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基质小泡的分子生物学

Molecular biology of matrix vesicles.

作者信息

Anderson H C

机构信息

Department of Pathology and Laboratory Medicine, University of Kansas Medical Center, Kansas City 66160, USA.

出版信息

Clin Orthop Relat Res. 1995 May(314):266-80.

PMID:7634645
Abstract

Matrix vesicles are extracellular 100-nanometer-diameter membrane-invested particles selectively located within the matrix of bone, cartilage, and predentin. They serve as the initial site of calcification in all skeletal tissues. Matrix vesicle biogenesis occurs by polarized budding and pinching off of vesicles from specific regions of the outer plasma membrane of chondrocytes, osteoblasts, and odontoblasts. Seeding of selected areas of matrix with matrix vesicles explains the localized distribution of subsequent zones of mineralization. Matrix vesicle biogenesis in the growth plate is linked to the chondrocyte cell cycle and reflects a stage in programmed cell death (apoptosis). Generation of initial hydroxyapatite mineral crystals occurs within the matrix vesicle membrane during Phase 1 of biologic mineralization. Phase 1 is controlled by phosphatases (including alkaline phosphatase) and Ca-binding molecules with which the matrix vesicles are well endowed. Phase 2 of biologic mineralization begins with breakdown of matrix vesicle membranes, exposing preformed hydroxyapatite to the extracellular fluid after which mineral crystal proliferation is governed by extracellular conditions. Phase 1 and Phase 2 of mineralization are under cellular control. Phase 1 is initiated by cells generating calcifiable matrix vesicles and releasing them into sites of intended calcification. Phase 2 is controlled by cells regulating extracellular ionic conditions and matrix composition.

摘要

基质小泡是直径为100纳米的细胞外膜包颗粒,选择性地位于骨、软骨和前期牙本质的基质中。它们是所有骨骼组织钙化的起始部位。基质小泡的生物发生是通过软骨细胞、成骨细胞和成牙本质细胞外质膜特定区域的极化出芽和小泡掐断来实现的。用基质小泡对基质的选定区域进行播种解释了随后矿化区域的局部分布。生长板中的基质小泡生物发生与软骨细胞周期相关,并反映了程序性细胞死亡(凋亡)的一个阶段。在生物矿化的第1阶段,初始羟基磷灰石矿物晶体在基质小泡膜内形成。第1阶段由磷酸酶(包括碱性磷酸酶)和基质小泡中富含的钙结合分子控制。生物矿化的第2阶段始于基质小泡膜的破裂,使预先形成的羟基磷灰石暴露于细胞外液,此后矿物晶体的增殖受细胞外条件控制。矿化的第1阶段和第2阶段受细胞控制。第1阶段由产生可钙化基质小泡并将其释放到预期钙化部位的细胞启动。第2阶段由调节细胞外离子条件和基质组成的细胞控制。

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