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Morphological and biochemical characterization of mineralizing primary cultures of avian growth plate chondrocytes: evidence for cellular processing of Ca2+ and Pi prior to matrix mineralization.

Advances in the culture of mineralizing growth plate chondrocytes provided an opportunity to study endochondral calcification under controlled conditions. Here we report that these cultures synthesize large amounts of proteins characteristically associated with mineralization: type II and X collagens, sulfated proteoglycans, alkaline phosphatase, and the bone-related proteins, osteonectin and osteopontin. Certain chondrocytes appeared to accumulate large amounts of Ca2+ and Pi during the mineralization process: laser confocal imaging revealed high levels of intracellular Ca2+ in their periphery and X-ray microanalytical mapping revealed the presence of many Ca(2+)- and Pi-rich cell surface structures ranging from filamentous processes 0.14 +/- 0.02 microns by 0.5-2.0 microns, to spherical globules 0.70 +/- 0.27 microns in diameter. Removal of organic matter with alkaline sodium hypochlorite revealed numerous deposits of globular (0.77 +/- 0.19 micron) mineral (calcospherites) in the lacunae around these cells. The size and spatial distribution of these mineral deposits closely corresponded to the Ca(2+)-rich cell surface blebs. The globular mineral progressively transformed into clusters of crystallites. Taken with earlier studies, these findings indicate that cellular uptake of Ca2+ and Pi leads to formation of complexes of amorphous calcium phosphate, membrane lipids, and proteins that are released as cell surface blebs analogous to matrix vesicles. These structures initiate development of crystalline mineral. Thus, the current findings support the concept that the peripheral intracellular accumulation of Ca2+ and Pi is directly involved in endochondral calcification.

Animals↗

Stable transfection of nonosteogenic cell lines with tissue nonspecific alkaline phosphatase enhances mineral deposition both in the presence and absence of beta-glycerophosphate: possible role for alkaline phosphatase in pathological mineralization.

It is documented that alkaline phosphatase (AP) plays an important role in bone mineralization. Considering that TN-AP is expressed in periodontal ligament fibroblasts, renal epithelial cells, and vascular endothelial cells, and that TN-AP is both a calcium-/phosphate-binding protein and a phosphohydrolytic enzyme, we hypothesize that membrane-bound AP also plays an important role in the initiation of physiological and pathological mineralizations in tissues other than bone and cartilage. To test this hypothesis, nonosteoblast cell lines, including a fibroblast line, a renal epithelial line, and a capillary endothelial line, were stably transfected to express high levels of rat bone AP on their cell surfaces. These rat bone AP-expressing cells were then cultured on filter membranes in the presence or absence of beta-glycerol phosphate. von Kossa staining for calcium phosphate and transmission electron microscopy with electron diffraction analysis for minerals were employed to investigate the effect of membrane AP on extracellular calcium phosphate mineralization. Our results indicated that AP expression on these nonosteoblast-like cell surfaces have induced extracellular hydroxyapatite (HAP) mineralization. Our findings support the concept that membrane-bound AP contributes to extracellular apatitic mineralization by mechanisms that do not necessarily involve its hydrolase activity. They also suggest that AP might be important for the initiation of pathological mineralization in nonosteogenic tissues.

Alkaline Phosphatase↗

Effect of supplementation of calcium and vitamin D on bone mineral density and bone mineral content in peri- and post-menopause women; a double-blind, randomized, controlled trial.

