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Student Center Anatomy and Physiology, Second Edition
The unity of form and function
Kenneth S. Saladin
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Chapter 8: Bone Tissue

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Tissues and Organs of the Skeletal System

The study of bones is called [1] . Although a bone has several tissues, the hard, mineralized tissue that preserves best is called [2] . Bones specialized for leverage are in a class called [3] bones. Those specialized to enclose and protect soft organs are [4] bones. The first type has a long shaft or [5] enclosing a [6] cavity, and has an expanded head or [7] enclosing a layer of spongy osseous tissue called the [8] . A bone is covered with a connective tissue membrane called the [9] . Between the shaft and the head, children have a cartilaginous growth zone called the [10] .

Histology of Osseous Tissue

[11] cells arise from embryonic fibroblasts and multiply continually. They divide and differentiate into [12] , which deposit the organic matrix of bone and become osteocytes as they become entrapped in it. The cells that dissolve bone, called [13] , develop from the same bone marrow cells that produce [14] of the blood. Osteocytes are in touch with each other by slender cellular processes passing through narrow channels called [15] .

The organic matter of osseous tissue includes fibers of the protein [16] and a [17] called chondroitin sulfate. The inorganic matter is largely made up of crystals of calcium phosphate salt called [18] . In [19] bone, most of the matrix is organized into osteons, which consist of multiple layers of [20] organized around a central canal. Spongy bone consists of slender plates and rods called [21] . Of the kinds of bone marrow, [22] performs a hemopoietic role, whereas [23] is mostly adipose tissue.

Bone Development

Most bones form by a process called [24] , which begins with a cartilage model. The [25] center in this bone begins as a region of hypertrophied chondrocytes. As the matrix between these breaks down, the chondrocytes die and the center is invaded by a bud of vascular connective tissue. This forms a hollow space called the [26] . At each end of this is a region called the [27] where cartilage of the heads of the bone continues to be converted to osseous tissue. The 27 has five zones including the zone of [28] , in which chondrocytes begin to multiply rapidly but are not yet enlarged, the zone of [29] , a region in which they enlarge, and the zone of [30] , where the matrix between cell columns begins to calcify. Secondary ossification centers form in the [31] of the bone around the time of [32] .

Even after a bone is formed, it continues to undergo [33] , meaning changes in size and shape in response to mechanical stress, gravity, hormones, and other factors. To increase in length, a bone can only undergo [34] growth, in which new osteons are added at the surface. Achondroplastic [35] results from a genetic anomaly in which the chondrocytes of this growth zone fail to multiply.

Physiology of Osseous Tissue

The process of taking minerals from the blood and incorporating them into osseous tissue is called mineral [36] . The crystals formed in this process only develop if the product of blood calcium and phosphate concentrations reaches a threshold value called the [37] . The process of dissolving bone and releasing minerals into the blood is called mineral [38] . In part, this involves an osteoclast enzyme called [39] , which digests collagen.

Calcium balance in the blood must be carefully controlled because a calcium deficiency, called [40] , can cause tetany and suffocation, whereas a calcium excess, called [41] , can depress neuromuscular function. The latter condition is normally prevented in children by the hormone [42] , which inhibits osteoclasts and stimulates osteoblasts. In both children and adults, calcium deficiency is normally prevented by [43] hormone, which has the opposite effects as well as promoting calcium absorption and reduced calcium excretion. Calcium absorption also depends on an active form of vitamin D called [44] , produced by the coordinated action of the skin, [45] , and [46] .

Bone Disorders

Bone fractures are classified in several ways. For example, a/an [47] fracture is one in which a bone breaks through the skin, and a/an [48] fracture is one in which it does not. Any 47 fracture is also a/an [49] fracture, meaning the two broken ends of the bone are no longer in anatomical alignment with each other. A fracture that goes only part way across a bone, leaving the two pieces joined, is a/an [50] fracture. A twisting motion may produce a/an [51] fracture, which coils around a bone. The healing of a fracture begins with a blood clot called a fracture [52] , which becomes infiltrated with blood vessels, fibroblasts, and osteogenic cells to form [53] tissue. As cartilage and then minerals form in this tissue, it becomes a soft and then a hard [54] . Most fractures can be set by [55] , a procedure that does not require surgical exposure of the bone. The most common bone disease is not fractures, but a demineralization disease called [56] , seen most frequently in postmenopausal white women. This condition leads to bone weakness and susceptibility to fractures and spinal deformities such as "widow’s hump."


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