Distribution of carbon isotopes ((13)C/(12)C) in cells and temporal organization of cellular processes]

Recent studies on fractionation of carbon isotopes in biological systems are reviewed. It follows that direct experimental proofs have been obtained that 1) basic fractionation of carbon isotopes in the cell is related to isotope effect in pyruvate decarboxylation; 2) fractionation of carbon isotopes in the above reaction in vivo proceeds with exhausting substrate pool. The latter provides natural relationship between metabolites isotope distribution and sequence of their synthesis in the cell cycle, or with the temporal organization of cellular metabolism. The non-steady and periodic pattern of pyruvate decarboxylation due to the exhausting substrate pool well agrees with the existing notions on reciprocal oscillations in the cell glycolytic chain. Experimental data are presented corroborating indirectly the existence of oscillations in bacterial cells. Earlier proposed model of the mechanism of carbon isotope fractionation based on the above principles can be used for analysing changes in isotopic characteristics of the organisms and interpreting their relations with metabolic processes.     

Carbon isotope (13C/12C) effect of photorespiration in photosynthetic organisms. Evidence for existence, probable mechanism

Experimental evidence in favor of the new phenomenon predicted for photosynthesizing organisms, the fractionation of carbon isotopes in photorespiration is presented. A possible mechanism of this process is discussed. The fractionation of carbon in isotopes photorespiration occurs in the oxygenase phase of the functioning of ribulosebisphosphate carboxylase/oxygenase (rubisco), the key enzyme of photosynthesis, which is capable to act as carboxylase and oxygenase. Which function of the enzyme is active depends on CO2/O2 concentration ratio, which periodically changes in a cell. The key reaction in the mechanism of carbon isotope fractionation in photorespiration is glycine decarboxylation, which results in the splitting and removal from the cell of CO2 enriched with 12C and the accumulation of 13C photorespiratory carbon flow. The coupling of photorespiration and CO2 photoassimilation gives rise to two isotopically different carbon flows, which fill up separate carbohydrate pools, which are the sources of carbon in the following syntheses in the dark phase of photosynthesis. This enables one to identify, from the carbon isotope ratio of metabolites, their involvement in the photorespiratory and assimilatory carbon flows, to investigate the pathways of carbon metabolism, and to estimate more thoroughly the biosynthetic role of photorespiration.     

The confounding effects of source isotopic heterogeneity on consumer–diet and tissue–tissue stable isotope relationships

Stable isotope analysis of consumer tissues document patterns of resource use because data are linearly related to isotope compositions of their source(s) (i.e., food, water, etc.). Deviations in parameters estimated for these relationships can arise from variations in consumer tissue-diet spacing (Δ(TS)) and the level of isotopic heterogeneity in the source(s). We present a set of simple hypotheses that distinguish between the effects of Δ(TS) and source isotope heterogeneity. The latter may arise via mixed diets, during tissue turnover, or by isotopic routing of dietary components. We apply these concepts to stable carbon and nitrogen isotope relationships between gut contents and body tissues of large mammal herbivores from mixed C(3)/C(4) South African savannas and test predictions based on the compound- and/or time-specific data archived within each material. Predicted effects of source isotope heterogeneity are readily detected in carbon isotope relationships between materials representing different time periods or comprising bulk versus protein-only diet components. Differences in Δ(TS) of carbon isotopes across mammal herbivore species with very different feeding niches (and diet isotope compositions) are likely to be small or non-existent in these habitats. Variations in Δ(TS) estimated for nitrogen isotopes are much greater, leading to inconsistencies that cannot be explained by diet or trophic level effects alone. The effects of source heterogeneity on isotopic relationships generate numerical artefacts that have been misinterpreted as variations in Δ(TS). We caution against generalized application of hypotheses based on assumptions of source isotopic homogeneity, even for single diets commonly used in laboratory studies. More careful consideration of how heterogeneity affects consumer-diet relationships is needed for many field and laboratory systems.     

