Biosynthesis of the beta-diketones of barley spike epicuticular wax.

[1-¹⁴C]acetate and [2-¹⁴C]acetate were incorporated into the β-diketones of barley spike epicuticular wax via the peduncle. Utilizing column chromatography with dry copper acetate, the β-diketones were isolated and the labeling pattern in the hentriacontan-14, 16-dione determined after its degradation. A modified iodoform procedure was used to give myristic and palmitic acids. Radio-gas chromatography was then performed on the products of chemical α-oxidation of the separated fatty acids. This procedure, in effect, gave the specific activity of every carbon atom of hentriacontan-14,16-dione except carbon-1 to carbon-5 (from myristic acid) and carbon-27 to carbon-31 (from palmitic acid) for each labeled substrate. The specific activity of carbon-15 was determined by an indirect method. On the basis of these data it is suggested that the hentriacontan-14,16-dione is synthesized from the carbon-31 end of the molecule by elongation as follows. C₂ units are added, perhaps to a mixture of short chain precursors, to give a chain with 12 carbon atoms. This chain is then elongated to one with 16 carbon atoms so that the four added carbon atoms are uniformly labeled. Following this, the chain with 16 carbon atoms is elongated with C₂ units to give the complete molecule. Possibly some change in mechanism occurs in this last elongation process when the chain is 22 carbon atoms long. Barley spike wax β-diketones contain about 2% nonacosan-13, 15-dione which seems to be synthesized in an analogous manner.     

An automatic carbon-14 gas analyzer for organic compounds and biological samples

The present paper concerns automatic measurement of the radioactivity of substances labeled with carbon-14 isotope. The organic compounds or biological samples are combusted in an oxygen chamber. The oxygen excess is converted by hydrogen into water vapor in a reactor filled with copper and copper oxide. The water is retained by condensation and the carbon dioxide is swept by means of a counting gas, preferably propane or butane or a mixture of such gases, into an anticoincidence counter. The carbon-14 gas analyzer allows the measurement of carbon-14 isotope with high accuracy and sensitivity in a fully automated way, entirely free of manual intervention.     

Formation of organic products in self-radiolyzed calcium carbonate

Summary Calcium carbonate labeled with carbon-14 was self-irradiated by means of the -decay of its carbon-14. A number of products containing one or two carbon atoms were identified by high performance liquid chromatography. Formic and oxalic acids were produced in relatively high yields, while glyoxylic, glycolic, and acetic acids, as well as formaldehyde and methanol, were formed in lower yields. These results support the suggestion that carbonates subjected to ionizing radiation could have been a source of carbon for organic synthesis on the primitive earth.     

Distribution of carbon-14 assimilated by wheat awns

The pattern of distribution of carbon assimilated by awns was investigated in two lines of Triticum aestivum. Single awns on basal florets of spikelets in the central part of the ear were dosed with ¹⁴CO₂. Five days after dosing, 99% of the carbon-14 recovered was in the spikelet bearing the awn. Of the carbon-14 exported from the treated awn 57% went to the grain of the first floret, 1% to the second, 28% to the third and 7% to the fourth.     

Metabolism of steroidal lactones by the fungus Corynespora cassiicola CBS 161.60 results in a mechanistically unique intramolecular ring-D cyclization resulting in C-14 spiro-lactones

The fungus Corynespora cassiicola metabolises exogenous steroids in a unique and highly specific manner. Central to this, is the ability of this organism to functionalise substrates (androgens, progestogens) at the highly stereochemically hindered 8β-position of the steroid nucleus. A recent study has identified that 8β-hydroxylation occurs through inverted binding in a 9α-hydroxylase. In order to discern the metabolic fate of more symmetrical molecules, we have investigated the metabolism of a range of steroidal analogues functionalised with ring-D lactones, but differing in their functional group stereochemistry at carbon-3. Remarkably, the 3α-functionalised steroidal lactones underwent a mechanistically unique two step intramolecular cyclisation resulting in the generation of a ring-D spiro-carbolactone. This rapid rearrangement initiated with hydroxylation at carbon 14 followed by transesterification, resulting in ring contraction with formation of a butyrolactone at carbon-14. Remarkably this rearrangement was found to be highly dependent on the stereochemistry at carbon-3, with the β-analogues only undergoing 9α-hydroxylation. The implications of these findings and their mechanistic bases are discussed.     

