Abstract
Cholesterol monohydrate (ChM) is the major organic component of most gallbladder stones in Western populations [1]. An essential thermodynamic prerequisite for the precipitation of cholesterol (Ch) from bile is that bile becomes supersaturated with Ch [2]. Although Ch is virtually insoluble in water, it is present in high concentrations in the hepatic and gallbladder biles of adult human beings [2], where it is solubilized in thermodynamically stable bile salt (BS) and BS-phospholipid (PL) micelles and dispersed in a thermodynamically metastable state by unilamellar PL-Ch vesicles [3]. Hepatic secretion of vesicles appears to be the principal conduit for PL and Ch secretion into bile [4]. Since the transhepatic flux of BS drives PL-Ch secretion, i.e., vesicle exocytosis [5], the origin of supersaturated bile must perforce lie in the hypersecretion of Ch-enriched vesicles in the face of normal BS secretion or the normal secretion of Ch-enriched vesicles in the face of BS hyposecretion [6].
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© 1990 Springer-Verlag, Berlin Heidelberg
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Carey, M.C. (1990). Increased Biliary Lithogenicity Through Cholesterol Supersaturation. In: Swobodnik, W., Soloway, R.D., Ditschuneit, H. (eds) Gallstone Disease. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-74619-2_1
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DOI: https://doi.org/10.1007/978-3-642-74619-2_1
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