Isotope effect studies of the pyridoxal 5'-phosphate dependent histidine decarboxylase from Morganella morganii

The pyridoxal 5'-phosphate dependent histidine decarboxylase from Morganella morganii shows a nitrogen isotope effect k14/k15 = 0.9770 +/- 0.0021, a carbon isotope effect k12/k13 = 1.0308 +/- 0.0006, and a carbon isotope effect for L-[alpha-2H]histidine of 1.0333 +/- 0.0001 at pH 6.3, 37 degrees C. These results indicate that the overall decarboxylation rate is limited jointly by the rate of Schiff base interchange and by the rate of decarboxylation. Although the observed isotope effects are quite different from those for the analogous glutamate decarboxylase from Escherichia coli [Abell, L. M., & O'Leary, M. H. (1988) Biochemistry 27, 3325], the intrinsic isotope effects for the two enzymes are essentially the same. The difference in observed isotope effects occurs because of a roughly twofold difference in the partitioning of the pyridoxal 5'-phosphate-substrate Schiff base between decarboxylation and Schiff base interchange. The observed nitrogen isotope effect requires that the imine nitrogen in this Schiff base is protonated. Comparison of carbon isotope effects for deuteriated and undeuteriated substrates reveals that the deuterium isotope effect on the decarboxylation step is about 1.20; thus, in the transition state for the decarboxylation step, the carbon-carbon bond is about two-thirds broken.     

稳定同位素技术在土壤跳虫研究上的应用

稳定同位素技术的发展和应用是20世纪90年代生态学研究方法最重要的进步之一.许多生态学过程都伴随着同位素比率的变化,根据这些变化可以追踪生态系统的物质循环和能量流动.近年来,许多学者把稳定同位素技术引入到土壤生态学,主要用于研究土壤碳循环和土壤生物之间的营养关系,在很大程度上提升了对地下生态系统的理解.跳虫作为土壤动物群落的重要组分,它的食性和营养位置一直存在着许多不确定性.稳定同位素技术的应用,为确定跳虫的食物来源、营养位置和营养关系提供了一个强大的工具.本文综述了稳定同位素技术在跳虫食性和营养级研究上的应用,并指出了不足之处以及今后的发展方向.     

Isotope effect studies of the pyruvate-dependent histidine decarboxylase from Lactobacillus 30a

The decarboxylation of histidine by the pyruvate-dependent histidine decarboxylase of Lactobacillus 30a shows a carbon isotope effect of k12/k13 = 1.0334 +/- 0.0005 and a nitrogen isotope effect k14/k15 = 0.9799 +/- 0.0006 at pH 4.8, 37 degrees C. The carbon isotope effect is slightly increased by deuteriation of the substrate and slightly decreased in D2O. The observed nitrogen isotope effect indicates that the imine nitrogen in the substrate-Schiff base intermediate complex is ordinarily protonated, and the pH dependence of the carbon isotope effect indicates that both protonated and unprotonated forms of this intermediate are capable of undergoing decarboxylation. As with the pyridoxal 5'-phosphate dependent enzyme, Schiff base formation and decarboxylation are jointly rate-limiting, with the intermediate histidine-pyruvate Schiff base showing a decarboxylation/Schiff base hydrolysis ratio of 0.5-1.0 at pH 4.8. The decarboxylation transition state is more reactant-like for the pyruvate-dependent enzyme than for the pyridoxal 5'-phosphate dependent enzyme. These studies find no particular energetic or catalytic advantage to the use of pyridoxal 5'-phosphate over covalently bound pyruvate in catalysis of the decarboxylation of histidine.     