中国晚期旧石器的碳-14断代和问题

根据已公布的47个碳-14数据,进而分析10处中国晚期遗址的年代和问题,并提出不同的看法。文中强调:露天遗址中碳-14数据的异常现象,往往与各种原因形成的再次堆积有关。因此必须注意样品的采集和避免引用孤零的碳-14数据,同时还要结合地层和文化性质的分析,才可能保证断代的准确性。     

Biosynthesis of methyl branched hydrocarbons of the German cockroach Blattella germanica (L.) (orthoptera,blattellidae)

The precursors and directionality of synthesis of the methyl branched cuticular hydrocarbons and the female contact sex pheromone, 3,11-dimethyl-2-nonacosanone, of the German cockroach, Blattella germanica, were investigated by radiotracer and carbon-13 NMR techniques. The amino acids [G-³H]valine, [4,5-³H]isoleucine and [3,4-¹⁴C₂]methionine labeled the hydrocarbon fraction in a manner indicating that the carbon skeletons of all three amino acids serve as the methyl branch group donor. The incorporation of [1,4-¹⁴C₂]- and [2,3-¹⁴C₂]succinates into the hydrocarbon and acylglycerol/polar lipid fractions indicated that succinate also served as a precursor to methylmalonyl-CoA. Carbon-13 NMR analyses showed that [1-¹³C]propionate labeled the carbon adjacent to the tertiary carbon, and, for the 3,x-dimethylalkanes, that carbon-4 and not carbon-2 was enriched. [1-¹³C]Acetate labeled carbon-2 of these hydrocarbons. This indicates that the methyl branching groups of the 3,x-dimethylalkanes were inserted early in the chain elongation process. [3,4,5-¹³C₃]Valine labeled the methyl, tertiary and carbon adjacent to the tertiary carbon of the methyl branched alkanes. Thus, the methyl branched hydrocarbon was formed by the insertion of methylmalonyl units derived from propionate, isoleucine, valine, methionine and succinate early in chain elongation.     

Induction of kranz anatomy and C4-like biochemical characteristics in a submerged amphibious plant by abscisic acid

The amphibious leafless sedge Eleocharis vivipara develops C4-like traits as well as Kranz anatomy under terrestrial conditions, but it develops C3-like traits without Kranz anatomy under submerged conditions. When submerged plants are exposed to aerial conditions, they rapidly produce new photosynthetic tissues with C4-like traits. In this study, experiments were performed to determine whether abscisic acid (ABA), a plant stress hormone, could induce the formation of photosynthetic tissues with Kranz anatomy and C4-like biochemical traits under water in the submerged form. When the submerged plants were grown in water containing 5 &mgr;M ABA, they developed new photosynthetic tissues with Kranz anatomy, forming well-developed Kranz (bundle sheath) cells that contained many organelles. The ABA-induced tissues accumulated large amounts of phosphoenolpyruvate carboxylase, pyruvate orthophosphate dikinase, and NAD-malic enzyme at the appropriate cellular sites. The tissues had 3.4 to 3.8 times more C4 enzyme activity than did tissues of the untreated submerged plants. Carbon-14 pulse and carbon-12 chase experiments revealed that the ABA-induced tissues fixed higher amounts of carbon-14 into C4 compounds and lower amounts of carbon-14 into C3 compounds as initial products than did the submerged plants and that they exhibited a C4-like pattern of carbon fixation under aqueous conditions of low carbon, indicating enhanced C4 capacity in the tissues. This report provides an example of the hormonal control of the differentiation of the structural and functional traits required for the C4 pathway.     

