Microdetermination of inorganic sulfate using thin-layer plates

Inorganic sulfate was precipitated on cellulose thin-layer plates with the radioactive reagent, ¹³³BaCl₂. Excess reagent was removed by repeated washings with an acidic BaCl₂ solution. The residual activity was transferred to vials by cutting out the point of application and its immediate surroundings. Counting was performed in a scintillation well γ-counting system. The concentration-activity curve was linear.     

Inhibition of trehalose breakdown increases new carbon partitioning into cellulosic biomass in Nicotiana tabacum

Validamycin A was used to inhibit in vivo trehalase activity in tobacco enabling the study of subsequent changes in new C partitioning into cellulosic biomass and lignin precursors. After 12-h exposure to treatment, plants were pulse labeled using radioactive ¹¹CO₂, and the partitioning of isotope was traced into [¹¹C]cellulose and [¹¹C]hemicellulose, as well as into [¹¹C]phenylalanine, the precursor for lignin. Over this time course of treatment, new carbon partitioning into hemicellulose and cellulose was increased, while new carbon partitioning into phenylalanine was decreased. This trend was accompanied by a decrease in phenylalanine ammonia-lyase activity. After 4 d of exposure to validamycin A, we also measured leaf protein content and key C and N metabolite pools. Extended treatment increased foliar cellulose and starch content, decreased sucrose, and total amino acid and nitrate content, and had no effect on total protein.     

Incorporation of 14C-Labelled Glycerol and γ-Aminobutyric Acid into Vitamin B6 in a Cell-suspension of Achromobacter cycloclastes

Incorporation of ¹⁴C from various ¹⁴C-labelled compounds into vitamin B₆ (abbreviate as B₆) in a cell-suspension of B₆-producing bacteria, Achromobacter cycloclastes A.M.S. 6021, was studied by using a newly designed purification procedure of the radioactive B₆. The procedure consisted of Sephadex G–25 gel filtration, Dowex 50W–X8 column chromatography, Amberlite CG–50 column adsorption, powdered cellulose partition column chromatography, crystallization and sublimatography. It was observed that the labels both from 1,3- and from 2-labelled glycerol were clearly incorporated into B₆ and the label of ¹⁴C-labelled γ-aminobutyric acid was also incorporated. The incorporation of ¹⁴C from ¹⁴C-labelled glycerol or γ-aminobutyric acid was affected by the addition of cold γ-aminobutyric acid or glycerol. The implication of these compounds as precursors of B₆ was discussed.     

Initiation of ovalbumin synthesis in chicken oviduct magnum: Transient labeling of the NH2-terminus by methionine

The incorporation of [³⁵S]methionine into ovalbumin, a protein containing NH₂-terminal N-acetylglycine, has been studied in chicken oviduct magnum cells. The purification of [³⁵S]methionine-labeled ovalbumin from total oviduct proteins was accomplished by dialysis of a crude extract at pH 3.6 followed by chromatography on carboxymethyl cellulose. The radioactive ovalbumin eluted from the column in three peaks (P₀, P₁, and P₂-containing 0, 1, and 2 moles of phosphate, respectively, per mole of ovalbumin). The kinetics of labeling of peaks P₀ and P₁ showed that the ratio of radioactivity in NH₂-terminal methionine to total incorporation was greater at 2 min of labeling than at later times. The transient labeling of the NH₂-terminus of ovalbumin with methionine indicates that methionine is the initiator amino acid for the synthesis of this protein, which in its mature form contains NH₂-terminal N-acetylglycine.     

