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Minerals: exercise performance and supplementation in athletes.

This paper examines whether mineral supplements are necessary for athletes, and whether these supplements will enhance performance. Macrominerals (calcium, magnesium, and phosphorus) and trace minerals (zinc, copper, selenium, chromium, and iron) are described. Calcium supplements are important for the health of bones. Athletes tend to have enhanced calcium status as assessed by bone mineral density, with the notable exception of female amenorrhoeic athletes. Magnesium status is adequate for most athletes, and there is no evidence that magnesium supplements can enhance performance. Phosphorus status is adequate for athletes. Phosphorus supplementation over an extended period of time can result in lowered blood calcium, however, some studies have shown that acute 'phosphate loading' will enhance performance. Athletes may have a zinc deficiency induced by poor diet and loss of zinc in sweat and urine. Limited data exist on the relationship of performance and zinc status. Widespread deficiencies in copper have not been documented, and there are no data to suggest that copper supplementation will enhance performance. There is no reason to suspect a selenium deficiency in athletes. The relationship between selenium status and performance has not been established, but selenium may play a role as an antioxidant. Because of the low intakes of chromium for the general population, there is a possibility that athletes may be deficient. Exercise may create a loss in chromium because of increased excretion into the urine. Many athletes, particularly female, are iron depleted, but true iron deficiencies are rare. Iron depletion does not affect exercise performance but iron deficiency anaemia does. Iron supplements have not been shown to enhance performance except where iron deficiency anaemia exists. In conclusion, poor diets are perhaps the main reason for any mineral deficiencies found in athletes, although in certain cases exercise could contribute to the deficiency. Mineral supplementation may be important to ensure good health, but few studies have definitively documented any beneficial effect of mineral supplementation on performance.

Exercise↗

Effect of a two-year supplementation with low doses of antioxidant vitamins and/or minerals in elderly subjects on levels of nutrients and antioxidant defense parameters.

BACKGROUND: Eighty-one elderly hospitalized subjects (> 65 years) were recruited for a double-blind placebo-controlled study to examine low dose supplementation of antioxidant vitamins and minerals on biological and functional parameters of free radical metabolism. Subjects were randomly assigned to one of the four treatment groups, daily receiving for 2 years: placebo group; mineral group: 20 mg zinc, 100 micrograms selenium; vitamin group: 120 mg vitamin C (Vit C), 6 mg beta-carotene (beta CA), 15 mg vitamin E (Vit E); mineral and vitamin group: Zn 20 mg, Se 100 micrograms, Vit C 120 mg, beta CA 6 mg, Vit E 15 mg. RESULTS: Fifty-seven subjects completed the study. A large frequency of Vit C, Zn and Se deficiencies were observed at baseline. As early as 6 months of treatment, a significant increase in vitamin and mineral serum levels was observed in the corresponding groups. The increases ranged from 1.1-4.0 fold depending on the nutrient. Antioxidant defense, studied in vitro with a test using red blood cells in presence of 2,2'-azo-bis (2-amidinopropane) by hydrochloride, showed an increase of cell resistance in patients receiving vitamins (p = 0.002); it was positively correlated with serum Vit C (p < 0.0001), alpha-tocopherol/cholesterol (p = 0.06), beta CA (p = 0.0014), serum Cu and Se (p < 0.05). Moreover, red blood cell antioxidant defense was reduced in elderly compared with young control subjects (50% hemolysis time: 69 +/- 14 mn and 109 +/- 12 mn, respectively). Erythrocyte glutathione peroxidase activity was enhanced in groups receiving minerals, whereas no significant change was observed for other indicators of oxidative stress (erythrocyte superoxide dismutase activity, thiobarbituric acid-reactive substances, total glutathione, reduced and oxidized forms). DISCUSSION: Our results provide experimental evidence that a low dose supplementation with vitamins and minerals was able to normalize biological nutrient status as early as 6 months of treatment. In addition, our data indicate that antioxidant defense in elderly subjects was improved with low doses of vit C, vit E and beta CA as studied by means of a functional test utilizing red blood cells challenged in vitro with free radicals.

Aged↗

Effect of dietary protein and minerals on calcium and zinc utilization.

