, as shown by substrate weight loss, was observed in the pH range of 8.4 to 8.8. Only minor differences were seen in the Klason lignin, carbohydrate, protein, and ash contents of the APPLS produced by cultures at each pH. The effects of pH on the degradation of a spruce (Picea pungens) [¹⁴C-lignin]lignocellulose and a Douglas fir (Pseudotsuga menziesii) [¹⁴C-glucan]-lignocellulose were also determined at pH values between 6.5 and 9.5 (0.5 pH unit intervals). The incubations were carried out for 3 weeks at 37°C with bubbler-tube cultures. The percentage of initial ¹⁴C recovered as ¹⁴CO₂, ¹⁴C-labeled water-soluble products, and [¹⁴C]APPL was then determined. The mineralization of lignin and cellulose to CO₂ was optimal at pHs 6.5 and 7.0, respectively. However, the optimum for lignin and cellulose solubilization was pH 8.5, which correlated with the pH 8.5 optimum for APPL production. Overall, the data show that, whereas lignin mineralization is optimal at neutral to slightly acidic pHs, lignocellulose degradation with lignin solubilization and APPL production is promoted by alkaline pHs. These findings indicate that lignin-solubilizing actinomycetes may play an important role in the metabolism of lignin in neutral to alkaline soils in which ligninolytic fungi are not highly competitive.     

Mineralization and solubilization of synthetic lignin by manganese peroxidases from Nematoloma frowardii and Phlebia radiata

Crude and purified manganese peroxidase from the white-rot fungi Nematoloma frowardii and Phlebia radiata catalyzed the partial depolymerization of a [¹⁴C-ring]labelled synthetic lignin into water-soluble fragments (30–50%). The in vitro depolymerization of the ¹⁴C-labelled lignin was accompanied by a release of ¹⁴CO₂ ranging from 4 to 6%. Small quantities of the thiol mediator glutathione stimulated the depolymerization of lignin resulting in a mineralization and solubilization of up to 10 and 64%, respectively. Most of the water-soluble substances formed had molecular masses around 0.7 kDa, although a higher-molecular mass fraction was also detectable (>2 kDa). Photometric assays using 2,2′-azinobis(3-ethylbenzothiazolinesulphonate) as an indicator demonstrated that high levels of Mn(III), which were very probably responsible for the depolymerization and mineralization of the ¹⁴C-labelled lignin, were adjusted within the first 24 h of incubation. The manganese peroxidase catalyzed depolymerization process was not necessarily dependent on H₂O₂; also in the absence of the H₂O₂-generating system glucose/glucose oxidase, effective solubilization and mineralization of lignin dehydrogenation polymerizate occurred, due to the in part superoxide dismutase sensitive, ‘oxidase-like’ activity of MnP which probably produces radical species and peroxides from malonate.     

Participation of C6C1 unit in the biosynthesis of ephedrine in Ephedra

Feeding of benzoic acid-[7-¹⁴C], benzaldehyde-[7-¹⁴C] and cinnamic acid-[3-¹⁴C] to Ephedra distachya resulted in efficient incorporations of ¹⁴C into the α-carbon atom of the side chain of l-ephedrine. Thus ephedrine was shown to be biosynthesized by the condensation of a C₆C₁ portion which is derived from phenylalanine via cinnamate and an unidentified C₂-N fragment.     

Biosynthesis of pterocarpan,isoflavan and coumestan metabolites of Medicago sativa: chalcone,isoflavone and isoflavanone precursors

Comparative feeding experiments in CuCl₂,- and UV-treated lucerne (Medicago sativa) seedlings have shown that 2′,4,4′-trihydroxychalcone-[carbonyl-¹⁴C] and formononetin-[Me-¹⁴C] but not 2′,4′-dihydroxy-4-methoxychalcone-[carbonyl- ¹⁴C] or daidzein-[4-¹⁴C] were incorporated into the phytoalexins demethylhomopterocarpin, sativan and vestitol, and also into 9-O-methylcoumestrol. The synthesis of 9-O-methylcoumestrol is greatly stimulated by this abiotic treatment but coumestrol production is not noticeably affected. Daidzein and the trihydroxychalcone were precursors of coumestrol. The results are interpreted in favour of a mechanism in which methylation is an integral part of the aryl migration process associated with the biosynthesisof 4′-methoxyisoflavonoids. Formononetin, 2′,7-dihydroxy-4′-methoxyisoflavone-[Me-¹⁴C], 7-hydroxy-4′-methoxyisoflavanone-[Me-¹⁴C] and 2′,7-dihydroxy-4′-methoxyisoflavanone-[Me-¹⁴C] were all excellent precursors of demethylhomopterocarpin, sativan, vestitol and 9-O-methylcoumestrol, and thus a metabolic grid may be involved in their biosynthetic origin.     

A Study of Formate Production and Oxidation in Leaf Peroxisomes during Photorespiration

When glycolate was metabolized in peroxisomes isolated from leaves of spinach beet (Beta vulgaris L., var. vulgaris) formate was produced. Although the reaction mixture contained glutamate to facilitate conversion of glycolate to glycine, the rate at which H₂O₂ became “available” during the oxidation of [1-¹⁴C]glycolate was sufficient to account for the breakdown of the intermediate [1-¹⁴C]glyoxylate to formate (C₁ unit) and ¹⁴CO₂. Under aerobic conditions formate production closely paralleled ¹⁴CO₂ release from [1-¹⁴C]glycolate which was optimal between pH 8.0 and pH 9.0 and was increased 3-fold when the temperature was raised from 25 to 35 C, or when the rate of H₂O₂ production was increased artificially by addition of an active preparation of fungal glucose oxidase.