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Congener-specific carbon isotopic analysis of technical PCB and PCN mixtures using two-dimensional gas chromatography-isotope ratio mass spectrometry.

Analysis of stable carbon isotope fractionation is a useful method to study the sources and fate of anthropogenic organic contaminants such as polychlorinated biphenyls (PCBs) in the environment. To evaluate the utility of carbon isotopes, determination of isotopic ratios of 13C/12C in source materials, for example, technical PCB preparations, is needed. In this study, we determined delta13C values of 31 chlorobiphenyl (CB) congeners in 18 technical PCB preparations and 15 chloronaphthalene (CN) congeners in 6 polychlorinated naphthalene preparations using two-dimensional gas chromatography-combustion furnace-isotope ratio mass spectrometry (2DGC-C-IRMS). Development of 2DGC-IRMS enabled improved resolution and sensitivity of compound-specific carbon isotope analysis (CSIA) of CB or CN congeners. Delta13C values of PCB congeners ranged from -34.4 (Delors) to -22.0/1000 (Sovol). Analogous PCB preparations with similar chlorine content, but different geographical origin, had different delta13C values. PCB preparations from Eastern European countries--Delors, Sovol, Trichlorodiphenyl, and Chlorofen--had distinct delta13C values. PCB mixtures showed increased 13C depletion with increasing chlorine content. Delta13C values for individual CB congeners varied depending on the degree of chlorination in technical mixtures. Delta13C values of CN congeners in Halowaxes ranged from -26.3 to -21.7/1000 and these values are within the ranges observed for PCBs. This study establishes the range of delta13C values in technical PCB and PCN preparations, which may prove to be useful in the determination of sources of these compounds in the environment. This is the first study to employ 2DGC-IRMS analysis of delta13C values in technical PCB and PCN preparations.

Carbon Isotopes↗

Kinetic isotope effects on cytochrome P-450-catalyzed oxidation reactions: full expression of the intrinsic isotope effect during the O-deethylation of 7-ethoxycoumarin by liver microsomes from 3-methylcholanthrene-induced hamsters.

The intrinsic primary deuterium isotope effect for the O-deethylation of 7-ethoxycoumarin has been estimated by the Northrop method [D. B. Northrop (1977) in Isotope Effects on Enzyme-Catalyzed Reactions (Cleland, W. W., O'Leary, M. H., and Northrop, D. B., eds.), pp. 122-152, University Park Press, Baltimore] for the microsomal cytochrome P-448 system from 3-methylcholanthrene-induced hamster livers. The intrinsic isotope effect (Dk = 5.5) was found to be equivalent to the observed deuterium isotope effect, demonstrating that the isotope effect for this reaction was fully expressed by this cytochrome P-448 system. These data unequivocally demonstrate that C-H bond cleavage is the rate-limiting step in the overall reaction catalyzed by this system. The decrease in the rate of product formation, occurring as a consequence of deuterium substitution, resulted in a reduction in the quantity of substrate metabolized but was not accompanied by the change in regiospecificity observed in previous studies with a hepatic cytochrome P-448 isozyme purified from 3-methylcholanthrene-induced rats. These data demonstrate that the catalytic site of the hamster isozyme(s) offers more constraints to 7-ethoxycoumarin reorientation than does the catalytic site of the rat liver isozyme.

Animals↗

Application of isotopically labeled methylmercury for isotope dilution analysis of biological samples using gas chromatography/ICPMS.

An isotope dilution (ID) procedure for the determination of methylmercury (MMHg) in biological samples using an inductively coupled plasma mass spectrometer as detector after the capillary gas chromatographic separation (CGC/ICPMS) has been developed. For the first time, open-focused-microwave pretreatment has been used in conjunction with ID. Optimum conditions for the measurement of isotope ratios on the fast transient chromatographic peaks have been established. Mass bias was found to be about 1.5%/mass unit and was corrected by using the simultaneously measured thallium signals at 203Tl and 205Tl. After mass-bias correction, deviation of the theoretical mercury ratio values was found to be as low as 0.2%. Isotope ratio precisions based on the peak areas measurements were 0.3% RSD for 20 pg injected (as Hg absolute). The absolute detection limits were in the range of 20-30 fg for 202Hg and 201Hg. Methylmercury enriched in 201Hg has been synthesized by direct reaction with methylcobalamine. The concentration of the MMHg spike has been measured by reverse isotope dilution with a natural MMHg standard. The capabilities of CGC/ICPMS to measure isotope ratios were used to optimize sample derivatization by aqueous ethylation with NaBEt4 with respect to MMHg degradation pathways and quantitative recovery. The accuracy of the method developed has been validated with biological certified reference materials (CRM-463, DORM-1).

