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CLINICAL STUDY |
Endocrinology and Diabetology Unit, Department of Medical-Surgical Sciences, University of Milan, IRCCS Policlinico San Donato, 20097 San Donato Milanese, Milan, Italy1 Endocrine Unit, Department of Medical Sciences, University of Milan, IRCCS Fondazione Ospedale Maggiore, Mangiagalli e Regina Elena, Milan, Italy2 Laboratory of Molecular Biology, IRCCS Policlinico San Donato, San Donato Milanese, Milan, Italy3 Endocrine Surgery, IRCCS Fondazione Ospedale Maggiore, Mangiagalli e Regina Elena, Milan, Italy4 Department of Preventive Medicine, University of Milan, IRCCS Fondazione Ospedale Maggiore, Mangiagalli e Regina Elena, Milan, Italy
(Correspondence should be addressed to S Corbetta; Email: sabrina.corbetta{at}unimi.it)
| Abstract |
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Design and methods: We tested the hypothesis that the 206M polymorphic variant of SLC26A6 gene might contribute to the risk of kidney stones in PHPT. DNA samples from 145 PHPT patients and 129 age- and sex-matched healthy subjects were genotyped.
Results: The homozygous 206V genotype was the most frequent both in PHPT patients and controls (79.3 and 74.4%), while heterozygosity for the 206M allele was detected in 20.0 and 23.3% respectively. The homozygous 206M genotype was extremely rare, occurring in 0.7 and 2.3% of PHPT and healthy subjects respectively. In the PHPT cohort, the prevalence of urolithiasis did not differ between the V/V and V/M+M/M groups and urine oxalate excretions did not correlate with the genotype. Considering the subset of PHPT stone formers (n=74), calciuria was lower in V/M+M/M patients with respect to V/V stone-formers (4.40±1.88 vs 5.92±2.62 mg/kg per 24 h; mean±S.D., P=0.034). Finally, the SLC26A6 206M alleles were significantly related to the presence of hypertension (73.3 vs 47.8%), showing an OR of 4.8.
Conclusions: Though the SLC26A6 206M polymorphism did not correlate with kidney stone development in PHPT patients, PHPT stone-formers harbouring the M allele had a lower hypercalciuria. This observation and the high prevalence of hypertension associated with the 206M polymorphism need further investigation.
| Introduction |
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The role of urine oxalate excretion is poorly defined, though urine oxalate excretion has been indicated as a risk factor for nephrolithiasis (6, 7). With the exception of the few conditions genetically determined, hyperoxaluria is due to excessive intestinal absorption. Recently, the anion-exchanger SLC26A6 (also known as Cl– formate exchanger (CFEX) and putative anion transporter (PAT)1 has been recognised as a key molecule in oxalate metabolism (11, 12). SLC26A6 is a member of the SLC26 sulphate transporter family, a family of multifunctional anion exchangers. In the intestine, SLC26A6 mediates oxalate excretion and thereby limits the net absorption of ingested oxalate, a process critical for the prevention of hyperoxaluria and calcium oxalate nephrolithiasis (12, 13). In human kidney, SLC26A6 is expressed in distal segments of proximal tubules, where it mediates oxalate-dependent NaCl absorption (11), in parts of the thin and thick ascending limbs of Henle's loops, macula densa, distal convoluted tubules and a subpopulation of intercalated cells of collecting ducts (14). Aronson et al. reported that mice lacking the anion exchanger Slc26a6 showed hyperoxalemia and hyperoxaluria, which ameliorated under an oxalate-free diet, and a high incidence of calcium oxalate urolithiasis (12). This genetic manipulation clearly demonstrates that intestinal oxalate excretion plays a critical role in decreasing oxalate filtered load, preventing hyperoxalemia and reducing the risk of stone disease (15).
The human SLC26A6 gene resides on chromosome 3p21.3 and has several known splice variants encoding different isoforms. Up to now no mutation has been identified in humans, while valine replacement by methionine at amino acid 206 position of the long N-terminal isoform, which corresponds to the amino acid 185 position of the short N-terminal isoform, is the only non-synonymous polymorphism reported for this gene in the human SNP database up to now (http://www.ncbi.nlm.nih.gov/SNP/snp_ref.cgi?rs=13324142). Recently, the human V206M variant has been demonstrated in vitro to exhibit reduced Cl–/oxalate exchange activity (20). In the present study, we first investigated the clinical impact of the human V206M polymorphic variants in a population at high risk of nephrolithiasis, such as PHPT patients.
