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Aca - Departamento de Física - Universidad Técnica Federico Santa ...

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V Encuentro Sud Americano <strong>de</strong> Colisiones Inelásticas en la Materia<br />

Chemical Characterization of Fish-Otoliths using Micro-PIXE<br />

Stori, E. M. 1 , Dias, J. F. 1 , Favero, J. M. 2 , Dias, J. F. 2<br />

1 Laboratório <strong>de</strong> Implantação Iônica – Instituto <strong>de</strong> <strong>Física</strong>, Universida<strong>de</strong> Fe<strong>de</strong>ral do Rio Gran<strong>de</strong> do Sul, Av. Bento<br />

Gonçalves 9500, Porto Alegre, RS , Brasil<br />

2 Instituto <strong>de</strong> Oceanografia – Universida<strong>de</strong> Estadual <strong>de</strong> São Paulo – São Paulo, SP, Brasil<br />

email address corresponding author: elistori@gmail.com<br />

Fishes contain a group of three pairs of<br />

bone structures in their ear that are responsible<br />

for hearing and equilibrium. These structures<br />

grow in layers that look like rings if<br />

sectioned (figure 1). [1]<br />

of interest and its position in the otolith.<br />

[5][6]<br />

The knowledge of the trace elements<br />

present in different rings would allow to establish<br />

a relation between different places the<br />

fish have lived and the stages of its life.<br />

Figure 2 shows calcium maps of a juvenile<br />

fish otolith, in which can be observed<br />

the growth rings through the difference of<br />

intensity of the calcium signal.<br />

Figure 1. Sectioned otolith showing growth rings [2]<br />

There are very well <strong>de</strong>veloped studies<br />

that relate the rings in the otoliths with the<br />

fishes’ age. While in adult’s otoliths the rings<br />

may represent years of age, in juvenile fishes<br />

and larvae the rings represent days. [1]<br />

Moreover, the otoliths may give information<br />

of fish migration pattern or their origin<br />

by <strong>de</strong>termining the trace elements contained<br />

in them. [3][4]<br />

The micro-PIXE technique (micro-<br />

Particle Induced X-Ray Emission) is not<br />

regularly used to <strong>de</strong>termine trace elements in<br />

otoliths. Its advantages inclu<strong>de</strong> the non<strong>de</strong>structive<br />

character of the technique, and<br />

the possibility of a spacial characterization of<br />

the elements, enabling a more accurate analysis<br />

of the relation between the trace element<br />

(a)<br />

(b)<br />

Figure 2. Calcium maps of a juvenile fish otolith (a)<br />

the entire otolith and (b) a more <strong>de</strong>tailed map of the<br />

central region of the otolith.<br />

20 Valparaíso, Chile

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