BACKGROUND: Osteoporosis is a serious global health problem for the future, that is why improving diagnostic methods and prevention of this disease could be helpful. OBJECTIVES: To assess the effects of calcium supplementations combined with Vitamin D on bone mineral density (BMD) and bone mineral content (BMC) in a representative sample of peri- and post-menopausal women in a double-blind, a randomized, controlled trial was untaken. DESIGN: A total of 120 women aged over 45 were included in a randomised placebo-controlled, double-blind trial on the effect of a daily dietary supplementation of calcium and Vitamin D on bone mineral density and bone mineral content; over a 30-month period. METHODS: Dietary intake assessment; dual-energy X-ray absorptiometry to measure total body and segmental bone mineral density and bone mineral content at beginning of the study and every 15 months were undertaken. RESULTS: There was no significant change in dietary calcium or Vitamin D intakes in either of the treatment groups during the 30-month intervention period. The change in total BMD in the calcium group was significantly different from that in the placebo group (P <0.005). The placebo group lost a total BMD at a rate of about 0.4% per year. There was an inverse correlation between BMD and age. CONCLUSIONS: The effect of calcium and Vitamin D supplementation on bone mineral density of calcium has been demonstrated in this group of young adult women. Our results showed the positive effect of calcium and Vitamin D supplementation in women both peri- and post-menopausal status; for this reason a supplementation of calcium and Vitamin D should be recommended as a strategic option in helping to prevent early postmenopausal bone loss.

Analysis of Variance↗

Effect of parenteral calcium and phosphorus therapy on mineral retention and bone mineral content in very low birth weight infants.

HYPOTHESIS: If calcium and phosphorus are administered to very low birth weight infants in amounts larger than those currently used in standard parenteral nutrition solutions, apparent retention of calcium and phosphorus (intake minus urinary excretion) will increase and bone mineralization will improve. DESIGN: Randomized, controlled, double-blind trial. SETTING: Neonatal intensive care unit. PATIENTS: Twenty-four very low birth weight infants (< 1.2 kg) expected to receive parenteral nutrition exclusively for approximately 3 weeks beginning 3 days after birth. INTERVENTIONS: Infants received parenteral nutrition solutions, either the standard mixture containing 1.25 mmol calcium and 1.5 mmol phosphorus per deciliter (group STAND: n = 12, birth weight 921 +/- 171 gm, gestational age 27 +/- 2 weeks (mean +/- SD)) or 1.7 mmol calcium and 2.0 mmol phosphorus per deciliter (group HIGH: n = 12, 857 +/- 180 gm, 27 +/- 2 weeks). MAIN OUTCOME MEASURES: Intake, urinary excretion, and apparent retention of calcium, phosphorus, and magnesium every 3 days during parenteral nutrition therapy. Serum indexes of mineral status twice during therapy. Bone mineral content of the distal segment of the left radius at 1, 4, 8, and 26 weeks. RESULTS: Apparent calcium retention (1.2 +/- 0.2 vs 1.6 +/- 0.2 mmol.kg-1.d-1) and phosphorus retention (1.4 +/- 0.2 vs 1.8 +/- 0.4 mmol.kg-1.d-1) differed significantly (p < 0.01) between groups STAND and HIGH, respectively; neither changed with the duration of parenteral nutrition therapy. Serum calcium, magnesium, parathyroid hormone, 25-hydroxyvitamin D, and osteocalcin concentrations were similar in both groups. Serum phosphorus concentration was significantly higher in group HIGH than in group STAND (p = 0.025). The absolute bone mineral content and the rate of increase in bone mineral content between 1 and 4, 1 and 8, and 1 and 26 weeks were significantly greater in group HIGH than in group STAND. CONCLUSIONS: Increased parenteral intakes of calcium and phosphorus resulted in greater retention of these minerals during parenteral nutrition therapy and in greater bone mineral content after therapy.

Bone Density↗

The Saskatchewan Pediatric Bone Mineral Accrual Study: bone mineral acquisition during the growing years.

To investigate bone mineral accretion in growing children, the Saskatchewan Pediatric Bone Mineral Accrual Study was initiated in 1991. The study involves the collection of dietary and physical activity information along with anthropometric growth and maturity measurements every 6 months and dual-energy X-ray absorptiometer (DXA) bone scans of the whole body, AP lumbar spine and proximal femur taken annually. The study has now finished its 6th year and 68 males and 72 females from an original sample of 228 elementary schoolchildren are still involved. To investigate how bone mineral at clinically important sites proceeds in relation to maturation we developed distance and velocity growth curves for height and bone mineral content (BMC) for the AP lumbar spine, the femoral neck and the whole body. In both boys and girls, over 35% of total body and AP spine bone mineral and over 27% of the bone mineral at the femoral neck was laid down during the 4-year adolescent period surrounding peak linear growth velocity. The clinical significance of these values can be appreciated by consideration of the fact that as much bone mineral will be laid down during these 4 adolescent growing years as most people will lose during all of adult life.

