Atomic force microscopy of the morphology of the matrix and mineral components of the otolith of Hyperoglyphe antarctica.

Abstract:

:The sagittal otolith of Hyperoglyphe antarctica (Centrolophidae: Teleostei) has a prismatic structure in which the anti-sulcal growth axes of each prism consist of a series of nested cones each composed of a mineral layer followed by an organic matrix layer. Broken sections show the mineral layers to be composed of stacks of crystals. Otolith matrix that has been decalcified and air-dried, or critical-pont-dried, retains a periodic structure of repeating high and low matrix density. At high magnifications, both broken whole crystal surfaces and decalcified matrix surfaces have a granular structure. Chloroxbleached whole otoliths also show a granular crystalline structure. At higher magnifications, the air-dried matrix showed a parallel fiber structure with similar dimensions to keratin fibers. © 1995 Wiley-Liss, Inc.

journal_name

J Morphol

journal_title

Journal of morphology

authors

Gauldie RW,Xhie J

doi

10.1002/jmor.1052230208

subject

Has Abstract

pub_date

1995-02-01 00:00:00

pages

203-214

issue

2

eissn

0362-2525

issn

1097-4687

journal_volume

223

pub_type

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