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Sturgeon and paddlefish (Acipenseridae) sagittal otoliths are composed of the calcium carbonate polymorphs vaterite and calcite.

Identifieur interne : 000031 ( Main/Merge ); précédent : 000030; suivant : 000032

Sturgeon and paddlefish (Acipenseridae) sagittal otoliths are composed of the calcium carbonate polymorphs vaterite and calcite.

Auteurs : B M Pracheil [États-Unis] ; B C Chakoumakos [États-Unis] ; M. Feygenson [États-Unis] ; G W Whitledge [États-Unis] ; R P Koenigs [États-Unis] ; R M Bruch [États-Unis]

Source :

Journal of fish biology [ 1095-8649 ] ; 2016.

RBID : pubmed:27461067

Abstract

This study sought to resolve whether sturgeon (Acipenseridae) sagittae (otoliths) contain a non-vaterite fraction and to quantify how large a non-vaterite fraction is using neutron diffraction analysis. This study found that all otoliths examined had a calcite fraction that ranged from 18 ± 6 to 36 ± 3% by mass. This calcite fraction is most probably due to biological variation during otolith formation rather than an artefact of polymorph transformation during preparation.

DOI: 10.1111/jfb.13085
PubMed: 27461067

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Le document en format XML

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Sturgeon and paddlefish (Acipenseridae) sagittal otoliths are composed of the calcium carbonate polymorphs vaterite and calcite.

Sturgeon and paddlefish (Acipenseridae) sagittal otoliths are composed of the calcium carbonate polymorphs vaterite and calcite.

Source :

Abstract

Links toward previous steps (curation, corpus...)

Links to Exploration step

Le document en format XML

Pour manipuler ce document sous Unix (Dilib)

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Pour générer des pages wiki