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- W2382108770 abstract "Biosilica, more specifically hydrated amorphous silica, often referred to as opal, is the second most abundant mineral type formed by organisms, with only the carbonate minerals exceeding it in abundance and distribution. As the predominant contributor to biosilica in the oceans, diatoms are known for the intricate geometries and spectacular patterns of their silica- based cell walls. Biochemical studies demonstrate that diatom biosilica is a composite material containing several general organic components in addition to inorganic silica, such as polysaccharides, long-chain polyamines and zwitterionic proteins. Functional studies on these organic components indicate that they play a crucial role in guiding silica precipitation as well as in the formation of species-specific nanopatterns. This article gives an overview of current knowledge on the function of above-mentioned organic and biological molecules in biosilicification. Moreover, some studies of biomimetic mineralization using model organic additives and in vitro experiments using molecules extracted from organisms are also involved. An insight into the silicification mechanisms in diatoms will link the global cycles for Si and C mechanistically, whereas identification and classification of the components in diatoms may assist us in deeper understanding of material sources of petroleum and the evolutionary development of diatoms." @default.
- W2382108770 created "2016-06-24" @default.
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- W2382108770 date "2011-01-01" @default.
- W2382108770 modified "2023-09-22" @default.
- W2382108770 title "Organic Matrix-Mineral Interaction during Cell Wall Silicification in Diatoms" @default.
- W2382108770 hasPublicationYear "2011" @default.
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