Akisaka T, Gay C V
Am J Anat. 1985 Aug;173(4):269-86. doi: 10.1002/aja.1001730404.
The epiphyseal cartilage in mouse tibia and fibula was investigated with the freeze-fracture method. Cytodifferentiation of growth plate chondrocytes was found to be marked by changes in both cell membrane and extracellular matrix vesicle membranes. Exocytosis and endocytosis were observed in all zones of differentiation, with endocytosis being predominant in the reserve and proliferative zones and exocytosis occurring with greatest frequency during hypertrophy. Intramembraneous particles (IMPs) on the plasma membrane were distributed evenly on the reserve and proliferative cell membranes, whereas in the hypertrophic zone IMPs tended to be distributed asymmetrically. Several types of matrix vesicles were identifiable on the basis of IMP distribution: IMP-free, IMP-aggregated, and IMP-random. The distribution pattern of IMPs on vesicles varied with differentiation of the chondrocytes. For proliferative and prehypertrophic cells, most matrix vesicles belonged to the IMP-random category. IMP-aggregated and IMP-free matrix vesicles became increasingly frequent in the later stages of differentiation, particularly in the late hypertrophic stage. IMPs were observed more frequently on the convex protoplasmic fracture face of matrix vesicles than on the concave exoplasmic fracture face, as was also observed for the plasma membrane. Matrix vesicles formation appears to occur by budding from chondrocyte projections and bulges at the smooth surfaces of the cells and from cell disintegration. Crystals of mineral were apparent in cross-fractured matrix vesicles of the calcifying zone, but not in the other zones.
采用冷冻断裂法对小鼠胫骨和腓骨的骨骺软骨进行了研究。发现生长板软骨细胞的细胞分化以细胞膜和细胞外基质小泡膜的变化为标志。在分化的所有区域均观察到胞吐作用和胞吞作用,其中胞吞作用在储备区和增殖区占主导,而胞吐作用在肥大期出现的频率最高。质膜上的膜内颗粒(IMPs)在储备细胞和增殖细胞膜上分布均匀,而在肥大区IMPs倾向于不对称分布。根据IMPs的分布可识别出几种类型的基质小泡:无IMPs、IMPs聚集和IMPs随机分布型。基质小泡上IMPs的分布模式随软骨细胞的分化而变化。对于增殖细胞和前肥大细胞,大多数基质小泡属于IMPs随机分布型。IMPs聚集和无IMPs的基质小泡在分化后期,尤其是肥大后期变得越来越常见。与质膜情况相同,在基质小泡的凸面原生质断裂面上观察到的IMPs比在凹面外质断裂面上更频繁。基质小泡的形成似乎是通过软骨细胞突起、细胞光滑表面的凸起以及细胞解体出芽而发生的。在钙化区的交叉断裂基质小泡中可见矿物质晶体,而在其他区域则没有。