Alterations in circadian rhythmicity in calcium oxalate renal stone formers.

Y Touitou, C Touitou, G Charransol, A Reinberg, J Thomas, A Bogdan, C Barthelemy, P Desgrez
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Abstract

The circadian (circannual for oxalic acid) variations of 13 urinary variables (volume, creatinine, calcium, oxalic acid, glycolic acid, 17-ketosteroids, 17-hydroxycorticosteroids, phosphates, urea, uric acid, chloride, sodium, and potassium) have been documented in 7 calcium oxalate renal stone formers and 7 healthy men (control group). Urine was collected every 4 h over a period of 24 h. All subjects had the same synchronization: diurnal activity from 07(00) to 23(00) +/- 1 h and nocturnal rest; meals were given at fixed clock hours (08(00), 12(30) and 20(00) +/- 1 h). A statistically-significant rhythm (p less than 0.05) was validated for all variables except urea and calcium in healthy men. In renal stone formers, 6 variables (calcium, oxalic acid, and glycolic acid in particular) had no detectable circadian rhythm. However, a periodicity of c. 8 h (ultradian rhythm) was demonstrated for calcium and oxalic acid with peaks being located around 02(00), 10(00), and 18(00). No circannual variations in oxalic acid output could be observed. The present study shows an alteration of the periodicity of calcium and oxalic metabolisms, i.e. the loss of a circadian (24-h) rhythm and the occurrence of an ultradian rhythm of 8 h. The risk of calcium-oxalate crystallisation appears thus greater at 02(00), 10(00), and 18(00). Furthermore, any study dealing with oxalic acid excretion should state the season of urine collection when comparing renal stone formers and healthy subjects, as significant differences in oxaluria may appear during the summer months and not during the rest of the year.

草酸钙肾结石患者昼夜节律性的改变。
在7名草酸钙肾结石患者和7名健康男性(对照组)中记录了13项尿液变量(体积、肌酐、钙、草酸、乙醇酸、17-酮类固醇、17-羟基皮质类固醇、磷酸盐、尿素、尿酸、氯化物、钠和钾)的昼夜节律变化(草酸的周期变化)。在24小时的时间内,每4小时收集一次尿液。所有受试者具有相同的同步性:从07(00)到23(00)+/- 1小时的日间活动和夜间休息;在固定的时钟时间(08(00)、12(30)和20(00)+/- 1小时)进食。除尿素和钙外,健康男性的所有变量都有统计学意义的节律(p < 0.05)。在肾结石患者中,6个变量(尤其是钙、草酸和乙醇酸)没有可检测到的昼夜节律。然而,钙和草酸的周期为c. 8 h(超昼夜节律),峰值位于02(00),10(00)和18(00)左右。草酸产量未见年际变化。目前的研究表明,钙和草酸代谢的周期性发生了变化,即昼夜节律(24小时)的丧失和8小时的超昼夜节律的发生。因此,草酸钙结晶的风险在02(00)、10(00)和18(00)时显得更大。此外,在比较肾结石患者和健康受试者时,任何关于草酸排泄的研究都应说明收集尿液的季节,因为草酸排泄的显著差异可能出现在夏季,而不是在一年中的其他时间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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