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Regional characteristics of sulfur and lead isotope ratios in the atmosphere at several Chinese urban sites.

Sulfur and lead isotope ratios in the atmosphere were measured at several selected sites (Harbin, Changchun, Dalian, Waliguan, Shanghai, Nanjing, Guiyang) in China and Tsukuba (Japan), to reveal regional sources characteristics over Eastern Asia. Average S isotope ratios for SO2 and sulfate in the atmosphere in China were close to those of the coals used in each region, indicating a considerable contribution of coal combustion to the sulfur compounds in the atmosphere. Most northern cities had around 5% sulfur isotope ratio, while Guiyang, a southwestern city in China, showed a considerably lower sulfur isotope ratio (about -3%) because of the unusually light sulfur isotope ratio of coals in this region. These were considerably different from the value (-1.4%) for Tsukuba (Japan). Lead isotope ratios also suggested that coal combustion considerably contributed to atmospheric lead in some cases in China. At the same time, influences by the emission of Chinese lead ores were also observed in northern cities. Seasonal variations of both sulfur and lead isotope ratios indicated the existence of a certain amount of industrial sources other than coal combustion. In addition, fractionation effect between SO2 and sulfate showed a seasonal tendency (high in winter (0-6%) and low in summer (-1-3%)), suggesting the oxidation pathway of SO2 changed seasonally.

Air Pollution↗

Polycyclic aromatic hydrocarbon purification procedures for compound specific isotope analysis.

Purification and isotope analysis methods were developed to accurately measure the stable carbon isotope ratio of individual PAHs in environmental samples. Sample extracts were separated into several fractions by column chromatography and were purified by high-performance liquid chromatographic and thin-layer chromatographic techniques. The mean recovery of the purification method for all compounds was approximately 80%. The purity of isolates was verified by GC/MS in the full scan mode. The accuracy and precision of the method were verified using authentic standards of known isotopic compositions. The standard deviation for multiple analyses ranged between 0.1 and 0.4%o for standard material and between 0.1 and 0.7%o for environmental extracts after purification. The purification and isotope analysis methods were used to discern the sources of PAHs in environmental samples using variations in stable carbon isotopic compositions of individual compounds. Itwas confirmed thatthe purification method effectively purifies environmental samples while retaining original isotopic signatures so that PAH content and stable isotopic compositions can be used to infer contaminant sources in complex environmental settings.

Carbon Isotopes↗

The origin of chondritic macromolecular organic matter: a carbon and nitrogen isotope study.

The N and C abundances and isotopic compositions of acid-insoluble carbonaceous material in thirteen primitive chondrites (five unequilibrated ordinary chondrites, three CM chondrites, three enstatite chondrites, a CI chondrite and a CR chondrite) have been measured by stepped combustion. While the range of C isotopic compositions observed is only delta 13C = 30%, the N isotopes range from delta 15N approximately -40 to 260%. After correction for metamorphism, presolar nanodiamonds appear to have made up a fairly constant 3-4 wt% of the insoluble C in all the chondrites studied. The apparently similar initial presolar nanodiamond to organic C ratios, and the correlations of elemental and isotopic compositions with metamorphic indicators in the ordinary and enstatite chondrites, suggest that the chondrites all accreted similar organic material. This original material probably most closely resembles that now found in Renazzo and Semarkona. These two meteorites have almost M-shaped N isotope release profiles that can be explained most simply by the super-position of two components, one with a composition between delta 15N = -20 and -40% and a narrow combustion interval, the other having a broader release profile and a composition of delta 15N approximately 260%. Although isotopically more subdued, the CI and the three CM chondrites all appear to show vestiges of this M-shaped profile. How and where the components in the acid-insoluble organics formed remains poorly constrained. The small variation in nanodiamond to organic C ratio between the chondrite groups limits the local synthesis of organic matter in the various chondrite formation regions to at most 30%. The most 15N-rich material probably formed in the interstellar medium, and the fraction of organic N in Renazzo in this material ranges from 40 to 70%. The isotopically light component may have formed in the solar system, but the limited range in nanodiamond to total organic C ratios in the chondrite groups is consistent with most of the organic material being, presolar.

