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Apatite mineralization in teeth of the chiton Acanthopleura echinata
Journal article   Peer reviewed

Apatite mineralization in teeth of the chiton Acanthopleura echinata

A.P. Lee, L.R. Brooker, D.J. Macey, W. van Bronswijk and J. Webb
Calcified Tissue International, Vol.67(5), pp.408-415
2000
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Abstract

Raman spectroscopy has been used to demonstrate, for the first time, that calcium mineralization in the core of the major lateral teeth of the chiton Acanthopleura echinata takes place as an ordered process, with crystalline carbonated apatite being the first mineral deposited. Deposition begins at the top of the tooth core, under the so-called tab region, progresses down the interior surface of the tab and lepidocrocite layer, and then extends outwards to the anterior surface. Mineralization is not initiated until the lepidocrocite layer has isolated the core of the tooth from the magnetite cap. The last region to be infiltrated is the anterior basal region of the tooth cusp, immediately above the junction zone. The junction zone is also a region of high ion density, as determined by energy dispersive spectroscopy (EDS) analysis, but we show here for the first time that it is free of mineral deposits, acting instead as a transfer and storage region.

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Collaboration types
Domestic collaboration
Citation topics
2 Chemistry
2.165 Nanofibers, Scaffolds & Fabrication
2.165.1082 Calcium Carbonate Crystallization
Web Of Science research areas
Endocrinology & Metabolism
ESI research areas
Biology & Biochemistry
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