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Time lapse imaging techniques for comparison of mineralization dynamics in primary murine osteoblasts and the late osteoblast/early osteocyte-like cell line MLO-A5.

机译:延时成像技术,用于比较原代鼠成骨细胞和晚期成骨细胞/早期骨细胞样细胞系MLO-A5的矿化动力学。

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Mineralization of bone matrix and osteocyte differentiation occur simultaneously and appear interrelated both spatially and temporally. Although these are dynamic events, their study has been limited to using static imaging approaches, either alone or in combination with chemical and biochemical analysis and/or genetic manipulation. Here we describe the application of live cell imaging techniques to study mineralization dynamics in primary osteoblast cultures compared to a late osteoblast/early osteocyte-like cell line, MLO-A5. Mineral deposition was monitored using alizarin red as a vital stain for calcium. To monitor differentiation into an osteocyte-like phenotype, the calvarial cells were isolated from transgenic mice expressing green fluorescent protein (GFP) driven by an 8-kb dentin matrix protein-1 (Dmp1) promoter that gives osteocyte-selective expression. Time lapse imaging showed that there was a lag phase of 15-20 h after beta-glycerophosphate addition, followed by mineral deposition that wasrapid in primary osteoblast cultures but more gradual in MLO-A5 cultures. In primary osteoblast cultures, mineral was deposited exclusively in association with clusters of cells expressing Dmp1-GFP, suggesting that they were already differentiating into osteocyte-like cells. In MLO-A5 cells, the first indication of mineralization was the appearance of punctate areas of alizarin red fluorescence of 4-7 mum in diameter, followed by mineral deposition throughout the culture in association with collagen fibrils. A high amount of cell motility was observed within mineralizing nodules and in mineralizing MLO-A5 cultures. These studies provide a novel approach for analyzing mineralization kinetics that will enable us to dissect in a time-specific manner the essential players in the mineralization process.
机译:骨基质的矿化和骨细胞的分化同时发生,并在空间和时间上相互关联。尽管这些是动态事件,但他们的研究仅限于使用静态成像方法,无论是单独使用还是与化学和生化分析和/或基因操作结合使用。在这里,我们描述了活细胞成像技术在研究成骨细胞与早期成骨细胞/早期骨细胞样细胞系MLO-A5相比的矿化动力学中的应用。使用茜素红作为钙的重要染色剂来监测矿物质的沉积。为了监测向骨细胞样表型的分化,从表达绿色荧光蛋白(GFP)的转基因小鼠中分离了颅骨细胞,该绿色荧光蛋白由提供骨细胞选择性表达的8-kb牙本质基质蛋白-1(Dmp1)启动子驱动。延时成像显示,添加β-甘油磷酸后有一个15-20小时的滞后阶段,随后是矿物质沉积,在原代成骨细胞培养物中迅速消失,而在MLO-A5培养物中逐渐消失。在原代成骨细胞培养物中,矿物质仅与表达Dmp1-GFP的细胞簇相关地沉积,表明它们已经分化为骨细胞样细胞。在MLO-A5细胞中,矿化的第一个迹象是出现了直径为4-7微米的茜素红色荧光的点状区域,随后是整个培养物中的矿物质沉积以及胶原纤维。在矿化的结节和矿化的MLO-A5培养物中观察到大量的细胞运动。这些研究提供了一种新颖的方法来分析矿化动力学,这将使我们能够以特定时间的方式剖析矿化过程中的重要参与者。

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