Animals↗

High accuracy isotope dilution analysis for the determination of ethanol using gas chromatography-combustion-isotope ratio mass spectrometry.

A procedure was established for the determination of ethanol in water samples by isotope dilution analysis. After spiking the sample with labelled [13C2]ethanol, it was analysed by gas chromatography-combustion-isotope ratio mass spectrometry. Results are reported for two certified reference materials and also ethanol solutions prepared for a CITAC (Co-operation on International Traceability in Analytical Chemistry) interlaboratory comparison. The certified reference materials were certified using the dichromate titration method at nominal levels of 80 and 200 mg per 100 mL. The CITAC solutions were prepared gravimetrically at nominal levels of 50, 80 and 200 mg per 100 mL. The results of the analysis agree well to within 0.5% of the gravimetric values of the different samples. The relative expanded standard uncertainties (with a coverage factor equal to 2) associated with the results varied between 0.18 and 0.37%, a range that encompassed the gravimetric values for the different samples. A complete uncertainty budget was also drawn up so that the different contributions could be identified and quantified. The main contributions were due to variations in the measured isotope amount ratios and a 'between' blend component introduced to quantify the contribution of factors such as the degree of matching of the isotope amount ratios between standards and samples used in the isotope dilution analysis.

Journal Article↗

Determination of inorganic chlorine stable isotopes by continuous flow isotope ratio mass spectrometry.

Chlorine stable isotope analyses of inorganic samples were conducted using continuous flow isotope ratio mass spectrometry (CF-IRMS) coupled with gas chromatography (GC). Inorganic chloride was precipitated in the form of silver chloride (AgCl) by using silver nitrate in a standard methodology. Chlorine stable isotope analysis was carried out on methyl chloride (CH3Cl) after converting AgCl into CH3Cl by reacting it with methyl iodide (CH3I). The reaction between AgCl and CH3I took place in 20 mL size vials. Addition of CH3I was performed in a glove bag under helium flow. An Agilent 6890 gas chromatograph equipped with a CTC Analytics CombiPAL autosampler and a DB-5MS 60 m column was used to separate CH3Cl from CH3I. This new technique uses samples as small as 0.2 mg of AgCl (1.4 micromol of Cl-). The chlorine stable isotope analysis using continuous flow technology showed excellent precision and accuracy. The internal precision using pure CH3Cl gas is better than +/-0.04 per thousand (+/-STDV). The external precision using seawater standard is better than +/-0.07 per thousand (+/-STDV) for n=12. Moreover, the sample analysis time is much shorter and many more samples can be analyzed in one day than by using the conventional off-line techniques.

Chlorine↗

[Isotopic composition of the delta-18O--delta-13C from the otoliths of reef fish from Taiaro (Tuamotu, French Polynesia): isotopic and biological implications].

Nuclei (larval stage) and outer parts (adult stage) of fish otoliths from the Taiaro closed lagoon (French Polynesia) and adjacent ocean have been analysed for the C-O isotopic compositions. delta 18O values of the nuclei of both populations indicate that isotopic equilibrium is reached. This implies that the lagoonal fish population has done its complete biological cycle in the lagoon and represents an adaptation in a closed system. delta 18O values of the outer parts show a slight isotopic disequilibrium (< 0.2@1000) interpreted in term of vital effect. All the delta 13C values exhibit a strong isotopic disequilibrium related to metabolic activity.

Animals↗

Stable isotope ratios as a tool in microbial forensics--Part 2. Isotopic variation among different growth media as a tool for sourcing origins of bacterial cells or spores.