The utilization of most minerals can be altered not only by varying the dietary levels of protein, carbohydrate, fiber, fat, and vitamins but also by varying the forms of macronutrients fed. Interactions among minerals are frequent and sometimes complex. Thus, all assessments of mineral requirements should include discussions of the effects of interactions on mineral bioavailability. Some of these interactions occur in the gut and affect the absorption of minerals. Other interactions affect the metabolism, transport and storage of minerals, and ultimately their excretion in urine or in endogenous gut secretions.

Animals↗

Effect of mineral oil and/or cholestyramine in the diet on biliary and intestinal elimination of 2,4,5,2',4',5'-hexabromobiphenyl in the rhesus monkey.

Addition of mineral oil to the diet (5%) of two rhesus monkeys that were dosed 29 wk earlier with 2,4,5,2',4',5'-hexabromobiphenyl (HBB) produced a 175% increase in fecal excretion of HBB. A third rhesus monkey was provided with a complete biliary bypass, which permitted the reintroduction of the monkey's own bile or the introduction of the same amount of exogenous bile, which was obtained from control donor monkeys. This experimental design made it possible to measure the portion of fecal excretion that was due to biliary elimination and the portion that was due to intestinal elimination. The effect of mineral oil and/or cholestyramine (CSA) on biliary and intestinal elimination of HBB in the rhesus monkey was then investigated. The results show that (1) fecal excretion of HBB and/or metabolites is due to both biliary and intestinal elimination; (2) during the first 2 wk after completion of dosing, mineral oil does not influence fecal excretion of HBB significantly; (3) 6-7 wk after completion of dosing, mineral oil enhances fecal excretion of HBB by 50%; (4) 8 wk after the last dose of HBB, 4% CSA in the diet increases fecal excretion of HBB and/or metabolites by about 50%; (5) mineral oil specifically stimulates intestinal elimination of HBB; and (6) combined administration of mineral oil and CSA results in an additive effect.

Animals↗

Bone mineral mass in adult lacto-ovo-vegetarian and omnivorous males.

Past studies indicate postmenopausal women who eat meat may experience greater bone mineral loss than lacto-ovo-vegetarian women. The present study extends those findings by comparing bone mineral in adult lacto-ovo-vegetarian and omnivorous males. Bone mineral mass was determined by direct photon absorptiometry in 320 lacto-ovo-vegetarian and 320 omnivorous males 20 to 79 yr old. Lacto-ovo-vegetarians were Seventh-day Adventists committed to their diet for at least 20 yr. Measurements were made at a cortical site along the radius. No statistical differences were identified between bone mineral mass in the lacto-ovo-vegetarian and omnivorous males in any decade examined. When contrasted against significant differences between bone mineral mass in postmenopausal omnivores and lacto-ovo-vegetarians, the data presented here may be interpreted as indicating that some factor associated with meat consumption is increasing bone mineral losses in postmenopausal females while having no observable effect in males.

Absorptiometry, Photon↗

Efficacy of calcium glycerophosphate vs conventional mineral salts for total parenteral nutrition in low-birth-weight infants: a randomized clinical trial.

To test the efficacy of calcium glycerophosphate (CaGlyP) vs the conventional mineral salts, calcium gluconate plus KH2PO4 + K2HPO4 (CaGluc + P), in promoting mineral retention, 72-h mineral balance, biochemical status, net acid excretion, and growth were assessed in 16 low-birth-weight infants receiving total parenteral nutrition (TPN) containing approximately 1.5 mmol Ca and P.kg-1.d-1 for 5 d. Net retentions of calcium (1.2 +/- 0.2 vs 1.0 +/- 0.2 mmol.kg-1.d-1, means +/- SD) and phosphorus (1.1 +/- 0.3 vs 0.8 +/- 0.3 mmol.kg-1.d-1) from CaGluc + P vs CaGlyP, respectively, were similar, as were retentions of magnesium and sodium, urinary pH, and net acid excretion. Plasma ionized calcium, inorganic phosphorus, alkaline phosphatase, and osteocalcin were normal and not different between groups. CaGlyP is as effective as CaGluc + P in promoting mineral retention and normal mineral homeostasis. However, at intakes of less than or equal to 1.5 mmol Ca and P.kg-1.d-1 from either mineral salt, retention represented only 60% and 45%, respectively, of the predicted intrauterine accretion for calcium and phosphorus. Larger intakes permitted by the more-soluble CaGlyP may be desirable for infants receiving TPN.

