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| CURRENT ISSUE | ARCHIVES | JASN Express | ONLINE SUBMISSION | |
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Received October 1, 2007
Accepted on January 2, 2008
CLINICAL EPIDEMIOLOGY |
,
,
,
*Slone Epidemiology Center at Boston University,
Channing Laboratory, Department of Medicine, Brigham and Women’s Hospital, Harvard Medical School, and
Massachusetts General Hospital, Boston, Massachusetts;
Division of Urologic Surgery, Duke University Medical Center, Durham, North Carolina; and ||University of Massachusetts Memorial Medical Center, Worcester, Massachusetts
1 To whom correspondence should be addressed. E-mail: dkaufman{at}slone.bu.edu.
| Abstract |
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Most kidney stones are composed primarily of calcium oxalate. Oxalobacter formigenes is a Gram-negative, anaerobic bacterium that metabolizes oxalate in the intestinal tract and is present in a large proportion of the normal adult population. It was hypothesized that the absence of O. formigenes could lead to increased colonic absorption of oxalate, and the subsequent increase in urinary oxalate could favor the development of stones. To test this hypothesis, a case-control study involving 247 adult patients with recurrent calcium oxalate stones and 259 age-, gender-, and region-matched control subjects was performed. The prevalence of O. formigenes, determined by stool culture, was 17% among case patients and 38% among control subjects; on the basis of multivariate analysis controlling demographic factors, dietary oxalate, and antibiotic use, the odds ratio for colonization was 0.3 (95% confidence interval 0.2 to 0.5). The inverse association was consistently present within strata of age, gender, race/ethnicity, region, and antibiotic use. Among the subset of participants who completed a 24-h urine collection, the risk for kidney stones was directly proportional to urinary oxalate, but when urinary factors were included in the multivariable model, the odds ratio for O. formigenes remained 0.3 (95% confidence interval 0.1 to 0.7). Surprisingly, median urinary oxalate excretion did not differ with the presence or absence of O. formigenes colonization. In conclusion, these results suggest that colonization with O. formigenes is associated with a 70% reduction in the risk for being a recurrent calcium oxalate stone former.
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