Cholelithiasis (Gallstones) Cholelithiasis -Stone in gallbladder. Two main types of gallstones. Cholesterol stones Pigment stones
Risk Factors for Gallstones 1) Cholesterol Stones: Demography: Northern Europe, US Advancing age Female sex hormones -Female gender -Oral contraceptives -Pregnancy Obesity
Rapid weight reduction Gallbladder stasis Inborn disorders of bile acid metabolism Hyperlipidemia syndromes
2) Pigment Stones: Demography: Asian more than Western, rural more than urban. Chronic hemolytic syndromes Biliary infection Gl disorders: ileal disease ( Crohn disease), ileal resection or bypass, cystic fibrosis with pancreatic insufficiency
However, 80% of individuals have no identifying risk factors other than age and gender. Heredity: Family history increases risk.
Age and gender differences- Major role of h ypersecretion of biliary of cholesterol. Estrogen exposure- OCP use and during pregnancy increases expression of hepatic lipoprotein receptors and stimulates hepatic HMG-CoA reductase activity, enhancing both cholesterol uptake and biosynthesis E xcess biliary secretion of cholesterol. Obesity-increase biliary cholesterol secretion .
Rapid weight reduction- Cholesterol level ↑& amount of bile salts ↓. Long periods of starvation ↓ gallbladder contractions- not enough to empty out bile gallstones form Gallbladder stasis-favorable for both cholesterol and pigment gallstone formation. Hereditary factors
Pathogenesis of Cholesterol Stones Cholesterol is rendered soluble in bile by aggregation with water-soluble bile salts and water-insoluble lecithins , both of which act as detergents. When cholesterol concentrations exceed solubilizing capacity of bile ( supersaturation ), cholesterol can no longer remain dispersed and nucleates into solid cholesterol monohydrate crystals.
Four conditions contribute to formation of cholesterol gallstones (1) supersaturation of bile with cholesterol (2) hypomotility of gallbladder (3) accelerated cholesterol crystal nucleation (4) hypersecretion of mucus in gallbladder traps nucleated crystals accretion of more cholesterol and appearance of macroscopic stones.
Pathogenesis of Pigment Stones Disorders that are associated with elevated levels of unconjugated bilirubin in bile, such as chronic hemolytic anemias , severe ileal dysfunction or bypass, and bacterial contamination of biliary tree, increase risk of developing pigment stones.
Unconjugated bilirubin is normally a minor component of bile, but increases when infection of biliary tract leads to release of microbial β- glucuronidases , which hydrolyze bilirubin glucuronides . Thus, infection of biliary tract with Escherichia coli, Ascaris lumbricoides , or liver fuke C. sinensis , increases risk of pigment stone formation.
In hemolytic anemias secretion of conjugated bilirubin into bile increases. About 1% of bilirubin glucuronides are deconjugated in biliary tree, and in setting of chronically increased secretion of conjugated bilirubin, there is sufficiently large amount of deconjugated bilirubin left to allow pigment stones to form.
MORPHOLOGY Cholesterol stones- Arise exclusively in gallbladder. 100% pure (rare) to around 50% cholesterol. Pure cholesterol stones- pale yellow, round to ovoid, have a finely granular, hard external surface which on transection reveals a glistening radiating crystalline palisade.
With increasing proportions of calcium carbonate, phosphates, and bilirubin , stones take on a gray-white to black color, may be lamellated . Usually multiple stones present. Rarely, a very large stone fill fundus.
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Surfaces of multiple stones may be rounded or faceted, because of tight apposition. Stones composed largely of cholesterol- radiolucent; sufficient calcium carbonate found in 10-20% of cholesterol stones- radiopaque .
Pigment gallstones Brown to black. Black pigment stones are found in sterile gallbladder bile and brown stones in infected large bile ducts. Black stones contain oxidized polymers of calcium salts of unconjugated bilirubin , small amounts of calcium carbonate, calcium phosphate, and mucin glycoprotein, and some cholesterol monohydrate crystals.
Brown stones contain similar compounds along with some cholesterol and calcium salts of palmitate and stearate . Black stones-rarely greater than 1.5 cm in diameter, present in great number; are quite friable.
Their contours are usually spiculated and molded. Brown stones- laminated and soft and may have a soaplike or greasy consistency. 50-75% of black stones are radiopaque due to calcium salts while brown stones, containing calcium soaps, are radiolucent.
Clinical features 70-80% asymptomatic throughout life. Remainder symptomatic. Pain- constant or "colicky" (spasmodic) from an obstructed gallbladder or when small gallstones move down-stream and lodge in biliary tree.
Inflammation of gallbladder with stones also generates pain. Pain is localized to right upper quadrant or epigastrium that may radiate to right shoulder or back.
COMPLICATIONS Infammation of gallbladder ( cholecystitis ) More severe complications- empyema perforation fistulas infammation of biliary tree ( cholangitis ) obstructive cholestasis and pancreatitis.
Occasionally a large stone may erode directly into an adjacent loop of small bowel, generating intestinal obstruction (“gallstone ileus ”). I ncreased risk of gallbladder carcinoma.