| Methods |
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The study included 145 consecutive unrelated Italian patients (121 females and 24 males; mean age at presentation 61.7±12.8 years, 50 of them described in a previous study (6)) referred to our Departments between 2000 and 2007 for diagnosis and management of PHPT. As controls, 129 age- and sex-matched subjects recruited among subjects referred to our outpatient Endocrine Units for subclinical thyroid diseases. Subjects were eligible as controls if they were Caucasian, had no personal or family history of kidney stones, had normal serum creatinine, calcium and phosphate, and were not taking any drug. Diagnoses of PHPT were made on the basis of high ionised calcium levels in the presence of elevated or inappropriately normal serum PTH levels (plasma ionised calcium 1.51±0.15 mmol/l (1.31–2.10), n.v. 1.15–1.29 mmol/l; total serum calcium 2.76±0.23 mmol/l (2.29–3.61), n.v. 2.20–2.60 mmol/l; serum PTH 172.0±118.0 pg/ml (38–620), n.v. 10–65 pg/ml; mean±S.D. (range)). The diagnosis of PHPT was confirmed by surgery in 77 patients (57% of the cohort). The series included 11 unrelated patients with familial PHPT. Genetic analysis of genomic DNA revealed nine different MEN1 gene mutations in nine patients (primers available on request).
All patients had normal serum creatinine. Fifty-three percent (n=77) of the patients presented with a previously established diagnosis of arterial blood hypertension according to the World Health Organization (SBP>135 and DBP>85 mmHg) that was appropriately treated. Anti-hypertensive therapy was modified in order to avoid administration of diuretics, with a washout period of at least 3 months. Nephrolithiasis, defined as a history of renal colics with stone expulsions and/or imaging identification or asymptomatic ultrasound imaging of stones, was identified in 51% of the patients (n=74). Stone composition was available in a minority of cases and revealed calcium oxalate stones. Urine sediment analysis performed in 50 PHPT subjects as previously described (6) showed calcium oxalate crystals in 82% of cases of crystalluria. Osteoporosis, defined as a T-score lower than -2.5 at least in one of the sites evaluated with dual energy X-ray absorptiometry (DEXA at femur and lumbar spine level) was present in 50% of the patients (n=73). No patients have been taking anti-fracture drugs (bisphosphonates or vitamin D) in the 3 months preceding the study.
Patients or controls with known bowel disease or resection as well as with cystic fibrosis have been excluded.
The study complies with the Helsinki Declaration revised in 2000 and was approved by the local Ethical Committee (IRCCS Fondazione Ospedale Maggiore Policlinico, Mangiagalli e Regina Elena, Milan, Italy). All participants signed an informed consent form, which included consent for genetic testing.
Laboratory tests
Venous blood samples after overnight fasting were obtained from all patients under a free diet for measurement of ionised calcium, total calcium, phosphate, intact PTH and creatinine, as previously reported (6). Plasma ionised calcium was measured by a potentiometric method (Radiometer ABL System 625, Copenhagen, Denmark) on heparinised blood samples within 30 min from blood collection. Serum intact PTH was measured by a chemiluminescent method (Nichols Institute Diagnostics, San Juan Capistrano, CA, USA), with intra- and interassay coefficients of variation of <4.5 and <10.0% respectively. Serum 1,25-dihydroxyvitamin D3 was assessed by RIA kit (Immunodiagnostic Systems Ltd, Boldon, UK), with an intra- and interassay coefficients of variation of <8 and <10% respectively. Calcium, phosphate and creatinine were measured in 24 h urine collections (from 0700 h of the day before to 0700 h of the examination day) in all patients, while oxalate were determined in 50 randomly selected subjects (32 stone-formers and 18 non-stone formers) by enzymatic commercial kit using oxalate oxidase (Greiner Diagnostic Gmbh, Bahlingen, Germany; CV 5.6%) in a 24 h urine sample. Glomerular filtration rates were estimated by creatinine clearance calculation for all patients. All patients underwent an ultrasound examination of the urinary tract. All had bone mineral density evaluation by DEXA of the lumbar spine L2–L4 and the proximal femur (femoral neck).
DNA extraction and genotyping
Genomic DNA was extracted from 200 µl peripheral blood of each patients and control samples by High Pure PCR Template Preparation Kit (Roche Diagnostics) according to the manufacturer's specifications.
The SNP at position 804 CT of SLC26A6 mRNA long N-terminal variant was genotyped using the TaqMan MGB allelic discrimination system assessed with the ABI PRISM 7900HT sequence detector machine and its correlated software SDS 2.3 (Applied Biosystems, Foster City, CA, USA) (17). Polymerase chain reaction was performed with a total volume of 25 µl, which contained 10 ng DNA, 1X TaqMan Universal PCR Master Mix (Applied Biosystems), each primer at a concentration of 36 µM, and each probe at a concentration of 8 µM. Primers and Probes of the 804 CT polymorphism were obtained from Applied Biosystems (Assay ID: C_25627247_10). The amplification was done under the following conditions: 95 °C for 10 min to activate the AmpliTaq Gold enzyme, followed by 40 cycles of 15 s at 92 °C (denaturation) and 1 min at 60 °C (annealing/extension). The fluorescence levels were measured with an ABI PRISM 7900HT (Applied Biosystems) before and after the PCR amplification. The allelic discrimination results were determined after the amplification by performing an end-point read. Quality control samples were included in the genotyping assay: each allelic discrimination session contained two water (first and last negative controls) and three unblinded controls for the three different genotypes.
