Haversian canal
Haversian canals are a series of microscopic tubes in the outermost region of bone called cortical bone. They allow blood vessels and nerves to travel through them to supply the osteocytes.
Structure
Each Haversian canal generally contains one or two capillaries and many nerve fibres. The channels are formed by concentric layers called lamellae, which are approximately 50 μm in diameter. The Haversian canals surround blood vessels and nerve cells throughout bones and communicate with osteocytes through connections called canaliculi. This unique arrangement is conducive to mineral salt deposits and storage which gives bone tissue its strength. Active transport is used to move most substances between the blood vessels and the osteocytes.
Haversian canals are contained within osteons, which are typically arranged along the long axis of the bone in parallel to the surface. The canals and the surrounding lamellae form the functional unit, called a Haversian system, or osteon.
Clinical significance
Fracture
Blood vessels in the Haversian canals are likely to be damaged by bone fracture. This can cause haematoma.
Haversian canals may be wider in patients with rheumatoid arthritis. They are also more likely to contain osteoclasts that break down bone structure. These differences are studied with light microscopy.
History
Haversian canals were first described by British physician Clopton Havers, after whom they are named. He described them in his 1691 work ''Osteologica Nova.''
Human bones are densely vascularized as in many other mammals. Even though some authors tried to identify a correlation between endothermy and secondary Haversian reconstruction, this feature is absent in many living mammals and birds while others possess only scattered Haversian systems. Scattered Haversian canals are also found in ectotherms like cryptodira turtles. Among extinct groups, dense Haversian vascularization is only present in stem-birds and stem-mammals while scattered Haversian systems can be found in ichthyosaurs, phytosaurs, basal stem-mammals, Limnoscelis, and temnospondyls. When endosteal Haversian systems are considered, the phylogenetic distribution becomes even broader.