The Biosynthesis of Sepedonin

The origin of each carbon of anhydrosepedonin produced by Sepedonium chrysospermum has been elucidated by carbon-14 tracer method. At first, the degradation pathways adequate to such object was studied. The radioactivity incorporated in sepedonin and anhydrosepedonin was considerably high when acetate-1-¹⁴C, acetate-2-¹⁴C and formate-¹⁴C were used as the precursor. The feature of the labeling pattern of anhydrosepedonin was analogous to those of the other fungal tropolones. The carbon atom derived from formate was almost exclusively situated at C-7 position of the tropolone ring. As a whole, the labeling pattern demonstrated that anhydrosepedonin might be synthesized through the poly-ketomethylene pathway.     

Labelling patterns of carbon-14 in net plankton during a winter-spring bloom

Weekly surface samples were collected in lower Narragansett Bay, Rhode Island, during the 1975 winter-spring bloom and fractionated by nets to nannoplankton (<20 μm) and total (< 158 μm) size fractions. Each size fraction was assayed for paniculate carbon, nitrogen, carbohydrate, protein, chlorophyll a, and cell counts. The <20 μm values were subtracted from the <158 μm values to estimate the composition of the 20 μm to 158 μm fraction (termed net plankton). As nutrients (primarily nitrogen) decreased to undetectable levels with the culmination of the diatom bloom, the ratios of protein/carbohydrate, carbohydrate/carbon, and carbon/chlorophyll a in the net plankton indicated the diatom population was increasingly nutrient-limited. Each size fraction was also incubated at a saturating light intensity with carbon-14; following filtration, the cells were extracted with solvents to obtain labelled polysaccharide and protein. The daily rates of polysaccharide and protein synthesis in the net plankton declined as the bloom entered the stationary phase. When the diatom population was at its maximum density the majority of the carbon-14 was found in the ethanol-soluble fraction; this may be due to high light intensities or nutrient effects.     

Action Spectrum of Coccolith Formation

The action spectrum of coccolith formation in Coccolithus huxleyi was determined by measuring the uptake of carbon-14 in coccoliths in four-hour experiments as a function of light intensity at each of seven wavelengths. An action spectrum | of photosynthetic carbon assimilation was obtained at the same time. The coccolith action spectrum had peaks at wavelengths of about 440 nm and 670 nm. probably corresponding to the regions of maximum cellular absorption and carbon assimilation. However, blue light appeared to be relatively more efficient in coccolith formation than in carbon assimilation. The results suggest that light-dependent coccolith formation may be catalyzed by two photochemical reactions, one mediated by chloroplast pigments and the other by some pigment absorbing specifically in the blue part of the spectrum.     

Effects of Mineral Salts on Short-term Incorporation of Carbon Dioxide inChlorella

The effects of various mineral salts have been studied, bothsingly and in combination, on the uptake and distribution ofphotosynthetically incorporated carbon-14 in Chlorella. Whenmagnesium sulphate, potassium nitrate, and potassium phosphatewere combined in the same concentrations as are found in thenormal nutrient solution, the uptake of carbon-14 was increasedand more radioactivity was incorporated into the amino-acids,with a decrease in the percentage of radioactivity in the sugarphosphates when compared to the controls in distilled water.The most striking effect of the addition of just one salt wasobtained with salts containing nitrogen, particularly ammoniumchloride, which in one experiment increased the radioactivityfound in the amino-acids from 9.9 per cent. (expressed as percentageof the total soluble radioactivity found in this group of compounds)in the controls to 57 per cent., while the radioactivity inthe sugar phosphates fell from 64 to 7 per cent., correspondingly.The total uptake of carbon dioxide by the cells supplied withammonium chloride was three times as great as that in the controlsin distilled water. The relevance of these findings to the methodology involvedin experiments dealing with the path of carbon in photosynthesisis discussed, with particular emphasis upon the concept of a‘steady state’ and how it is thought this may bestbe achieved.     