Carbon↗

Doubly labeled water method: in vivo oxygen and hydrogen isotope fractionation.

The accuracy and precision of the doubly labeled water method for measuring energy expenditure are influenced by isotope fractionation during evaporative water loss and CO2 excretion. To characterize in vivo isotope fractionation, we collected and isotopically analyzed physiological fluids and gases. Breath and transcutaneous water vapor were isotopically fractionated. The degree of fractionation indicated that the former was fractionated under equilibrium control at 37 degrees C, and the latter was kinetically fractionated. Sweat and urine were unfractionated. By use of isotopic balance models, the fraction of water lost via fractionating routes was estimated from the isotopic abundances of body water, local drinking water, and dietary solids. Fractionated water loss averaged 23% (SD = 10%) of water turnover, which agreed with our previous estimates based on metabolic rate, but there was a systematic difference between the results based on O2 and hydrogen. Corrections for isotopic fractionation of water lost in breath and (nonsweat) transcutaneous loss should be made when using labeled water to measure water turnover or CO2 production.

Body Water↗

Stable isotope techniques in human nutrition research: concerted action is needed.

Use of stable isotopes in applied nutrition has been a developing field for over 60 years. The past 20 years has seen improvements in computer and mass-spectrometer technology that has opened up even greater possibilities in the understanding of human metabolism. While improvements in technology can bring great opportunities, it can also cause problems if there is no consensus among the stable isotope user-community on standardization of new techniques and methods. Users of stable isotopes have traditionally been split into two groups; those who work with heavy isotopes (e.g., 58Fe, 70Zn) and those who work with light isotopes (e.g., 2H218O). Standardization issues have been addressed by the light isotope users and awareness of this type of problem is starting to emerge within the heavy isotope community.

Bias↗

Stable isotopic abundances as reflections of ingestion practices.

The proportions of stable isotopes found in biological tissues (e.g., 13C/12C, 15N/14N, or 18O/16O) are constant only on a macroscopic scale. Sensitive mass spectrometric measurements of the isotope ratio or isotopic abundance for each element show that the tissue (and organism) displays small excursions in these abundances, which are reflections of isotope fractionations that occur in prior stages of the food chain. These excursions can be detected in respiratory CO2 in urine, and in stool, with changes over time intervals as short as 2 hours or as long as 6-12 months. Perturbation of these stable isotopic abundances has been used to demonstrate phenomena as gross as the change in carbon sources of milk proteins when cows are moved from winter silage to summer pastures, or as subtle as the utilization of a single feeding of complex carbohydrates by infants by measuring the isotopic abundance of their respiratory CO2. The use of marker molecules enriched with 13C, 15N, or 18O thus provides a nonpharmacological, nonradioactive, and under ideal conditions, noninvasive procedure to document the ingestion of single or multiple doses of the pharmacological agent being tested. Such generic markers are potentially suitable for all study populations, regardless of developmental age, reproductive activity, or degree of compliance.

Breath Tests↗

The use of stable isotope techniques for nutritional and metabolic research in paediatrics.

