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PubMed1989

Mechanistic studies on the bovine liver mitochondrial dihydroorotate dehydrogenase using kinetic deuterium isotope effects.

Dihydroorotates deuteriated at both C5 and C6 have been prepared and used to probe the mechanism of the bovine liver mitochondrial dihydroorotate dehydrogenase. Primary deuterium isotope effects on kcat are observed with both (6RS)-[5(S)-2H]- and (6RS)-[6-2H] dihydroorotates (3 and 6, respectively); these effects are maximal at low pH. At pH 6.6, DV = 3.4 for the C5-deuteriated dihydroorotate (3), and DV = 2.3 for the C6-deuteriated compound (6). The isotope effects approach unity at pH 8.8. Analysis of the pH dependence of the isotope effects on kcat reveals a shift in the rate-determining step of the enzyme mechanism as a function of pH. Dihydroorotate oxidation appears to require general base catalysis (pKB = 8.26); this step is completely rate-determining at low pH and isotopically sensitive. Reduction of the cosubstrate, coenzyme Q6, is rate-limiting at high pH and is isotopically insensitive; this step appears to require general acid catalysis (pKA = 8.42). The results of double isotope substitution studies and analysis for substrate isotope exchange with solvent point toward a concerted mechanism for oxidation of dihydroorotate. This finding serves to distinguish further the mammalian dehydrogenase from its parasitic cognate, which catalyzes a stepwise oxidation reaction [Pascal, R., & Walsh, C.T. (1984) Biochemistry 23, 2745].

Animals↗
PubMed1981

Multiple isotope effect probes of glutamate decarboxylase.

The enzymatic decarboxylation of glutamic acid shows a carbon isotope effect k12/k13 = 1.018 at 37 degree C, pH 4.7. In D2O under otherwise identical conditions, k12/k13 = 1.009. Under the same conditions solvent isotope effects are Vmax H2O/Vmax D2O = 5.0 and (Vmax/Km)H2O/(Vmax/Km)D2O = 2.6. With the assumption that the carbon isotope effect on the decarboxylation step is in the usual range (1.05--1.07), it is possible to derive relative rates and solvent isotope effects for all steps in the enzyme mechanism. Substrate binding in approximately 2-fold weaker in H2O than in D2O, probably because of the desolvation which accompanies binding of the substrate to the enzyme. A proton inventory analysis of the reaction shows that the Schiff base interchange has a large solvent isotope effect composed of relatively small contributions from at least four separate sites. A conformation change probably accompanies this step. The decarboxylation step shows a solvent isotope effect of approximately 2. Schiff base interchange and decarboxylation are both partially rate determining. The pH dependence of the isotope effects indicates that the initial step in the reaction can occur by way of two different pathways.

Carbon Isotopes↗
PubMed1981

Kinetic and isotope effect studies of maize phosphoenolpyruvate carboxylase.

Carbon isotope effects for the carbon atom arising from bicarbonate have been measured for the phosphoenolpyruvate carboxylase from maize. At pH 7.5, 25 degrees C, the isotope effect is K12/k13 = 1.0029 +/- 0.0005 in the presence of Mg2+. The isotope effect decreases with increasing pH, reaching a value of 0.9973 at pH 10.0. All these isotope effects are relative to HCO3(-) taken as the starting state. If CO2 is considered the starting state, the isotope effects are all inverse. These values suggest that the carboxylation of phosphoenolpyruvate occurs by way of a stepwise mechanism involving an enzyme-bound carboxyphosphate intermediate, with formation of the intermediate being the primary rate-determining step. Steady-state kinetics reveal that Vmax is independent of pH over the range pH 7.5-10.0 Vmax/Km (phosphoenolpyruvate) is bell shaped in the same interval. Two pKa values near 7 are observed; the first is attributed to ionization of the phosphate group of phosphoenolpyruvate and the second to an unidentified group on the enzyme. Activity of the enzyme also depends on protonation of a group on the enzyme with a pKa near 10. Several metal ions were tested as activators of phosphoenolpyruvate carboxylase. Under saturating conditions, Mg2+ and Mn2+ show equal activity but different carbon isotope effects. Co2+ has about half the activity of Mg2+ and shows an inverse carbon isotope effect.

