Abstract
The organic matrix in molluscan shells can be roughly divided into a water-soluble and a water-inso1uble matrix, those demarcation between which is sometimes not quite clear. Ca-binding components have been isolated from the water-soluble matrix [1,2]. Because of the capacity of such components for binding of Ca2+, many authors have postulated reactions whereby these molecules might promote nucleation of CaCO3 crystals [3,4]. Although diversity of matrices has been reported by many authors [5, 6], the complete fractionation of such a matrix and the identificaiton of each component, contained in the matrix have not yet been achieved.
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© 1991 Springer-Verlag Tokyo
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Samata, T. (1991). Structure and Function of the Organic Matrix in the Nacreous Layer of Pinctada fucata . In: Suga, S., Nakahara, H. (eds) Mechanisms and Phylogeny of Mineralization in Biological Systems. Springer, Tokyo. https://doi.org/10.1007/978-4-431-68132-8_4
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DOI: https://doi.org/10.1007/978-4-431-68132-8_4
Publisher Name: Springer, Tokyo
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