Department of Mechanical & Industrial Engineering, Montana State University, Bozeman, MT, USA.
Department of Biomedical Sciences, College of Idaho, Caldwell, ID, USA.
Bone. 2024 Sep;186:117163. doi: 10.1016/j.bone.2024.117163. Epub 2024 Jun 8.
Osteocytes engage in bone resorption and mineralization surrounding their expansive lacunar-canalicular system (LCS) through peri-LCS turnover. However, fundamental questions persist about where, when, and how often osteocytes engage in peri-LCS turnover and how these processes change with aging. Furthermore, whether peri-LCS turnover is associated with natural variation in cortical tissue strain remains unexplored. To address these questions, we utilized confocal scanning microscopy, immunohistochemistry, and scanning electron microscopy to characterize osteocyte peri-LCS turnover in the cortical (mid-diaphysis) and cancellous (metaphysis) regions of femurs from young adult (5 mo) and early-old-age (22 mo) female C57BL/6JN mice. LCS bone mineralization was measured by the presence of perilacunar fluorochrome labels. LCS bone resorption was measured by immunohistochemical marker of bone resorption. The dynamics of peri-LCS turnover were estimated from serial fluorochrome labeling, where each mouse was administered two labels between 2 and 16 days before euthanasia. Osteocyte participation in mineralizing their surroundings is highly abundant in both cortical and cancellous bone of young adult mice but significantly decreases with aging. LCS bone resorption also decreases with aging. Aging has a greater impact on peri-LCS turnover dynamics in cancellous bone than in cortical bone. Lacunae with recent peri-LCS turnover are larger in both age groups. While peri-LCS turnover is associated with variation in tissue strain between cortical quadrants and intracortical location for 22 mo mice, these associations were not seen for 5 mo mice. The impact of aging on decreasing peri-LCS turnover may have significant implications for bone quality and mechanosensation.
骨细胞通过周围的腔隙 - 管道系统 (LCS) 进行骨吸收和矿化,从而参与周围的 LCS 转换。然而,关于骨细胞何时以及如何频繁地参与周围的 LCS 转换,以及这些过程如何随年龄变化等基本问题仍然存在。此外,周围的 LCS 转换是否与皮质组织应变的自然变化有关仍未得到探索。为了解决这些问题,我们利用共聚焦扫描显微镜、免疫组织化学和扫描电子显微镜来描述年轻成年(5 个月)和早期老年(22 个月)雌性 C57BL/6JN 小鼠股骨皮质(骨干)和松质(干骺端)区域骨细胞的周围 LCS 转换。LCS 骨矿化通过氟染料标记的存在来测量。LCS 骨吸收通过骨吸收的免疫组织化学标志物来测量。从连续的氟染料标记估计周围 LCS 转换的动态,其中每只小鼠在安乐死前 2 至 16 天之间接受两次标记。年轻成年小鼠的皮质和松质骨中,骨细胞参与周围矿化的能力非常丰富,但随着年龄的增长而显著下降。LCS 骨吸收也随年龄增长而减少。衰老对松质骨中周围 LCS 转换动力学的影响大于皮质骨。在两个年龄组中,最近进行周围 LCS 转换的腔隙更大。虽然周围 LCS 转换与 22 个月龄小鼠皮质骨和皮质骨内不同象限之间的组织应变变化有关,但在 5 个月龄小鼠中没有观察到这些关联。衰老对周围 LCS 转换减少的影响可能对骨质量和机械感觉有重大影响。