Carey M C
Department of Medicine, Harvard Medical School, Brigham and Women's Hospital, Boston, MA.
Recenti Prog Med. 1992 Jul-Aug;83(7-8):379-91.
Gallstones are composed principally of cholesterol monohydrate crystals (cholesterol stones) or the acid salt of calcium bilirubinate (pigment stones). Cholesterol stones and the black variety of pigment gallstones form in sterile gallbladder bile whereas brown pigment gallstones form in infected bile. Biliary supersaturation is the principal pathophysiological defect and is hepatic in origin. Supersaturation results from excessive secretion of cholesterol or bilirubin conjugates, the precursors of unconjugated bilirubin, and/or, deficient secretion of bile salt and lecithin, the solubilizers of these otherwise insoluble lipids. As has now being clarified for cholesterol stones, an imbalance in pro- and antinucleating biliary proteins, hypersecretion of gallbladder mucin and gallbladder dysmotility possibly from cholesterol "toxicity" to sarcolemma, all interact to promote nucleation. Crystallisation results in suspension of cholesterol crystals or bilirubinate salts in gallbladder mucin gel and is known as "biliary sludge". It is believed today that this stage is essential for evolution of both cholesterol and pigment stones. Brown pigment gallstones form principally in the bile ducts. These stones result from infection of the biliary tree, most commonly due to obstruction from migrating gallbladder stones. Chemical compositions of brown and black pigment stones are different: In black stones, calcium bilirubinate is polymerized and oxidatively degraded but in brown stones, calcium bilirubinate is present as the unpolymerised salt. Brown stones differ also from black stones in containing calcium fatty acid soaps, a result of bacterial phospholipase A1 hydrolysis of biliary lecithin. Both types of pigment gallstones may contain crystalline inorganic calcium salts especially carbonate (gallbladder stones) and phosphate (bile ducts stones). Since a molecular understanding of the multiple defects that lead to cholesterol and pigment gallstones is becoming a reality, the future holds much promise for gallstone prevention.
胆结石主要由一水合胆固醇晶体(胆固醇结石)或胆红素钙盐(色素结石)组成。胆固醇结石和黑色色素胆结石形成于无菌的胆囊胆汁中,而棕色色素胆结石形成于感染的胆汁中。胆汁过饱和是主要的病理生理缺陷,其起源于肝脏。过饱和是由于胆固醇或胆红素结合物(未结合胆红素的前体)分泌过多,和/或胆汁盐和卵磷脂(这些原本不溶性脂质的增溶剂)分泌不足所致。正如现在已经明确的胆固醇结石情况一样,促核和抗核胆汁蛋白失衡、胆囊粘蛋白分泌过多以及可能由于胆固醇对肌膜的“毒性”导致的胆囊运动障碍,都相互作用促进成核。结晶导致胆固醇晶体或胆红素盐悬浮在胆囊粘蛋白凝胶中,这被称为“胆泥”。如今人们认为这个阶段对于胆固醇结石和色素结石的形成都是必不可少的。棕色色素胆结石主要在胆管中形成。这些结石是由于胆道系统感染所致,最常见的原因是胆囊结石移位造成的梗阻。棕色和黑色色素结石的化学成分不同:在黑色结石中,胆红素钙聚合并氧化降解,但在棕色结石中,胆红素钙以未聚合的盐形式存在。棕色结石与黑色结石的不同之处还在于含有钙脂肪酸皂,这是细菌磷脂酶A1水解胆汁卵磷脂的结果。两种类型的色素胆结石都可能含有结晶性无机钙盐,尤其是碳酸盐(胆囊结石)和磷酸盐(胆管结石)。由于对导致胆固醇结石和色素结石的多种缺陷的分子层面理解正在成为现实,胆结石预防的未来充满希望。