Bicarbonates↗
PubMed2002

15N kinetic isotope effects on uncatalyzed and enzymatic deamination of cytidine.

15N isotope effects and solvent deuterium isotope effects have been measured for the hydrolytic deamination of cytidine catalyzed by Escherichia coli cytidine deaminase and for the uncatalyzed reaction proceeding spontaneously in neutral solution at elevated temperatures. The primary (15)(V/K) arising from the exocyclic amino group for wild-type cytidine deaminase acting on its natural substrate, cytidine, is 1.0109 (in H(2)O, pH 7.3), 1.0123 (in H(2)O, pH 4.2), and 1.0086 (in D(2)O, pD 7.3). Increasing solvent D(2)O content has no substantial effect on k(cat) but enhances k(cat)/K(m), with a proton inventory showing that the fractionation factors of at least two protons increase markedly during the reaction. Mutant cytidine deaminases with reduced catalytic activity show more pronounced (15)N isotope effects of 1.0124 (Glu91Ala), 1.0134 (His102Ala), and 1.0158 (His102Asn) at pH 7.3 in H(2)O, as expected for processes in which the chemical transformation of the substrate becomes more rate determining. The isotope effect of mutant His102Asn is 1.033 after correcting for protonation of the -NH(2) group, and represents the intrinsic isotope effect on C-N bond cleavage. This result allows an estimation of the forward commitment of the reaction with the wild-type enzyme. The observed (15)N kinetic isotope effect of the pyrimidine N-3, for wild-type cytidine deaminase acting on cytidine, is 0.9879, which is consistent with protonation and rehybidization of N-3 with hydroxide ion attack on the adjacent carbon to create a tetrahedral intermediate. These results show that enzymatic deamination of cytidine proceeds stepwise through a tetrahedral intermediate with ammonia elimination as the major rate-determining step. The primary (15)N isotope effects observed for the uncatalyzed reaction at pH 7 (1.0021) and pH 12.5 (1.0034) were found to be insensitive to changing temperatures between 100 and 185 degrees C. These results show that the uncatalyzed and the enzymatic deaminations of cytidine proceed by similar mechanisms, although the commitment to C-N bond breaking is greater for the spontaneous reaction.

Cytidine↗
PubMed2003

Substrate specificity and kinetic isotope effect analysis of the Eschericia coli ketopantoate reductase.

Ketopantoate reductase (EC 1.1.1.169), an enzyme in the pantothenate biosynthetic pathway, catalyzes the NADPH-dependent reduction of alpha-ketopantoate to form D-(-)-pantoate. The enzyme exhibits high specificity for ketopantoate, with V and V/K for ketopantoate being 5- and 365-fold higher than those values for alpha-ketoisovalerate and 20- and 648-fold higher than those values for alpha-keto-beta-methyl-n-valerate, respectively. For pyridine nucleotides, V/K for beta-NADPH is 3-500-fold higher than that for other nucleotide substrates. The magnitude of the primary deuterium kinetic isotope effects on V and V/K varied substantially when different ketoacid and pyridine nucleotide substrates were used. The small primary deuterium kinetic isotope effects observed using NADPH and NHDPH suggest that the chemical step is not rate-limiting, while larger primary deuterium isotope effects were observed for poor ketoacid and pyridine nucleotide substrates, indicating that the chemical reaction has become partially or completely rate-limiting. The pH dependence of (D)V using ketopantoate was observed to vary from a value of 1.1 at low pH to a value of 2.5 at high pH, while the magnitude of (D)V/K(NADPH) and (D)V/K(KP) were pH-independent. The value of (D)V is large and pH-independent when alpha-keto-beta-methyl-n-valerate was used as the ketoacid substrate. Solvent kinetic isotope effects of 2.2 and 1.2 on V and V/K, respectively, were observed with alpha-keto-beta-methyl-n-valerate. Rapid reaction analysis of NADPH oxidation using ketopantoate showed no "burst" phase, suggesting that product-release steps are not rate-limiting and the cause of the small observed kinetic isotope effects with this substrate pair. Large primary deuterium isotope effects on V and V/K using 3-APADPH in steady-state experiments, equivalent to the isotope effect observed in single turnover studies, suggests that chemistry is rate-limiting for this poorer reductant. These results are discussed in terms of a kinetic and chemical mechanism for the enzyme.

