Amizuka Norio, Hasegawa Tomoka, Oda Kimimitsu, Luiz de Freitas Paulo Henrique, Hoshi Kazuto, Li Minqi, Ozawa Hidehiro
Department of Developmental Biology of Hard Tissue, Graduate School of Dental Medicine, Hokkaido University, Sapporo, Japan.
Front Biosci (Elite Ed). 2012 Jan 1;4(6):2085-100. doi: 10.2741/e526.
Cartilage calcification is carried out by chondrocytes as they hypertrophy and begin to secrete matrix vesicles. Calcification initiates when calcium phosphates appear inside these matrix vesicles, forming hydroxyapatite crystals that eventually break through the membrane to form calcifying globules, as in bone calcification. However, the extracellular environment in cartilage is different from that in bone: cartilage is abundant in proteoglycans but contains a small amount of osteopontin. Hypertrophic chondrocytes secrete vesicles in the cartilaginous matrix of intercolumnar septae only, forming well-calcified longitudinal septae and poorly-calcified transverse partitions. Such pattern of vesicle deposition permits the invasion of endothelial cells, which infiltrate into cartilage and induce migration of osteogenic and osteoclastic cells. Osteoclasts resorb the excess of calcified globules in the partitions, shaping calcified cartilage cores paralleling the longitudinal axis of long bones. After the formation of these calcified cartilage cores, endochondral ossification involves a series of well-defined events in which osteogenic cells deposit new bone onto the cartilage core and form primary trabecules. This review presents the histology of epiphyseal cartilage calcification and endochondral ossification.
软骨钙化是由软骨细胞在肥大并开始分泌基质小泡时进行的。当磷酸钙出现在这些基质小泡内时,钙化开始,形成羟基磷灰石晶体,最终突破膜形成钙化小球,就像在骨钙化中一样。然而,软骨中的细胞外环境与骨中的不同:软骨富含蛋白聚糖,但骨桥蛋白含量较少。肥大的软骨细胞仅在柱状间隔的软骨基质中分泌小泡,形成钙化良好的纵向间隔和钙化不良的横向分隔。这种小泡沉积模式允许内皮细胞侵入,内皮细胞渗入软骨并诱导成骨细胞和破骨细胞迁移。破骨细胞吸收分隔中多余的钙化小球,形成与长骨纵轴平行的钙化软骨核心。在这些钙化软骨核心形成后,软骨内成骨涉及一系列明确的事件,其中成骨细胞在软骨核心上沉积新骨并形成初级小梁。本综述介绍了骨骺软骨钙化和软骨内成骨的组织学。