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    For other uses, see Bone (disambiguation), including "Bones" which redirects here.



    Bone, also called osseous tissue, (Latin: "os") is a type of hard endoskeletal connective tissue found in many vertebrate animals. Bone is the main tissue of body organs; organs that support body structures, protect internal organs, (in conjunction with muscles) facilitate movement; and are involved with cell formation, calcium metabolism, and mineral storage. The bones of an animal are, collectively, known as the skeleton. Bone has a different composition than cartilage, and both are derived from mesoderm. In common parlance, cartilage can also be called "bone", certainly when referring to animals that only have cartilage as hard connective tissue, such as cartilaginous fish (Chondrichthyes) like sharks. True bone is present in bony fish (Osteichthyes) and all tetrapods.

    There are several evolutionary alternatives to bone. These evolutionary solutions are not completely functionally analogous to bone.

      A true endoskeleton (that is, protective tissue derived from mesoderm) is also present in Echinoderms. Porifera (sponges) possess simple endoskeletons that consist of calcareous or siliceous spicules and a spongin fiber network.

    Bones are studied in osteology. Bones can be prepared for study by several methods, such as maceration. Maceration is done by boiling fleshed bone with dish detergent and a little bleach until all large particles are off. The bones are then cleaned by hand, usually with a toothbrush and a degreaser.


        Bone
            Functions
            Structure
                Bone cells
                Matrix
            Formation
            Bone pathologies
            Exposed bone
            Terminology
            Notes
            See also

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    Functions

    Long bones can be connected to skeletal muscles via tendons. Bones connect at joints by ligaments. The interaction between bone and muscle is studied in biomechanics. The red bone marrow, located in the spongy bone matrix, allows for bones to produce red blood cells (hemopoiesis). Also, the bone marrow located at the bones diaphysis allow for white blood cells to be produced.

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    Structure











    Bone is a relatively hard and lightweight composite material, formed mostly of calcium phosphate in the chemical arrangement termed calcium hydroxyapatite. It has relatively high compressive strength but poor tensile strength. While bone is essentially brittle, it does have a degree of significant elasticity contributed by its organic components (chiefly collagen). Bone has an internal mesh-like structure, the density of which may vary at different points.

    Bone can be either compact or cancellous (spongy). Cortical (outer layer) bone is compact; the two terms are often used interchangeably. Cortical bone accounts for 80% of the total bone mass of the adult skeleton. Because of its high density it accounts for approximately 10% of the total surface area. Cancellous bone is trabecular (has an open, meshwork or sponge-like structure). It has a relatively high surface area (about 10 times that of cortical bone) and it accounts for approximately 20% of the total bone mass.

    Bone can also be either woven or lamellar. Woven bone forms quickly during periods of repair or rapid growth. Woven bone is unique in its ability to form spontaneously without a pre-existing strucure. It is so called because of its primitive, disorganized appearance. Its collagen fibres, which are few, are randomly oriented, accounting for its low strength. Lamellar bone forms slowly during periods of repair or typical growth. It does not form spontaneously. Lamellar bone forms only on calcified hyaline cartilage or bone. It is so called because its structure, observed microscopically, consists of a uniform system of layers, or lamellae. In contrast to woven bone, lamellar bone's collagen fibres, which are many, are oriented in parallel, accounting for its greater strength. Woven bone often forms initially and, as either growth or repair continues, it is replaced by lamellar bone. This process is known as "bony substitution."

    Long bones are tubular in structure (e.g. the tibia). The central shaft of a long bone is called the diaphysis, and has a hollow middle—the medullary cavity filled with bone marrow. Surrounding the medullary cavity is a thin layer of cancellous bone that also contains marrow. The extremities of the bone are called the epiphyses and are mostly cancellous bone covered by a relatively thin layer of compact bone. In children, long bones are filled with red marrow, which is gradually replaced with yellow marrow as the child ages.

    Short bones (e.g. finger bones) have a similar structure to long bones, except that they are shorter.

    Flat bones (e.g. the skull and ribs) consist of two layers of compact bone with a zone of cancellous bone sandwiched between them.

    Irregular bones are bones which do not conform to any of the previous forms (e.g. vertebrae).

    All bones consist of living cells embedded in a mineralised organic matrix that makes up the main bone material.


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    Bone cells

    Osteoblasts are typically viewed as bone forming cells. They are located near to the surface of bone and their functions are to make osteoid (a protein mixture which is secreted by osteoblasts. When it mineralizes, it becomes bone. Osteoid is primarily composed of Type I collagen.) and manufacture hormones, such as prostaglandins, which act on bone itself. Osteoblasts are mononucleate. Active osteoblasts are situated on the surface of osteoid seams. They robustly produce alkaline phosphatase, a chemical that has a role in the mineralisation of bone, as well as many matrix proteins.

    Bone lining cells (BLCs) share a common lineage with osteogenic (bone forming) cells. They function as a barrier for certain ions, induced osteogenetic cells. They are flattened, mononucleate cells which line bone.