Alcohol Oxidoreductases↗
PubMed1998

Carbon-13 isotope effect studies of Trypanosoma brucei ornithine decarboxylase.

Carbon isotope effect studies were undertaken with the wild-type pyridoxal 5'-phosphate (PLP)-dependent enzyme ornithine decarboxylase (ODC) from Trypanosoma brucei and with several active site mutants of the enzyme. For the decarboxylation of the optimal substrate, L-ornithine, by wild-type ODC, the observed carbon isotope effect (k12/k13) is 1.033 at pH 7.3. In comparison to the expected intrinsic isotope effect (k12/k13 = 1.06) for decarboxylation, this value suggests that both the rate of decarboxylation and the rate of Schiff base interchange with L-ornithine are partially rate-limiting for the reaction steps up to decarboxylation. In contrast, with the alternate substrate L-Lys, which shows lower catalytic efficiency, the carbon isotope effect increased to 1.063, demonstrating that decarboxylation has become the rate-limiting step. For the mutant enzymes, E274A ODC and C360A ODC, with L-ornithine as substrate the carbon isotope effect also approaches the intrinsic limit. Glu-274 was previously demonstrated to play a direct role in carbanion stabilization, and thus the large carbon isotope effect (k12/k13 = 1.055) is consistent with an impaired rate of decarboxylation compared to wild-type ODC. In contrast, for K69A ODC, the isotope effect is almost entirely suppressed, suggesting that Schiff-base formation (which now must occur from enzyme-bound PLP, rather than from an enzyme-bound PLP-Schiff base) has become rate-determining.

Animals↗
PubMed2005

Quantification of sequential chlorinated ethene degradation by use of a reactive transport model incorporating isotope fractionation.

Compound-specific isotope analysis (CSIA) enables quantification of biodegradation by use of the Rayleigh equation. The Rayleigh equation fails, however, to describe the sequential degradation of chlorinated aliphatic hydrocarbons (CAHs) involving various intermediates that are controlled by simultaneous degradation and production. This paper shows how isotope fractionation during sequential degradation can be simulated in a 1D reactive transport code (PHREEQC-2). 12C and 13C isotopes of each CAH were simulated as separate species, and the ratio of the rate constants of the heavy to light isotope equaled the kinetic isotope fractionation factor for each degradation step. The developed multistep isotope fractionation reactive transport model (IF-RTM) adequately simulated reductive dechlorination of tetrachloroethene (PCE) to ethene in a microcosm experiment. Transport scenarios were performed to evaluate the effect of sorption and of different degradation rate constant ratios among CAH species on the downgradient isotope evolution. The power of the model to quantify degradation is illustrated for situations where mixed sources degrade and for situations where daughter products are removed by oxidative processes. Finally, the model was used to interpret the occurrence of reductive dechlorination at a field site. The developed methodology can easily be incorporated in 3D solute transport models to enable quantification of sequential CAH degradation in the field by CSIA.

Biodegradation, Environmental↗
PubMed2006

Tracing source pollution in soils using cadmium and lead isotopes.