Absorptiometry, Photon↗

Effect of mineral and organic soil constituents on microbial mineralization of organic compounds in a natural soil.

This research addressed the effect of mineral and organic soil constituents on the fate of organic compounds in soils. Specifically, it sought to determine how the associations between organic chemicals and different soil constituents affect their subsequent biodegradation in soil. Four C-labeled surfactants were aseptically adsorbed to montmorillonite, kaolinite, illite, sand, and humic acids. These complexes were mixed with a woodlot soil, and CO(2) production was measured over time. The mineralization data were fitted to various production models by nonlinear regression, and a mixed (3/2)-order model was found to most accurately describe the mineralization patterns. Different mineralization patterns were observed as a function of the chemical and soil constituents. Surfactants that had been preadsorbed to sand or kaolinite usually showed similar mineralization kinetics to the control treatments, in which the surfactants were added to the soil as an aqueous solution. Surfactants that had been bound to illite or montmorillonite were typically degraded to lesser extents than the other forms, while surfactant-humic acid complexes were degraded more slowly than the other forms. The desorption coefficients (K(d)) of the soil constituent-bound surfactants were negatively correlated with the initial rates of degradation (k(1)) and estimates of CO(2) yield (P(o)) as well as actual total yields of CO(2). However, there was no relationship between K(d) and second-stage zero-order rates of mineralization (k(o)). Microbial community characteristics (biomass and activity) were not correlated with any of the mineralization kinetic parameters. Overall, this study showed that environmental form had a profound effect on the ultimate fate of biodegradable chemicals in soil. This form is defined by the physicochemical characteristics of the chemical, the composition and mineralogy of the soil, and the mode of entry of the chemical into the soil environment.

Journal Article↗

Long-term strontium ranelate administration in monkeys preserves characteristics of bone mineral crystals and degree of mineralization of bone.

UNLABELLED: In monkeys, long-term strontium ranelate administration results in a dose-dependent bone strontium uptake (mainly into newly formed bone) that preserves the degree of mineralization of bone and the bone mineral at the crystal level, showing its safety at bone mineral level. INTRODUCTION: Strontium ranelate simultaneously increases bone formation and decreases bone resorption, leading to prevention of bone loss and increase in bone mass and bone strength in normal and ovariectomized rats. This study investigated the interactions of stable strontium (Sr) with bone mineral in monkeys after long-term strontium ranelate treatment and after a period of treatment withdrawal. MATERIALS AND METHODS: Iliac bone was obtained from untreated monkeys, monkeys at the end of a 52-week strontium ranelate administration (200, 500, 1250 mg/kg/day orally), and in parallel groups 10 weeks after the end of strontium ranelate administration (same three doses; n = 3-7). Sr uptake and distribution in bone mineral were quantified by X-ray microanalysis, changes at the crystal level by X-ray diffraction, and the degree of mineralization of bone (DMB) by quantitative microradiography. RESULTS: After strontium ranelate administration, dose-dependent Sr uptake occurred into cortical and cancellous bone, with higher content (1.6 times) in new than in old bone. This Sr uptake decreased (50%) 10 weeks after treatment withdrawal; the decrease occurred almost exclusively in new bone. At the end of strontium ranelate treatment and after its withdrawal, a preservation of crystal characteristics was observed, suggesting that Sr was only faintly linked to crystals by ionic substitution and of DMB. CONCLUSIONS: These results show the absence of a deleterious effect of long-term strontium ranelate treatment on bone mineralization, confirming the histomorphometric observations made in postmenopausal osteoporotic women treated with strontium ranelate.

Animals↗

Studies of alkaline phosphatase inhibition by p-bromotetramisole in non-mineralizing and mineralizing neonatal hamster tooth germs in vitro.