Body Height↗

Major mineral concentrations in human milk do not change after maximal exercise testing.

Fourteen healthy, lactating women (aged 25-38 y and between 2 and 8 mo postpartum) participated in both a maximal graded exercise test and a 30-min rest period to determine the influence of exercise on the concentration of selected milk minerals and electrolytes. Treatment order was randomized and treatments were conducted on different days. Milk was expressed before treatment and at 10, 30, and 60 min postexercise or after the rest period. Milk was wet-ashed by using nitric and sulfuric acids. Aliquots were analyzed for total phosphorus concentration by colorimetric assay and for calcium, magnesium, sodium, and potassium by inductively coupled plasma atomic emission spectrophotometry. Baseline mineral concentrations were not significantly different (P>0.05). Repeated expression of milk at 10, 30, and 60 min did not show significantly altered mineral concentrations (P>0.05). Interwoman variation was responsible for most of the variation in mineral concentrations. A portion of this may be explained by the variation in stage of lactation, which is known to affect mineral composition. Stage of lactation was inversely correlated with concentration of calcium, total phosphorus, magnesium, and sodium (P<0.05). In conclusion, maximal exercise did not alter concentrations of phosphorus, calcium, magnesium, potassium, or sodium in milk. Thus, with respect to mineral concentrations in milk, there is no contraindication for exercise during lactation.

Adult↗

Effect of dietary mineral composition on nutritional equivalency of amino acid mixtures and casein in rats.

The effect of dietary mineral composition on the quality of amino acid mixtures and intact casein was examined in growing rats fed for 28 days under "conventional" conditions. When 25% demineralized casein (DC) was the sole dietary protein source, the widely-used mineral mixture by Harper (MMH) supported growth poorly (3.2 g/day), but a new formula mineral mixture (MM2) containing sufficient amounts of zinc gave a growth rate of over 8 g/day for 21 days. With a crude casein (CC) diet, rats grew at the same rate regardless of mineral mixtures. The growth-supporting power of amino acid mixtures, one of which simulated casein (AA-A) and another patterned after Rogers and Harper to give maximal growth of rats (AA-B), was compared with those of DC and CC with addition of MMH or MM2. When the protein source was DC, AA-A or AA-B, MM2 significantly improved the growth over that of rats fed MMH. The growth-stimulating effect of MM2 was greater when added to DC diet than when added to AA-A diet. When MM2 was added to AA-B diet, the growth rate greatly increased and reached that of rats fed DC diet containing MM2 (over 8 g/day), showing a nutritional equivalency between the amino acid mixture and intact protein. Drawbacks inherent in MMH did not appear with CC diet, because CC contained considerable amounts of zinc. When a highly purified amino acid-sucrose diet is used, dietary minerals become most limiting for growth even under conventional conditions. Thus, the previous conflicting results concerning nutritional equivalency of amino acid mixtures and protein can be explained by inadequate mineral sources.

Amino Acids↗

An in vitro system for measuring intrinsic dietary mineral exchangeability: alternative to intrinsic isotopic labeling.

The primary purpose for the in vitro system described here was to provide an alternative method to intrinsic isotopic labeling for determining exchangeability of intrinsic food mineral with extrinsic inorganic mineral or one of its isotopes. In this system, foods or food mixtures extrinsically tagged with an isotope of the mineral of interest are incubated successively in media simulating peptic or pancreatic digestion. Radioactivity and mineral measurements are made on a)the mixture before digestion and after b)peptic and c)successive peptic pancreatic (P-Pa) digestion. Exchangeability is determined by comparing the specific activity in the peptic and P-Pa digest supernatants to that in the mixture before digestion. In addition, determination of the total soluble mineral after P-Pa digestion provides a measurement of potential bioavailability. The procedure was tested for calcium (Ca) exchangeability and bioavailability from a number of foods and food combinations with 45Ca as the tracer. It could be used for any mineral, however, including non-nutrient or toxic elements. It is likely to be most useful in association with human studies carried out with extrinsic stable (non-radioactive) or short-lived radioactive isotopes that are unsuitable for intrinsic labeling.

