The effect of aging on intestinal absorption and status of calcium, magnesium, zinc, and copper in rats: A stable isotope study

Many investigators have reported changes in mineral status with age but conflicting observations were done concerning mineral absorption. This study was conducted to clarify the effect of aging on intestinal absorption and status of minerals, using a stable isotope approach. To do so, 40 rats of different ages: 9, 22, 44, and 88 weeks were fed with a semi-purified diet for a total of 30 days. At the beginning of the 4th week, the rats received a stable isotope solution containing (44)Ca, (25)Mg, (67)Zn, and (65)Cu. Individual feces and urine were then collected during 4 consecutive days in order to measure stable isotopes by inductively coupled plasma/mass spectrometry (ICP/MS) and blood and tissues were sampled for mineral status determination. Intestinal absorption of (44)Ca and (67)Zn considerably decreased with age, whereas intestinal (25)Mg absorption decreased only moderately and intestinal (65)Cu absorption was unaffected. Plasma and bone calcium (Ca) were not modified with age whereas urinary Ca excretion considerably increased. Plasma and erythrocyte magnesium (Mg) levels were unaffected with age whereas urinary Mg excretion and Mg bone level decreased. Plasma zinc (Zn) level decreased and bone Zn level increased with age whereas red blood cell and liver Zn level and urinary Zn excretion remained unchanged. Plasma Cu level increased with age whereas liver and bone Cu levels and urinary Cu excretion remained unchanged. These results show that the effect of aging on the intestinal mineral absorption and status differ largely according to the mineral considered. Further studies are required under different nutritional conditions to explore the underlying mechanisms during aging and to adjust a better nutrition of the elderly.     

Stable isotopes of minerals as metabolic tracers in human nutrition research

Enriched stable isotopes used as tracers have proven to be valuable in studies of the absorption and metabolism of minerals. Unlike radioisotopes, they can be used in high-risk population groups such as infants, children, and pregnant or lactating women. Estimates of mineral absorption can be made from the oral administration of a single tracer or from two tracers, one given orally and the other intravenously (IV). It is possible to determine the metabolism of the mineral with modeling based on the amount of the tracer or tracers in different biological samples. One of the key decisions in studies of this type is determining which enriched isotope and what amount to use. An example is given of calculations to estimate and compare the amounts of tracers needed for an absorption study. Methods for calculating the amounts of tracer in oral and IV doses are presented, and limits of detection and quantitation are discussed in terms of percent of enrichment and related to isotope ratio measurement precision. A general review of the use of mass spectrometric instruments for quantifying various stable isotopes is given.     

Cholesterol absorption and turnover in rhesus monkeys as measured by two methods

We compared the absorption of cholesterol in seven rhesus monkeys (four high-responders and three low-responders) as measured by two methods: 1) the dual isotope plasma ratio method of Zilversmit (1972. Proc. Soc. Exp. Biol. Med. 140: 862) and 2) the single isotopic meal feeding technique of Borgstr?m (1969. J. Lipid Res. 10: 331). We also compared the cholesterol pool sizes calculated by kinetic analysis of the plasma cholesterol specific activity decay curves obtained after simultaneous administration of [(3)H]- and [(14)C]cholesterol, one given intravenously and the other orally. The ratio of orally to intravenously administered cholesterol radioactivity in plasma did not attain constancy until 6 weeks after isotope administration. Therefore, the percent absorption of cholesterol was calculated by the Zilversmit method 8 weeks after the administration of isotopes. The mean percent absorption of cholesterol by the Borgstr?m method was 66.3 +/- 5.1 (S.E.) and by the Zilversmit method was 70.3 +/- 7.4. The differences were not statistically significant. However, in two of seven monkeys the percent absorption of cholesterol calculated by the Zilversmit method was higher by 10.4 and 22.6 percentage points than the values obtained by the Borgstr?m method. Cholesterol absorption by either method was higher in the high-responding monkeys than in the low-responding group. The sizes of the rapidly exchangeable pool or the minimum estimate of the total body pool of cholesterol were similar for all monkeys or for either the low-responding or the high-responding animals and were also similar when calculated using the data from either the orally or the intravenously administered radioactive cholesterol. Cholesterol synthesis was significantly higher in the low-responding monkeys (115 mg/day) than in the high-responding (64 mg/day). The present study and our previous studies support the hypothesis that a major factor causing the difference in response of plasma cholesterol to dietary cholesterol between the high- and low-responding rhesus monkeys is a difference in the intestinal absorption of cholesterol.-Bhattacharyya, A. K., and D. A. Eggen. Cholesterol absorption and turnover in rhesus monkeys as measured by two methods.     