Comparison of whole wood and cellulose carbon and oxygen isotope series from Pinus nigra ssp. laricio (Corsica/France)

Stable isotopes in tree rings have widely been used for palaeoclimate reconstructions since tree rings record climatic information at annual resolution. However, various wood components or different parts of an annual tree-ring may differ in their isotopic compositions. Thus, sample preparation and subsequent laboratory analysis are crucial for the isotopic signal retained in the final tree-ring isotope series used for climate reconstruction and must therefore be considered for the interpretation of isotope–climate relationships. This study focuses on wood of Corsican Pine trees (Pinus nigra ssp. laricio) as this tree species allows to reconstruct the long-term climate evolution in the western Mediterranean. In a pilot study, we concentrated on methodological issues of sample preparation techniques in order to evaluate isotope records measured on pooled whole tree-ring cellulose and whole tree-ring bulk wood samples. We analysed 80-year long carbon and oxygen chronologies of Corsican Pine trees growing near the upper tree line on Corsica. Carbon and oxygen isotope records of whole tree-ring bulk wood and whole tree-ring cellulose from a pooled sample of 5 trees were correlated with the climate parameters monthly precipitation, temperature and the self-calibrating Palmer Drought Severity Index (sc-PDSI). Results show that the offsets in carbon and oxygen isotopes of bulk wood and cellulose are not constant over time. Both isotopes correlate with climate parameters from late winter and summer. The carbon and oxygen isotope ratios of cellulose are more sensitive to climatic variables than those of bulk wood. The results of this study imply that extraction of cellulose is a pre-requisite for the reconstruction of high-resolution climate records from stable isotope series of P. nigra ssp. laricio.     

Isotope effect studies of chicken liver NADP malic enzyme: role of the metal ion and viscosity dependence

The role of the metal ion in the oxidative decarboxylation of malate by chicken liver NADP malic enzyme and details of the reaction mechanism have been investigated by 13C isotope effects. With saturating NADP and the indicated metal ion at a total concentration 10-fold higher than its Km, the following primary 13C kinetic isotope effects at C4 of malate [13(V/Kmal)] were observed at pH 8.0: Mg2+, 1.0336; Mn2+, 1.0365; Cd2+, 1.0366; Zn2+, 1.0337; Co2+, 1.0283; Ni2+, 1.025. Knowing the partitioning of the intermediate oxalacetate between decarboxylation to pyuvate and reduction to malate allows calculation of the intrinsic carbon isotope effect for decarboxylation. For Mg2+ as activator, this was 1.049 with NADP and 1.046 with 3-acetylpyridine adenine dinucleotide phosphate, although the intrinsic primary deuterium isotope effects on dehydrogenation were 5.6 and 4.2, and the partition ratios of the oxalacetate intermediate for decarboxylation as opposed to hydride transfer were 0.11 and 3.96 (the result of the different redox potentials of NADP and the acetylpyridine analogue). The close agreement of the intrinsic 13C isotope effects with each other and with the 13C isotope effect for the Mg2+-catalyzed nonenzymatic decarboxylation of oxalacetate of 1.0489 [Grissom, C. B., & Cleland, W. W. (1986) J. Am. Chem. Soc. 108, 5582] indicates a similarity of transition states for these reactions. It was not possible to calculate reasonable intrinsic carbon isotope effects with the other metal ions by use of the partitioning ratio of oxalacetate because of decarboxylation by another mechanism.(ABSTRACT TRUNCATED AT 250 WORDS)     

Stable isotopes provide independent support for the use of mesowear variables for inferring diets in African antelopes

We examine the relationship between mesowear variables and carbon and nitrogen isotopes in 16 species of African antelope (Mammalia: Bovidae). We show significant differences in carbon and nitrogen isotope values between individuals exhibiting sharp versus round cusps, and high versus low occlusal relief. We show significant correlations between mesowear variables and both carbon and nitrogen isotopes. We find significant correlations between mesowear score and nitrogen, but not carbon isotopes. Finally, we find no significant correlations between hypsodonty index and either isotope examined. Our results provide strong support for the use of mesowear variables in palaeodietary reconstructions of antelopes. Our results further suggest that for the antelopes examined here, mesowear signals are a direct result of diet, while hyposodonty may be the result of phylogenetic legacy.     

