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David Appleton, MPharm, is a
preregistration student and
Brian Lockwood, PhD, MRPharmS, is
senior lecturer in pharmacy
School of Pharmacy and Pharmaceutical
Sciences,
University of Manchester |
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SUMMARY
Our skeletons provide us with a strong yet light protective framework,
due to a unique structure comparable to reinforced concrete. Bone is
not merely an inert material, however, but a highly dynamic metabolic
reservoir of calcium ions. The skeleton stores 99 per cent of all calcium
ions contained in the body. There are two main types of bone in the
skeleton. These are distinguished by their microscopic architecture:
· Cortical bone is hard and dense, and comprises the shafts of
the long bones which bear most of the body’s weight.
· Cancellous or trabecular bone is found in the ends of long bones,
vertebrae and pelvis. This has a honeycomb like appearance, with plates
known as trabeculae arranged in such a way as to provide resistance to
forces. There is also a greater internal surface area and blood supply
than in cortical bone, which means it is involved in calcium homeostasis.
Bone consists of an organic phase (matrix) and an inorganic mineral
phase, together with a highly varied population of cells responsible
for its development and maintenance. The matrix is composed of structural
proteins, collagen and mucopolysaccharides, which provide resistance
and flexibility. The main mineral present is hydroxyapatite (crystalline
calcium phosphate) which is responsible for the rigidity and compressibility
of bone.
Bone growth (modelling) begins in fetal development and continues to
between 25–40 years of age when peak bone mass is said to be attained.
During puberty there is an accelerated period of growth where most of
this mass is laid down. The timing and nature of this process is initially
dictated by genetic factors, followed by environmental factors in adulthood,
which are described below.
After modelling there follows a process of consolidation, known as remodelling,
which is necessary to allow the skeleton to respond to external forces
and maintain body mineral levels. Up to 10 per cent of existing bone
per year3 is restructured, at sites known as bone multicellular units.
Bone multicellular units consist of teams of osteoblasts and osteoclasts
acting in a co-ordinated fashion under the influence of numerous cellular
factors. The resorption process follows a clear series of stages lasting
approximately 100 days:
· Osteoclasts initiate remodelling through specific activation of
their membrane receptors. They attach to internal bone surfaces and secrete
protons and enzymes which degrade and release minerals from the tissue.
· Osteoblasts then replace the resorbed material with immature matrix
protein (osteoid), which later becomes mineralised.
Examples of factors necessary for co-ordinating osteoblasts and osteoclasts
include:
· Calcium availability
· Mechanical forces experienced by the skeleton
· Endocrine, autocrine and paracrine factors
The last category is of particular significance once peak bone mass
is attained.
Full article PDF 110K |