Gallstones: Overview, symptoms, and causes
Cholelithasis, more commonly known as gallstones, are hardened deposits of bile in the gallbladder. Approximately 10 to 15% of Americans experience gallstones in their lifetime. To understand gallstones and why they develop, one needs to understand the gallbladder and how it functions Gallbladder The gallbladder is a small, hollow organ located beneath the liver that stores bile in high concentrations. Bile is a bitter alkaline fluid produced by the liver to support digestion. The liver sends bile into the gallbladder by means of the common hepatic duct. When food containing fat enters the digestive tract, the intestines release cholecystokinin. The cholecystokinin causes the gallbladder to contract and release the bile from the gallbladder into the small intestines through the common bile duct to digest fats. Bile is made up of water and bile salts or acids. These acids include—taurocholic acid and glycocholic acid (derivatives of cholic acid) and taurochenodeoxycholic acid and glycochenodeoxycholic acid (derivatives of chenodeoxycholic acid). Gallstones can be divided into two categories: cholesterol or pigment. Cholesterol gallstones Most gallstones, about 75%, are made up of cholesterol. Cholesterol gallstones result from biliary supersaturation caused by: An increased secretion of cholesterol into the gallbladder Gallbladder hypomotility—a case in which crystals remain in the gallbladder so long they become stones Accelerated cholesterol nucleation and crystallization Mucin (a glycoprotein component of mucus) gel accumulation Pigment gallstones Pigment gallstones can be black or brown depending on what they are made of.