Stable isotopes of carbon and nitrogen in soil ecological studies

The development of stable isotope techniques is one of the main methodological advances in ecology of the last decades of the 20th century. Many biogeochemical processes are accompanied by changes in the ratio between stable isotopes of carbon and nitrogen (¹²C/¹³C and ¹⁴N/¹⁵N), which allows different ecosystem components and different ecosystems to be distinguished by their isotopic composition. Analysis of isotopic composition makes it possible to trace matter and energy flows through biological systems and to evaluate the rate of many ecological processes. The main concepts and methods of stable isotope ecology and patterns of stable isotope fractionation during organic matter decomposition are considered with special emphasis on the fractionation of isotopes in food chains and the use of stable isotope studies of trophic relationships between soil animals in the field.     

Distribution of the heavy isotope of carbon (13C) in biological systems

Causes conditioning fractionation of carbon isotopes in biological systems are considered. Concepts of E. M. Galimov are discussed. According to these concepts distribution of carbon isotopes between biomolecules and their fragments is quaziequilibrium, i. e. it differs from the equilibrium one by a constant multiplier, which is the same for all the biomolecules of an organism but different for various organisms. These concepts have no theoretical grounds and do not agree with the experimental evidence available. An analysis of experimental data, as well as theoretical considerations, indicate that the observed differences in isotope composition of metabolytes and their fragments in the living organisms are conditioned by the kinetic isotope effects of carbon at the stages of their enzymic transformations and by the portion of substances participating in the reaction. It means that these differences do not depend directly on the constants characterizing the equilibrium distribution of carbon isotopes between corresponding compounds and between different groups inside their molecules.     

An approach to the theory of quantitative and double label autoradiography

The distributions of grains and tracks per cell, as functions of the isotope content in the cell, are basic to all quantitative autoradiography. In this paper a formulation of these distributions in terms of the distribution of grains per disintegration is suggested. An empirical method for evaluating this distribution for various isotopes and various geometrical relationships between source and emulsion is described. The results are used to examine the usefulness of different techniques for double labelling autoradiography.     

Carbon isotopes in functional soil ecology

Soil is an integral part of terrestrial ecosystems. Many soil ecologists interested in soil ecosystem functioning rely, to some degree, on stable isotope methodologies. The study of the natural abundance of carbon isotopes, especially (13)C but also (14)C, in the environment and the use of stable carbon isotope tracers have proved very useful in investigating the soil carbon cycle and soil trophic relationships. Recent methodological and technical advances have greatly extended the possibilities for the application of stable carbon isotopes to terrestrial ecology and have vastly improved our knowledge of belowground ecosystem functioning and will continue to do so. A better understanding of soil processes is invaluable in predicting the future impacts of global environmental change on terrestrial ecosystems.     

The isotope effect in the glycine dehydrogenase reaction is the cause of the intramolecular isotope inhomogeneity of glucose carbon of starch synthesized during photorespiration

The isotope distribution of glucose-6-phosphate in the main pathways of its biosynthesis (in the processes of CO2 assimilation and photorespiration in the Calvin cycle and during resynthesis from the degradation products of lipids and proteins) was analyzed. For reconstructing the isotope distribution of glucoso-6-phosphate synthesized in the Calvin cycle during photorespiration, the functioning of the cycle with regard to its coupling with the glycolate chain, which together constitute the photorespiration chain, was considered. In the glycine dehydrogenase reaction of the glycolate cycle, there arises an isotope effect, which determines the distribution of isotopes in the glucose-6-phosphate and other photorespiration products. The isotope effect of the glycine dehydrogenase reaction increases at the expense of the exhaustion of glucose resources feeding the photorespiration chain. As a result, atoms C-3 and C-4 of glucose become enriched with the heavy isotope, and subsequent mixing of atoms and the specificity of interactions in the photorespiration chain lead to an isotope weighting of the other atoms and an uneven distribution of carbon isotopes in glucose-6-phosphate and other photorespiration products. A comparison of the glucose-6-phosphate isotope patterns in different pathways of the synthesis with the experimental data on the distribution of carbon isotopes in starch glucose of storing plant organs led to the conclusion that the starch resources are predominantly formed at the expense of glucose-6-phosphate of photorespiration. This is consistent with the earlier observed enhancement of photorespiration at the stage of plant maturation.     