Reconstruction of source water using the δ18O of tree ring phenylglucosazone: A potential tool in paleoclimate studies

The oxygen isotope ratios of tree ring cellulose have a great potential as proxy for the oxygen isotope ratios of source water, which is related to climate. However, source water isotopic signatures can be masked by plant physiological and biochemical processes during cellulose synthesis. To minimize biochemical effects in the recording of source water, we modified the cellulose molecule to phenylglucosazone, which only has oxygen attached to carbon 3–6 (O_C3–6) of the cellulose glucose moieties, thus eliminating the oxygen attached to carbon 2 of the cellulose glucose moieties (O_C-2). Here we developed a method to use small amounts of inter and intra-annual tree ring cellulose for phenylglucosazone synthesis. Using this new method we tested if the oxygen isotope ratios of source water reconstructed from tree ring phenylglucosazone (δ¹⁸O_sw^PG) and the observed source water (δ¹⁸O_sw^obs) would have a better agreement than those reconstructed from the tree ring cellulose molecule. Annual tree ring samples were obtained from Pinus sylvestris (1997–2003) (Finland) and Picea abies (1971–1992) (Switzerland) and intra-annual tree ring samples were obtained from Pinus radiata (October 2004–March 2006) (New Zealand), each near a meteorological station where precipitation and relative humidity (RH) were measured periodically. The δ¹⁸O of tree ring cellulose and tree ring phenylglucosazone for each of the three species were then used to back calculate the δ¹⁸O of source water according to a previous published empirical equation. As expected, the δ¹⁸O of tree ring phenylglucosazone was superior than cellulose in the reconstruction of source water available to the plant. Deviation between δ¹⁸O_sw^PG and δ¹⁸O_sw^obs was in part correlated with variation in atmospheric relative humidity (RH) which was not observed for the cellulose molecule. We conclude that this new method can be applicable to inter and intra-annual tree ring studies and that the use of the tree ring phenylglucosazone will significantly improve the quality of paleoclimate studies.     

A Comparative Analysis of in vitro cellulose synthesis from cell-free extracts of mung bean (Vigna radiata,Fabaceae) And Cotton (Gossypium hirsutum,Malvaceae)

A comparison of cellulose synthesized in vitro from primary walls of etiolated mung bean (Vigna radiata) seedlings and secondary walls of cotton fibers (Gossypium hirsutum) was made by applying conditions found to be essential for in vitro cellulose I assembly from cotton (Kudlicka et al., 1995, Plant Physiology, vol. 107, pp. 111–123). Mung bean fractions including the plasma membrane (PM), the first solubilized fraction (SE₁), and the second solubilized fraction (SE₂), incorporated more radioactive UDP-Glc into the total product than the same fractions from secondary walls. A significant difference was found with the mild digitonin solubilized fraction (SE₁), which produced eight times more total product than the SE₁ fraction of cotton. However, the SE₁ fraction from cotton produced a larger quantity of cellulose (32.1%) than from mung bean (6.9%). Treatment of the in vitro product by acetic/nitric acid reagent (AN) for varying periods of time demonstrated that cellulose synthesized in vitro from mung bean was more easily degraded than cellulose from cotton fibers. This would suggest that cellulose I produced in vitro from the cotton SE₁ fraction may have a higher crystallinity and DP than cellulose I produced in vitro from mung bean. The fibrils of cellulose produced by the SE, fraction of mung bean were loosely associated and not arranged into a compact bundle as in case of cellulose I synthesized by the cotton SE₁ fraction. The electron diffraction patterns (ED) of both products show reflections characteristic for cellulose I. Products from the SE₂ fraction of mung bean and cotton reveal similarities with the cellulose II allomorph synthesized, as well as abundant β-1,3-glucan.     

Direct preparation of radioactive fullerenes as a tracer for applications

The C₆₀ and C₇₀ fullerenes were irradiated by high-energy γ-rays and charged particles. The irradiated samples were dissolved in CS₂ and/or toluene and filtered to remove insoluble by-products. Finally, radioactive fullerenes and products labeled with¹¹C or¹³N were isolated and detected in the liquid phase by radiochromatography. It was found that (1) not only¹¹C or¹³N radioactive monomer fullerenes but also their dimers (trimers and, possibly, tetramers) were produced by recoil implantation process following nuclear reaction and (2) the radioactive fullerene labeled with¹¹C yields has led to high yields.     