Tracing the source of heavy metals in the environment is of key importance for our understanding of their pollution and natural cycles in the surface Earth reservoirs. Up to now, most exclusively Pb isotopes were used to effectively trace metal pollution sources in the environment. Here we report systematic variations of Cd isotope ratios measured in polluted topsoils surrounding a Pb-Zn refinery plant in northern France. Fractionated Cd was measured in soil samples surrounding the refinery, and this fractionation can be attributed to the refining processes. Despite the Cd isotopic ratios being precisely measured, the obtained uncertainties are still large compared to the total isotopic variation. Nevertheless, for the first time, Cd isotopically fractionated by industrial processes may be traced in the environment. On the same samples, Pb isotope systematics suggested that materials actually used by the refinery were not the major source of Pb in soils, probably because refined ore origins changed over the 100 years of operation. On the other hand, Cd isotopes and concentrations measured in topsoils allowed identification of three main origins (industrial dust and slag and agriculture), assuming that all Cd ores are not fractionated, as suggested by terrestrial rocks so far analyzed, and calculation of their relative contributions for each sampling point. Understanding that this refinery context was an ideal situation for such a study, our results lead to the possibility of tracing sources of anthropogenic Cd and better constrain mixing processes, fluxes, transport, and phasing out of industrial input in nature.

Cadmium↗
PubMed2005

Isotope effects on the enzymatic and nonenzymatic reactions of chorismate.

The important biosynthetic intermediate chorismate reacts thermally by two competitive pathways, one leading to 4-hydroxybenzoate via elimination of the enolpyruvyl side chain, and the other to prephenate by a facile Claisen rearrangement. Measurements with isotopically labeled chorismate derivatives indicate that both are concerted sigmatropic processes, controlled by the orientation of the enolpyruvyl group. In the elimination reaction of [4-2H]chorismate, roughly 60% of the label was found in pyruvate after 3 h at 60 degrees C. Moreover, a 1.846 +/- 0.057 2H isotope effect for the transferred hydrogen atom and a 1.0374 +/- 0.0005 18O isotope effect for the ether oxygen show that the transition state for this process is highly asymmetric, with hydrogen atom transfer from C4 to C9 significantly less advanced than C-O bond cleavage. In the competing Claisen rearrangement, a very large 18O isotope effect at the bond-breaking position (1.0482 +/- 0.0005) and a smaller 13C isotope effect at the bond-making position (1.0118 +/- 0.0004) were determined. Isotope effects of similar magnitude characterized the transformations catalyzed by evolutionarily unrelated chorismate mutases from Escherichia coli and Bacillus subtilis. The enzymatic reactions, like their solution counterpart, are thus concerted [3,3]-sigmatropic processes in which C-C bond formation lags behind C-O bond cleavage. However, as substantially larger 18O and smaller 13C isotope effects were observed for a mutant enzyme in which chemistry is fully rate determining, the ionic active site may favor a somewhat more polarized transition state than that seen in solution.

Chorismic Acid↗
PubMed2003

Improved detection of added water in orange juice by simultaneous determination of the oxygen-18/oxygen-16 isotope ratios of water and ethanol derived from sugars.

A procedure for the analysis of the oxygen-18/oxygen-16 isotope ratio of ethanol derived from the sugars of orange juice using the preparation steps of the SNIF-NMR method followed by pyrolysis-isotope ratio mass spectrometry is presented. The isotopic fractionation induced by the isotope effects of fermentation and distillation have been investigated, and it is shown that reproducible results can be obtained when appropriate analytical conditions are used. It is also shown that the oxygen isotope distribution in the water and organic matter pools of fruits remains quite stable during the harvest period and is not altered by the precipitation rate within the last few days before the fruits are picked. Due to the robustness of the method and the fact that most of the oxygen-18 enrichment from the initial sugars is still present in the end-product, ethanol appears as a convenient internal reference to circumvent the spatial and temporal variability observed for the oxygen-18/oxygen-16 isotope ratio of water. A very strong correlation is observed between the isotopic deviations of ethanol and water, which is altered in the event of a water addition, even at a low level. Combining the information brought by these two parameters leads to a more efficient authenticity testing tool, which avoids false positive cases and provides a lower detection limit for added water in juices not made from concentrate, whatever the origin of the sample tested.

Beverages↗
PubMedDate not supplied

Quantification in proteomics through stable isotope coding: a review.

