Renal hypercalciuria: ¿Is it different from idiopathic hypercalciuria?

被引:0
|
作者
Spivacow, Francisco Rodolfo [1 ]
Del Valle, Elisa [1 ]
de Brum, Ariadna [1 ]
Di Cello, Natalia [1 ]
机构
[1] Univ Salvador USAL, Inst Invest Metab IDIM, Buenos Aires, Argentina
来源
关键词
Renal hypercalciuria; difference with idiopathic hypercalciuria; CALCIUM-SENSING RECEPTOR; GENE; NEPHROLITHIASIS; EXPRESSION; EXCRETION; SODIUM;
D O I
暂无
中图分类号
R5 [内科学]; R69 [泌尿科学(泌尿生殖系疾病)];
学科分类号
1002 ; 100201 ;
摘要
Introduction: : Idiopathic hyper calciuria is the leading risk factor in oxalo-calcium stones and a secondary cause of osteoporosis. It occurs in families with a probably polygenic trait, which involves alterations in intestinal, bone, and renal calcium management. Some studies suggest that more than 50% of calcium excretion is genetically determined, most frequently observed in first- degree relatives. The objective of our study was to evaluate whether there are clinical, biochemical, and densitometric differences between patients with renal hypercalciuria and idiopathic hypercalciuria. Material and methods: 112 hypercalciuric patients were included, half with elevated PTH. Results: : Renal hypercalciuric patients, Group I (n = 56) were older (p < 0.001) and heavier (p < 0.05) than patients with idiopathic hypercalciuria Group II (n = 56). A higher level of iPTH (p <0.001) and serum crosslap (p <0.05) was presented in patients with renal hypercalciuria. No significant differences were found between the groups in the presence of kidney stones and bone density. According to the presence (n = 32) or absence (n = 24) of kidney stones in Group I (renal hypercalciuria), there were also no significant changes. Conclusion: : renal hypercalciuria is a variant of idiopathic hypercalciuria, which to date does not show significant differences with the remaining variants of idiopathic hypercalciuria. Prospective studies with longer- term follow-ups, including genetic evaluation, will confirm the existence or absence of these differences.
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页码:120 / 126
页数:7
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