Comparative Biochemistry and Physiology Part A 120 (1998) 551 – 556
Movement of water in fish otoliths
R.W. Gauldie *, C.E. Thacker, I.F. West, L. Wang
Hawaii Institute of Geophysics and Planetology, School of Ocean, Earth Sciences and Technology, Uniersity of Hawaii, 2525 Correa Road,
Honolulu, HI 96822, USA
Received 28 March 1996; received in revised form 12 March 1998; accepted 1 May 1998
Abstract
The diffusion of small organic and inorganic solvent molecules and larger dye molecules into fish otoliths has long been utilized
in clearing and staining otoliths to facilitate age estimation studies. This study quantifies the diffusivity of water into otoliths of
Beryx splendens as a general analog of small molecule diffusivity in otoliths. The effects on the optical properties of otoliths of
the diffusion of solvent and dye molecules into otoliths are also discussed. © 1998 Elsevier Science Inc. All rights reserved.
Keywords: Otolith; Diffusion; Water; Beryx splendens
1. Introduction
Recent studies [21,22] have shown that the chemical
composition of fish otoliths change when they are
soaked in water or ethanol because many ions (Na
+
,
Cl
-
, etc.) are not bound in the crystal structure of the
otolith and diffuse out of the otolith into surrounding
fluid. Similarly, direct measurements have shown that
the large
222
Rn molecule, the intermediate daughter
product in the radioactive decay of
226
Ra to
210
Pb, also
diffuses out of otoliths [9]. Diffusion of ions out of the
otolith draws attention to the reverse process, diffusion
of ions and molecules into the otolith.
There has always been indirect evidence for the ready
diffusion of water and other solvents into otoliths.
Otoliths are often treated with substances such as wa-
ter, oil, solvents and dyes to facilitate reading their
optical patterns. The diffusion of water into otoliths
causes an increase in light transmission, hence the use
of the term ‘clearing’ in the otolith literature. The
optical patterns of teleost otoliths are widely used both
for aging and extracting life history patterns of fish.
Numerous optical techniques exist for reading the in-
formation stored in otoliths; they range from viewing
whole otoliths under a light microscope, through exam-
ination of broken and burned sections under oil, to
counting microincrements [2,15,26,29]. Otoliths may
also be cleared with substances such as water, glycerin,
alcohols or xylene to increase the contrast of internal
features [2,15,18]. These procedures are effective be-
cause the crystal structure of the otolith is porous and
rapidly takes up fluids. Dyes that react with calcified
tissues have also been used to stain otoliths. Calcium-
specific stains such as alizarin red and calcein, as well as
the antibiotic tetracycline, produce bands on otoliths
that are discernible under visible as well as ultraviolet
light [1,7,23,28]. Non-calcium-specific stains such as
fluorescein have been used to increase the internal
contrast of otoliths [5]. Flain [5] also reported clearing
of otoliths rendered opaque by formalin by soaking
them for at least a week in a 3% solution of trisodium
orthophosphate. These techniques are used not only to
facilitate estimates of age, but also to mark fish for later
identification. This paper provides a quantitative mea-
sure of the uptake of water molecules into the otolith
that can be used as an analog of small molecule diffu-
sion in otoliths.
* Corresponding author. Present address: 76 Inglis Street, Seatoun,
Wellington, New Zealand. Tel.: +64 4 3885486.
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