Comparative studies on absorption of radioactive stronium and calcium from the gastrointestinal tract.
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Twenty-one unselected patients with recurrent nephrolithiasis and normocalcemic hypercalciuria with or without hypophosphatemia and 18 normal subjects were studied with an oral calcium tolerance test and for 3- to 5-day periods while consuming a low normal (400 mg) and high-normal (1000 mg) calcium intake. The oral calcium tolerance test consisted of the measurement of the calcemic, calciuric, and parathyroid (assessed by determinations of serum immunoreactive parathyroid hormone and nephrogenous cAMP) responses to acute 1000- or 350-mg doses of calcium. Nineteen patients displayed normal results for basal serum calcium, parathyroid function, and fasting calcium excretion, and striking calcemic (mean increase in serum calcium, 0.9 vs. 0.2 mg/dl in the normal subjects) and calciuric (mean increase in urinary calcium, 0.33 vs. 0.15 mg calcium/100 ml GF in the normal subjects) responses to the 1000-mg calcium tolerance test, associated with a mean 54% suppression in nephrogenous cAMP. These patients were operationally defined as having "absorptive" hypercalciuria. The variable occurrence of hypophosphatemia in this group suggested that the pathogenesis of "absorptive" hypercalciuria may be complex and/or multifactorial. There were strong positive correlations between the calciuric response to the calcium tolerance test and fractional isotopic calcium absorption (r = 0.75, P less than 0.00), the calcemic responses to the test (r = 0.71, P less than 0.001) and the calciuric responses noted on the 1000- vs. the 400-mg daily calcium intake (r = 0.78, P less than 0.001). Two patients displayed low or low normal basal serum calcium, increased parathyroid function, increased fasting calcium excretion, and a striking calciuric but minimal calcemic response to the 1000-mg calcium tolerance test, associated with a moderate suppression in nephrogenous cAMP. These patients were operationally defined as having "renal" hypercalciuria. Several lines of evidence indicated that the hyperparathyroidism in these patients was physiological or secondary, including the near normalization of parathyroid function on the daily 1000-mg calcium intake. A steep slope of calcium excretion on calcium intake (due to increased calcium absorption) was noted in all hypercalciuric patients and accounted for the significantly improved diagnostic accuracy of screening patients for hypercalciuria on the high-normal calcium intake. The simple measurement of total cAMP excretion (nanomoles per 100 ml GF) and urinary calcium on the 1000-mg daily calcium intake seemed to provide reliable separation of patients with "renal" from those with "absorptive" hypercalciuria. A physiological (350 mg) dose of oral calcium produced a 30% suppression of nephrogenous cAMP in normal subjects; this suggests that dietary calcium exerts an important control of parathyroid function under physiological circumstances.
UNLABELLED: Bone loss is a current limitation for long-term space exploration. Bone markers, calcitropic hormones, and calcium kinetics of crew members on space missions of 4-6 months were evaluated. Spaceflight-induced bone loss was associated with increased bone resorption and decreased calcium absorption. INTRODUCTION: Bone loss is a significant concern for the health of astronauts on long-duration missions. Defining the time course and mechanism of these changes will aid in developing means to counteract these losses during space flight and will have relevance for other clinical situations that impair weight-bearing activity. MATERIALS AND METHODS: We report here results from two studies conducted during the Shuttle-Mir Science Program. Study 1 was an evaluation of bone and calcium biochemical markers of 13 subjects before and after long-duration (4-6 months) space missions. In study 2, stable calcium isotopes were used to evaluate calcium metabolism in six subjects before, during, and after flight. Relationships between measures of bone turnover, biochemical markers, and calcium kinetics were examined. RESULTS: Pre- and postflight study results confirmed that, after landing, bone resorption was increased, as indicated by increases in urinary calcium (p < 0.05) and collagen cross-links (N-telopeptide, pyridinoline, and deoxypyridinoline were all increased >55% above preflight levels, p < 0.001). Parathyroid hormone and vitamin D metabolites were unchanged at landing. Biochemical markers of bone formation were unchanged at landing, but 2-3 weeks later, both bone-specific alkaline phosphatase and osteocalcin were significantly (p < 0.01) increased above preflight levels. In studies conducted during flight, bone resorption markers were also significantly higher than before flight. The calcium kinetic data also validated that bone resorption was increased during flight compared with preflight values (668 +/- 130 versus 427 +/- 153 mg/day; p < 0.001) and clearly documented that true intestinal calcium absorption was significantly lower during flight compared with preflight values (233 +/- 87 versus 460 +/- 47 mg/day; p < 0.01). Weightlessness had a detrimental effect on the balance in bone turnover such that the daily difference in calcium retention during flight compared with preflight values approached 300 mg/day (-234 +/- 102 versus 63 +/- 75 mg/day; p < 0.01). CONCLUSIONS: These bone marker and calcium kinetic studies indicated that the bone loss that occurs during space flight is a consequence of increased bone resorption and decreased intestinal calcium absorption.