A compartmental model of magnesium metabolism in healthy men based on two stable isotope tracers

The aim of this study was to build a compartmental model of magnesium (Mg) kinetics by using data collected from six healthy adult men after oral administration of 26Mg and intravenous administration of 25Mg. Blood, urine, and feces were collected for 12 days after administration of the isotopes. Isotopic ratios were determined by inductively coupled plasma-mass spectrometry. Data were analyzed for each subject using SAAMII. We began with a compartmental model previously proposed (Avioli LV and Berman M. J Appl Physiol 21: 1688-1694, 1966) and developed an alternative approach to resolve the discrepancy between model-predicted curves and experimental data. This analysis enables the exploration of 25% of total body Mg that exchanges rapidly from plasma compartment with two extraplasma pools. One of the extraplasma compartments contains 80% of the exchangeable Mg with a transport rate of 48 +/- 13 mg/h. The second exchanges 179 +/- 88 mg of Mg/h. The model permitted estimation of kinetic parameters as well as fractional Mg absorption and fecal endogenous excretion.     

Zinc metabolism and homeostasis: The application of tracer techniques to human zinc physiology

Tracer kinetic techniques based on zinc stable isotopes have a vital role in advancing knowledge of human zinc physiology and homeostasis. These techniques have demonstrated the complexity of zinc metabolism, and have been critical to estimating the size and interrelationships of those pools of zinc that exchange rapidly with zinc in plasma and which are likely to be especially important for zinc dependent biology. This paper presents findings from recent research linking a steady state compartmental model with non-steady state post-prandial sampling from the intestine, utilizing a combination of intestinal intubation/perfusion and stable isotope tracer kinetic techniques. The gastrointestinal tract has a central role in maintaining whole body zinc homeostasis. While the fractional absorption of zinc from a meal depends on the quantity of exogenous zinc and on such dietary factors as phytic acid, the fractional absorption does not appear to be dependent on the size of the rapidly exchanging pool of the host. In contrast, the quantity of endogenous zinc excreted via the intestine is positively correlated with both the amount of absorbed zinc and the zinc `status' of the host, and thus this process has an equally critical role in maintaining zinc homeostasis. The observed alterations in zinc metabolism in some disease states can be understood in the context of known homeostatic processes. In other conditions, however, such alterations as inflammation-associated hyperzincuria and zinc redistribution, the links between homeostatic perturbation and cellular biology are yet to be explained. Thus the challenge remains for research at the whole body level to carefully characterize zinc distribution and exchange under diverse circumstances, while research at the cellular level must elucidate the regulatory processes and the factors to which they respond.     

Zinc,copper, and iron nutrition studied with enriched stable isotopes

Enriched stable isotopes were used in nutrition studies of normal, healthy adults to measure zinc, copper, and iron absorption. After obtaining baseline values for zinc, copper, and iron absorption from diets adequate in all nutrients, the effects of age, pregnancy, and deveral dietary variables were studied. Stable isotopes of zinc, copper, and iron were incorporated into diets. Complete fecal samples were collected and the unabsorbed isotopes remaining in the samples were measured by thermal ionization mass spectrometry, the most precise analytical method for the determination of stable mineral isotopes. Stable isotopes were also infused in five young men to evaluate the potential of studying mineral utilization and kinetics with stable isotopes. The results of these studies demonstrate that a number of factors can affect mineral absorption, but the specific effects differ for different minerals. Isotopic enrichments could be measured in urine and blood, so kinetic studies of utilization of essential minerals are now feasible with enriched stable isotopes. Continued use of stable isotopes to determine mineral absorption, combined with stable-isotope studies of mineral utilization, balance data, and biochemical indicators of mineral status, should result in a better understanding of mineral requirements and metabolism under a variety of conditions.     

An evaluation of four methods for measuring cholesterol absorption by the intestine in man

Critical comparisons have been made in 12 patients of four methods for measuring cholesterol absorption from the intestine. Methods I-III depend on the use of labeled cholesterol (intravenously or continuous labeling orally) in conjunction with sterol balance measurements; Method IV can be carried out with only a single test dose containing labeled cholesterol plus labeled beta-sitosterol. In the latter technique absorption is calculated as the loss of cholesterol relative to beta-sitosterol during intestinal transit. Method III (isotopic steady-state method) proved to be undependable because of uncertainties in determining the existence of an isotopic steady state. However, Method IV gave good agreement with Methods I and II, and it appears to have certain practical as well as theoretical advantages. Although Method IV requires collections of stools for up to 8 days, it is nevertheless the most rapid and the simplest of all the methods for estimating absorption. It can also be used in certain situations, such as in fur-licking animals, when Methods I and II are inadequate. Therefore, this method would seem to be a valuable addition to other isotopic techniques for estimating cholesterol absorption in man.     

