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Recovery of substances secreted into the intestine and their return to the liver through portal venous blood; bile salt recycling is a major example.

An aggregate containing amphipathic molecules such as bile salts and products of lipid digestion, helping deliver poorly water-soluble lipids to intestinal absorptive surfaces.

Gallstones contain chiefly cholesterol and/or bile pigment, with variable calcium salts and an organic matrix. They are mixtures with different predominant components, not one compound with a universal formula. The period word cholesterin denotes cholesterol.

Cholesterol-rich stones contain crystalline cholesterol, often with a smaller pigmented nucleus and layers of other material. Mixed stones combine cholesterol, pigment, calcium salts and an organic matrix including mucin. Pigment stones contain much less cholesterol; a major constituent is calcium bilirubinate, related to the bile pigment bilirubin. Minor inorganic constituents can include calcium carbonate and calcium phosphate. Not every visibly dark stone has the same composition, and no fixed percentage follows from the question.^[ref]

The useful modern subdivision of pigment stones is into black and brown types. Black stones commonly contain polymerised pigment with calcium salts; brown stones include calcium bilirubinate and calcium salts of fatty acids, particularly in infected stagnant duct bile. These refinements explain why neither “all stones are cholesterol” nor “all stones are lime salts” is adequate.^[ref]

Chemical examination should distinguish the fractions rather than infer them merely from the external colour. Cholesterol can be extracted with a suitable organic solvent and recognised in recrystallised material; microscopy can show characteristic plate-like crystals. A mineral residue after removal or destruction of organic matter indicates an inorganic fraction, but residue alone cannot identify a particular salt. Layering, facets and colour describe growth and packing and are not chemical analyses. In particular, calcium bilirubinate is not interchangeable with calcium carbonate, and cholesterol is not a bile salt.

Chyle is intestinal lymph enriched with absorbed dietary lipids; its usual route ends in the venous circulation at the left jugulosubclavian junction. The milky appearance after a fat-containing meal is chiefly due to suspended lipid-rich particles, now called chylomicrons.

Formation begins with lipid digestion in the small intestine. Pancreatic lipase helps hydrolyse dietary triglycerides; bile salts help the digestion products reach the intestinal absorptive surface in mixed micelles. Enterocytes take up the products, reconstruct much of the long-chain triglyceride, and package it with other lipids and apolipoproteins into chylomicrons. These leave the basolateral side of the enterocytes and enter the central lacteals of the intestinal villi. Thus the particles carried in chyle are not simply intact globules of a meal passing through an open hole from the intestinal lumen.^[ref]

From the lacteals, chyle enters lymphatic channels in the intestinal wall and then collecting vessels in the mesentery. These vessels pass through mesenteric lymph nodes, with afferent vessels entering and efferent vessels leaving the nodes. Successive collectors join the intestinal lymphatic trunk or trunks. They usually communicate with the cisterna chyli, an expanded origin of the thoracic duct in the upper lumbar region, near the bodies of L1–L2 and to the right of the aorta. The cisterna chyli also receives lymph from lumbar trunks; the stream beyond it therefore contains material from more than the intestine. A conspicuous sac is not present in every individual.

The thoracic duct passes through the aortic hiatus of the respiratory diaphragm and ascends in the posterior mediastinum, typically between the aorta and azygos vein, behind the oesophagus. It crosses towards the left in the middle or upper thorax, continues to the root of the neck and arches to its terminal venous opening. The usual endpoint is the left venous angle, where the left internal jugular vein joins the left subclavian vein; terminal branches and the precise opening show anatomical variation. It is not normally the right venous angle or a direct entrance into the portal vein.^[ref]

The flow is promoted by intrinsic contraction of collecting lymphatic vessels, movements of surrounding muscles and respiratory changes of pressure. Lymphatic valves limit backward movement. Lymph nodes are interposed biological structures, not pumps that propel every particle independently.^[ref]

This route applies particularly to the long-chain dietary lipids carried by chylomicrons. Most absorbed glucose and amino acids, and much shorter-chain fatty acid material, follow portal vascular routes instead. Confusing these pathways would obscure the reason for asking separately about chyle. In a classical anatomical demonstration, the mesenteric channels of an appropriately fed animal appear white, and an injected or dissected preparation can trace their continuity towards the thoracic duct. The timing after a fatty meal matters: an empty-looking channel in a fasted preparation does not prove absence of a lymphatic vessel. The molecular account of chylomicrons is a modern explanation of the older gross observation.

The liver is both a metabolic processing organ and the producer of bile. These functions must be distinguished: much of what the liver contributes to the body enters the blood, whereas bile is its secretion into the digestive system.

Portal venous blood brings absorbed materials from the alimentary organs to the liver, while the hepatic artery supplies oxygenated blood. Within the hepatic sinusoids, the incoming blood encounters hepatocytes and scavenging Kupffer cells. Hepatocytes take up, transform, store and release substances; their bile canaliculi conduct bile towards the bile ducts. The organ's position therefore makes it a useful regulator between absorption from a meal and supply to the rest of the body.

Its main non-biliary functions include the following:

This modern list extends beyond the knowledge and biochemical vocabulary of 1867. It is consistent with the organ's combined metabolic, storage and clearance roles, rather than treating bile production as the whole explanation.^[ref]

Bile contains water, electrolytes, bile salts, phospholipids, cholesterol and bilirubin conjugates. Hepatocytes form the primary secretion; ductal epithelium modifies it. The gallbladder stores and concentrates bile between meals and releases it into the duodenum. Production of bile must therefore be distinguished from its intermittent delivery to a meal.

Its two central functions are assistance with lipid digestion and nutrient absorption, and excretion of selected waste substances. Amphipathic bile salts help disperse dietary fat and form mixed micelles carrying products of lipid digestion to the absorptive surface of the small intestine. They thereby promote uptake of fatty acids, monoglycerides, cholesterol and fat-soluble vitamins. Bile is not itself a source of pancreatic lipase, nor does emulsification chemically hydrolyse triglycerides. Biliary bilirubin, produced through haem breakdown, provides an excretory route; cholesterol and selected other substances also leave in bile. Most secreted bile salts are recovered, especially in the terminal ileum, and return through the portal vein: the enterohepatic circulation conserves the useful detergent.^[ref]

Two comparisons reveal why both sorts of function matter. First, compare a fresh liver extract with an extract prepared after an appropriate controlled interval: testing for reducing sugar and isolating glycogen distinguishes a stored precursor from newly liberated glucose. A reliable interpretation needs prompt sampling and controls because post-mortem glycogenolysis can change the result after the animal has died; detecting sugar in an organ alone does not prove where all of it was made. Secondly, in classical biliary fistula observations, diverting bile away from the intestine while collecting it separately allowed its output to be measured and the loss of normal fat assimilation to be examined. Comparing faecal fat with and without delivery of bile distinguishes a digestive contribution from a merely excretory one. The modern explanation is that loss of intestinal bile salts impairs mixed micelle formation, while jaundice from retained biliary pigment is a separate consequence of failed pigment elimination.