The nature of calcium phosphate in mineralizing vertebrate tissues

Authors
Citation
Wj. Landis, The nature of calcium phosphate in mineralizing vertebrate tissues, PHOSPHOR SU, 146, 1999, pp. 185-188
Citations number
19
Categorie Soggetti
Inorganic & Nuclear Chemistry
Journal title
PHOSPHORUS SULFUR AND SILICON AND THE RELATED ELEMENTS
ISSN journal
10426507 → ACNP
Volume
146
Year of publication
1999
Pages
185 - 188
Database
ISI
SICI code
1042-6507(1999)146:<185:TNOCPI>2.0.ZU;2-#
Abstract
This presentation will describe and summarize aspects of the chemical, biol ogical and physical nature of the mineral deposited in the normal vertebrat e skeletal and dental systems. Bone, calcifying cartilage and tendon, denti n, cementum and enamel mineral is a calcium phosphate, most often referred to as apatite and commonly denoted as Ca-10(PO4)(6)(OH)(2). The mineral is composed of crystals of a unique size and shape, having an unusual chemistr y including similar to 3-5% carbonate and 5-10% [HPO4] (2-), and serving as a reservoir for other cationic and anionic species. Apatite composition va ries in the type and degree of ion substitution, number of atomic vacancies , crystallinity, and age and maturation Nucleation, growth, and development of the crystals are mediated by organic matrix molecules specific for each tissue, notably collagen in all except enamel. Amelogenin protein modulate s apatite formation in part in the latter tissue. The interactions between such organic molecules and the mineral crystals are complex and not entirel y understood, but they ultimately lead to organic-inorganic composites with remarkable integrity, mechanical strength, distinct form and additional ph ysical properties that are functionally representative.