Since the anthrax attacks of 2001 the need for methods to trace the origins of microbial agents has become urgent. The stable isotope ratios of bacteria record information from both the nutrients and the water used to make their culture media and could potentially be used to provide information about their growth environment. We present a survey of carbon (C), nitrogen (N), and hydrogen (H) stable isotope ratios in 516 samples of bacteriological culture media. The observed variation was consistent with expected isotopic variation in the plant and animal products upon which the media are based. The variation is sufficient to translate into substantial isotope variation in cultures grown on different batches of media, and thus to allow investigators to determine whether seized media could have been used to produce seized bioweapons agents.

Agar↗

Determining isotopic life history trajectories using bone density fractionation and stable isotope measurements: a new approach.

A number of recent studies have attempted to trace diet at different stages of an individual's life by comparing isotope ratios of bone from different gross anatomical sites within the skeleton. In this study we develop this approach further by separating bone of differing mineral densities within one skeletal element, where each density fraction represents a different period of time. Isotope ratios are measured for these fractions. Each density fraction represents a period of bone formation and maturation, where younger (more recently formed) bone is less well-mineralized and therefore less dense than relatively older packets of bone. In an adult, bone is therefore able to partition approximately the last 15 years of life. Bone fractions were recovered by stepped ultracentrifugation in a series of organic solvents of increasing density, and then collagen was recovered by decalcification in dilute acid, and stable carbon isotope ratios ((13)C/(12)C) were measured. Bone density microstructure was checked for bacterial remodelling using backscattered electron imaging in a scanning electron microscope. Our results indicate that the bone density fractionation method is applicable to archaeological material, here extending to a maximum of 5,000 years BP, and that collagen can successfully be extracted from such fractions. The carbon isotope values for bone fractions of different densities patterned out as expected in one modern control bone and in specimens from five archaeological human skeletons, including three precolonial hunter-gatherers and two 18th/19th century individuals. The latter two are known (from previous assessments) to have undergone marked changes in diet during their lifetimes. Postmortem alteration was evident in some of the specimens examined. The bone density fractionation approach has allowed greater resolution of diet than has hitherto been possible and has provided access to the elusive last years and months of an individual's life.

Adult↗

Amount-dependent isotopic fractionation during compound-specific isotope analysis.

The performance of a gas chromatography-combustion-isotope ratio mass spectrometry system (GC-C-IRMS) with respect to the dependence of delta(13)C values on the amount of sample is presented. Particular attention is paid to the localization of the amount-dependent isotopic fractionation within the system. Injection experiments with varying amounts of gases (CO(2), n-hexane, and toluene) revealed that neither the detector unit nor the combustion reactor, but rather the conditions in the split/splitless injector, contributed to this effect. Although optimization of injector parameters was performed and a reduction of this adverse effect from 3 to 1 per thousand was achieved, it was not possible to eliminate isotopic fractionation completely. Consequently, additional injector parameters have to be considered and adjusted to achieve injection conditions free of fractionation. For routine analysis of the compound-specific delta(13)C analysis of different biomarkers in many environmental samples, perfect optimization may not always be reached. Therefore, in order to prevent systematic errors in the measured delta(13)C values due to different sample concentrations, it is suggested that correction for the remaining unknown amount-dependent fractionation can be made by means of co-analyzing standards of varying analyte concentrations and known delta(13)C values. Residual overall amount-dependent isotope-fractionation can thus be corrected mathematically.

Algorithms↗

Isotopic ((13)C) analysis of dissolved organic carbon in stream water using an elemental analyzer coupled to a stable isotope ratio mass spectrometer.

A technique for measurement of the stable isotope composition of dissolved organic carbon (DOC) in stream water, using an elemental analyzer (EA) coupled to an isotope ratio mass spectrometer (IRMS), is described. Stream water samples were concentrated by rotary evaporation, acidified to remove dissolved inorganic carbon (DIC), and dried in silver cups prior to analysis. Precision was evaluated with standards (alanine and humic acid), and with stream water samples with varying (13)C enrichment. Standards and samples were also prepared in sealed quartz tubes for high-temperature combustion (HTC) and analyzed by dual inlet for comparison. The delta(13)C values of natural abundance standards and samples measured by the two techniques differed by <or=0.3 per thousand. Isotopically enriched stream water samples analyzed using the EA and HTC methods had comparable delta(13)C and atom % values (differed by <or=6%). Expensive quartz vessels and the extensive time required for sample lyophilization, combustion and cryogenic separation of combustion products before isotopic analysis for the HTC method are eliminated with the EA method. Overall, the EA method is simpler, faster, and more economical than the HTC method, and it can be used for (13)C-enriched as well as natural abundance samples.

