LaMont J T, Ventola A S, Trotman B W, Soloway R D
Hepatology. 1983 May-Jun;3(3):377-82. doi: 10.1002/hep.1840030316.
Mucin glycoproteins, a secretory product of the gallbladder, are thought to contribute to the matrix or nucleus of gallstones. Human black pigment stones originate in the gallbladder and have as their major constituent calcium bilirubinate, as well as inorganic salts and small amounts of cholesterol. The object of this study was to estimate the amount of glycoprotein in black pigment stones and to isolate gallbladder mucin from dissolved stones. Black pigment stones containing 18 to 65% calcium bilirubinate were first dissolved in 12.5 mM EDTA/0.1 N NaOH and decolorized, then subjected to glycoprotein assay. The mean glycoprotein content of eight stones was 12.4%. In separate experiments, pigment stones were partially dissolved by brief exposure to EDTA/NaOH to minimize glycoprotein breakdown, and the glycoproteins isolated by gel filtration and ultracentrifugation. Pigment stones contained two glycoprotein fractions on Sepharose 4B; a high molecular weight mucin glycoprotein in the void volume and a lower molecular fraction in the included volume. Mucin was further purified by density gradient ultracentrifugation in cesium chloride. Three separate mucin fractions had an average buoyant density of 1.48 gm per ml which is typical for these glycoproteins. Bile pigment was associated with high molecular weight mucin even after extensive dialysis, gel filtration, and density gradient ultracentrifugation. The identity of mucin was further established by beta-elimination of glycoproteins in alkaline borohydride which yielded galactosaminitol from cleavage of O-glycosidic bonds. Our results indicate that mucin glycoproteins are present in significant concentrations in human black pigment stones and can be purified from stones solubilized in EDTA/NaOH. The association of bile pigment with gallbladder mucin, even after extensive purification, is consistent with the hypothesis that mucin contributes to the matrix of pigment gallstones.
粘蛋白糖蛋白是胆囊的一种分泌产物,被认为有助于胆结石的基质或核心形成。人类黑色色素结石起源于胆囊,其主要成分是胆红素钙,还有无机盐和少量胆固醇。本研究的目的是估计黑色色素结石中糖蛋白的含量,并从溶解的结石中分离出胆囊粘蛋白。首先将含有18%至65%胆红素钙的黑色色素结石溶解于12.5 mM乙二胺四乙酸/0.1 N氢氧化钠中并脱色,然后进行糖蛋白测定。八颗结石的平均糖蛋白含量为12.4%。在单独的实验中,通过短暂暴露于乙二胺四乙酸/氢氧化钠使色素结石部分溶解,以尽量减少糖蛋白的分解,然后通过凝胶过滤和超速离心分离糖蛋白。色素结石在琼脂糖4B上含有两个糖蛋白组分;一个存在于空体积中的高分子量粘蛋白糖蛋白和一个存在于内体积中的较低分子量组分。通过在氯化铯中进行密度梯度超速离心进一步纯化粘蛋白。三个单独的粘蛋白组分的平均浮力密度为每毫升1.48克,这是这些糖蛋白的典型特征。即使经过广泛的透析、凝胶过滤和密度梯度超速离心,胆色素仍与高分子量粘蛋白相关。通过在碱性硼氢化物中对糖蛋白进行β-消除反应进一步确定了粘蛋白的身份,该反应从O-糖苷键的裂解中产生半乳糖胺醇。我们的结果表明,粘蛋白糖蛋白在人类黑色色素结石中以显著浓度存在,并且可以从溶解于乙二胺四乙酸/氢氧化钠中的结石中纯化出来。即使经过广泛纯化,胆色素与胆囊粘蛋白的关联也与粘蛋白有助于色素胆结石基质形成的假设一致。