首页> 外文期刊>Journal of bone and mineral research: the official journal of the American Society for Bone and Mineral Research >Subcellular elevation of cytosolic free calcium is required for osteoclast migration
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Subcellular elevation of cytosolic free calcium is required for osteoclast migration

机译:破骨细胞迁移需要细胞内游离钙的亚细胞升高

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Osteoclasts are multinucleated cells responsible for the resorption of bone and other mineralized tissues during development, physiological remodeling, and pathological bone loss. Osteoclasts have the ability to resorb substrate while concurrently migrating. However, the subcellular processes underlying migration are not well understood. It has been proposed that, in other cell types, cytosolic free Ca2+ concentration ([Ca2+]i) regulates cell protrusion as well as retraction. Integration of these distinct events would require precise spatiotemporal patterning of subcellular Ca 2+. The large size of osteoclasts offers a unique opportunity to monitor patterns of Ca2+ during cell migration. We used ratiometric imaging to map [Ca2+]i within rat and mouse osteoclasts. Migration was characterized by lamellipodial outgrowth at the leading edge, along with intermittent retraction of the uropod. Migrating osteoclasts displayed elevation of [Ca2+]i in the uropod, that began prior to retraction. Dissipation of this [Ca2+]i gradient by loading osteoclasts with the Ca2+ chelator BAPTA abolished uropod retraction, on both glass and mineralized substrates. In contrast, elevation of [Ca2+]i using ionomycin initiated prompt uropod retraction. To investigate downstream effectors, we treated cells with calpain inhibitor-1, which impaired uropod retraction. In contrast, lamellipodial outgrowth at the leading edge of osteoclasts was unaffected by any of these interventions, indicating that the signals regulating outgrowth are distinct from those triggering retraction. The large size of mature, multinucleated osteoclasts allowed us to discern a novel spatiotemporal pattern of Ca 2+ involved in cell migration. Whereas localized elevation of Ca 2+ is necessary for uropod retraction, lamellipod outgrowth is independent of Ca2+ - a heretofore unrecognized degree of specificity underlying the regulation of osteoclast migration.
机译:破骨细胞是多核细胞,负责发育,生理重塑和病理性骨丢失期间骨骼和其他矿化组织的吸收。破骨细胞具有在同时迁移的同时吸收底物的能力。然而,关于迁移的亚细胞过程还没有被很好地理解。已经提出,在其他细胞类型中,胞浆中游离的Ca2 +浓度([Ca2 +] i)会调节细胞的突出和收缩。这些不同事件的整合将需要精确的时空模式的亚细胞Ca 2+。大尺寸的破骨细胞提供了独特的机会来监控细胞迁移过程中Ca2 +的模式。我们使用比例成像来绘制大鼠和小鼠破骨细胞中的[Ca2 +] i。迁移的特征是前沿的片状脂质体生长,以及尾足的间歇性收缩。移生的破骨细胞在尾足中显示出[Ca2 +] i的升高,这是在收回之前开始的。通过向破骨细胞中加入Ca2 +螯合剂BAPTA来消除[Ca2 +] i梯度,可消除玻璃和矿化基质上的uropod缩回。相比之下,使用离子霉素升高[Ca2 +] i会导致尾足类动物迅速缩回。为了研究下游效应子,我们用钙蛋白酶抑制剂-1处理了细胞,钙蛋白酶抑制剂-1损害了uropod的回缩。相反,破骨细胞前缘的片状脂质体生长不受这些干预措施的影响,表明调节生长的信号与触发收缩的信号不同。成熟的多核破骨细胞很大,这使我们能够辨别参与细胞迁移的新型Ca 2+时空模式。 Ca2 +的局部升高对于尾足的缩回是必需的,而lamellipod的生长则独立于Ca2 +-破骨细胞迁移的调控迄今尚未被认识到的特异性程度。

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