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Genetic hypercalciuric stone-forming (GHS) rats, bred to maximize urine (u) calcium (Ca) excretion, demonstrate increased intestinal Ca absorption, increased bone Ca resorption, and reduced renal Ca reabsorption, all leading to elevated uCa compared to the parental Sprague-Dawley (SD) rats. GHS rats have increased numbers of vitamin D receptors (VDRs) at each site, with normal levels of 1,25(OH)₂D₃ (1,25D), suggesting their VDR is undersaturated with 1,25D. We have shown that 1,25D induces a greater increase in uCa in GHS than SD rats. To examine the effect of the increased VDR on the osseous response to 1,25D, we fed GHS and SD rats an ample Ca diet and injected either 1,25D [low dose (LD) 12.5 or high dose (HD) 25 ng/100 g body weight/day] or vehicle (veh) daily for 16 days. Femoral areal bone mineral density (aBMD, by DEXA) was decreased in GHS+LD and GHS+HD relative to GHS+veh, while there was no effect on SD. Vertebral aBMD was lower in GHS compared to SD and further decreased in GHS+HD. Both femoral and L6 vertebral volumetric BMD (by μCT) were lower in GHS and further reduced by HD. Histomorphometry indicated a decreased osteoclast number in GHS+HD compared to GHS+veh or SD+HD. In tibiae, GHS+HD trabecular thickness and number increased, with a 12-fold increase in osteoid volume but only a threefold increase in bone volume. Bone formation rate was decreased in GHS+HD relative to GHS+veh, confirming the mineralization defect. The loss of BMD and the mineralization defect in GHS rats contribute to increased hypercalciuria; if these effects persist, they would result in decreased bone strength, making these bones more fracture-prone. The enhanced effect of 1,25D in GHS rats indicates that the increased VDRs are biologically active.

Hypercalciuria is the most common metabolic abnormality found in patients with calcium-containing kidney stones. Patients with hypercalciuria often excrete more calcium than they absorb, indicating a net loss of total-body calcium. The source of this additional urinary calcium is almost certainly the skeleton, the largest repository of calcium in the body. Hypercalciuric stone formers exhibit decreased bone mineral density (BMD), which is correlated with the increase in urine calcium excretion. The decreased BMD also correlates with an increase in markers of bone turnover as well as increased fractures. In humans, it is difficult to determine the cause of the decreased BMD in hypercalciuric stone formers. To study the effect of hypercalciuria on bone, we utilized our genetic hypercalciuric stone-forming (GHS) rats, which were developed through successive inbreeding of the most hypercalciuric Sprague-Dawley rats. GHS rats excrete significantly more urinary calcium than similarly fed controls, and all the GHS rats form kidney stones while control rats do not. The hypercalciuria is due to a systemic dysregulation of calcium homeostasis, with increased intestinal calcium absorption, enhanced bone mineral resorption, and decreased renal tubule calcium reabsorption associated with an increase in vitamin D receptors in all these target tissues. We recently found that GHS rats fed an ample calcium diet have reduced BMD and that their bones are more fracture-prone, indicating an intrinsic disorder of bone not secondary to diet. Using this model, we should better understand the pathogenesis of hypercalciuria and stone formation in humans to ultimately improve the bone health of patients with kidney stones.

We investigated the frequency of hypercalcemia and/or hypercalciuria following parathyroid hormone (PTH) 1-34 and 1-84 administration in a crossover trial. Ten postmenopausal osteoporotic women previously treated with bisphosphonates were subdivided into two groups of five patients each. A 24-h urine collection to determine baseline calcium (Ca) and creatinine (Cr) the day before administration of PTH was followed by determination of serum ionized Ca (Ca(2+)), Cr, 25(OH)D, and 1,25(OH)(2)D at baseline. Thereafter, 100 mcg of PTH(1-84) or 20 mcg of PTH(1-34) was administered. A 24-h urinary collection and blood samples 2, 4, and 24-h after each PTH administration were again taken. One week after the first PTH administration patients were rechallenged with the second PTH. The PTH peptides did not differ with respect to changes in Ca(2+) at 2, 4, and 24 h postinjection; at the last time point the values were virtually identical to the initial values. There was no difference in urinary Ca on the day following PTH injection compared to baseline, in terms both of Ca/Cr and of Ca excretion. The two PTH peptides did not differ with respect to changes in 1,25(OH)(2)D at 2, 4, and 24 h considering both the absolute values and the percent changes with respect to baseline (24-h 1-84 = 125.6 + or - 58.6 pg/ml, 153% increase; 1-34 = 124.1 + or - 64.7, 130%). Our results indicate no difference in postinjection serum Ca(2+), 1,25(OH)(2)D, or urinary Ca excretion after a single dose of either PTH(1-84) or PTH(1-34) in patients previously treated with bisphosphonates.