Abstract

To investigate potential differences in stone composition with regard to the type of Primary Hyperoxaluria (PH), and in relation to the patient’s medical therapy (treatment naïve patients versus those on preventive medication) we examined twelve kidney stones from ten PH I and six stones from four PH III patients. Unfortunately, no PH II stones were available for analysis. The study on this set of stones indicates a more diverse composition of PH stones than previously reported and a potential dynamic response of morphology and composition of calculi to treatment with crystallization inhibitors (citrate, magnesium) in PH I. Stones formed by PH I patients under treatment are more compact and consist predominantly of calcium-oxalate monohydrate (COM, whewellite), while calcium-oxalate dihydrate (COD, weddellite) is only rarely present. In contrast, the single stone available from a treatment naïve PH I patient as well as stones from PH III patients prior to and under treatment with alkali citrate contained a wide size range of aggregated COD crystals. No significant effects of the treatment were noted in PH III stones. In disagreement with findings from previous studies, stones from patients with primary hyperoxaluria did not exclusively consist of COM. Progressive replacement of COD by small COM crystals could be caused by prolonged stone growth and residence times in the urinary tract, eventually resulting in complete replacement of calcium-oxalate dihydrate by the monohydrate form. The noted difference to the naïve PH I stone may reflect a reduced growth rate in response to treatment. This pilot study highlights the importance of detailed stone diagnostics and could be of therapeutic relevance in calcium-oxalates urolithiasis, provided that the effects of treatment can be reproduced in subsequent larger studies.

Highlights

  • The primary hyperoxalurias (PH I, II and III) are rare, but underdiagnosed autosomal-recessively inherited disorders of the glyoxylate metabolism [1,2]

  • Infantile oxalosis occurring with generalized nephrocalcinosis and end-stage renal disease (ESRD) within the first 3 years of life constitutes the most severe Primary Hyperoxaluria (PH) I subgroup and still poses a major therapeutic challenge [1,2,16]

  • Augmenting deductions from the current literature, we found that PH I and especially PH III stones are not always uniform in appearance and composition

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Summary

Introduction

The primary hyperoxalurias (PH I, II and III) are rare, but underdiagnosed autosomal-recessively inherited disorders of the glyoxylate metabolism [1,2]. Recurring urolithiasis and/or progressive nephrocalcinosis (the latter not yet observed in PH III) usually occurring early in childhood are their clinical hallmarks [1,2,3,4]. Rare (estimated prevalence rate ,3 per 106 population [6,7,8,9,10,11,12] with higher rates reported from some inbred populations [13,14]). Infantile oxalosis occurring with generalized nephrocalcinosis and ESRD within the first 3 years of life constitutes the most severe PH I subgroup (up to 20% of cases) and still poses a major therapeutic challenge [1,2,16]

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