The effects of l and d-, p-bromotetramisole (pBTM) on alkaline phosphatase were studied in relation to 45Ca2+, 32phosphate and 3H-thymidine uptakes in non-mineralizing second (M2) and mineralizing first (M1) maxillary hamster molar tooth germs under the conditions of organ culture. At the concentration used in culture (10(-3)M), l-pBTM completely inhibited alkaline phosphatase activity in tooth germ homogenates. About 30% of the enzyme activity was inhibited by d-pBTM at the same concentration. In culture, there were no significant differences between the effects of l and d-pBTM isomers on all the parameters measured. In the non-mineralized M2 molars, l and d-pBTM significantly reduced both TCA-soluble and TCA-insoluble 32phosphate uptakes but not 45Ca2+. However, 3H-thymidine uptake was also significantly decreased. In M1 molars, the pBTM isomers significantly reduced the uptake of TCA-soluble 32phosphate and 45Ca2+ but not TCA-insoluble 32phosphate. Ouabain, a specific inhibitor of Na+-K+-ATPase (but not alkaline phosphatase), also significantly reduced 3H-thymidine uptake to the same extent as the pBTM isomers in the non-mineralizing M2 molars, but it did not significantly affect either 32phosphate (TCA-soluble and TCA-insoluble) or 45Ca2+ uptake. Although this inhibitor significantly reduced both 45Ca2+ and TCA-soluble 32phosphate uptake in the mineralizing M1 molars, this effect was much less dramatic than was the case with the pBTM isomers. The reduced 45Ca2+ uptake in the M1 molars is probably a consequence of reduced mineralization since in the non-mineralizing M2 molars calcium uptake was not significantly affected by the pBTM isomers.(ABSTRACT TRUNCATED AT 250 WORDS)

Alkaline Phosphatase↗

Effects of replacing sulfate with hydroxychloride sources of trace minerals on mineral status and production performance in dairy cows.

The objectives were to determine the effects of replacing sulfate with hydroxychloride sources of Cu, Mn, and Zn on mineral status and production performance in dairy cows. One hundred forty-one Holstein cows were stratified by parity group prepartum as nulliparous (lactation 0) or parous cows (lactation >0) and, within parity, cows were blocked by genomic breeding value for ECM yield (nulliparous cows) or recently completed lactation 305-d ECM (parous cows) and then randomly assigned to 1 of 2 treatments. Treatments were supplemental sources of Cu, Mn, and Zn as sulfate trace minerals (STM) or hydroxychloride trace minerals (HTM). Diets were formulated to contain approximately 16, 60, and 60 mg/kg of Cu, Mn, and Zn, respectively, and treatments were fed from 246 d of gestation to 105 d of lactation. Cows were weighed twice weekly prepartum and intake of DM, milk yield, and postpartum BW were measured daily, and composition of milk was analyzed twice weekly. Blood was sampled pre- and postpartum and hepatic tissue collected at 10 (50 STM and 52 HTM cows) and at 50 d postpartum (17 STM and 18 HTM cows) and analyzed for concentrations of minerals. Treatment did not affect intake or measures of energy balance prepartum. Numerical results between parentheses are presented following the sequence of STM and HTM. Concentrations of trace minerals in serum differed between treatments only prepartum and those of Cu (1.291 vs. 1.183 &#xb1; 0.031 mg/L) and Zn (1.307 vs. 1.211 &#xb1; 0.031 mg/L) were greater for cows fed STM compared with cows fed HTM; however, the opposite response was observed for serum Mn (1.628 vs. 1.754 &#xb1; 0.038 &#xb5;g/L). Treatment did not affect liver Mn or Zn concentration, but for Cu, cows fed STM had greater concentration in the liver on d 10 postpartum compared with cows fed HTM (310 vs. 296 &#xb1; 7 mg/kg DM); however, the opposite response was observed on d 50 and cows fed STM had smaller concentration of Cu in liver than those fed HTM (287 vs. 318 &#xb1; 9 mg/kg DM). Cows fed HTM produced an additional 1.0 kg colostrum than STM cows (5.21 vs. 6.22 &#xb1; 0.63 kg), thus resulting in increased yield of colostrum solids. Treatment did not affect the content or yield of IgG in colostrum. Cows fed HTM produced 1.3 kg/d more milk (41.7 vs. 43.0 &#xb1; 0.5 kg/d) and 1.5 kg/d more energy-corrected milk (42.5 vs. 44.0 &#xb1; 0.6 kg/d) in the first 15 wk of lactation compared with cows fed STM. The estimated NEL content of the postpartum diet consumed by cows, after accounting for the different energy sinks and DMI, was 3.4% greater for HTM than STM (1.68 vs. 1.74 &#xb1; 0.02 Mcal/kg). Replacing sulfate with hydroxychloride sources of Cu, Mn, and Zn had small effects on the concentrations of those minerals in tissues and improved production performance in the first 15 wk of lactation.