Stable isotope methods are increasingly used in paediatrics for clinical diagnosis and research due to marked improvements in analytical technologies and better availability of suitable tracers. The safety of stable isotopes is of major importance for use in children. Large amounts of deuterium well above the doses applied under clinical conditions may induce adverse effects. In contrast, heavier stable isotopes such as 13C, 15N or 18O do not induce adverse effects even at the highest enrichments obtained, and they are safe. Breath tests with measurements of 13CO2 enrichment after oral application of a tracer can reliably evaluate helicobacter pylori infection and gastric emptying kinetics. Combined with an estimation of total CO2 production, 13CO2 breath tests allow estimation of the absorption and oxidation of 13C-labelled substrates, such as medium- and long-chain triglycerides, and demonstrates the beneficial effect of carnitine supplements on fat oxidation in primary carnitine deficiency. The study of metabolic processes may require the sampling of blood for isotopic analyses of metabolites of the applied tracer. Gas chromatography-isotope ratio mass spectrometry can detect tracer in individual components from small plasma samples. The high precision enabled us to utilize the small differences in natural 13C-enrichment between dietary fats to study fatty acid turnover in term infants, in whom the dietary fat source was switched to corn oil with a slightly higher 13C-content. With this approach we demonstrated active conversion of linoleic into arachidonic acid. We also applied biotechnologically produced, U-13C labelled linoleic and alpha-linolenic acids to infants and detected the conversion of these essential fatty acids to their longer chain polyunsaturated derivatives, with an apparent change of conversion activity with age. Moreover, it has become possible to measure tissue protein synthesis from small biopsy samples obtained in situ without surgery, such as forceps biopsies of rectal tumors. These few examples of recent developments demonstrate the great clinical and scientific potential of stable isotope methods in future paediatric applications.

Carbon Isotopes↗

Concentration dependence of methyl palmitate isotope ratios by electron impact ionization gas chromatography/mass spectrometry.

Isotope ratios must be measured precisely when stable isotopic tracers are used for in vivo metabolic kinetic studies since low enrichments are generally achieved above relatively high natural abundance backgrounds. We have observed that the (m + 1)/(m + 0) isotope ratio for the molecular ion of methyl palmitate (measured by electron impact ionization selected ion monitoring gas chromatography/mass spectrometry) is limited by a dependence of the isotope ratio on the quantity of sample analyzed. Since it is not practical to analyze exactly the same quantity of sample in a series of samples, this concentration dependence decreases the apparent precision of the isotope ratio measurement. The apparent natural abundance (m + 1)/(m + 0) isotope ratio increased from approximately 0.185 (0.2 nmol analyzed) to 0.20 (2.0 nmol). The concentration dependence was not altered as the quadrupole tuning resolution was varied and did not appear to arise from system non-linearity. The major source of concentration dependence derived from hydrogen abstraction during ion-molecule collisions within the ionization chamber. The concentration dependence was decreased as the repeller voltage increased and ion residence times in the source were reduced. Furthermore, the integrated (m + 1) peak ares increased with the square of the (m + 0) peak area, consistent with a bimolecular ion-molecule collision process. A simple mathematical correction for the concentration dependence afforded a ten-fold improvement in the coefficient of variation of the isotope ratio measurement.(ABSTRACT TRUNCATED AT 250 WORDS)

Gas Chromatography-Mass Spectrometry↗

Incorporation of stable isotope-labeled arachidonic acid into cellular phospholipid molecular species and analysis by fast atom bombardment tandem mass spectrometry.

The source of arachidonic acid metabolized to eicosanoids by 5-lipoxygenase was studied in a cultured neoplastic mast cell using a stable isotope tracer and tandem mass spectrometry strategy. Selected reaction monitoring and fast atom bombardment were used to analyze eight major arachidonate molecular species of glycerophosphocholine, nine major molecular species of glycerophosphoethanolamine, three major species of glycerophosphocholine, nine major molecular species of glycerophosphoethanolamine, three major species of glycerophosphoinositol, and three major glycerophosphoserine molecular species. Incubation of the mast cells with (2H8)arachidonic acid led to a time-dependent isotopic incorporation in each of these molecular species. Following stimulation with calcium ionophore A23187, the isotope incorporation of leukotriene B4 (LTB4) was found to be higher than that of the major arachidonate-containing glycerophospholipid molecular species. The isotope incorporation of LTB4 was similar to that found for free arachidonic acid present in the unstimulated cell. In order to prevent direct labeling of the intracellular, free arachidonic acid pool, (2H4)linoleic acid was added to the culture medium as a biochemical precursor of labeled arachidonic acid. There was a time-dependent increase of the specific incorporation of labeled arachidonic acid into each of the phospholipid molecular species of each lipid class after incubation with (2H4)linoleic acid. Importantly, (2H4)linoleic acid incubation also resulted in deuterium-labeled arachidonic acid in the free arachidonic acid, intracellular pool. The arachidonic acid isotopic incorporation in this pool very closely correlated with the isotopic incorporation of LTB4 (correlation coefficient 0.97) synthesized after A23187 stimulation, while the isotopic incorporation of the extracellularly released, not esterified arachidonic acid, after stimulation, did not.(ABSTRACT TRUNCATED AT 400 WORDS)

Animals↗

Determination of amino acid isotope enrichment using liquid chromatography-mass spectrometry.

