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Titlebook: Biological Mineralization and Demineralization; Report of the Dahlem G. H. Nancollas Conference proceedings 1982 Dr. S. Bernhard, Dahlem Ko

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期刊全称Biological Mineralization and Demineralization
期刊简称Report of the Dahlem
影响因子2023G. H. Nancollas
视频video
学科分类Dahlem Workshop Report
图书封面Titlebook: Biological Mineralization and Demineralization; Report of the Dahlem G. H. Nancollas Conference proceedings 1982 Dr. S. Bernhard, Dahlem Ko
影响因子normal and pathological mineralization in vertebrates but also with the interesting problems involved in the formation of in­ tracellular deposits of calcium oxalate in plants. Here cal­ cium carbonate and silica may also be involved in the mineral­ ization processes. Calcium carbonate is an important component in the formation of mollusc and avian shells. The observation that both calcite and aragonite may be formed in biogenic cal­ cium carbonate raises important questions as to what factors control the formation of the final mineral phase. There is little doubt that thermodynamically less stable phases may be kinetically stabilized for long periods of time by other mole­ cules present in vivo. In normal mineralization, calcium salts may initially be deposited both within the cells and extracel­ lularly. In the latter case, the role of matrix vesicles and the ways in which the matrix components might control mineral­ ization were especially emphasized. There is clearly a need for more structural and functional information involving cells, matrix components, and their associated crystals. The develop­ ment of further techniques involving mutants, chromofluors, and fixatives for pr
Pindex Conference proceedings 1982
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The Mechanisms of Chrystal Growth and Dissolution,al lattice. Also ripening, agglomeration, epitaxy, and inhibition are treated. Future progress will be assisted by measurements of well-defined parameters in simple solutions parallel with experiments in “biological media,” and interpretation in terms of precise molecular models.
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Structure, Properties, and Function of Mineralized Tissue Components Group Report,on, etc. The precision of replication of mineral form, type, and distribution in each species is impressive and argues for the existence of finely tuned initiating and regulatory factors, restrictive volumes, and critical surfaces that modulate these mineral forms.
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Mechanisms of Normal Biological Mineralization of Calcium Carbonates,lluscs is primarily a sulfated, high molecular weight glycoprotein that selectively binds calcium. This glycoprotein is assigned a primary role in crystal nucleation in the ionotropic nucleation hypothesis. Postnucleation growth may be controlled in varying degrees by the bathing medium and by the insoluble matrix.
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