Nitrogen isotope effects on glutamate decarboxylase from Escherichia coli

The nitrogen isotope effect on the decarboxylation of glutamic acid by glutamate decarboxylase from Escherichia coli has been measured by comparison of the isotopic composition of the amino nitrogen of the product gamma-aminobutyric acid isolated after 10-20% reaction with that of the starting glutamic acid. At pH 4.7, 37 degrees C, the isotope effect is k14/k15 = 0.9855 +/- 0.0006 when compared to unprotonated glutamic acid. Interpretation of this result requires knowledge of the equilibrium nitrogen isotope effect for Schiff base formation. This equilibrium isotope effect is k14/k15 = 0.9824 for the formation of the unprotonated Schiff base between unprotonated valine and salicylaldehyde. Analysis of the nitrogen isotope effect on decarboxylation of glutamic acid and of the previously measured carbon isotope effect on this same reaction [O'Leary, M.H., Yamada, H., & Yapp, C.J. (1981) Biochemistry 20, 1476] shows that decarboxylation and Schiff base formation are jointly rate limiting. The enzyme-bound Schiff base between glutamate and pyridoxal 5'-phosphate partitions approximately 2:1 between decarboxylation and return to the starting state. The nitrogen isotope effect also reveals that the Schiff base nitrogen is protonated in this intermediate.     

Stable carbon isotope analysis of nucleic acids to trace sources of dissolved substrates used by estuarine bacteria

The natural abundance of stable carbon isotopes measured in bacterial nucleic acids extracted from estuarine bacterial concentrates was used to trace sources of organic matter for bacteria in aquatic environments. The stable carbon isotope ratios of Pseudomonas aeruginosa and nucleic acids extracted from cultures resembled those of the carbon source on which bacteria were grown. The carbon isotope discrimination between the substrate and total cell carbon from bacterial cultures averaged 2.3% +/- 0.6% (n = 13). Furthermore, the isotope discrimination between the substrate and nucleic acids extracted from bacterial cultures was 2.4% +/- 0.4% (n = 10), not significantly different from the discrimination between bacteria and the substrate. Estuarine water samples were prefiltered through 1-micron-pore-size cartridge filters. Bacterium-sized particles in the filtrates were concentrated with tangential-flow filtration and centrifugation, and nucleic acids were then extracted from these concentrates. Hybridization with 16S rRNA probes showed that approximately 90% of the nucleic acids extracted on two sample dates were of eubacterial origin. Bacteria and nucleic acids from incubation experiments using estuarine water samples enriched with dissolved organic matter from Spartina alterniflora and Cyclotella caspia had stable carbon isotope values similar to those of the substrate sources. In a survey that compared diverse estuarine environments, stable carbon isotopes of bacteria grown in incubation experiments ranged from -31.9 to -20.5%. The range in isotope values of nucleic acids extracted from indigenous bacteria from the same waters was similar, -27.9 to -20.2%. Generally, the lack of isotope discrimination between bacteria and nucleic acids that was noted in the laboratory was observed in the field.(ABSTRACT TRUNCATED AT 250 WORDS)     

Stable carbon isotope analysis of nucleic acids to trace sources of dissolved substrates used by estuarine bacteria.