Animals↗

Retinoic acid induces rapid mineralization and expression of mineralization-related genes in chondrocytes.

Numerous studies of experimental hypo- and hypervitaminosis A have long suggested that retinoic acid (RA) is involved in chondrocyte maturation during endochondral ossification and skeletogenesis. However, the specific and direct roles of RA in these complex processes remain unclear. Based on recent studies from our laboratories, we tested the hypothesis that RA induces the expression of genes associated with the terminal mineralization phase of chondrocyte maturation and promotes apatite deposition in the extracellular matrix. Cell populations containing chondrocytes at advanced stages of maturation were isolated from the upper portion of Day 18 chick embryo sterna and grown for 2 weeks in monolayer until confluent. The cells were then treated with low doses (10-100 nM) of RA for up to 6 days in the presence of a phosphate donor (beta-glycerophosphate) but in the absence of ascorbic acid. Within 4 days of treatment, RA dramatically induced expression of the alkaline phosphatase (APase), osteonectin, and osteopontin genes, caused a several-fold increase in APase activity, and provoked massive mineral formation while it left type X collagen gene expression largely unchanged. The mineral had a mean Ca/Pi molar ratio of 1.5; Fourier transform infrared spectra confirmed that it represented hydroxyapatite. Mineralization was completely abolished by treatment with parathyroid hormone; this profound effect confirmed that RA induced cell-mediated mineralization and not nonspecific precipitation. When cultures were treated with both RA and ascorbic acid, there was a slight further increase in APase activity and increased calcium accumulation. The effects of RA were also studied in cultures of immature chondrocytes isolated from the caudal portion of sternum; however, RA only had minimal effects on mineralization and gene expression in these cells. Thus, RA appears to be a rapid, potent, maturation-dependent, ascorbate-independent promoter of terminal maturation and matrix calcification in chondrocytes.

Alkaline Phosphatase↗

Mineral particles, mineral fibers, and lung cancer.

The total fibrous and nonfibrous mineral content of the lung has been analyzed in a series of 14 men with lung cancer but no history of occupational dust exposure, and in a series of 14 control men matched for age, smoking history, and general occupational class. The lung cancer patients had an average of 525 +/- 369 X 10(6) exogenous mineral particles and 17.4 +/- 19.6 X 10(6) exogenous mineral fibers/g dry lung, while the controls had averages of 261 +/- 175 mineral particles and 4.7 +/- 3.2 X 10(6) mineral fibers/g dry lung. These differences are statistically significant for both particles and fibers. Kaolinite, talc, mica, feldspars, and crystalline silica comprised the majority of particles of both groups. Approximately 90% of the particles were smaller than 2 micron in diameter and approximately 60% smaller than 1 micron; the mean particle size in the cancer group was 1.1 +/- 0.2 micron and in the control group 1.3 +/- 0.2 micron. In both groups, patients who had smoked more than 35 pack years had greater numbers of particles than patients who had smoked less than 35 pack years. It is concluded that, in this study, lungs from patients with lung cancer had statistically greater numbers of mineral particles and fibers than lungs from controls, and that smoking influences total long-term retention of particles from all sources.

Aged↗

Vitamin D metabolism, mineral homeostasis, and bone mineralization in term infants fed human milk, cow milk-based formula, or soy-based formula.