Statistical analysis
Quantitative variables in the text were described as mean±S.D. Differences among means were tested by using t-test, or one-way ANOVA with Bonferroni post-test where data were normally distributed. Otherwise, Mann–Whitney rank-sum test was performed. Chi-squared analysis test was used to test the hypothesis of no difference between patients and controls alleles frequency. Fisher's exact test was applied whenever expected values were <5. Correlations between variables were analysed by Pearson's coefficient. A multiple logistic regression model was used to define independent risk factors for the occurrence of hypertension in PHPT patients. P<0.05 was considered statistically significant. Statistical analysis was performed using the SPSS version 12.0 statistical package (SPSS Inc., Chicago, IL, USA).
| Results |
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Considering the subset of stone-formers patients (n=74), the V/V group did not differ from the V/M+M/M group for age, sex, severity of hyperparathyroidism (plasma ionised and serum total calcium and phosphorus levels, serum PTH levels and serum 1,25-dihydroxyvitamin D3) and prevalence of osteoporosis (Table 3). Conversely, urine calcium excretion levels were significantly lower in the V/M+M/M with respect to V/V stone-formers (4.40±1.88 vs 5.92±2.62 mg/kg per 24 h; P=0.034; Table 3). A trend to such a difference in mean urine calcium excretion levels between the V/M+M/M and the V/V stone formers was present also in the subset of PHPT patients evaluated for the urine oxalate excretion.
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| Discussion |
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The present study failed to find any significant association between the polymorphic variants of the human SLC26A6 gene and the development of kidney stones in this cohort of PHPT patients. In particular, the urine oxalate excretions were not related to the V206M genotypes. Admittedly, three major points need to be considered about the discrepancy between clinical negative data presented here and the available experimental data about SLC26A6 V206M variant (16). First, functional data about the human 206M were relative to its homozygotic condition. In the present study, the M/M genotype was extremely rare both in PHPT and healthy cohorts, namely one PHPT patient and three healthy controls, making difficult to evaluate its actual clinical impact. Secondly, as far as the renal oxalate excretions are concerned, several acquired conditions might influence urine oxalate concentrations, overcoming the effect of the genetic background (23, 24, 25, 26). In particular, high levels of 1,25-dihydroxyvitamin D3 might induce high calcium and consequently oxalate intestinal absorption (23, 24), although in the present series of PHPT patients serum 1,25-dihydroxyvitamin D3 levels were not significantly correlated with urine oxalate concentrations. Third, it has been suggested that oxalate can affect stone formation and growth independently from the direct effect of elevated urine concentrations, for example via interactions with the renal epithelium (25).
Although nephrolithiasis was present with the same frequency in PHPT patients independently from SLC26A6 genotype, we investigated the potential effect of the 206M allele in the subset of PHPT stone-formers. The present cohort of PHPT patients showed a high prevalence of kidney stones. Interestingly, stone-formers harbouring the 206M allele showed a less severe urine calcium excretion, in the absence of differences in sex, age, renal function and PHPT severity. Therefore, though there is no experimental evidence that SCL26A6 could be involved in urine calcium excretion, it is tempting to speculate that the SLC26A6 M allele might contribute to the occurrence of kidney stones in PHPT patients with relatively low urine calcium excretion.
Finally, the study showed that 206M allele was significantly related to the presence of hypertension and was associated with a fourfold increased risk for hypertension also after correction for age, BMI and GFR. In vitro data suggested a model by which oxalate might facilitate NaCl entry across the apical membrane of proximal tubule cells (26). In particular, the SLC26A6 transporter appears to primarily contribute to transtubular NaCl absorption by mediating Cl– oxalate exchange in the intact proximal tubule under physiological conditions (12, 13, 27). Since Slc26a6-null mice were normotensive and showed no significant difference in plasma and urine concentrations of urea, Na+, Cl– in comparison with the wild-type animals, the association between 206M allele and hypertension in PHPT patients was an unexpected finding. However, it should be considered that the NaCl facilitating function of the Cl– exchanger has been demonstrated in the proximal tubule, while the exchanger might be involved in the NaCl reabsorption in other segment of nephron where it has been demonstrated to be expressed and where its function is still obscure (14). Moreover, other genes as well as PTH itself might interact and modulate the function of the SLC26A6 exchanger at renal tubule level. The unexpected association of 206M variant with hypertension deserves further study in order to better understand the role of the Cl– oxalate exchanger in the physiology of renal NaCl absorption in humans.
In conclusion, this study reports that the 206M polymorphic variant of SLC26A6 gene is not associated with an increased risk of nephrolithiasis in PHPT patients. However, the observation that PHPT stone-formers harbouring the M allele showed relatively lower renal calcium excretion suggests a potential, though minor, role for the SLC26A6 activity in the risk of kidney stones development. Further studies are needed to confirm the association of 206M variant with high prevalence of hypertension in other populations and to understand the molecular and biological events responsible for this relationship.
| Declaration of interest |
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