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A review of phosphate mineral nucleation in biology and geobiology

机译:磷酸盐矿物成核的生物学和地球生物学研究进展

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摘要

Relationships between geological phosphorite deposition and biological apatite nucleation have often been overlooked. However, similarities in biological apatite and phosphorite mineralogy suggest that their chemical formation mechanisms may be similar. This review serves to draw parallels between two newly described phosphorite mineralization processes, and proposes a similar novel mechanism for biologically controlled apatite mineral nucleation. This mechanism integrates polyphosphate biochemistry with crystal nucleation theory. Recently, the roles of polyphosphates in the nucleation of marine phosphorites were discovered. Marine bacteria and diatoms have been shown to store and concentrate inorganic phosphate (Pi) as amorphous, polyphosphate granules. Subsequent release of these P reserves into the local marine environment as Pi results in biologically induced phosphorite nucleation. Pi storage and release through an intracellular polyphosphate intermediate may also occur in mineralizing oral bacteria. Polyphosphates may be associated with biologically controlled apatite nucleation within vertebrates and invertebrates. Historically, biological apatite nucleation has been attributed to either a biochemical increase in local Pi concentration or matrix-mediated apatite nucleation control. This review proposes a mechanism that integrates both theories. Intracellular and extracellular amorphous granules, rich in both calcium and phosphorus, have been observed in apatite-biomineralizing vertebrates, protists, and atremate brachiopods. These granules may represent stores of calcium-polyphosphate. Not unlike phosphorite nucleation by bacteria and diatoms, polyphosphate depolymerization to Pi would be controlled by phosphatase activity. Enzymatic polyphosphate depolymerization would increase apatite saturation to the level required for mineral nucleation, while matrix proteins would simultaneously control the progression of new biological apatite formation.
机译:地质磷矿沉积与生物磷灰石成核之间的关系经常被忽略。然而,生物磷灰石和磷矿矿物学的相似性表明它们的化学形成机理可能相似。这项审查旨在绘制两个新描述的磷矿成矿过程之间的相似之处,并提出了一种类似的新型机制,可生物控制磷灰石矿物成核。该机制将多磷酸盐生物化学与晶体成核理论相结合。最近,发现了多磷酸盐在海洋磷矿成核中的作用。海洋细菌和硅藻已显示出可以存储和浓缩无定形多磷酸盐颗粒的无机磷酸盐(Pi)。这些磷储备随后释放到当地海洋环境中,这是由于Pi导致生物诱导的磷矿成核。 Pi的储存和通过细胞内多磷酸盐中间体的释放也可能发生在矿化口腔细菌中。多磷酸盐可能与脊椎动物和无脊椎动物中的生物控制的磷灰石成核有关。从历史上看,生物磷灰石成核是由于局部Pi浓度的生化增加或基质介导的磷灰石成核控制所致。这篇综述提出了一种将两种理论融为一体的机制。在磷灰石生物矿化的脊椎动物,原生生物和腕足动物中观察到了富含钙和磷的细胞内和细胞外无定形颗粒。这些颗粒可以代表聚磷酸钙的储存。与细菌和硅藻产生的亚磷酸酯成核不同,多磷酸盐解聚为Pi的方式将受磷酸酶活性的控制。酶促多磷酸盐解聚反应将使磷灰石饱和度增加到矿物质成核所需的水平,而基质蛋白将同时控制新的生物磷灰石形成过程。

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