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Osteopenia resulting from pharmacologic doses of glucocorticoids is well known. Previously, there has been no satisfactory quantitative model describing the kinetics of calcium flow in subjects on chronic steroid use. A mathematical model of calcium isotope interaction with bone is described and applied to determine an estimate of kinetic parameters characterizing these changes. Calcium tracer dilution kinetics after a bolus injection of 42Ca were measured in 14 subjects with juvenile dermatomyositis, 6 on prednisone regimens and 8 on treatment regimens without prednisone. Irreversible tracer loss from plasma bone is found to be significantly reduced (P = 0.043) in the glucocorticoid-treated patients compared with patients on nonsteroid regimens. Reversible flow to bone is noted to be similar in the two groups. These results suggest a direct effect of glucocorticoids on osteoblast function.
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The relationship between variations in diaphragmatic contractility and corresponding changes in total tissue levels of 45Ca and adenosine 3',5'-cyclic monophosphate (cAMP) was examined. The contractile performance of perfused contracting rat diaphragms was manipulated with theophylline (10(-4) M), induced fatigue, or both. The increased contractility associated with theophylline was related to significant increases in 45Ca levels without changes in cAMP levels. Fatigue-diminished contractility was associated with increases in both 45Ca and cAMP levels. The increased 45Ca and cAMP levels associated with fatigue persisted, even in the presence of theophylline. Calcium channel blockade with 10(-4) M verapamil blocked the positive inotropic influence of theophylline as well as the theophylline-associated increase in 45Ca levels. Verapamil had no effect on either the fatigue-associated decreases in contractility or the fatigue-enhanced 45Ca uptake. The results of this study strongly suggest that the enhanced contractility associated with theophylline is related to its influence on cellular calcium metabolism. The elevated level of isotopic calcium measured in fatigued muscle probably represents calcium sequestered in the sarcoplasmic reticulum, the result of cAMP-enhanced Ca-adenosine triphosphatase activity.
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BACKGROUND: Early childbearing may limit skeletal consolidation and increase calcium demands in adolescents. OBJECTIVE: The purpose of this study was to characterize calcium absorption in pregnant and lactating adolescents. DESIGN: Fractional calcium absorption was evaluated in 23 adolescents (mean +/- SD age: 16.5 +/- 1.4 y) during the third trimester of pregnancy (34.7 +/- 1.0 wk gestation) and again in 15 of these adolescents 31 +/- 8 d after delivery. Eight adolescents were breastfeeding their infants during the follow-up study. Fractional calcium absorption was determined by using oral ((46)Ca or (44)Ca) and intravenous ((42)Ca) stable calcium isotopes. Total-body and lumbar spine bone mineral density were measured in adolescents during the postpartum period by using dual-energy X-ray absorptiometry. RESULTS: Fractional calcium absorption was significantly greater during pregnancy than at 3-4 wk postpartum [0.526 +/- 0.152 (n = 23) compared with 0.297 +/- 0.108 (n = 15); P < 0.0001]. Lumbar spine z scores measured 19-44 d after delivery (n = 15) were significantly associated with calcium intake during pregnancy (y = -3.53 + 0.107x; R(2) = 0.355, P < 0.02) and were inversely related to fractional calcium absorption during pregnancy (y = 3.489 - 6.66x; R(2) = 0.52, P = 0.002). A total of 33% (5/15) of adolescents had lumbar spine z scores that met the definition of osteopenia (n = 3) or osteoporosis (n = 2) in the early postpartum period. CONCLUSIONS: Calcium absorption in adolescents was significantly higher during the third trimester of pregnancy than in the early postpartum period, and higher calcium intakes during pregnancy appeared to be protective against loss of trabecular bone at the lumbar spine.
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Some patients with hypercalciuria are thought to have enhanced enteric calcium absorption, with a major component of recent diet contributing to urinary calcium. This mechanism has been difficult to test with the usual calcium loading procedures. We employed dual stable calcium isotope tracers to quantitate the components of urinary calcium excretion in 38 healthy female children. The mean urinary calcium excretion in these girls was 2.4 mg/kg per day. The contribution of recent diet to this total was a mean of 0.2 mg/kg per day. The maximum dietary contribution to urinary calcium excretion was 0.86 mg/kg per day. Recent diet contributes a mean of 8% to total dietary calcium excretion. This novel method permits precise quantitation of the contributions of recent diet and tissue stores to urinary calcium excretion. In these healthy girls, the fraction of urinary calcium derived from diet is trivial.
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