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首页> 外文期刊>The Biochemical Journal >Natural variation in the extent of phosphorylation of bone phosphoproteins as a function of in vivo new bone formation induced by demineralized bone matrix in soft tissue and bony environments.
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Natural variation in the extent of phosphorylation of bone phosphoproteins as a function of in vivo new bone formation induced by demineralized bone matrix in soft tissue and bony environments.

机译:骨磷蛋白磷酸化程度的自然变化与软组织和骨骼环境中脱矿质骨基质诱导的体内新骨形成有关。

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Implants of allogenic demineralized bone matrix were placed in distinct in vivo environments, i.e. calvarial (bony) and subcutaneous (soft tissue) sites. Detailed analyses of the biochemical components were performed. Quantitative levels of osteopontin (OPN), bone sialoprotein (BSP) and calcium phosphate (Ca-P) deposition within each implant environment varied as a function of new bone formation, and were substantially different in samples from calvarial and subcutaneous sites. Quantification of the extent of phosphorylation of affinity-purified OPN and BSP from such implants indicated that: (i) the number of mols of phosphoserine (P-Ser)/mol of affinity-purified OPN or BSP varied as a function of implant time and bone formation within both implant sites, and (ii) the 'effective P-Ser concentration' provided by the total OPN and BSP within each implant site varied and increased as a function of time, being approx. 5-fold higher for BSP in calvarial compared with subcutaneous implants. Peak levels of mols of P-Ser/mol of BSP coincided with maximum rates of Ca-P deposition in calvarial implants. Levels of OPN phosphorylation from both calvarial and subcutaneous implants also indicated fluctuations as a function of bone formation. Hence the present study, for the first time, provides direct evidence of natural variation in the extent of phosphorylation of both OPN and BSP as a function of time of mineralized tissue formation. Further evaluation of the data provides the first evidence of a direct and linear relationship between the rate of Ca-P deposition and the ratio of P-Ser-BSP/P-Ser-OPN for calvarial implants. Data for subcutaneous implants failed to provide such correlation. Overall, the present work demonstrates that the natural biological progression of the process of biomineralization follows strict criteria consistent with the anatomical location. Biomineralization fails to proceed in the same way in a soft tissue environment.
机译:同种异体脱钙骨基质的植入物被放置在不同的体内环境中,即颅骨(骨)和皮下(软组织)部位。进行了生化成分的详细分析。在每个植入物环境中,骨桥蛋白(OPN),骨唾液蛋白(BSP)和磷酸钙(Ca-P)的沉积水平随新骨形成的变化而变化,并且在颅盖和皮下部位的样品中存在显着差异。对此类植入物中亲和纯化的OPN和BSP磷酸化程度的量化表明:(i)亲和纯化的OPN或BSP的磷酸丝氨酸(P-Ser)摩尔数/摩尔随植入时间的变化而变化,并且(ii)每个植入部位内总OPN和BSP所提供的“有效P-Ser浓度”随时间的变化而变化,并随时间增加,大约为2。与皮下植入物相比,颅骨中BSP的含量高5倍。 P-Ser摩尔/ BSP摩尔的峰值水平与颅盖植入物中Ca-P沉积的最大速率一致。颅骨和皮下植入物的OPN磷酸化水平也表明,波动是骨形成的函数。因此,本研究首次提供了直接的证据,证明了OPN和BSP的磷酸化程度随矿化组织形成时间的变化而自然变化。数据的进一步评估为颅盖植入物的Ca-P沉积速率与P-Ser-BSP / P-Ser-OPN之比之间的直接和线性关系提供了第一个证据。皮下植入物的数据未能提供这种相关性。总的来说,目前的工作表明生物矿化过程的自然生物学进展遵循与解剖位置一致的严格标准。生物矿化在软组织环境中无法以相同的方式进行。

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