Decomposition of 14C-labeled cellulose substrates in litter and soil from a beechwood on limestone

The decomposition of three different ¹⁴C-labeled cellulose substrates (plant holocellulose, plant cellulose prepared from ¹⁴C-labeled beech wood (Fagus sylvatica) and bacterial cellulose produced by Acetobacter xylinum) in samples from the litter and mineral soil layer of a beechwood on limestone was studied. In a long-term (154 day) experiment, mineralization of cellulose materials, production of ¹⁴C-labeled water-soluble compounds, and incorporation of ¹⁴C in microbial biomass was in the order Acetobacter cellulose > holocellulose > plant cellulose in both litter and soil. In general, mineralization of cellulose, production of ¹⁴C-labeled water-soluble compounds, and incorporation of ¹⁴C in microbial biomass were more pronounced, but microbial biomass ¹⁴C declined more rapidly in litter than in soil. In short-term (14 day) incubations, mineralization of cellulose substrates generally corresponded with cellulase and xylanase activities in litter and soil. Pre-incubation with trace amounts of unlabeled holocellulose significantly increased the decomposition of ¹⁴C-labeled cellulose substrates and increased cellulase activity later in the experiment but did not affect xylanase activity. The sum of ¹⁴CO₂ production, ¹⁴C in microbial biomass, and ¹⁴C in water-soluble compounds is considered to be a sensitive parameter by which to measure cellulolytic activity in soil and litter samples in short-term incubations. Shorter periods than 14 days are preferable in assays using Acetobacter cellulose, because the decomposition of this substrate is more variable than that of holocellulose and plant cellulose.Offprint requests to: S. Scheu.     

Role of Aerobic Microbial Populations in Cellulose Digestion by Desert Millipedes

I examined the role of aerobic microbial populations in cellulose digestion by two sympatric species of desert millipedes, Orthoporus ornatus and Comanchelus sp. High numbers of bacteria able to grow on media containing cellulose, carboxymethyl cellulose, or cellobiose as the substrate were found in the alimentary tracts of the millipedes. Enzyme assays indicated that most cellulose and hemicellulose degradation occurred in the midgut, whereas the hindgut was an important site for pectin degradation. Hemicellulase and β-glucosidase in both species and possibly C_x-cellulase and pectinase in O. ornatus were of possible microbial origin. Degradation of [¹⁴C]cellulose by millipedes whose gut floras were reduced by antibiotic treatment and starvation demonstrated a reduction in ¹⁴CO₂ release and ¹⁴C assimilation and an increase in ¹⁴C excretion over values for controls. It appears that the millipede-bacterium association is mutualistic and makes available to millipedes an otherwise mostly unutilizable substrate. Such an association may be an important pathway for decomposition in desert ecosystems.     

Oxygen-18 Content of Atmospheric Oxygen Does Not Affect the Oxygen Isotope Relationship between Environmental Water and Cellulose in a Submerged Aquatic Plant, Egeria densa Planch

We determined that the oxygen isotopic composition of cellulose synthesized by a submerged plant, Egeria densa Planch., is related to the isotopic composition of environmental water by a linear function, δ¹⁸O cellulose = 0.48 δ¹⁸O water + 24.1%‰. The observation of a slope of less than 1 indicates that a portion of cellulose oxygen is derived from an isotopically constant source other than water. We tested whether this source might be molecular oxygen by growing plants in the presence of high concentrations of ¹⁸O in the form of O₂ bubbled into the bottom of an aquarium. Cellulose synthesized during this experiment did not have significantly different oxygen isotope ratios than that synthesized by control plants exposed to O₂ of normal ¹⁸O abundance. We propose that oxygen in organic matter recycled from senescent portions of the plant is incorporated into cellulose. Our findings indicate that paleoclimatic models linking the oxygen isotope composition of environmental water to cellulose from fossil plants will have to be modified to account for contributions of oxygen from this or other sources besides water.     

