Department of Cell Biology, Washington University, St. Louis, Missouri.
Veterans Affairs Medical Center, Pittsburgh, Pennsylvania.
Am J Physiol Cell Physiol. 2020 Jan 1;318(1):C111-C124. doi: 10.1152/ajpcell.00120.2019. Epub 2019 Sep 18.
Bone differs from other connective tissues; it is isolated by a layer of osteoblasts that are connected by tight and gap junctions. This allows bone to create dense lamellar type I collagen, control pH, mineral deposition, and regulate water content forming a compact and strong structure. New woven bone formed after degradation of mineralized cartilage is rapidly degraded and resynthesized to impart structural order for local bone strength. Ossification is regulated by thickness of bone units and by patterning via bone morphogenetic receptors including activin, other bone morphogenetic protein receptors, transforming growth factor-β receptors, all part of a receptor superfamily. This superfamily interacts with receptors for additional signals in bone differentiation. Important features of the osteoblast environment were established using recent tools including osteoblast differentiation in vitro. Osteoblasts deposit matrix protein, over 90% type I collagen, in lamellae with orientation alternating parallel or orthogonal to the main stress axis of the bone. Into this organic matrix, mineral is deposited as hydroxyapatite. Mineral matrix matures from amorphous to crystalline hydroxyapatite. This process includes at least two-phase changes of the calcium-phosphate mineral as well as intermediates involving tropocollagen fibrils to form the bone composite. Beginning with initiation of mineral deposition, there is uncertainty regarding cardinal processes, but the driving force is not merely exceeding the calcium-phosphate solubility product. It occurs behind a epithelial-like layer of osteoblasts, which generate phosphate and remove protons liberated during calcium-phosphate salt deposition. The forming bone matrix is discontinuous from the general extracellular fluid. Required adjustment of ionic concentrations and water removal from bone matrix are important details remaining to be addressed.
骨组织与其他结缔组织不同;它被一层成骨细胞所隔离,这些细胞通过紧密连接和缝隙连接连接在一起。这使得骨骼能够形成致密的板层型 I 型胶原蛋白,控制 pH 值、矿物质沉积,并调节含水量,形成致密而坚固的结构。在矿化软骨降解后形成的新编织骨会迅速降解并重新合成,为局部骨强度赋予结构秩序。骨化受骨单位的厚度和通过骨形态发生受体(包括激活素、其他骨形态发生蛋白受体、转化生长因子-β受体)的模式调节,这些受体都是受体超家族的一部分。该超家族与骨分化中的其他信号的受体相互作用。最近的工具,包括体外成骨细胞分化,确立了成骨细胞环境的重要特征。成骨细胞在板层中沉积基质蛋白,超过 90%的 I 型胶原蛋白,其方向与骨骼的主要应力轴平行或正交。在这个有机基质中,矿物质沉积为羟磷灰石。矿化基质从无定形成熟化为结晶羟磷灰石。这个过程至少包括钙磷矿物的两个相变以及涉及原胶原蛋白纤维的中间产物,以形成骨复合材料。从矿物质沉积的开始,就存在对主要过程的不确定性,但驱动力不仅仅是超过钙磷溶解度产物。它发生在成骨细胞的上皮样层后面,成骨细胞产生磷酸盐并去除钙磷盐沉积过程中释放的质子。形成的骨基质与一般细胞外液不连续。需要调整离子浓度和从骨基质中去除水分,这是仍待解决的重要细节。