Carbon Isotopes↗

Isotope ratio monitoring of small molecules and macromolecules by liquid chromatography coupled to isotope ratio mass spectrometry.

In the field of isotope ratio mass spectrometry, the introduction of an interface allowing the connection of liquid chromatography (LC) and isotope ratio mass spectrometry (IRMS) has opened a range of new perspectives. The LC interface is based on a chemical oxidation, producing CO2 from organic molecules. While first results were obtained from the analysis of low molecular weight compounds, the application of compound-specific isotope analysis by irm-LC/MS to other molecules, in particular biomolecules, is presented here. The influence of the LC flow rate on the CO2 signal and on the observed delta13C values is demonstrated. The limits of quantification for angiotensin III and for leucine were 100 and 38 pmol, respectively, with a standard deviation of the delta13C values better than 0.4 per thousand. Also, accuracy and precision of delta13C values for elemental analyser-IRMS and flow injection analysis-IRMS (FIA-LC/MS) were compared. For compounds with molecular weights ranging from 131 to 66,390 Da, precision was better than 0.3 per thousand, and accuracy varied from 0.1 to 0.7 per thousand. In a second part of the work, a two-dimensional (2D)-LC method for the separation of 15 underivatised amino acids is demonstrated; the precision of delta13C values for several amino acids by irm-LC/MS was better than 0.3 per thousand at natural abundance. For labelled mixtures, the coefficient of variation was between 1% at 0.07 atom % excess (APE) for threonine and alanine, and around 10% at 0.03 APE for valine and phenylalanine. The application of irm-LC/MS to the determination of the isotopic enrichment of 13C-threonine in an extract of rat colon mucosa demonstrated a precision of 0.5 per thousand, or 0.001 atom %.

Amino Acids↗

Measurement of 15N/14N isotopic composition in individual plasma free amino acids of human adults at natural abundance by gas chromatography-combustion isotope ratio mass spectrometry.

We describe a high-precision methodology to determine the 15N/14N isotopic composition of 13 plasma free amino acids out of 500 microliters plasma, measured as N-pivaloyl-i-propyl amino acid esters by gas chromatography-isotope ratio mass spectrometry. It is now possible to measure 15N isotopic natural abundances in plasma free amino acids, which has not been the case previously because of the minimum requirement of 60 ml plasma to supply, e.g., 1 mg free leucine, for example, when performing a conventional preparative isolation. Data from seven healthy American and German subjects reveal a similar delta 15N pattern in plasma free amino acids, although there are small differences in individual amino acids. Phenylalanine and threonine showed the lowest abundance (-12 and -5/1000 delta 15N, respectively), whereas alanine, leucine, proline, and ornithine ranged between +10 and +15/1000 delta 15N. Lysine ranged between +1 and +4/1000 delta 15N and showed the lowest variation of all measured amino acids. The metabolically related aromatic amino acids, phenylalanine and tyrosine, differ by 15/1000 in their 15N abundance. The isolation of amino acids by cation-exchange chromatography resulted in a small alteration of 15N/14N isotopic composition in the amino acids glycine, lysine, and glutamic acid of maximal 1.2, 0.4, and, 0.4/1000, respectively, but the remaining amino acids were unchanged. The method described offers new possibilities for the investigation of the amino acid metabolism in vivo.

Adult↗

Changes in delta 13C stable isotopes in multiple tissues of insect predators fed isotopically distinct prey.

