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Structural organisation of the cusps of the radula teeth of the chiton Plaxiphora albida
Journal article   Peer reviewed

Structural organisation of the cusps of the radula teeth of the chiton Plaxiphora albida

D J Macey, Lesley R Brooker, J A Webb and T G St. Pierre
Acta Zoologica, Vol.77(4), pp.287-294
1996
url
https://doi.org/10.1111/j.1463-6395.1996.tb01274.xView
Published Version

Abstract

Zoology radula teeth chiton Plaxiphora albida
The structure, morphology and organisation of the cusps of the major lateral radula teeth of the chiton Plaxiphora albida have been examined using light, transmission and scanning electron microscopy, together with energy dispersive X-ray analysis and Mössbauer spectroscopy. In this chiton species, both the anterior and posterior surfaces of the major lateral teeth are composed of magnetite, which is indicated to be non-stoichiometric and associated with some maghemite, together with small amounts of phosphorus and silicon. This outer layer surrounds an inner core region of the tooth, which only reaches the surface through a small window zone on the anterior surface and which contains large amounts of iron and phosphorus presumably in the form of iron(III) phosphate. The organic matrix, on which the teeth are constructed, consists of a zone of densely packed fine fibres at the surface of the tooth, underlain by larger fibres which become sparser deeper into the cusp. The core region is characterized by the presence of densely packed short fibres. In contrast to the situation found in most other species of chiton, large fibres of the organic matrix extend throughout the region of magnetite mineralization, leading to the suggestion that the matrix exerts more control over the mineralization of magnetite than has previously been thought.

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Anatomy & Morphology
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