磷灰石
碱性磷酸酶
矿化(土壤科学)
化学
周质间隙
生物矿化
结晶
磷酸盐
钙
无机化学
磷酸酶
酸性磷酸酶
矿物学
大肠杆菌
生物化学
化学工程
酶
有机化学
氮气
工程类
基因
作者
Agnès Hirschler,Jacques Lucas,J. Hubert
标识
DOI:10.1080/01490459009377877
摘要
Abstract Apatite formation from organic matter (ribonucleic acid) and calcium carbonate (cuttlebone) requires intervention of microorganisms. We have attempted to characterize this mineral formation process by locating the alkaline phosphatase and the crystals formed. Alkaline phosphatase, which is important for the liberation of the necessary components, was localized in the periplasmic space of Providencia rettgeri in the same manner as in Escherichia coli. Accordingly, the release of inorganic phosphate and the formation of apatite may occur at this site. However, electron microscope observations revealed the presence of extracellular apatite; moreover, apatite particles that were formed with or without bacteria (with alkaline phosphatase from hydrolyzed ribonucleic acid as phosphorus source) were closely similar in size and appearance. The formation of apatite can thus be qualified as biologically induced mineralization. Nevertheless, a bacterial cell can also act as a nucleator for apatite crystallization, but this would appear exceptional.
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