Traditionally, researchers have used measurements of carbon stable isotopes to infer the composition of consumers' diets. However, since consumer's tissues may process carbon isotopes differently, particularly following a diet shift, it is possible to use measurements of carbon isotopes in multiple tissues to determine not only the composition of an individual's diet, but also the temporal dynamics thereof. This study examined how stable isotopes of carbon (13C/12C, expressed as delta 13C) changed in different adult tissues of two predacious beetles, Harmonia axyridis and Coccinella septempunctata (Coleoptera: Coccinellidae). In the laboratory, we switched ladybeetles from a C3-based diet (soybean aphids, Aphis glycines) to a C4-based one (corn leaf aphids, Rhopalosiphum maidis). The delta 13C of metabolically active tissues such as the body fat and reproductive organs changed rapidly (< or =5 days) following the diet shift. Tissues expected to be more metabolically inert, such as wings, changed more slowly over the same period. Although these general patterns were largely similar between males and females, females had more rapid changes in delta 13C in fat and reproductive tissues. However, females showed a significant depletion in delta 13C after 10 days, while males' delta 13C continued to increase. Given the results of this experiment, it is now possible to distinguish between ladybeetles eating a mixed diet (beetles with multiple tissues at similar, intermediate, equilibrial delta 13C signatures) from those that have shifted diets (beetles with different tissues at distinctly different delta 13C values). Thus, this approach can be used broadly to infer not only what constitutes the diet of a consumer, but also the temporal history of dietary intake.

Animals↗

Isotope-specific analysis of Ni by ICP-MS: applications of stable isotope tracers to biokinetic studies.

Inductively coupled plasma mass spectrometry (ICP-MS) offers excellent detection limits and isotopic analysis of Ni in aqueous standards, but is prone to interferences--mainly from Ca-containing polyatomics--when biological matrices are analyzed for Ni. We have used multivariate calibration with principal components analysis (PCA) to correct for mass overlaps in serum digests. The resulting detection limit for Ni is below 1 microgram/l and the within-run imprecision is 6% at 1.46 micrograms Ni/l. In urine, the higher Ca content renders routine application of PCA problematic. We evaluated several methods of pre-concentration, and have developed a method of Ca oxalate precipitation that allows direct analysis of Ni in the diluted supernatant. The stable isotope 62Ni and the radiosotope 63Ni were co-administered i.v. to rats and the serum and urinary clearances were determined by liquid scintillation counting and ICP-MS. Ni measurements by both methods were in excellent agreement, and serum clearance fit a double exponential decay consistent with the two-compartment model of Onkelinx et al. [24]. A human volunteer ingested 61Ni (20 micrograms Ni/kg body wt.) in water after an overnight fast. Identical serum levels, peaking near 35 micrograms/l at 2 h, were measured by electrothermal atomic absorption spectrometry and ICP-MS with PCA. Urinary excretion of 61Ni measured by ICP-MS demonstrated absorption of 30% of the administered dose. We conclude that Ni isotopes can be measured in body fluids by ICP-MS at levels that allow stable isotope tracer studies in humans.

Adult↗

Sector field inductively coupled plasma mass spectrometry, another tool for plutonium isotopes and plutonium isotope ratios determination in environmental matrices.

The transfer of radio nuclides into the different compartments of the environment are widely studied and leads to the elaboration of transfer models in order to evaluate potential impact onto the environment and humans. Accurate experimental data are needed to validate these models for all types of matrices (air, water, sediments, soils, biota and food...). Among these radionuclides, 238Pu, 239Pu, 240Pu and 241Pu, are often mentioned. They have been released into the environment by nuclear weapon tests, nuclear facilities, reactors or satellite accidents. These different sources have different 240Pu/239Pu ratios and therefore this ratio is used to provide information on the source of contamination into the environment. The most conventional analytical tools used for plutonium isotope determination are liquid scintillation and alpha spectrometry, and thermal ionisation mass spectrometry (TIMS) is still considered as the primary method for determination of plutonium isotope ratios. During the last decade, mass spectrometers equipped with plasma ion sources and sector field analysers were developed and can offer now another alternative method for the accurate determination of isotope content and ratios of long-lived radionuclides in environmental samples. This paper presents and discusses the results obtained for 239Pu, 240Pu and 241Pu content and isotope ratios by sector field ICP-MS in different environmental matrices.

Environmental Monitoring↗

Isotope ratios of molybdenum determined by thermal ionization mass spectrometry for stable isotope studies of molybdenum metabolism in humans.