A peptide-mediated and hydroxyl radical HO*-involved oxidative degradation of cellulose by brown-rot fungi

A special low-molecular-weight peptide named Gt factor, was isolated and purified from the extracellular culture of brown-rot fungi Gloeophyllum trabeum via gel filtration chromatography and HPLC. It has been shown to reduce Fe³⁺ to Fe²⁺. Electron paramagnetic resonance (EPR) spectroscopy revealed Gt factor was able to drive H₂O₂ generation via a superoxide anion O₂ ^.- intermediate and mediate the formation of hydroxyl radical HO^. in the presence of O₂. All the results indicated that Gt factor could oxidize the cellulose, disrupt the inter- and intrahydrogen bonds in cellulose chains by a HO^. -involved mechanism. This resulted in depolymerization of the cellulose, which made it accessible for further enzymatic hydrolysis.     

Bio-hydrogen production from cellulose by sequential co-culture of cellulosic hydrogen bacteria of <Emphasis Type="Italic">Enterococcus gallinarum</Emphasis> G1 and <Emphasis Type="Italic">Ethanoigenens harbinense</Emphasis> B49

Microbial conversion of lignocellulose to hydrogen is a fascinating way to provide a renewable energy source. A mesophilic bacterium strain G1 that had high cellulose degradation and hydrogen production activity (2.38 mmol H₂ g⁻¹ cellulose) was isolated from rumen fluid and identified as the Enterococcus gallinarum. Hydrogen production from cellulose by using sequential co-cultures of a cellulosic-hydrolysis bacterium G1 and Ethanoigenens harbinense B49 was investigated. With an initial Avicel concentration of 5 g l^−l, the sequential co-culture with G1 and strain Ethanoigenens harbinense B49 produced H₂ yield approximately 2.97 mmol H₂ g⁻¹ cellulose for the co-culture system.     

Variations in the natural abundance of oxygen-18 and deuterium in plant carbohydrates

Variations in the natural abundance of ¹⁸O and ²H in plant cellulose are influenced by the isotopic composition of the water directly involved in metabolism—the metabolic water fraction. The isotopic distinction between the metabolic source water and total tissue water must reflect the formation of isotopic gradients within the tissue that are influenced by the rate of water turnover, by properties of the water conducting system and by environmental conditions. It seems that the ¹⁸O abundance in the metabolic water is conserved in cellulose with a relatively constant isotope effect. The relationship of the ²H abundance between metabolic water and cellulose is more complex. Hydrogen incorporated into photosynthetic products during primary reduction steps is highly depleted in ²H. However, a large proportion of these hydrogens are subsequently replaced by exchange with water, leading to ²H enrichment during heterotrophic metabolism. Deciphering the oxygen isotope ratio of cellulose could help in providing insights into the carbon and oxygen fluxes exchanged between plants and the atmosphere. This is because the ¹⁸O abundance in cellulose records the ¹⁸O abundance in the metabolic water, which in turn, controls the oxygen isotopic signatures of the CO₂ and O₂ released by plants into the atmosphere. The hydrogen isotope effects associated with carbohydrate metabolism provide insights into the autotrophic state of a plant tissue. This is because the hydrogen isotope ratio of carbohydrates must reflect the net effects of the two opposing isotope effects associated with photosynthesis and heterotrophic metabolism.     

The use of natural abundance stable isotopic ratios to indicate the presence of oxygen-containing chemical linkages between cellulose and lignin in plant cell walls