    Osteocytes originate from osteoblasts which have migrated into and become trapped and surrounded by bone matrix which they themselves produce. The space which they occupy is known as a lacuna. Osteocytes have many processes which reach out to meet osteoblasts probably for the purposes of communication. Their functions include to varying degrees: formation of bone, matrix maintenance and calcium homeostasis. They possibly act as mechano-sensory receptors—regulating the bones' response to stress.

    Osteoclasts are the cells responsible for bone resorption. Osteoclasts are large, multinucleated cells located on bone surfaces in what are called Howship's lacunae. These lacunae, or resorption pits, are left behind after the breakdown of bone and often present as scalloped surfaces. Because the osteoclasts are derived from a monocyte stem-cell lineage, they are equipped with engulfment strategies similar to circulating macrophages. Osteoclasts mature and/or migrate to discrete bone surfaces. Upon arrival active enzymes, such as tartrate-resistant acid phosphatase, are secreted against the mineral substrate.

    The process of bone resorption releases stored calcium into the systemic circulation and is an important process in regulating calcium balance. As bone formation actively fixes circulating calcium in its mineral form, resorption actively unfixes it thereby increasing circulating calcium levels. These processes occur in tandem at site-specific locations and are known as bone turnover or remodeling. Osteoblasts and osteoclasts, coupled together via paracrine cell signalling, are referred to as bone remodeling units. The iteration of remodeling events at the cellular level is influential on shaping and sculpting the skeleton both during growth as well as after.

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    Matrix

    The matrix comprises the other major constituent of bone. It has inorganic and organic parts. The inorganic is mainly crystalline mineral salts and calcium, which is present in the form of hydroxyapatite. The matrix is initially laid down as unmineralized osteoid (manufactured by osteoblasts). Mineralisation involves osteoblasts secreting vesicles containing alkaline phosphatase. This cleaves phosphate groups and acts as the foci for calcium and phosphate deposition. The vesicles then rupture and act as a centre for crystals to grow on.

    The organic part of matrix is mainly Type I collagen. This is made intracellularly as tropocollagen and then exported. It then associates into fibrils. Also making up the organic part of matrix include various growth factors, the functions of which are not fully known. Other factors present include GAGs, osteocalcin, osteonectin, bone sialo protein and Cell Attachment Factor.

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    Formation



    The formation of bone during the fetal stage of development occurs by two methods: intramembranous and endochondral ossification.

      Intramembranous ossification mainly occurs during formation of the flat bones of the skull; the bone is formed from mesenchyme tissue.
      Endochondral ossification occurs in long bones, such as limbs; the bone is formed from cartilage.

    Intramembranous ossification

      Development of ossification center
      Calcification
      Formation of trabeculae
      Development of periosteum

    Endochondral ossification

      Development of cartilage model
      Growth of cartilage model
      Development of the primary ossification center
      Development of medullary cavity
      Development of the secondary osification center

    Endochondral ossification begins with points in the cartilage called "primary ossification centers." They mostly appear during fetal development, though a few short bones begin their primary ossification after birth. They are responsible for the formation of the diaphyses of long bones, short bones and certain parts of irregular bones. Secondary ossification occurs after birth, and forms the epiphyses of long bones and the extremities of irregular and flat bones. The diaphysis and both epiphyses of a long bone are separated by a growing zone of cartilage (the epiphyseal plate). When the child reaches skeletal maturity (18 to 25 years of age), all of the cartilage is replaced by bone, fusing the diaphysis and both epiphyses together (epiphyseal closure).

    Marrow can be found in almost any bone that holds cancellous tissue. In newborns, all such bones are filled exclusively with red marrow (or hemopoietic marrow), but as the child ages it is mostly replaced by yellow marrow (or fatty marrow). In adults, red marrow is mostly found in the flat bones of the skull, the ribs, the vertebrae and pelvic bones.

    Remodeling is the process of resorption followed by replacement of bone with little change in shape and occurs throughout a person's life. Its purpose is the release of calcium and the repair of micro-damaged bones (from everyday stress). Repeated stress results in the bone thickening at the points of maximum stress. It has been hypothesized that this is a result of bone's piezoelectric properties, which cause bone to generate small electrical potentials under stress.

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    Bone pathologies
    One of the most common bone illnesses is a bone fracture. Bones heal by natural processes, but untended and unsupported can lead to misgrown bone.

    Other illnesses are for example osteoporosis, osteonecrosis and bone cancer (osteosarcoma). The joints can be affected by arthritis.

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    Exposed bone
    Bone penetrating the skin and being exposed to the outside, apart from the effect of injury, occasionally is a normal feature:-
      One very obvious case is deer's antlers.
      The extinct predatory fish Dunkleosteus, instead of teeth, had sharp edges of hard exposed bone along its jaws.

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    Terminology

    Several terms are used to refer to features and components of bones:



    Several terms are used to refer to specific features of long bones:



    Several terms are used to describe the orientation of bones with respect to axes of the body, generally those anatomical terms of location, especially:



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    Notes





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    See also

     
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    This article is licensed under the GNU Free Documentation License [copyleft]. It uses material from the Wikipedia article "Bone". link