Blumer Michael J F
Department of Anatomy, Histology and Embryology, Institute of Clinical and Functional Anatomy, Medical University Innsbruck, Müllerstrasse 59, A-6010 Innsbruck, Austria.
Ann Anat. 2021 May;235:151704. doi: 10.1016/j.aanat.2021.151704. Epub 2021 Feb 16.
The bones are of mesenchymal or ectomesenchymal origin, form the skeleton of most vertebrates, and are essential for locomotion and organ protection. As a living tissue they are highly vascularized and remodelled throughout life to maintain intact. Bones consist of osteocytes entrapped in a mineralized extracellular matrix, and via their elaborated network of cytoplasmic processes they do not only communicate with each other but also with the cells on the bone surface (bone lining cells). Bone tissue develops through a series of fine-tuned processes, and there are two modes of bone formation, referred to either as intramembranous or endochondral ossification. In intramembranous ossification, bones develop directly from condensations of mesenchymal cells, and the flat bones of the skull, the clavicles and the perichondral bone cuff develop via this process. The bones of the axial (ribs and vertebrae) and the appendicular skeleton (e.g. upper and lower limbs) form through endochondral ossification where mesenchyme turns into a cartilaginous intermediate with the shape of the future skeletal element that is gradually replaced by bone. Endochondral ossification occurs in all vertebrate taxa and its onset involves differentiation of the chondrocytes, mineralization of the extracellular cartilage matrix and vascularization of the intermediate, followed by disintegration and resorption of the cartilage, bone formation, and finally - after complete ossification of the cartilage model - the establishment of an avascular articular cartilage. The epiphyseal growth plate regulates the longitudinal growth of the bones, achieved by a balanced proliferation and elimination of chondrocytes, and the question whether the late hypertrophic chondrocytes die or transform into osteogenic cells is still being hotly debated. The complex processes leading to endochondral ossification have been studied for over a century, and this review aims to give an overview of the histological and molecular events, arising from the long bones' (e.g. femur, tibia) development. The fate of the hypertrophic chondrocytes will be discussed in the light of new findings obtained from cell tracking studies.
骨骼起源于间充质或外间充质,构成大多数脊椎动物的骨架,对运动和器官保护至关重要。作为一种活组织,它们血管高度丰富,且在整个生命过程中不断重塑以保持完整。骨骼由包埋在矿化细胞外基质中的骨细胞组成,通过其精细的细胞质突起网络,它们不仅相互通信,还与骨表面的细胞(骨衬细胞)进行交流。骨组织通过一系列微调过程发育,有两种骨形成模式,即膜内成骨或软骨内成骨。在膜内成骨过程中,骨骼直接由间充质细胞凝聚形成,颅骨的扁骨、锁骨和软骨膜骨环通过此过程发育。中轴骨(肋骨和椎骨)和附肢骨骼(如上肢和下肢)通过软骨内成骨形成,其中间充质转变为具有未来骨骼元素形状的软骨中间体,该中间体逐渐被骨替代。软骨内成骨发生在所有脊椎动物类群中,其起始涉及软骨细胞的分化、细胞外软骨基质的矿化和中间体的血管化,随后是软骨的崩解和吸收、骨形成,最后 - 在软骨模型完全骨化后 - 形成无血管的关节软骨。骨骺生长板调节骨骼的纵向生长,这通过软骨细胞的平衡增殖和清除来实现,而晚期肥大软骨细胞是死亡还是转化为成骨细胞的问题仍在激烈争论中。导致软骨内成骨的复杂过程已经研究了一个多世纪,本综述旨在概述长骨(如股骨、胫骨)发育过程中的组织学和分子事件。肥大软骨细胞的命运将根据细胞追踪研究获得的新发现进行讨论。