Background: A direct relation exists between sodium and calcium excretion, but randomized studies evaluating the sustained effect of a low-salt diet on idiopathic hypercalciuria, one of the main risk factors for calcium-oxalate stone formation, are still lacking.

Calcium-sensing receptor (CaSR) is a plasma membrane protein that regulates tubular reabsorption of Ca. To establish its role in idiopathic hypercalciuria, the association of urinary Ca excretion with the polymorphisms of CASR gene has been studied in healthy subjects and in hypercalciuric and normocalciuric Ca stone formers. CASR exon 7 single nucleotide polymorphisms (SNP), G/T at codon 986, G/A at codon 990, and C/G at codon 1011, were evaluated by PCR amplification and direct sequencing in 97 normocalciuric stone formers, 134 hypercalciuric stone formers, and 101 normocalciuric healthy controls. Four haplotypes were defined on the basis of CASR gene SNP: haplotype 1 was characterized by the most frequent sequence; haplotypes 2, 3, or 4 by the presence of a single polymorphic variant at codon 986, 990, or 1011, respectively. The relative risk of hypercalciuria was calculated with multinomial logistic regression and was significantly increased only in individuals carrying haplotype 3 (Odds ratio, 13.0 [95% confidence interval, 1.7 to 99.4]). Accordingly, Ca excretion was higher in subjects bearing haplotype 3, whereas those bearing haplotype 2 showed a slight increase of plasma Ca concentration. Multiple regression analysis showed that haplotype 3 explained 4.1% of the total variance of Ca excretion and 12.6% of the variance explained by the variables considered in the study. In conclusion, CASR gene could be a component of the complex genetic background regulating Ca excretion. Arg990Gly polymorphism could facilitate activation of CaSR and increase Ca excretion and susceptibility to idiopathic hypercalciuria.

Background: Calcium nephrolithiasis is a multifactorial disease with a polygenic milieu. Association studies identified genetic polymorphisms potentially implicated in the pathogenesis of calcium nephrolithiasis. The present article reviews the mechanisms of calcium stone formation and the potential contribution of gene polymorphisms to lithogenic mechanisms. Summary: Endoscopy observations suggested that precipitation of calcium-oxalate on the Randall's plaque at the papilla surface may cause idiopathic calcium-oxalate stones. The Randall's plaque is a hydroxyapatite deposit in the interstitium of the kidney medulla, which resembles a soft tissue calcification. Conversely, calcium-phosphate stones may develop from crystalline deposits located at the tip of the Bellini duct. Polymorphisms of eleven genes have been associated with stones in genome-wide association studies and replicated candidate-gene association studies: VDR, SLC34A1, SLC34A4, CLDN14, and CaSR genes coding for proteins regulating tubular phosphate and calcium reabsorption; CaSR, MGP, OPN, PLAU, and UMOD genes coding for proteins preventing calcium salt precipitation; AQP1 gene coding for a water channel in the proximal tubule. The renal activity of the last gene, DGKH, is unknown. Polymorphisms in these genes may predispose to calcium-oxalate and -phosphate stones by increasing the risk of calcium-phosphate precipitation in the tubular fluid. Key Messages: Genetic findings suggest that tubular fluid supersaturation with respect to calcium and phosphate predisposes to calcium-oxalate stones by triggering cellular mechanisms that lead to the Randall's plaque formation. © 2014 S. Karger AG, Basel