Literature DB >> 3872644

Vitamin D status in urinary calcium stone formation.

J C Netelenbos, M J Jongen, W J van der Vijgh, P Lips, F C van Ginkel.   

Abstract

Serum vitamin D metabolites were measured in 160 normocalcemic urinary calcium stone formers and in 217 control subjects. No difference in concentrations of 25-hydroxy-vitamin D (25[OH]D), 24,25-dihydroxyvitamin D (24,25[OH]2D), and 1,25-dihydroxyvitamin D (1,25[OH]2D) was found between stone formers and control subjects. Values for 25(OH)D and 24,25(OH)2D were higher in hypercalciuric stone formers than in normocalciuric stone formers independent of seasonal fluctuation. No difference in concentration of serum 1,25(OH)2D was found between hypercalciuric and normocalciuric stone formers. No correlations were present between the serum concentrations of the measured vitamin D metabolites and of measures of calcium and phosphate metabolism. These findings suggest no major pathophysiologic role of the main vitamin D metabolites in urinary calcium stone formation.

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Year:  1985        PMID: 3872644

Source DB:  PubMed          Journal:  Arch Intern Med        ISSN: 0003-9926


  11 in total

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Review 4.  Bone mineral content in calcium renal stone formers.

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Authors:  Kristina L Penniston; Andrea N Jones; Stephen Y Nakada; Karen E Hansen
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6.  Prevalence of Vitamin D Inadequacy in Urolithiasis Patients.

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Review 7.  Association between Circulating Vitamin D Level and Urolithiasis: A Systematic Review and Meta-Analysis.

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Journal:  Nutrients       Date:  2018-03-17       Impact factor: 5.717

9.  Association between serum vitamin D levels and the risk of kidney stone: evidence from a meta-analysis.

Authors:  Hai Wang; Libo Man; Guizhong Li; Guanglin Huang; Ning Liu
Journal:  Nutr J       Date:  2016-03-31       Impact factor: 3.271

10.  Seasonal variations in urinary calcium, volume, and vitamin d in kidney stone formers.

Authors:  Kyrollis Attalla; Shubha De; Carl Sarkissian; Manoj Monga
Journal:  Int Braz J Urol       Date:  2018 Sep-Oct       Impact factor: 1.541

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