The change in amino acid enrichment, an indicator of a change in protein synthesis and/or degradation, is usually measured using gas chromatography-mass spectrometry and/or (GC-combustion) isotope ratio mass spectrometry. Unfortunately, often a complex and sensitive derivatization procedure and/or a large amount of sample is required. Also, these techniques are less suited to study intermediary metabolism, in which the simultaneous application (and thus measurement) of multiple amino acid tracers is preferred. Alternatively, in this study the possibilities of the coupling of liquid chromatography and mass spectrometry were explored, resulting in the measurement of both the concentration and isotope enrichment of o-phthaldialdehyde (OPA)-derivatizated plasma amino acids in one run. This was achieved by the injection of OPA-derivatizated amino acids into an automated HPLC system. After the elution of buffer salts and reagent excess to drain using column switching, the column effluent was directed via a fluorescence detector into a Thermoquest Model LCQ benchtop LC-MS. Mass spectrometric measurements were performed in "zoom-scan" mode, employing multiple scan events if the target components were not baseline separated. Best signal-to-noise ratio's were obtained using the LCQ's electrospray probe in the negative mode. Still, when working under standard conditions the total ion current of OPA-amino acid derivatives eluting at the beginning of the chromatogram (e.g., citrulline, arginine and glycine) was by a factor of 5 lower, compared to components eluting in the last part of the chromatogram (leucine, valine, and ornithine). These differences could be minimized by increasing the temperature of the heated capillary to 260 degrees C and by applying 5% collision energy (between the skimmer and the first octapole) to the first eluting components. A further improvement could not be obtained by the addition of makeup liquids like ammonia, acetic acid, methanol, or acetonitrile (up to 25% of column effluent flow). Considering these results and the fact that the first eluting amino acid derivatives are the most polar ones, we hypothesized that hydration of these components interferes with the ionization process. A linear calibration curve was obtained for both fluorescent response and total ion current (TIC) for all amino acids in the range from 5 to 1000 pmol per injection. The coefficient of variation of the fluorescent response was typically on the order of 1-4%, for the TIC this was between 4 and 9%. However, measurement of isotope ratios requires not only the determination of the area of the base peak, but also of the area of the (enriched) isotopomeric peak(s), having a much lower abundance. Therefore, isotope ratio measurements require the injection of at least 25 pmol of the amino acid derivative of interest (except for ARG 50 pmol) to obtain true ratio's. The accuracy of the isotope enrichment measurement was determined by the injection of a standard containing all major physiological amino acids (400 pmol each) and a standard at physiological concentrations (ranging from 50 pmol (CIT) to 350 pmol (VAL). Standard deviation of the isotopic ratios ranged from 0.1 to 0. 5% for the high (400 pmol) standards and from 0.2 to 0.8% for the low (physiological) standard, which is comparable with GC-MS. A plot of the results against the theoretical values gave a linear curve for all isotopes studied (R2 ranged from 0.9984 to 0.9997). However, the [1-13C]-enriched amino acids measured (LEU, GLY, and VAL) gave a closer agreement to the expected values as was found for [ureido-13C-5,5-2H2]-enriched citrulline and [guanidino-15N2]-enriched arginine. We could not determine whether this was due to the measurement procedure itself or resulting from an instability of the tracers in solution. Nevertheless, the results were reproducible and the theoretical value could be calculated using the tangent of the enrichment curves. (ABSTRACT TRUNCATED)

Amino Acids↗

Estimating the timing of diet shifts using stable isotopes.