The impact of metabolism on stable isotope dynamics: a theoretical framework

Stable isotope analysis is a powerful tool used for reconstructing individual life histories, identifying food-web structures and tracking flow of elemental matter through ecosystems. The mechanisms determining isotopic incorporation rates and discrimination factors are, however, poorly understood which hinders a reliable interpretation of field data when no experimental data are available. Here, we extend dynamic energy budget (DEB) theory with a limited set of new assumptions and rules in order to study the impact of metabolism on stable isotope dynamics in a mechanistic way. We calculate fluxes of stable isotopes within an organism by following fluxes of molecules involved in a limited number of macrochemical reactions: assimilation, growth but also structure turnover that is here explicitly treated. Two mechanisms are involved in the discrimination of isotopes: (i) selection of molecules occurs at the partitioning of assimilation, growth and turnover into anabolic and catabolic sub-fluxes and (ii) reshuffling of atoms occurs during transformations. Such a framework allows for isotopic routing which is known as a key, but poorly studied, mechanism. As DEB theory specifies the impact of environmental conditions and individual state on molecule fluxes, we discuss how scenario analysis within this framework could help reveal common mechanisms across taxa.     

Inferring foliar water uptake using stable isotopes of water

A growing number of studies have described the direct absorption of water into leaves, a phenomenon known as foliar water uptake. The resultant increase in the amount of water in the leaf can be important for plant function. Exposing leaves to isotopically enriched or depleted water sources has become a common method for establishing whether or not a plant is capable of carrying out foliar water uptake. However, a careful inspection of our understanding of the fluxes of water isotopes between leaves and the atmosphere under high humidity conditions shows that there can clearly be isotopic exchange between the two pools even in the absence of a change in the mass of water in the leaf. We provide experimental evidence that while leaf water isotope ratios may change following exposure to a fog event using water with a depleted oxygen isotope ratio, leaf mass only changes when leaves are experiencing a water deficit that creates a driving gradient for the uptake of water by the leaf. Studies that rely on stable isotopes of water as a means of studying plant water use, particularly with respect to foliar water uptake, must consider the effects of these isotopic exchange processes.     

稳定氢氧同位素定量植物水分来源的不确定性解析

稳定氢氧同位素技术被广泛运用于生态系统、特别是干旱区生态系统中植物水分来源的研究,其理论假设为"水分被植物根系吸收并向木质部运输过程中不发生氢氧同位素分馏"。生态系统中不同水源的氢氧同位素组成普遍存在显著差异,为从水源混合体中区分出各水源的贡献率提供了前提条件。但在实际应用过程中,诸多因素导致稳定氢氧同位素技术定量植物水分来源的结果具有不确定性。综合已有研究并加以分析,举证说明植物吸收水分相对于水源同位素变化的滞后性、水源同位素的季节性变化、蒸发作用和水源之间的混合作用对水源同位素的影响等导致植物水分来源定量结果不确定性的几个因素,以期为今后稳定氢氧同位素技术在植物水分来源领域的应用提供参考。     

Studies on zinc bioavailability from a representative diet in Chinese urban women of childbearing age using a double label stable isotope technique

The objectives of the study were to determine dietary zinc bioavailability by using a double label stable isotope technique, and to identify the zinc content and levels of some possible factors which may affect zinc utilization in a typical representative Chinese urban diet. Twenty urban women of childbearing age were fed a diet extrinsically labeled with 67Zn and received intravenous (i.v.) injections of 70Zn. Fecal monitoring, urine monitoring and chemical balance technique were used simultaneously for comparisons. Isotopic enrichment in feces and urine after oral and i.v. administration of stable zinc isotopes was measured to determine the ways of zinc absorption. The mean (+/-SD) zinc intake from the representative Chinese diet was 10.22+/-0.80 mg/day, which is lower than the reference nutrient intake (RNI) level (11.5 mg/day), and mainly came from the subsidiary foods (63%). The mean dietary Fe/Zn weight was 1.1+/-0.1. The phytate/zinc molar ratio in the diet was about 3:1. The phytic acidxCa/zinc molar ratio in the diet was about 45:1. The apparent and true absorption rates of 67Zn were 36.2+/-9.7% and 38.2+/-10.1%, respectively, which were higher than the apparent absorption determined by balance technique (29.7+/-10.6%). The mean fractional absorption (FA) determined in urine was 35.7+/-13.3. In conclusion, the subsidiary food is the main source of dietary zinc in this typical diet. The extrinsic labeling technique by use of stable isotopes was more reliable and accurate to determine zinc absorption. Moreover, the double isotopic tracer ratio (DITR) technique applied to urine samples was a more practical and valuable way to evaluate zinc absorption than other methods. It can be speculated that iron and phytic acid might not be the main inhibitors in the representative Chinese diet.     