This review focuses on techniques for quantification and identification in proteomics by stable isotope coding. Methods are examined for analyzing expression, post-translational modifications, protein:protein interactions, single amino acid polymorphism, and absolute quantification. The bulk of the quantification literature in proteomics focuses on expression analysis, where a wide variety of methods targeting different features of proteins are described. Methods for the analysis of post-translational modification (PTM) focus primarily on phosphorylation and glycosylation, where quantification is achieved in two ways, either by substitution or tagging of the PTM with an isotopically coded derivatizing agent in a single process or by coding and selecting PTM modified peptides in separate operations. Absolute quantification has been achieved by age-old internal standard methods, in which an isotopically labeled isoform of an analyte is synthesized and added to a mixture at a known concentration. One of the surprises is that isotope coding can be a valuable aid in the examination of intermolecular association of proteins through stimulus:response studies. Preliminary efforts to recognize single amino acid polymorphism are also described. The review ends with the conclusion that (1) isotope ratio analysis of protein concentration between samples does not necessarily relate directly to protein expression and rate of PTM and (2) that multiple new methods must be developed and applied simultaneously to make existing stable isotope quantification methods more meaningful. Although stable isotope coding is a powerful, wonderful new technique, multiple analytical issues must be solved for the technique to reach its full potential as a tool to study biological systems.

Isotopes↗
PubMed2001

Fractional zinc absorption using a single isotope tracer.

BACKGROUND: Fractional absorption of zinc (Zn) has been measured using dual isotopes of Zn given simultaneously. An oral test dose and an intravenous (i.v.) reference dose are administered, followed by the measurement of the double isotopic enrichment (E) in urine 48 h after administration. We postulated that an estimate of the %E in urine for a given i.v. dose of Zn may be used to eliminate the need for venipuncture and the second Zn isotope. OBJECTIVES: To determine a constant (k) for the Zn enrichment of urine after i.v. administration of a dose of labeled Zn in Zn-replete subjects. To use 'k' to calculate fractional absorption of Zn, and to compare these values to values obtained using the standard dual isotope method. DESIGN: Single-arm cohort. SETTING: The Hospital for Sick Children, Toronto, Canada. SUBJECTS: Twenty-three healthy adults were recruited from the Metropolitan Toronto area. Seventeen subjects completed the study. INTERVENTIONS: A 2.29 mg i.v. dose of (67)Zn followed immediately by a 2.50 mg oral dose of (70)Zn. RESULTS: Population mean percentage enrichment (%E) of (67)Zn in urine was 1.43 (95% CI 1.26, 1.60). The ratio of the i.v. dose to mean %E in urine (k) was estimated to be 1.60 mg (95% CI 1.43, 1.82). There was no difference in the mean fractional absorption of Zn calculated using the single compared to the dual isotope method: 12.58% (95% CI 2.22, 22.94) vs 12.68% (95% CI 4.52, 20.85), respectively (P=0.89). The correlation coefficient between the two methods was 0.81 (P<0.0001). CONCLUSIONS: The dual isotope method may be replaced by using a constant (k) and a single oral dose of isotopic-enriched Zn to estimate fractional absorption of Zn within a population. SPONSORSHIP: Gerber Products Company, Fremont, MI.

Administration, Oral↗
PubMed2005

Old Masters' lead white pigments: investigations of paintings from the 16th to the 17th century using high precision lead isotope abundance ratios.

White lead (2PbCO(3).Pb(OH)(2)), a common component in 17c. artists' painting materials, was singled out to investigate the potential of lead isotope abundance ratios in the field of authentication and origin assignment. Paintings by Peter Paul Rubens, Anthony van Dyck and other Old Masters of the Northern and Southern schools were chosen for this study. An interdisciplinary approach was chosen using both analytical instrumental methods, art technological and art historical knowledge. Minute samples taken from paintings from selected art collections worldwide were investigated using mass spectrometry, scanning electron microscopy (SEM) and energy-dispersive X-ray spectroscopy (EDX). The high precision lead isotope abundance ratios were measured by multiple collector inductively coupled plasma mass spectrometry (MC-ICP-MS). The determination of the calcium matrix influence with respect to possible bias effects to the isotope ratios gave clear decision support, to whether a result lies within the stated combined measurement uncertainty of the result, to eliminate time-consuming matrix separations. The scatter plots of the measured isotope abundance ratios for the painting pigments from P. P. Rubens, A. van Dyck and other Flemish painters exhibit a very narrow distribution forming a cluster. The range of the measured ratio (206)Pb/(204)Pb amounts to 0.55% and for the ratio (207)Pb/(204)Pb to 0.2%. The comparison of the data to cis-alpine (Italian) sample pigments from paintings from the same time period reveals a clear distinction between the two fields. With respect to the lead isotope data originating from the ores it is assumed that the pigment isotope ratio distribution can be explained by very distinct origin of raw materials. Presumably, no mixing of different lead ores from Europe took place. The comparison of the measured white lead isotope ratio values (Flemish paintings) and the data from ore samples led to the unexpected conclusion that local ores were not used for the pigment production but British or German sources.