Stable isotope analysis has become an important tool in studies of trophic food webs and animal feeding patterns. When animals undergo rapid dietary shifts due to migration, metamorphosis, or other reasons, the isotopic composition of their tissues begins changing to reflect that of their diet. This can occur both as a result of growth and metabolic turnover of existing tissue. Tissues vary in their rate of isotopic change, with high turnover tissues such as liver changing rapidly, while relatively low turnover tissues such as bone change more slowly. A model is outlined that uses the varying isotopic changes in multiple tissues as a chemical clock to estimate the time elapsed since a diet shift, and the magnitude of the isotopic shift in the tissues at the new equilibrium. This model was tested using published results from controlled feeding experiments on a bird and a mammal. For the model to be effective, the tissues utilized must be sufficiently different in their turnover rates. The model did a reasonable job of estimating elapsed time and equilibrial isotopic changes, except when the time since the diet shift was less than a small fraction of the half-life of the slowest turnover tissue or greater than 5-10 half-lives of the slowest turnover tissue. Sensitivity analyses independently corroborated that model estimates became unstable at extremely short and long sample times due to the effect of random measurement error. Subject to some limitations, the model may be useful for studying the movement and behavior of animals changing isotopic environments, such as anadromous fish, migratory birds, animals undergoing metamorphosis, or animals changing diets because of shifts in food abundance or competitive interactions.

Animals↗

Fatty acid carbon isotope ratios in humans on controlled diets.

Carbon stable isotope ratios for six serum fatty acids (FA) are reported for human subjects on controlled fat diets to determine the range of natural isotope abundance and to demonstrate the leveling effect of a well-controlled diet. Twenty-nine subjects were randomly assigned to one of three controlled diets containing high, medium, or low fat. Diets were consumed for 8 wk. Serum samples were collected at baseline (0), 5, 6, 7, and 8 wk. FA were extracted and methylated. Isotope ratios were analyzed by high-precision gas chromatography combustion-isotope ratio mass spectrometry. At baseline, mean delta 13C for 16:0b, 16:1a, 18:0a, 18:1c,18:2n-6d and 20:4n-6bc were -24.1, -21.7, -21.6, -25.6, -29.6, and -25.0/1000, respectively, with an average standard deviation of 1.9/1000. Most delta 13C decreased during the diet period and appeared to have stabilized by week 5 at -25.3, -21.9, -22.3, -26.5, -30.1, and -24.5/1000, respectively. Between-subjected variability decreased from 1.74 to 1.20/1000 on the controlled diets. Measurement variability was 0.53/1000. The within-subject variability during weeks 5-8 was 0.57/1000 (range of 0.32-0.84/1000), showing a minimum biological fluctuation on controlled diets. There was no diet group effect on delta 13C of serum FA. Except for 18:2, the delta 13C of experimental diets was lower than that of serum FA, consistent with observations in animals. These data show that carbon isotope ratios stabilize in response to controlled diets within 5 wk, reflecting the isotope ratio of their dietary source, and establish isotope ratio fluctuations for endogenous compounds for future studies.

Adult↗

A secondary isotope effect in the lipoxygenase reaction.

Fatty acids containing a prochiral tritium label have often been used in the study of enzymatic reactions which involve an obligatory step of hydrogen abstraction. In the lipoxygenase reaction, the primary isotope effect associated with this approach is detected as an isotopic enrichment of the substrate. Herein we characterize a previously unrecognized secondary isotope effect which changes the specific activity of both the substrate and product. The 12-lipoxygenase of human platelets removes the 10-LS hydrogen of arachidonic acid in the formation of 12-hydroperoxyeicosatetraenoic acid. We studied the specific activity changes associated with conversion of the enantiomerically labeled [10-DR-3H]arachidonic acid to 12-[10-3H]hydroxyeicosatetraenoic acid in aspirin-treated platelets. [3-14C]Arachidonic acid served as internal standard. The most pronounced change in 3H/14C ratio in the early stages of reaction was a 15-20% deficiency of tritium in the product. Later, the remaining arachidonate showed a marked increase in 3H/14C ratio. The changes in specific activity closely matched those predicted for a secondary isotope effect. Comparison of these data with the theoretical equations for a secondary isotope effect indicated the 10-DR-3H substrate reacted at about 84% of the rate of unlabeled molecules. Interestingly, this secondary isotope effect is similar in magnitude to the secondary isotope effect in autoxidation reactions, a finding compatible with a basic similarity in reaction mechanisms in enzymatic and non-enzymatic oxygenation of lipids.