Qualitative and quantitative understanding of the chemical linkages between the three major biochemical components (cellulose, hemicellulose and lignin) of plant cell walls is crucial to the understanding of cell wall structure. Although there is convincing evidence for chemical bonds between hemicellulose and lignin and the absence of chemical bonds between hemicellulose and cellulose, there is no conclusive evidence for the presence of covalent bonds between cellulose and lignin. This is caused by the lack of selectivity of current GC/MS-, NMR- and IR-based methods for lignin characterisation as none of these techniques directly targets the possible ester and ether linkages between lignin and cellulose. We modified the widely-accepted “standard” three-step extraction method for isolating cellulose from plants by changing the order of the steps for hemicellulose and lignin removal (solubilisation with concentrated NaOH and oxidation with acetic acid-containing NaClO₂, respectively) so that cellulose and lignin could be isolated with the possible chemical bonds between them intact. These linkages were then cleaved with NaClO₂ reagent in aqueous media of contrasting ¹⁸O/¹⁶O ratios. We produced cellulose with higher purity (a lower level of residual hemicellulose and no detectable lignin) than that produced by the “standard” method. Oxidative artefacts may potentially be introduced at the lignin removal stage; but testing showed this to be minimal.Cellulose samples isolated from processing plant-derived cellulose–lignin mixtures in media of contrasting ¹⁸O/¹⁶O ratios were compared to provide the first quantitative evidence for the presence of oxygen-containing ester and ether bonds between cellulose and lignin in Zea mays leaves. However, no conclusive evidence for the presence or lack of similar bonds in Araucaria cunninghamii wood was obtained.     

A high-temperature water vapor equilibration method to determine non-exchangeable hydrogen isotope ratios of sugar,starch and cellulose

The analysis of the non-exchangeable hydrogen isotope ratio (δ²H_ne) in carbohydrates is mostly limited to the structural component cellulose, while simple high-throughput methods for δ²H_ne values of non-structural carbohydrates (NSC) such as sugar and starch do not yet exist. Here, we tested if the hot vapor equilibration method originally developed for cellulose is applicable for NSC, verified by comparison with the traditional nitration method. We set up a detailed analytical protocol and applied the method to plant extracts of leaves from species with different photosynthetic pathways (i.e., C₃, C₄ and CAM). δ²H_ne of commercial sugars and starch from different classes and sources, ranging from ?157.8 to +6.4‰, were reproducibly analysed with precision between 0.2‰ and 7.7‰. Mean δ²H_ne values of sugar are lowest in C₃ (?92.0‰), intermediate in C₄ (?32.5‰) and highest in CAM plants (6.0‰), with NSC being ²H-depleted compared to cellulose and sugar being generally more ²H-enriched than starch. Our results suggest that our method can be used in future studies to disentangle ²H-fractionation processes, for improving mechanistic δ²H_ne models for leaf and tree-ring cellulose and for further development of δ²H_ne in plant carbohydrates as a potential proxy for climate, hydrology, plant metabolism and physiology.     

Effects of organic amendments on sulfate reduction activity,H2 consumption,and H2 production in salt marsh sediments

Sulfate reduction activity (SRA) was measured via the radioactive tracer (³⁵SO₄ ⁼) technique in sediment samples from the Canary Creek Marsh in Lewes, Delaware. Basal levels of SRA ranged from 130 to 319 nmoles of sulfate reduced/gram dry sediment/hour. With the exception of lactate and formate, all organic acids tested resulted in no stimulation of SRA, whereas straight chain alcohols (C₁-C₄) all gave a significant increase in SRA. In addition, H₂, glucose, and cellobiose caused a twofold or greater increase in SRA, while cellulose amendments did not alter SRA. Molybdate, an inhibitor of sulfate-reducing bacteria (SRB), caused a total inhibition in SRA. 2-Bromoethanesulfonic acid (BES), an inhibitor of methanogenic bacteria, caused a slight decrease in SRA. Hydrogen was not produced in detectable quantities in unamended samples but was produced in large amounts in glucose-amended samples. Hydrogen was rapidly consumed in unamended samples with molybdate additions causing a significant decrease in the rate of H₂ consumption. A variety of organic amendments was found to stimulate H₂ uptake. These studies suggest that SRB are stimulated by a large variety of organic amendments in situ and that SRB play a major role in maintaining low partial pressures of H₂ in marsh sediments.     