The production of lipids alternately labelled with carbon-13

Chlorella cells were shown to have similar fatty acid profiles when grown photoautotrophically or if grown photoheterotrophically with ethanoate (acetate) as carbon source. When supplied with ethanoate labelled with carbon-13 in the methyl group, the alga incorporated it into fatty acids with retention of the sequence of labelling on alternate carbon atoms, thus providing a convenient method for synthesising lipids in a form useful for nuclear magnetic resonance (NMR) studies of lipids in situ in membranes. Marine algae used in fish farming may have higher levels of very highly unsaturated fatty acids; proposals for producing these compounds labelled with carbon-13 are, therefore, presented, based on using centrally labelled glycerol. The scope for producing other substances labelled in a form suitable for NMR studies, such as carotenoids, is discussed.     

The mode of condensation of aspartic acid and dihydroxyacetone phosphate in quinolinate synthesis in Escherichia coli.

Dihydroxy [3-14C]acetone phosphate was prepared enzymatically from [1-14C]glucose and use as a substrate in a partially purified quinolinate synthetase system prepared from Escherichia coli mutants. Carbon-by-carbon degradation of the resulting [14C]quinolinate showed that 96% of the 14C was located in carbon-4, indicating that carbon-3 of dihydroxyacetone phosphate condenses with carbon-3 of aspartate in quinolinate synthesis in E. coli.     

The Origin of Carbons of Dihydrofuran Ring and C-6 in the Biosynthesis of Rotenone

For the investigation of rotenone biosynthesis, acetate-2-¹⁴C, mevalonic acid-2-¹⁴C lactone and methionine-methyl-¹⁴C were administered to Derris elliptica plants, respectively, and the distribution of carbon-14 in the labeled rotenone was determined by degradation. When mevalonic acid-2-¹⁴C lactone was incorporated into rotenone, the radioactivity was found equally in the carbons at both C-7′ and C-8′, indicating that these carbons are derived from the carbon-2 of mevalonic lactone. In the case of methionine-methyl-¹⁴C about 80% of the total radioactivity was found to enter two methoxyl groups. This result demonstrates that methionine is an efficient precursor of the methoxyl group. Furthermore, it is also suggested that methionine may be a precursor of the carbon at C-6.     

Metabolism of Glycine by Rumen Microorganisms

Rumen microorganisms rapidly metabolized glycine at rates varying from 0.014 to 0.241 mumole of glycine per ml per min. The main metabolic products were carbon dioxide, acetic acid, and ammonia; little glycine was incorporated into bacterial protein. Use of carboxyl or methylene-labeled glycine showed that the carbon dioxide came mainly from the carboxyl of glycine, whereas both carbons of acetic acid were derived partly from the methylene carbon of glycine and partly from carbon dioxide. The ratio of carbon-14 to nitrogen-15 in glycine isolated from the protein of rumen bacteria incubated in the presence of N(15)- and C(14)-labeled glycine indicated that most of the extracellular glycine incorporated into protein was incorporated without intervening deamination.     

Carbon Sequestration in Two Alpine Soils on the Tibetan Plateau

Soil carbon sequestration was estimated in a conifer forest and an alpine meadow on the Tibetan Plateau using a carbon-14 radioactive label provided by thermonuclear weapon tests (known as bomb-¹⁴C). Soil organic matter was physically separated into light and heavy fractions. The concentration spike of bomb-¹⁴C occurred at a soil depth of 4 cm in both the forest soil and the alpine meadow soil. Based on the depth of the bomb-¹⁴C spike, the carbon sequestration rate was determined to be 38.5 g C/m² per year for the forest soil and 27.1 g C/m² per year for the alpine meadow soil. Considering that more than 60% of soil organic carbon (SOC) is stored in the heavy fraction and the large area of alpine forests and meadows on the Tibetan Plateau, these alpine ecosystems might partially contribute to "the missing carbon sink".     