12-Hydroxy-5,8,10,14-eicosatetraenoic Acid↗

Fractionation of carbon (13C/12C) isotopes in glycine decarboxylase reaction.

Fractionation of carbon isotopes (13C/12C) by glycine decarboxylase (GDC) was investigated in mitochondrial preparations isolated from photosynthetic tissues of different plants (Pisum, Medicago, Triticum, Hordeum, Spinacia, Brassica, Wolffia). 20 mM glycine was supplied to mitochondria, and the CO2 formed was absorbed and analyzed for isotopic content. CO2 evolved by mitochondria of Pisum was enriched up to 8% in 12C compared to the carboxylic atom of glycine. CO2 evolved by mitochondria of the other plants investigated was enriched by 5-16% in 13C. Carbon isotope effects were sensitive to reaction conditions (pH and the presence of GDC cofactors). Theoretical treatment of the reaction mechanism enabled us to conclude that the value and even the sign of the carbon isotope effect in glycine decarboxylation depend on the contribution of the enzyme-substrate binding step and of the decarboxylation step itself to the overall reaction rate. Therefore, the fractionation of carbon isotopes in GDC reaction was revealed which provides essential isotopic effects in plants in addition to the well-known effect of carbon isotope fractionation by the central photosynthetic enzyme, ribulose-1,5-biphosphate carboxylase.

Amino Acid Oxidoreductases↗

An isotopic study of biogeochemical relationships between carbonates and organic carbon in the Greenhorn Formation.

Carbon-isotopic compositions of total carbonate, inoceramid carbonate, micritic carbonate, secondary cements, total organic carbon, and geoporphyrins have been measured in 76 different beds within a 17-m interval of a core through the Greenhorn Formation, an interbedded limestone and calcareous shale unit of Cretaceous age (Cenomanian-Turonian) from the Western Interior Seaway of North America. Results are considered in terms of variations in the processes of primary production (which led to the biosynthesis of the molecular precursors of the geoporphyrins) and in secondary processes (those mediating the transformation of primary organic material into sedimentary total organic carbon). It is shown that the porphyrin isotopic record reflects primary isotopic variations more closely than the TOC isotopic record, and that, in these sediments, TOC is enriched in 13C relative to its primary precursor by 0.6 to 2.8%. This enrichment is attributed to isotope effects within the consumer foodweb and is associated with respiratory heterotrophy. Variations in this secondary enrichment are correlated with variations in the isotopic composition of marine carbonate. This correlation is attributed to effects of environmental changes on the marine foodweb. These may have included increased atmospheric oxygen associated with the Cenomanian-Turonian oceanic anoxic event. The isotopic fractionation associated with fixation of carbon by primary producers is observed to have varied by 1.5% during the interval of deposition. It is suggested that this change is due to a variation in the makeup of the community of primary producers and/or to a decrease in the atmospheric abundance of CO2 during the oceanic anoxic event.

Animals↗

Stable carbon isotope fractionation in the search for life on early Mars.