Oxygen isotope fractionations across individual leaf carbohydrates in grass and tree species

Almost no δ¹⁸O data are available for leaf carbohydrates, leaving a gap in the understanding of the δ¹⁸O relationship between leaf water and cellulose. We measured δ¹⁸O values of bulk leaf water (δ¹⁸O_LW) and individual leaf carbohydrates (e.g. fructose, glucose and sucrose) in grass and tree species and δ¹⁸O of leaf cellulose in grasses. The grasses were grown under two relative humidity (rH) conditions. Sucrose was generally ¹⁸O‐enriched compared with hexoses across all species with an apparent biosynthetic fractionation factor (ε_bio) of more than 27‰ relative to δ¹⁸O_LW, which might be explained by isotopic leaf water and sucrose synthesis gradients. δ¹⁸O_LW and δ¹⁸O values of carbohydrates and cellulose in grasses were strongly related, indicating that the leaf water signal in carbohydrates was transferred to cellulose (ε_bio = 25.1‰). Interestingly, damping factor p_exp_x, which reflects oxygen isotope exchange with less enriched water during cellulose synthesis, responded to rH conditions if modelled from δ¹⁸O_LW but not if modelled directly from δ¹⁸O of individual carbohydrates. We conclude that δ¹⁸O_LW is not always a good substitute for δ¹⁸O of synthesis water due to isotopic leaf water gradients. Thus, compound‐specific δ¹⁸O analyses of individual carbohydrates are helpful to better constrain (post‐)photosynthetic isotope fractionation processes in plants.     

Technique for Measuring 14CO2 Uptake by Soil Microorganisms In Situ

Uptake of ¹⁴CO₂ in soils due to algae or sulfur-oxidizing bacteria was examined by incubation of soil samples with gaseous ¹⁴CO₂ and subsequent chemical oxidation of biologically fixed radioactive isotope to ¹⁴CO₂ for detection with a liquid scintillation counting system. The ¹⁴CO₂ was added to the soil in the gas phase so that no alteration of the moisture or ionic strength of the soil occurred. Wet oxidation of radioactive organic matter was carried out in sealed ampoules, and the ¹⁴CO₂ produced was transferred to a phenethylamine-liquid scintillation counting system with a simply constructed apparatus. The technique is inexpensive and efficient and does not require elaborate traps since several possible interfering factors were found to have no harmful effects. Experiments in coal mine regions and in geothermal habitats have demonstrated the ecological applicability of this technique for measurement of CO₂ fixation by sulfur-oxidizing bacteria and soil algae.     

Cell wall assembly in Fucus zygotes. II. Cellulose synthesis and deposition is controlled at the post-translational level

An alkali-insoluble cell wall component of Fucus distichus embryos is shown to be cellulose. Cellulose is not found in eggs, but within 20 min following fertilization is present in cell walls of zygotes. Incorporation of [³H]glucose or NaH¹⁴CO₃ confirms that this cellulose in zygotes of F. distichus and F. vesiculosus is newly synthesized, with the highest rate of synthesis occurring within the first 60 min. Use of specific inhibitors indicates that the increase in cellulose does not require protein or RNA synthesis. The evidence is consistent with the hypothesis that the initiation of cellulose synthesis triggered by fertilization is controlled at the post-translational level.     

Method for Simultaneous Measurement of Radioactive and Inactive CO(2) Evolved from Soil Samples During Incubation with Labeled Substrates

An apparatus is described which allows the simultaneous, continuous, and highly sensitive analysis of inactive and radioactive CO₂ evolved from ¹⁴C-supplemented soils or other materials. The apparatus consists of a control unit, a commercially available conductometric CO₂ analyzer, and fraction collector. A number of model experiments were conducted to demonstrate the potentials of the apparatus. These included analysis of the time course of priming action, when ¹⁴C-glucose was added to soil, separation of CO₂ respiration peaks caused by simultaneous degradation of radioactive and inactive soil supplements, and study of the effects of a fungicide, Benomyl, on degradation of ¹⁴C-labeled glucose. In the last experiment, partial degradation of the fungicide could also be followed.