Ossification
Development process in bones
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Through Bone, Cell (biology) and Health
In fracture healing, endochondral osteogenesis is the most commonly occurring process, for example in fractures of long bones treated by plaster of Paris, whereas fractures treated by open reduction and internal fixation with metal plates, screws, pins, rods and nails may heal by intramembranous osteogenesis.
Heterotopic ossification is a process resulting in the formation of bone tissue that is often atypical, at an extraskeletal location. Calcification is often confused with ossification. Calcification is synonymous with the formation of calcium-based salts and crystals within cells and tissue. It is a process that occurs during ossification, but not necessarily vice versa.
The exact mechanisms by which bone development is triggered remains unclear, but growth factors and cytokines appear to play a role.
Intramembranous ossification
Intramembranous ossification is one of two key processes during fetal skeletal development and is an essential process during the natural healing of bone fractures. It forms the flat bones of the skull, mandible, and hip bone among others.
Woven bone is formed when mesenchymal stem cells (MSCs), an unspecified cell that can develop into an osteoblast, initiate intramembranous ossification. First, a small group of adjacent MSCs differentiate into osteoblast and begin to replicate and form a small, dense cell clusters. This forms an ossification centre, at which point the osteoblasts begin secreting osteoid, an unmineralized collagen-proteoglycan matrix that can bind calcium. Binding calcium to the osteoid hardens the matrix and entraps the osteoblasts. This entrapment transforms the osteoblasts into osteocytes.
As osteoblasts continue to secrete osteoid, it surrounds blood vessels and forms trabecular, cancellous, or spongy bone. Over time, these blood vessels develop into red bone marrow. MSCs on the bone's surface form the periosteum, a membrane covering the outer surface of bones. MSCs on the inner surface of the periosteum develop into osteoblasts and secrete osteoid parallel with the existing matrix, which creates layers. The result of this is compact or cortical bone.
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Endochondral ossification
Endochondral ossification, or intracartilaginous ossification, is the formation of long bones and other bones. This requires a hyaline cartilage precursor. There are two centers of ossification for endochondral ossification.
The primary center
In long bones, bone tissue first appears in the diaphysis (middle of shaft). Chondrocytes multiply and form trabeculae. Cartilage is progressively eroded and replaced by hardened bone, extending towards the epiphysis. A perichondrium layer surrounding the cartilage forms the periosteum, which generates osteogenic cells that then go on to make a collar that encircles the outside of the bone and remodels the medullary cavity on the inside.
The nutrient artery enters via the nutrient foramen from a small opening in the diaphysis. It invades the primary center of ossification, bringing osteogenic cells (osteoblasts on the outside, osteoclasts on the inside.) The canal of the nutrient foramen is directed away from more active end of bone when one end grows more than the other. When bone grows at same rate at both ends, the nutrient artery is perpendicular to the bone.
Most other bones (e.g. vertebrae) also have primary ossification centers, and bone is laid down in a similar manner.
Secondary centers
The secondary centers generally appear at the epiphysis. Secondary ossification mostly occurs after birth (except for distal femur and proximal tibia which occurs during 9th month of fetal development). The epiphyseal arteries and osteogenic cells invade the epiphysis, depositing osteoclasts and osteoblasts which erode the cartilage and build bone, respectively. This occurs at both ends of long bones but only one end of digits and ribs.
Evolution
Several hypotheses have been proposed for how bone evolved as a structural element in vertebrates. One hypothesis is that bone developed from tissues that evolved to store minerals. Specifically, calcium-based minerals were stored in cartilage and bone was an exaptation development from this calcified cartilage. However, other possibilities include bony tissue evolving as an osmotic barrier, or as a protective structure.