Biological Availability↗

Localization and movement of mineral oil in plants by fluorescence and confocal microscopy.

Fluorescence and confocal laser scanning microscopy were explored to investigate the movement and localization of mineral oils in citrus. In a laboratory experiment, fluorescence microscopy observation indicated that when a 'narrow' distillation fraction of an nC23 horticultural mineral oil was applied to adaxial and opposing abaxial leaf surfaces of potted orange [Citrus x aurantium L. (Sapindales: Rutaceae)] trees, oil penetrated steadily into treated leaves and, subsequently, moved to untreated petioles of the leaves and adjacent untreated stems. In another experiment, confocal laser scanning microscopy was used to visualize the penetration into, and the subsequent cellular distribution of, an nC24 agricultural mineral oil in C. trifoliata L. seedlings. Oil droplets penetrated or diffused into plants via both stomata and the cuticle of leaves and stems, and then moved within intercellular spaces and into various cells including phloem and xylem. Oil accumulated in droplets in intercellular spaces and within cells near the cell membrane. Oil entered cells without visibly damaging membranes or causing cell death. In a field experiment with mature orange trees, droplets of an nC23 horticultural mineral oil were observed, by fluorescence microscopy, in phloem sieve elements in spring flush growth produced 4-5 months and 16-17 months after the trees were sprayed with oil. These results suggest that movement of mineral oil in plants is both apoplastic via intercellular spaces and symplastic via plasmodesmata. The putative pattern of the translocation of mineral oil in plants and its relevance to oil-induced chronic phytotoxicity are discussed.

Biological Transport↗

238U, 226Ra, 210Po concentrations of bottled mineral waters in Hungary and their committed effective dose.

Nowadays the consumption of bottled mineral waters has become very popular. The average consumption of these is 0.36 l d(-1) per person in Europe. A considerable segment of the population drinks almost only mineral water as drinking water, which is about 1 l d(-1). As is known, some kinds of mineral waters contain naturally occurring radionuclides in higher concentration than the usual drinking (tap) water. The WHO (1993) legislation concerning the drinking waters does not include the mineral waters. In our work, the concentrations of (226)Ra, (238)U and (210)Po were determined in mineral waters available in Hungary. To determine the (226)Ra concentration the emanation method was used. The (238)U and (210)Po concentrations were determined by alpha spectrometry using semiconductor detector. The dose contribution was calculated using the radionuclide concentrations and the dose conversion factors from the Basic Safety Standard IAEA (1995), for 1 l d(-1) mineral water consumption. In some cases the calculated doses were considerable higher than the limit for drinking waters. Especially for children the doses can be remarkably high.

Adolescent↗

Distinctive patterns of autoimmune response induced by different types of mineral oil.

Although mineral oils are generally considered nontoxic and have a long history of use in humans, the mineral oil Bayol F (incomplete Freund's adjuvant, IFA) and certain mineral oil components (squalene and n-hexadecane) induce lupus-related anti-nRNP/Sm or -Su autoantibodies in nonautoimmune mice. In the present study, we investigated whether medicinal mineral oils can induce other types of autoantibodies and whether structural features of hydrocarbons influence autoantibody specificity. Female 3-month-old BALB/c (16-45/group) mice each received an i.p. injection of pristane (C19), squalene (C30), IFA, three medicinal mineral oils (MO-F, MO-HT, MO-S), or PBS. Sera were tested for autoantibodies and immunoglobulin levels. Hydrocarbons were analyzed by gas chromatography/mass spectrometry. IFA contained mainly C15-C25 hydrocarbons, whereas MO-HT and MO-S contained C20-C40, and MO-F contained C15-C40. Pristane and n-hexadecane were found in IFA (0.17% and 0.10% w/v, respectively) and MOs (0.0026-0.027%). At 3 months, pristane and IFA induced mainly IgG2a, squalene IgG1, and MOs IgG3 and IgM in sera. Anti-cytoplasmic antibodies were common in mice treated with MO-F, as well as those treated with pristane, squalene, and IFA. Anti-ssDNA and -chromatin antibodies were higher in MO-F and MO-S than in untreated/PBS, squalene-, or IFA-treated mice, suggesting that there is variability in the induction of anti-nRNP/Sm versus -chromatin/DNA antibodies. The preferential induction of anti-chromatin/ssDNA antibodies without anti-nRNP/Sm/Su by MO-S and MO-F is consistent with the idea that different types of autoantibodies are regulated differently. Induction of autoantibodies by mineral oils considered nontoxic also may have pathogenetic implications in human autoimmune diseases.