The purpose of this study was to evaluate mechanisms of mineral homeostasis and mineralization in term infants with recommended vitamin D intakes. Infants fed human milk (nine), cow milk-based formula (11), or soy-based formula (11) were studied at 2 weeks and at 2, 4, 6, 9, and 12 months of age. While receiving 400 IU of vitamin D, all infants maintained serum vitamin D concentrations higher or equal to normal adult concentrations, and serum 25-hydroxyvitamin D levels were maintained at or above normal adult levels. Serum 1,25-dihydroxyvitamin D concentrations were higher than those of adults in the formula-fed but not in the human milk-fed infants. Serum calcium and phosphorus values were similar in all groups; however, urine phosphorus excretion and urine calcium excretion were adjusted to intakes. Serum parathyroid hormone values were normal in all groups. Bone mineral content significantly increased with age similarly in all groups; however, an apparent plateau occurred at 6 months of age in all groups. Bone width steadily increased with age. Taken as a whole, these data suggest that the vitamin D-sufficient term infant fed human milk, cow milk-based formula, or the soy-based formula studied can regulate mineral metabolism within acceptable physiologic limits to attain similar levels of serum minerals and bone mineral content.

Alkaline Phosphatase↗

Growth and bone mineralization of normal breast-fed infants and the effects of lactation on maternal bone mineral status.

To determine if human milk provides for adequate growth and bone mineralization during the lst yr of life, 91 term infants were evaluated. Infants were divided into three groups human milk alone, human milk with supplemental vitamin D, and Similac. Lactating mothers who were receiving supplements of calcium and vitamin D were also studied to determine the effects of lactation on their bone mineral status. Blood was drawn from infants and mothers for measurements of serum calcium, phosphate, alkaline phosphatase, and 25-hydroxyvitamin D. Bone mineral content was measured by photon absorptiometry. Growth was similar between breast-fed and formula-fed infants. Regardless of type of feeding, male infants grew heavier and longer than corresponding female infants. Serum calcium and phosphate levels were similar among the three infant groups: only 25-hydroxyvitamin D levels at 4 months and serum alkaline phosphatase at 2 wk and 6 months of age were different among the three infant groups. Biochemical and vitamin D values were similar among the lactating mothers. There were no differences in infant bone mineral content among the three groups, but male infants had higher bone mineral content than female infants. There were no effects of the duration of lactation of maternal bone mineral content or vitamin D status.

Aging↗

Orientation of mineral crystallites and mineral density during skeletal development in mice deficient in tissue nonspecific alkaline phosphatase.

Tissue nonspecific alkaline phosphatase (TNALP) is thought to play an important role in mineralization processes, although its exact working mechanism is not known. In the present investigation we have studied mineral crystal characteristics in the developing skeleton of TNALP-deficient mice. Null mutants (n = 7) and their wild-type littermates (n = 7) were bred and killed between 8 and 22 days after birth. Skeletal tissues were processed to assess mineral characteristics (small angle X-ray scattering, quantitative backscattered electron imaging), and to analyze bone by light microscopy and immunolabeling. The results showed a reduced longitudinal growth and a strongly delayed epiphyseal ossification in the null mutants. This was accompanied by disturbances in mineralization pattern, in that crystallites were not orderly aligned with respect to the longitudinal axis of the cortical bone. Among the null mutants, a great variability in the mineralization parameters was noticed. Also, immunolabeling of osteopontin (OPN) revealed an abnormal distribution pattern of the protein within the bone matrix. Whereas in the wild-type animals OPN was predominantly observed in cement and reversal lines, in the null mutants, OPN was also randomly dispersed throughout the nonmineralized matrix, with focal densities. In contrast, the distribution pattern of osteocalcin (OC) was comparable in both types of animals. It is concluded that ablation of TNALP results not only in hypomineralization of the skeleton, but also in a severe disorder of the mineral crystal alignment pattern in the corticalis of growing long bone in association with a disordered matrix architecture, presumably as a result of impaired bone remodeling and maturation.

