Erythrocyte transmembrane flux and renal clearance of oxalate in idiopathic calcium nephrolithiasis.

An anomaly in erythrocyte oxalate transport has been reported in patients with idiopathic calcium oxalate nephrolithiasis. Even if clinical and experimental evidence suggests a causal role of this cellular anomaly in calcium nephrolithiasis, a definitive answer to this fundamental question is still lacking. We approached this problem by searching for a possible relationship between the erythrocyte oxalate self-exchange anomaly and the renal clearance of this anion in stone formers. In 10 idiopathic calcium-oxalate renal stone formers, and 10 healthy subjects we evaluated the erythrocyte oxalate flux rate, and the renal fractional clearance of oxalate by a recently described enzymathic procedures for plasma oxalate determination. With respect to controls, stone formers had higher oxalate flux rate in erythrocytes, and higher oxalate renal fractional clearance with a significant direct correlation between the two parameters. These data are compatible with a membrane transport abnormality within the kidney of these stone formers, and the existence of a common defect of the oxalate transport shared by both erythrocytes and tubular renal cells. The latter may be crucial in the pathogenesis of calcium oxalate nephrolithiasis, by modifying the renal handling of oxalate.