Carbonates↗
PubMed1995

Use of a stable copper isotope (65Cu) in the differential diagnosis of Wilson's disease.

1. 65Cu/63Cu stable-isotope ratios have been measured in blood serum after oral administration of the stable isotope 65Cu. The incorporation of the isotope into the plasma protein pool was followed at various times for up to 3 days. The resulting patterns of enrichment in healthy control subjects, in Wilson's disease patients and in heterozygotes for the Wilson's disease gene, were similar in appearance to those found by others using copper radioactive isotopes. After an initially high enrichment at 2 h after dosage, the Wilson's disease cases, in contrast to the control subjects, did not show a secondary rise in isotope enrichment of the plasma pool after 72 h, demonstrating a failure to incorporate copper into caeruloplasmin. The Wilson's disease heterozygotes had variable degrees of impairment of isotope incorporation, not always distinguished from those of control subjects. 2. The stability of the isotope also permits the copper tracer to be followed for a longer period. Ten healthy subjects were studied for over 40 days, allowing the biological half-time of an oral dose of copper to be determined (median 18.5 days, 95% confidence interval 14-26 days). Known heterozygotes for the Wilson's disease gene were found to have a significantly increased biological half-time for removal of copper from the plasma pool (median 43 days, 95% confidence interval 32-77 days). 3. The incorporation of 65 Cu in patients with diseases of the liver (other than Wilson's disease) was found to be similar to that in control subjects, aiding differential diagnosis.

Adolescent↗
PubMed1996

Temperature dependence of the isotope chemistry of the heavy elements.

The temperature coefficient of equilibrium isotope fractionation in the heavy elements is shown to be larger at high temperatures than that expected from the well-studied vibrational isotope effects. The difference in the isotopic behavior of the heavy elements as compared with the light elements is due to the large nuclear isotope field shifts in the heavy elements. The field shifts introduce new mechanisms for maxima, minima, crossovers, and large mass-independent isotope effects in the isotope chemistry of the heavy elements. The generalizations are illustrated by the temperature dependence of the isotopic fractionation in the redox reaction between U(VI) and U(IV) ions.

Chemical Phenomena↗
PubMed1997

Study of magnesium bioavailability using stable isotopes and the inductively-coupled plasma mass spectrometry technique in the rat: single and double labelling approaches.

The present work aimed to investigate the feasibility of using stable isotopes and inductively-coupled plasma mass spectrometry (ICP/MS) to study Mg absorption in rats. Male Wistar rats, aged 7 weeks and weighing 180 g, were used. They were fed on a semi-purified diet containing 1070 mg Mg/kg, and had free access to feed and distilled water. In the first experiment, after a 16 d adaptation period, two doses of enriched 25Mg (6 and 12 mg) were administered by oral intubation, faeces and urine were collected daily and blood was sampled. Isotope ratios were determined by ICP/MS. 'True' absorption values, using the faecal isotope data, were 0.63 and 0.56 in rats receiving 6 and 12 mg 25Mg respectively, while apparent absorption was 0.50 for two successive periods of metabolic balance studies. Moreover, the oral isotope administration resulted in a measurable isotopic enrichment in plasma within hours which was still detectable on the third day following the isotope administration. In the second experiment, investigating the double labelling technique, similar rats were dosed simultaneously with 5 mg 26Mg orally (premixed with diet) and 0.29 mg 25Mg intravenously. The calculated Mg true absorption values were very similar when calculated from blood or urine data (0.38) but were lower than that obtained from faecal data (0.50). The possible causes of such an unexpected difference and limits of the double labelling technique for Mg absorption are discussed here. Together these results indicate that although 25Mg and 26Mg isotopes have high natural abundance, the described methodology permits meaningful investigations of Mg bioavailability and metabolism.