Alkaline Phosphatase↗

Effects of dietary zinc and iron supplementation on mineral excretion, body composition, and mineral status of nursery pigs.

Two experiments were conducted to evaluate the effects of dietary Zn and Fe supplementation on mineral excretion, body composition, and mineral status of nursery pigs. In Exp. 1 (n = 24; 6.5 kg; 16 to 20 d of age) and 2 (n = 24; 7.2 kg; 19 to 21 d of age), littermate crossbred barrows were weaned and allotted randomly by BW, within litter, to dietary treatments and housed individually in stainless steel pens. In Exp. 1, Phases 1 (d 0 to 7) and 2 (d 7 to 14) diets (as-fed basis) were: 1) NC (negative control, no added Zn source); 2) ZnO (NC + 2,000 mg/kg as Zn oxide); and 3) ZnM (NC + 2,000 mg/kg as Zn Met). In Exp. 2, diets for each phase (Phase 1 = d 0 to 7; Phase 2 = d 7 to 21; Phase 3 = d 21 to 35) were the basal diet supplemented with 0, 25, 50, 100, and 150 mg/kg Fe (as-fed basis) as ferrous sulfate. Orts, feces, and urine were collected daily in Exp. 1; whereas pigs had a 4-d adjustment period followed by a 3-d total collection period (Period 1 = d 5 to 7; Period 2 = d 12 to 14; Period 3 = d 26 to 28) during each phase in Exp. 2. Blood samples were obtained from pigs on d 0, 7, and 14 in Exp. 1 and d 0, 7, 21, and 35 in Exp. 2 to determine hemoglobin (Hb), hematocrit (Hct), and plasma Cu, (PCu), Fe (PFe), and Zn (PZn). Pigs in Exp. 1 were killed at d 14 (mean BW = 8.7 kg) to determine whole-body, liver, and kidney mineral concentrations. There were no differences in growth performance in Exp. 1 or 2. In Exp. 1, pigs fed ZnO or ZnM diets had greater (P < 0.001) dietary Zn intake during the 14-d study and greater fecal Zn excretion during Phase 2 compared with pigs fed the NC diet. Pigs fed 2,000 mg/kg, regardless of Zn source, had greater (P < 0.010) PZn on d 7 and 14 than pigs fed the NC diet. Whole-body Zn, liver Fe and Zn, and kidney Cu concentrations were greater (P < 0.010), whereas kidney Fe and Zn concentrations were less (P < 0.010) in pigs fed pharmacological Zn diets than pigs fed the NC diet. In Exp. 2, dietary Fe supplementation tended to increase (linear, P = 0.075) dietary DMI, resulting in a linear increase (P < 0.050) in dietary Fe, Cu, Mg, Mn, P, and Zn intake. Subsequently, a linear increase (P < 0.010) in fecal Fe and Zn excretion was observed. Increasing dietary Fe resulted in a linear increase in Hb, Hct, and PFe on d 21 (P < 0.050) and 35 (P < 0.010). Results suggest that dietary Zn or Fe additions increase mineral status of nursery pigs. Once tissue mineral stores are loaded, dietary minerals in excess of the body's requirement are excreted.

Animal Feed↗

[Relation of fingernail mineral concentrations to bone mineral density in elderly Japanese women].

Metacarpal bone mineral density, and concentrations of calcium (Ca), iron (Fe), magnesium (Mg), zinc (Zn) and phosphorus (P) in fingernails were measured in 30 elderly women. Significant correlation between bone mineral density and body weight was seen, and higher values of bone mineral density were observed in those subjects walking daily without the aid of a cane or assistance. Among the 5 minerals in fingernails, a high positive correlation was found between Ca and P concentrations. Concentration of Zn in fingernails was significantly but negatively correlated with bone mineral density (r = -0.399), and a significant positive correlation of Ca/Zn ratio of fingernails was observed with bone mineral density (r = 0.421). The content of Zn in nails may be affected by alterations in bone Zn status and a potential application of nail Zn level or Ca/Zn ratio as an indicator of senile osteoporosis is suggested.

Aged↗