Carbon Import into Developing Ovules of Pisum sativum: The Role of the Water Relations of the Seed Coat

We tested the hypothesis that the transport of carbon to developingpea ovules is controlled by the water potential of the seedcoat, in both the short-term (minutes to hours) and long-term(days). At 14 d after anthesis, when the embryo just fills theseed coat, the osmotic pressure of seed coat apoplast solutionwas about 1 MPa (equivalent to 400 mOsmol kg^–1). Transportof carbon into perfused attached seed coats at this stage ofdevelopment was monitored with radioactive carbon-11. Aftera small (50 mOsmol kg^–1) increment in the osmotic pressureof the bathing solution, transport of carbon increased abruptly,but after about 100 min it returned towards pretreatment values.Therefore, although osmotic pressure in the sink apoplast initiallyaffected carbon import, as expected from the M     

Ethylene production by wounded tissue of citrus fruit

Segments cut from young immature fruits and albedo discs excisedfrom both immature and mature fruits of Satsuma mandarin ormature fruits of Natsudaidai produced much ethylene during incubationat 26?C in the dark. Ethylene formation was markedly acceleratedby the application of abscisic acid but markedly delayed by3,5-dibromo-4-hydroxybenzoic acid. Both the stimulation andretardation decreased greatly during the course of incubation.Both compounds seem to be associated with the early stages ofethylene formation by wounded citrus fruit tissues. Albedo discs were fed ¹⁴C methionine labeled at one of threedifferent positions. Of the three radioanalogs (carbon-2, carbon-3and methyl carbon), the label at the 3 position was preferentiallyincorporated into ethylene. This agrees with the former observationthat ethylene is derived from carbon-3 and -4 of methionine.Incorporation of label into ethylene from L-[3-¹⁴C] methioninewas strongly inhibited by L-canaline, L-ethionine, 2,4-dinitrophenoland cycloheximide. Ethylene evolution was also strongly inhibitedby 2,4-dinitrophenol, KCN, NaN₃ and cycloheximide, but lesscompletely by L-canaline and L-ethionine. These results supportthe view that ATP and pyridoxal phosphate are utilized in activationof methionine to form ethylene. (Received October 25, 1977; )     

Metabolism of propionate to acetate in the cockroach Periplaneta americana

Carbon-13 NMR and radiotracer studies were used to determine the precursor to methylmalonate and to study the metabolism of propionate in the cockroach Periplaneta americana. [3,4,5-13C3]Valine labeled carbons 3, 4, and 26 of 3-methylpentacosane, indicating that valine was metabolized via propionyl-CoA to methylmalonyl-CoA and served as the methyl branch unit precursor. Potassium [2-13C]propionate labeled the odd-numbered carbons of hydrocarbons and potassium [3-13C]propionate labeled the even-numbered carbons of hydrocarbons in this insect. This labeling pattern indicates that propionate is metabolized to acetate, with carbon-2 of propionate becoming the methyl carbon of acetate and carbon-3 of propionate becoming the carboxyl carbon of acetate. In vivo studies in which products were separated by HPLC showed that [2-14C]propionate was readily metabolized to acetate. The radioactivity from sodium [1-14C]propionate was not incorporated into succinate nor into any other tricarboxylic acid cycle intermediate, indicating that propionate was not metabolized via methylmalonate to succinate. Similarly, [1-14C]propionate did not label acetate. An experiment designed to determine the subcellular localization of the enzymes involved in converting propionate to acetate showed that they were located in the mitochondrial fraction. Data from both in vivo and in vitro studies as a function of time indicated that propionate was converted directly to acetate and did not first go through tricarboxylic acid cycle intermediates. These data demonstrate a novel pathway of propionate metabolism in insects.