Alkanes↗

Recent insights into the coordinate regulation of body water and divalent mineral ion metabolism.

Traditionally, arginine vasopressin modulation of renal water, sodium, and urea excretion has been considered somewhat in isolation from factors that control divalent mineral ion homeostasis. Similarly, previous considerations of divalent mineral ion metabolism have focused mainly on the role of hormones, eg, parathyroid hormone and various forms of vitamin D, as principal modifiers of renal calcium handling. Recent data, however, have now suggested the existence of novel linkages that coordinate control of water and divalent mineral ion homeostasis. This article summarizes these data and highlights the fundamental roles of the extracellular calcium polyvalent cation-sensing receptor (CaR) as an integrator of water and divalent mineral ion homeostasis on a cellular, organ-specific, and whole-body basis. Organs where CaRs may integrate water and divalent mineral ion metabolism include endocrine tissues that express CaRs, the brain, various nephron segments of the kidney, bone, and the gastrointestinal tract. These new data suggest that considerable regulatory overlap exists between water and divalent mineral ion homeostasis.

Animals↗

Computed tomography scanning for the measurement of bone mineral in the human spine.

An investigation into the feasibility of using X-ray computed tomography (CT) to measure disease induced changes in bone mineral content of the human spine is described. A theoretical study of this type of measurement has been made using a mathematical model of osteomalacia. The measured EMI number changes linearly with the mineral content, and the sensitivity is shown to be 1.2 EMI units (EU: 500 scale)/1% change in mineral content in vertebral bone. The physical sensitivity to an equal mineral change in cortical bone is found to be 8.6 times greater. The mineral selectivity of the CT method is such that only about half the change in the EMI number arising from progressive osteomalacia reflects change in actual mineral content, while half is due merely to changes in bone density that accompany demineralization. In addition, the perturbing effects of beam hardening on measurement accuracy are evaluated and shown to be significant. Finally, an experimental measurement indicates that in practice the reproducibility of such measurements would be about 1 EU, and it is shown that the measured parameter correlates well with the calculated total linear attenuation coefficients.

Bone and Bones↗

Reduced bone mineralization in adolescent survivors of malignant bone tumors: comparison of quantitative ultrasound and dual-energy x-ray absorptiometry.

PURPOSE: To assess bone mineralization in adolescents with bone tumors at remission using quantitative digital ultrasound (QUS) and dual-energy x-ray absorptiometry (DEXA), and to compare the bone mineralization values obtained by both methods. METHODS: Patients studied were 36 adolescents (21 boys, 15 girls) who had completed treatment of a bone tumor at the University Hospital of the University of Navarra (Pamplona, Spain). QUS was performed at the distal metaphysis of the proximal phalanxes of the last four fingers of the nondominant hand. A DBM Sonic 1200 Ultrasound densitometer was used. DEXA measurements were made at the lumbar spine (vertebrae L1-L4) using the Hologic QDR 4500 W device. Calcium and vitamin D daily intake and grade of physical activity were recorded. RESULTS: Mean age at bone mineralization determination was 19.11 years. Disease-free survival was 4.97 years. Decreased bone mineralization was observed by both methods. Bone mineralization absolute values measured by QUS and DEXA were significantly correlated. The sensitivity, specificity, diagnostic accuracy, and positive and negative predictive values of QUS for predicting osteopenia were 36.4%, 80.0%, 66.7%, 44.4%, and 74.1%, respectively. Daily vitamin D intake was below the recommended dietary allowances. CONCLUSIONS: Adolescents in remission from bone tumors have low bone mineralization determined by DEXA or QUS.

