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.
| Original language | English |
|---|---|
| Pages (from-to) | 549-558 |
| Number of pages | 10 |
| Journal | Journal of Fish Biology |
| Volume | 90 |
| Issue number | 2 |
| DOIs | |
| State | Published - Feb 1 2017 |
Keywords
- Acipenser fulvescens