The natural abundance of stable carbon isotopes measured in bacterial nucleic acids extracted from estuarine bacterial concentrates was used to trace sources of organic matter for bacteria in aquatic environments. The stable carbon isotope ratios of Pseudomonas aeruginosa and nucleic acids extracted from cultures resembled those of the carbon source on which bacteria were grown. The carbon isotope discrimination between the substrate and total cell carbon from bacterial cultures averaged 2.3% +/- 0.6% (n = 13). Furthermore, the isotope discrimination between the substrate and nucleic acids extracted from bacterial cultures was 2.4% +/- 0.4% (n = 10), not significantly different from the discrimination between bacteria and the substrate. Estuarine water samples were prefiltered through 1-micron-pore-size cartridge filters. Bacterium-sized particles in the filtrates were concentrated with tangential-flow filtration and centrifugation, and nucleic acids were then extracted from these concentrates. Hybridization with 16S rRNA probes showed that approximately 90% of the nucleic acids extracted on two sample dates were of eubacterial origin. Bacteria and nucleic acids from incubation experiments using estuarine water samples enriched with dissolved organic matter from Spartina alterniflora and Cyclotella caspia had stable carbon isotope values similar to those of the substrate sources. In a survey that compared diverse estuarine environments, stable carbon isotopes of bacteria grown in incubation experiments ranged from -31.9 to -20.5%. The range in isotope values of nucleic acids extracted from indigenous bacteria from the same waters was similar, -27.9 to -20.2%. Generally, the lack of isotope discrimination between bacteria and nucleic acids that was noted in the laboratory was observed in the field.(ABSTRACT TRUNCATED AT 250 WORDS)     

The mechanism of carbon isotope fractionation in the metabolic process]

The mechanism of carbon isotope fractionation in metabolic paths of autotrophic organisms is considered. The principal features of the mechanism proposed are: 1) the emergence of a one-stage kinetic isotope effect of pyruvate decarboxylation during respiration resulting in the formation of two flows of the carbon substrate with different isotope compositions; 2) the multiplication of the one-stage isotope effect by means of the repeated circulation of a light isotope fraction (C2-fragments) in lipid-carbohydrate metabolism and by the simultaneous removal of a heavy isotope carbon dioxide in the Krebs cycle. On the basis of the above mechanism carbon isotope effects are explained of CO2 assimilation and respiration as well as sequential decrease of 13C content in the series of lipids, carbohydrates and proteins. The cuase of the enrichment of the whole organisms in the light isotope in respect to the carbon dioxide of the environment is discussed.     

Isotope effect studies of the role of metal ions in isocitrate dehydrogenase.

Pig heart NADP+-dependent isocitrate dehydrogenase requires a metal ion for activity. Under optimum conditions (pH 7.5, Mg2+ present), the carbon isotope effect is k12/k13 = 0.9989 +/- 0.0004 for the carboxyl carbon undergoing decarboxylation and hydrogen isotope effects are VmaxH/VmaxD = 1.09 +/- 0.04 and (Vmax/Km)H/(Vmax/Km)D = 0.76 +/- 0.12 with threo-D,L-[2-2H]isocitric acid. Deuterium isotope effects measured by the equilibrium perturbation technique under the same conditions are VH/VD = 1.20 for the forward reaction and 1.02 for the reverse reaction. Under these conditions the rate-determining step in the enzymatic reaction must be product release. Dissociation of isocitrate from the enzyme-isocitrate complex and the enzyme-NADP+ complex must be two or more orders of magnitude slower than the chemical steps. The catalytic activity of the enzyme is about tenfold lower in the presence of Ni2+ than in the presence of Mg2+. The carbon isotope effect in the presence of Ni2+ at pH 7.5 is k12/k13 = 1.0051 +/- 0.0012 and the hydrogen isotope effects are VmaxH/VmaxD = 0.98 +/- 0.07 and (Vmax/Km)H/(Vmax/Km)D = 1.11 +/- 0.14. Thus, the rate decrease caused by substitution of Ni2+ for Mg2+ must result from the effects of metal on substrate and product binding and dissociation, rather than effects of metal on catalysis. However, a more detailed analysis of the carbon isotope effects reveals that there is also a large metal effect on the rate of the decarboxylation step, consistent with the view that the carbonyl oxygen of the oxalosuccinate intermediate is coordinated to the metal during decarboxylation.