Absorptiometry, Photon↗

Calcium bioavailability from a calcium-rich mineral water, with some observations on method.

GOALS: The study was designed to determine whether high-calcium mineral water is an efficient additional source of dietary calcium, optimizing a method for calcium determination never used for mineral waters. BACKGROUND: It is generally agreed that an adequate calcium intake is necessary for the acquisition of an ideal peak bone mass and for the maintenance of the bone mineral density in adults, in postmenopausal women, and in the elderly. Mineral waters are calorie free, and some, with high calcium levels, might be significant sources of calcium. STUDY: The availability of the calcium contained in a high-calcium mineral water was measured in 27 healthy subjects. In 8 subjects the calcium availability of the water was compared with the calcium availability ingested with milk at the same calcium load. Milk and water were labeled extrinsically with 30 mg Ca. Fractional absorption from the oral dose was determined from plasma samples using ICP-MS technique. RESULTS: At an ingested calcium load of 3.18 mmol, percentage of absorption for water averaged 22.53 +/- 2.53 (mean +/- SD) for men, 22.57 +/- 2.10 (mean +/- SD) for premenopausal women and 21.62 +/- 3.12 (mean +/- SD) for postmenopausal women. Percentage absorption from milk was 23.15 +/- 4.06 (mean +/- SD). DISCUSSION: The calcium from the mineral water is thus highly bioavailable, at least as bioavailable as milk calcium, and ICP-MS appears to represent a reliable and reproducible method for calcium absorption from alimentary sources.

Adult↗

Soil factors controlling mineral N uptake by Picea engelmannii seedlings: the importance of gross NH4+ production rates.

* Hydroponic studies suggest that plant nitrogen (N) demand determines the rate of mineral N uptake; however, field observations show N limitation to be widespread. Field experiments are needed to understand soil factors controlling mineral N uptake. * We planted Picea engelmannii seedlings that had initially been grown from sterilized seeds, on a recently clearcut site. We applied a hybrid isotope dilution/pulse labelling technique to compare the gross production rate, concomitantly to the plant uptake rate, of soil mineral N. We also measured mineral N concentrations, microbial N, and percent ectomycorrhizal root tips. * Gross NH4+ production rate was the most important determinant of plant uptake rate. Exploratory path analysis suggested that plant uptake was also determined by microbial N, which was, in turn, determined by soil mineral N concentrations. Percent ectomycorrhizal root tips was negatively related to gross NO3- production rate and microbial N concentrations. * We conclude that nutrient flux density is important in controlling plant uptake. Mycorrhizal colonization may alter N dynamics in the rhizosphere without affecting mineral N uptake by seedlings.

Biological Transport, Active↗

Ectomycorrhizal weathering of the soil minerals muscovite and hornblende.

Ectomycorrhizal fungi are hypothesized to enhance mineral weathering in forest soils. Several studies have shown an increased uptake of mineral-derived nutrients by trees when in symbiosis with ectomycorrhizal fungi. However, it is difficult to determine from these studies if the improved nutrient uptake is the result of increased weathering or better exploitation of the substrate by the ectomycorrhizal fungi. In a pot experiment, Pinus sylvestris (Scots pine) seedlings were grown with or without ectomycorrhizal fungi, and with or without the mineral muscovite as the only potassium (K) source or the mineral hornblende as the only magnesium (Mg) source. After 27 wk, all pools of non-mineral-bound K or Mg were determined. The ectomycorrhizal fungus Paxillus involutus increased weathering of muscovite but not hornblende. The other ectomycorrhizal fungi tested, Piloderma croceum and Suillus bovinus, did not increase weathering of either muscovite or hornblende compared with the nonmycorrhizal trees. The P. involutus-mediated mobilization of K from muscovite resulted in increased K content of root plus adhering hyphae, but not of shoots. In conclusion, ectomycorrhizal fungi may increase weathering of minerals in response to nutrient deficiencies, but this response is species specific.

Minerals↗