Administration, Oral↗
PubMed2003

Determination of cholesterol absorption in humans: from radiolabel to stable isotope studies.

Hypercholesterolemia is a major health risk. Dietary cholesterol absorption is one important factor affecting levels of plasma and tissue cholesterol. Considerable effort has thus been devoted to develop reliable in vivo clinical methodologies to determine dietary cholesterol absorption in humans. The present paper summarises radiolabelled experiments and major advances in stable isotope technologies to determine cholesterol absorption. Initially, direct methods employing gastro-intestinal intubation were developed. Later, indirect methods using oral-faecal cholesterol balance permitted calculation of cholesterol mass absorption. Once the use of radiolabelled [3H, 14C]cholesterol balance was developed in healthy humans, it was finally possible to distinguish exogenous and endogenous cholesterol. Non-invasive and safer stable isotope (2H, 13C, 18O) labelled cholesterol tracers then replaced radioisotopes for use in infants and adults. Stable isotopes and radioisotopes showed identical cholesterol kinetics. The most promising contemporary stable isotope assessment of cholesterol absorption is a dual stable isotope dual tracer approach based on simultaneous administration of oral and intravenous differentially labelled cholesterol tracers, followed by plasma sampling for 3-4 d. Online GC/Combustion/IRMS and GC/Pyrolysis/IRMS allow minimal amounts of dual stable isotope cholesterol tracers to be detected. Using the dual stable isotope dual tracer approach, the percent cholesterol absorption in adult volunteers has been determined to be 50-70%.

Absorption↗
PubMedDate not supplied

Use of NADP archive samples to determine the isotope composition of precipitation: characterizing the meteoric input function for use in ground water studies.

Stable oxygen and hydrogen isotopes have been used in ground water studies to investigate recharge, mixing, ground water/surface water interaction, advective-diffusive transport, paleohydrogeologic interactions and to estimate ground water ages. Such studies require that the isotopic composition of precipitation be known, as precipitation is a major input to ground water and surface water systems. As oxygen-18 and deuterium data for precipitation are lacking across much of the United States, there is need to establish additional local meteoric water lines as isotope input functions across the region, as well as to develop better understanding of the isotopic climate linkages that control oxygen and hydrogen isotope ratios in precipitation. In the absence of long-term monitoring stations, one possible solution to this problem is to determine the delta 18O and delta 2H values of precipitation using archive samples collected at monitoring stations managed by the National Atmospheric Deposition Program (NADP). This study describes and interprets the seasonal delta 18O and delta 2H composition of archived precipitation samples collected in eastern Nebraska near the town of Mead during the years 1992-1994. Values for delta 18O range from -23.6 to -0.7@1000. Values for delta 2H range from -172 to 0@1000. Yearly arithmetic mean delta 18O and delta 2H values for the Mead station are -8.1@1000 and -53@1000, respectively. Weighted yearly means for delta 18O and delta 2H were -7.4@1000 and -48@1000, respectively. Mead values show a strong isotopic enrichment between winter and summer precipitation, and a strong delta 18O-T correlation (r2 = 0.91) for mean monthly values of about 0.5@1000 per degree Celsius. The local meteoric water line for the Mead site is delta 2H = 7.40 delta 18O + 7.32. Deuterium excess values suggest that most of the moisture across the region is derived primarily from a Gulf of Mexico source. The results of this study demonstrate that in the absence of long-term monitoring stations such as those operated globally by the International Atomic Energy Association, NADP archive samples can be used to determine the isotopic composition of precipitation, to characterize the local meteoric water line and establish the various climatic relationships, and define the meteoric input function for use in ground water studies.

Deuterium↗