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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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https://doi.org/10.1007/978-3-642-92735-5nts in cartilage and bone. In both tissues mineralization is confined to restricted compartments within the intercellular matrix. Structural properties of these compartments are analyzed in relation to a possible cellular control of calcification. Special attention is paid to the role of matrix vesi
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https://doi.org/10.1007/978-94-010-3634-4ontent (see (14)). Of the proteins found in nature, collagen is one of the largest. In terms of structure and function, it is among the simplest. In contrast, its biosynthesis is complex in that the initial RNA transcripts of the genes must be extensively processed in order to generate the functiona
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Zur chirurgischen Anatomie des Felsenbeins,nown, their kinetics of formation in vivo are largely unknown. A general paradigm for the study of in vivo mineralization has yet to be developed. The whole subject area is rife with speculation and half-baked ideas, some of which are my own. Some kinetic and mechanistic data about urinary stones ar
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https://doi.org/10.1007/978-3-642-66820-3mportance, and introductory remarks on enamel structure and composition. Four different approaches on the mechanisms of the acid interaction with dental enamel are discussed: a) the semipermeable membrane mechanism, in which a pH drop in the enamel is thought to be due to large positively charged mu
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Zur chirurgischen Anatomie des Felsenbeins,s, cell types and distribution, bathing fluids, and activities. Mineralized “compartments” are found in association with unicellular plants and animals and in species of most phyla of multicellular plants and animals. These minerals may be found in both intracellular preferred sites and in uniquely
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