Isotopic measurements and, more specifically, ratios of 13C to 12C in organic relative to inorganic deposits, are useful in reconstructing past biological activity on Earth. Organic matter has a lower ratio of 13C to 12C due largely to the preferential fixation of 12C over the heavier isotope by the major carbon-fixation enzyme, ribulose-1,5-bisphosphate carboxylase/oxygenase, although other factors (e.g., availability of source carbon, fixation by other carboxylating enzymes and diagenesis of organic material) also contribute to fractionation. Would carbon isotope discrepancies between inorganic and organic carbon indicate past biological activity on Mars? In order to answer this question, we analyse what is known about terrestrial biologic and abiologic carbon fixation and its preservation in the fossil record, and suggest what the isotope discrimination during possible biologic and abiologic carbon fixation on Mars might have been like. Primarily because isotopic signatures of abiotically fixed carbon overlap with those of biotic fixation, but also because heterotrophy does not significantly alter the isotopic signature of ingested carbon, fractionation alone would not be definitive evidence for life. However, a narrow range of fractionation, including no fractionation, would suggest biotic processes. Never-the-less, isotopic ratios in organic deposits on Mars would be extremely useful in analysing prebiotic, if not biotic, carbon transformations on Mars.

Carbon↗

Stable isotope fractionation analysis as a tool to monitor biodegradation in contaminated acquifers.

The assessment of biodegradation in contaminated aquifers has become an issue of increasing importance in the recent years. To some extent, this can be related to the acceptance of intrinsic bioremediation or monitored natural attenuation as a means to manage contaminated sites. Among the few existing methods to detect biodegradation in the subsurface, stable isotope fractionation analysis (SIFA) is one of the most promising approaches which is pronounced by the drastically increasing number of applications. This review covers the recent laboratory and field studies assessing biodegradation of contaminants via stable isotope analysis. Stable isotope enrichment factors have been found that vary from no fractionation for dioxygenase reactions converting aromatic hydrocarbons over moderate fractionation by monooxygenase reactions (epsilon=-3 per thousand) and some anaerobic studies on microbial degradation of aromatic hydrocarbons (epsilon=-1.7 per thousand) to larger fractionations by anaerobic dehalogenation reactions of chlorinated solvents (epsilon=between -5 per thousand and -30 per thousand). The different isotope enrichment factors can be related to the respective biochemical reactions. Based on that knowledge, we discuss under what circumstances SIFA can be used for a qualitative or even a quantitative assessment of biodegradation in the environment. In a steadily increasing number of cases, it was possible to explain biodegradation processes in the field based on isotope enrichment factors obtained from laboratory experiments with pure cultures and measured isotope values from the field. The review will focus on the aerobic and anaerobic degradation of aromatic hydrocarbons and chlorinated solvents as the major contaminants of groundwater. Advances in the instrumental development for stable isotope analysis are only mentioned if it is important for the understanding of the application.

Bacteria↗

Nitrogen isotope ratios in estuarine biota collected along a nutrient gradient in Narragansett Bay, Rhode Island, USA.

Stable nitrogen isotope ratios were used to study the incorporation of anthropogenically-derived nitrogen into the food webs of salt marsh systems along a contamination gradient in Narragansett Bay. Nitrogen isotope ratios (delta(15)N) were measured in six estuarine species collected from three marshes along this gradient, monthly from June to October between 1997 and 1999. A significant decrease in delta(15)N was found with distance along the estuary for four of the six species. Significant differences were found among monthly isotope ratios for some species. Nitrogen isotope ratios in sea lettuce (Ulva lactuca) increased during the summer season with highest delta(15)N values measured during September and October. This trend was most pronounced at the station receiving the highest nutrient inputs. Elevated delta(15)N values at this station appeared to correlate with seawater ammonia/nitrate concentration ratios. The temporal variations in delta(15)N suggest that care should be taken in species selection and the design of sampling schemes of studies using delta(15)N for monitoring anthropogenic nutrients in aquatic systems. Sampling programs designed to determine long-term trends should consider species that do not show rapid fluctuations in isotope ratios. The mud snail, Nassarius obsoletus, responded this way in the present study. Studies designed to measure short-term changes should include species such as U. lactuca, which rapidly respond to isotope changes. The results from this study also help to establish a baseline for nitrogen isotope values in Narragansett Bay. This information can be used to monitor future trends in nitrogen inputs to this estuary.

Animals↗