Dietary change and stable isotopes: a model of growth and dormancy in cave bears.

In order to discuss dietary change over time by the use of stable isotopes, it is necessary to sort out the underlying processes in isotopic variation. Together with the dietary signal other processes have been investigated, namely metabolic processes, collagen turnover and physical growth. However, growth and collagen turnover time have so far been neglected in dietary reconstruction based on stable isotopes. An earlier study suggested that cave bears (Ursus spelaeus) probably gave birth to cubs during dormancy. We provide an estimate of the effect on stable isotopes of growth and metabolism and discuss collagen turnover in a population of cave bears. Based on a quantitative model, we hypothesized that bear cubs lactated their mothers during their first and second winters, but were fed solid food together with lactation during their first summer. This demonstrates the need to include physical growth, metabolism and collagen turnover in dietary reconstruction. Whereas the effects of diet and metabolism are due to fractionation, growth and collagen turnover are dilution processes.     

Tracing origins and migration of wildlife using stable isotopes: a review

To understand the ecology of migratory animals it is important to link geographic regions used by individuals including breeding, wintering, and intermediate stopover sites. Previous conventional approaches used to track animal movements have relied on extrinsic markers and typically the subsequent recovery of individuals. This approach has generally been inappropriate for most small, or non-game animals. The use of intrinsic markers such as fatty acid profiles, molecular DNA analyses, and the measurement of naturally occurring stable isotopes in animal tissues offer alternative approaches. This paper reviews the use of stable isotope analyses (primarily δ¹³C, δ¹⁵N, δ³⁴S, δD, δ⁸⁷Sr) to trace nutritional origin and migration in animals. This approach relies on the fact that foodweb isotopic signatures are reflected in the tissues of organisms and that such signatures can vary spatially based on a variety of biogeochemical processes. Organisms moving between isotopically distinct foodwebs can carry with them information on the location of previous feeding. Such an approach has been used to track animal use of inshore versus offshore, marine versus freshwater, terrestrial C₃ versus marine, terrestrial mesic versus xeric, and C₃ versus C₄ or Crassulacean acid metabolism foodwebs. More recently, the use of stable hydrogen isotope analyses (δD) to link organisms to broad geographic origin in North America is based on large-scale isotopic contours of growing-season average δD values in precipitation. This technique, especially when combined with the assay of other stable isotopes, will be extremely useful in helping to track migration and movement of a wide range of animals from insects to birds and mammals. Future research to refine our understanding of natural and anthropogenic-induced isotopic gradients in nature, and to explore the use of stable isotopes of other elements, is recommended. Received: 1 July 1998 / Accepted: 9 December 1998     

Natural iron isotopic composition of blood is an indicator of dietary iron absorption efficiency in humans

Persistent impairments in the regulation of intestinal iron absorption result in iron deficiency or iron accumulation in the long term. Diagnosis remains difficult unless pathological symptoms develop as iron absorption varies strongly between meals and days. Variations in the natural iron isotopic composition of whole blood have recently been suggested as a novel parameter to assess long-term differences in intestinal absorption efficiency between individuals. In this study, baseline blood samples collected in two previous conventional iron absorption studies in Swiss and Thai women using stable isotope tracers were reanalyzed by multicollector inductively coupled plasma mass spectrometry. The natural iron isotopic compositions obtained were compared with fractional absorption from the test meals observed in these earlier trials. Correlations of natural blood iron isotopic composition and fractional absorption from the test meals were found to be highly significant in both cohorts (for Swiss women, r = 0.40, P = 0.01, n = 38; for Thai women, r = 0.57, P < 0.01, n = 24), with the blood of both ethnicities clearly differing in iron isotopic composition (P < 0.001). Combining the findings of this study and those of recent animal and human studies confirms that blood iron isotopic patterns may serve as a novel compound biomarker of iron metabolism to assess impairments in regulation of intestinal iron absorption in individuals or population groups.     

Xylose Test: Effect of Aspirin and Indomethacin

The xylose test was used to assess the effect of drugs on intestinal absorption. Both aspirin and indomethacin reduced the urinary output of xylose. By giving xylose intravenously as well as orally it was found that aspirin had a parenteral effect, probably impairing renal function, whereas indomethacin depressed intestinal absorption.     