Methods were developed to separate and purify Mo from biological samples and to measure isotopic ratios in 1 microgram of Mo. A magnetic sector, thermal ionization mass spectrometer was used with simultaneous collection of five isotopes. Isotopic ratios were corrected for mass fractionation by iterative normalization using the 96/98 ratio. Ion beam intensity was enhanced by using a double-filament configuration, loading samples onto evaporation filaments with silica gel and boric acid. A triple-isotope-dilution approach was used, so the method could be applied to two-tracer studies of Mo metabolism in human subjects. 94Mo was added to samples prior to purification to quantify the total Mo content of samples and to determine the amounts of enriched 97Mo and 100Mo appearing in urine and fecal samples of study participants. The three ratios, 94/98, 97/98, and 100/98, were determined with within-run precision of from 0.06 to 0.10% (RSD). Precision of the ratios between replicates was from 0.05 to 0.08%.

Boric Acids↗

Species-specific isotope dilution analysis and isotope pattern deconvolution for butyltin compounds metabolism investigations.

A methodology for the study of the absorption and metabolism of butyltin compounds in laboratory animals using isotopically enriched species was developed. The method is based on the oral administration of 119Sn-labeled monobutyltin (MBT), 118Sn-labeled dibutyltin (DBT), and 117Sn-labeled tributyltin (TBT) to the animals and the measurement of both the concentration and isotopic composition of these compounds in the different tissues by GC-ICPMS. The degradation of butyltin compounds during their metabolism was computed using least-squares isotope pattern deconvolution, and their concentration was measured by reverse isotope dilution analysis using natural-abundance MBT, DBT, and TBT standards. Male Wistar rats were used as models to evaluate the proposed methodology. Preliminary toxicological results obtained with one rat indicate that TBT is highly absorbed (64.4%), and it is found in all organs with relatively high levels in stomach and intestines. The apparent absorption of DBT was 27.3% and was mainly found in liver, kidney, and intestines. However, a large proportion of the found DBT is formed from the degradation of TBT (approximately 40% of the found DBT in liver is degraded TBT). The apparent absorption of MBT was found to be 12.5%, and the originally administered MBT was mainly recovered in the feces. However, MBT was clearly detected in liver, kidney, stomach, intestines, and urine as degradation products of DBT and TBT. Although a significant variability from rat to rat is expected to be obtained, the analytical variability provided by this methodology is small enough to yield meaningful biological results. The results obtained demonstrate that the developed methodology is able to follow qualitatively, quantitatively, and simultaneously the specific metabolic pathways of different species of a given element.

Animals↗

Isotope trapping and positional isotope exchange with rat and chicken liver phosphoenolpyruvate carboxykinases.

Isotope-trapping studies of the enzyme.MgGTP complex were carried out with rat liver cytosolic and chicken liver mitochondrial phosphoenolpyruvate carboxykinases. For the rat liver enzyme, MgGTP was partially trapped from both E.MgGTP and E.MgGTP.OAA complexes, consistent with a steady-state random mechanism. For the chicken liver enzyme, MgGTP was 100% trapped from the E.MgGTP.OAA complex, consistent with a steady-state ordered mechanism. The rate constants for the interaction of MgGTP with the free enzymes are approximately 10(7) M-1 S-1, somewhat lower than the diffusion limit for association. The dissociation rate for the enzyme.MgGTP complexes is 26-92 s-1, reflecting a tightly bound complex with high commitment to catalysis in the presence of oxaloacetate. Positional isotope-exchange studies were also carried out with phosphoenolpyruvate carboxykinases from rat and chicken. No exchange if the beta gamma-18O in [beta gamma-18O, gamma-18O3]GTP to form [beta-18O, gamma-18O3]GTP was detected in the absence of oxaloacetate. In the presence of oxaloacetate, no positional isotope exchange of [beta gamma-18O, gamma-18O3]GTP was detected during initial rate conditions. The results indicate that at least one of the products dissociates rapidly from the E.MgGDP.PEP.CO2 complex relative to the net rate of MgGTP formation from the E.MgGDP.PEP.CO2 complex. A rapid equilibrium between the central complexes in which the beta-phosphoryl of GDP is restricted with respect to torsional rotation cannot be excluded but is unlikely on the basis of the relative rates of catalysis and torsional rotation. The addition of Mn2+, an activator of phosphoenolpyruvate carboxykinase, did not influence the positional isotope-exchange results.(ABSTRACT TRUNCATED AT 250 WORDS)

Animals↗