GALLSTONE FORMATION : Local Factors - 08/09/11
Résumé |
In 1882, Langenbuch performed the first cholecystectomy.7, 58 At the time, he hypothesized that removing the gallbladder was necessary because it was a culprit in stone formation. Previously the gallbladder was believed to be a simple storage organ and an innocent bystander. Subsequent investigations have supported Langenbuch's hypothesis. Once the gallbladder is removed, formation of recurrent cholesterol gallstones is extremely rare. It is well documented that secretion of supersaturated bile by the liver is essential for cholesterol stone formation; however, this abnormality is not altered by cholecystectomy. In addition, gallbladder stasis is another well-recognized risk factor for stone formation. Together, these observations point to a role of local factors in gallstone pathogenesis. In the absence of a gallbladder, hepatic bile passes into the duodenum within minutes to hours. With an intact gallbladder, however, bile can be stored in the gallbladder for hours, days, or even weeks. This storage time is essential to allow cholesterol crystals to nucleate, calcium salts to precipitate, and stones to grow. In addition, the gallbladder may modify bile in a way that promotes stone formation, for example, by concentrating bile or by modifying the quantity and composition of biliary proteins. This article discusses factors promoting or inhibiting crystal nucleation and the role of the gallbladder in gallstone formation.
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| Address reprint requests to Sum P. Lee, MD, PhD, Department of Medicine, (111-GI-A), Veterans Affairs Puget Sound, Health Care System, 1660 South Columbian Way, Seattle, WA 98108–0597 Supported by grants DK 41678 and DK 46890 from the National Institutes of Health. |
Vol 28 - N° 1
P. 99-115 - mars 1999 Retour au numéroBienvenue sur EM-consulte, la référence des professionnels de santé.
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