Determination of selenium stable isotopes by gas chromatography–mass spectrometry with negative chemical ionisation

A gas chromatography mass spectrometric method using negative chemical ionisation was developed for the determination of stable isotopes of selenium for evaluation of selenium absorption and retention from foods in humans. The method involves an acid digestion to convert all selenium into selenite, which subsequently reacts with 4-nitro-o-phenylene-diamine to form a volatile piazselenole. The piazselenole, after extraction into an organic solvent, was analysed for its isotopic selenium composition by gas chromatography mass spectrometry. Negative chemical ionisation is reported for the first time for the determination of selenium stable isotopes and its analytical characteristics were compared to those of electron impact mass spectrometric ionisation, classically used for the determination of selenium. The negative chemical ionisation technique allowed accurate determination of total selenium by isotope dilution and of selenium isotope ratios in biological samples. The repeatability for total selenium and for stable isotope ratios was good (R.S.D.≤10%) within the range of 50 to 250 ng selenium. The detection limit for the investigated selenium isotopes was approximately 1 pg (signal to noise ratio at 3). The applicability of the developed stable isotope methodology was demonstrated by the determination of the selenium absorption and retention from foods in a pilot study using one human adult.     

Stable sulphur isotopes in plants: a review

The determination of the natural abundances of stable isotopes has become a useful method by which to study the transformations of elements in biological and ecological studies as well as to investigate the mechanisms of chemical reactions. Unlike carbon and nitrogen isotopes, however, stable sulphur isotopes are used infrequently, and their potential as tracers in biochemical and physiological studies are only beginning to be realized. This review provides an overview of research involving stable sulphur isotopes in studies of plant metabolism and pollution. Topics discussed include the mechanisms and accompanying isotopic fractionations involved during the uptake and assimilation of inorganic sulphur compounds by plants, the utility of plants as bioindicators of environmental sulphur pollution, and the emission of isotopically light H₂S by plants in response to high concentations of sulphur. Future advances in the field are proposed.     

Determination of stable molybdenum isotopes by thermionic mass spectrometry for tracer studies of molybdenum plant metabolism

A tracer technique based on multiple stable Mo isotopes and thermionic quadrupole mass spectrometry for isotopic analysis of plant tissue was developed and has been applied in the long-term study of foliar absorption of Mo by potato plants. As several tracers have been used the multivariate linear regression methods has been applied to calculate the portions of tracer Mo present in the potato samples from the isotopic ratios measured and to estimate their reproducibilities.In this paper solely the tracer portions transferred from the leaf into the tuber of the potato have been determined. Dependent on the time of contamination, tracer portions of 0.2 to 12% have been measured, corresponding to a maximum of 2.3% of the foliar application of the tracer molybdate. The reproducibilities of the tracer method as a whole (analytical determination and calculation of the tracer portions in the tracer plant samples) amounted to 7% at the maximum (with one exception); by contrast, the individual differences between the three plants investigated were much larger (up to 80%).     

A stable isotope dilution assay for disopyramide and its [13C, 15N]labelled analogue in biological fluids

The mass spectra of disopyramide phosphate and two stable isotopically labelled analogues have been obtained using electron impact and chemical ionization. The low isotopic purity of [13C, 15N)disopyramide phosphate was shown to be due to the low isotopic purity of the 15N label. A stable isotope dilution assay for disopyramide and [13C, 15N]disopyramide in biological fluids has been developed using [2H14]disopyramide phosphate as the internal standard. This assay will be used to analyse samples obtained after the co-administration of disopyramide phosphate intravenously and [13C, 15N]disopyramide phosphate orally to several animal species.     

Stable Isotope Techniques and Applications for Primatologists

Stable isotope biogeochemistry is useful for quantifying the feeding ecology of modern and extinct primates. Over the past three decades, substantial advances have been made in our knowledge of the physiological causes of isotopic patterns as well as effective methodology to prepare samples for isotopic analysis. Despite these advances, the potential of stable isotope biogeochemistry has yet to be fully exploited by primate researchers, perhaps due to the prolific and somewhat daunting nature of the isotopic literature. I here aim to present a cogent overview of stable isotope applications to nonhuman primate feeding ecology. I review the factors that influence ecological patterns in carbon, nitrogen, and oxygen stable isotopes. I present methods for collecting and preparing samples of tooth enamel and bone mineral hydroxyapatite, bone collagen, fur and hair keratin, blood, feces, and urine for isotope analysis. I discuss both the existing and potential applications of these isotopic patterns to primate feeding ecology. Lastly, I point out some of the pitfalls to avoid when interpreting and comparing isotopic results.