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The biomineralization of otoliths results mainly from the release of soluble Ca 2+ , which is in turn precipitated as CaCO 3 crystals. In some Carapidae, sagittae sections have been shown to reveal a three-dimensional asymmetry with a nucleus close to the sulcal side, an unusual position. This study seeks to understand otolith formation in Carapus boraborensis. The unusual shape of...
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