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Kidney Stones in Primary Hyperoxaluria: New Lessons Learnt

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 P...

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Autores principales: Jacob, Dorrit E., Grohe, Bernd, Geßner, Michaela, Beck, Bodo B., Hoppe, Bernd
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2013
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3734250/
https://www.ncbi.nlm.nih.gov/pubmed/23940605
http://dx.doi.org/10.1371/journal.pone.0070617
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author Jacob, Dorrit E.
Grohe, Bernd
Geßner, Michaela
Beck, Bodo B.
Hoppe, Bernd
author_facet Jacob, Dorrit E.
Grohe, Bernd
Geßner, Michaela
Beck, Bodo B.
Hoppe, Bernd
author_sort Jacob, Dorrit E.
collection PubMed
description 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.
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spelling pubmed-37342502013-08-12 Kidney Stones in Primary Hyperoxaluria: New Lessons Learnt Jacob, Dorrit E. Grohe, Bernd Geßner, Michaela Beck, Bodo B. Hoppe, Bernd PLoS One Research Article 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. Public Library of Science 2013-08-05 /pmc/articles/PMC3734250/ /pubmed/23940605 http://dx.doi.org/10.1371/journal.pone.0070617 Text en © 2013 Jacob et al http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are properly credited.
spellingShingle Research Article
Jacob, Dorrit E.
Grohe, Bernd
Geßner, Michaela
Beck, Bodo B.
Hoppe, Bernd
Kidney Stones in Primary Hyperoxaluria: New Lessons Learnt
title Kidney Stones in Primary Hyperoxaluria: New Lessons Learnt
title_full Kidney Stones in Primary Hyperoxaluria: New Lessons Learnt
title_fullStr Kidney Stones in Primary Hyperoxaluria: New Lessons Learnt
title_full_unstemmed Kidney Stones in Primary Hyperoxaluria: New Lessons Learnt
title_short Kidney Stones in Primary Hyperoxaluria: New Lessons Learnt
title_sort kidney stones in primary hyperoxaluria: new lessons learnt
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3734250/
https://www.ncbi.nlm.nih.gov/pubmed/23940605
http://dx.doi.org/10.1371/journal.pone.0070617
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