Doube M, Firth E C, Boyde A
Biophysics, Oral Growth and Development, Queen Mary University of London, London, United Kingdom.
Osteoarthritis Cartilage. 2007 Nov;15(11):1283-92. doi: 10.1016/j.joca.2007.04.003. Epub 2007 May 22.
To interrelate articular calcified cartilage thickness, mineralisation density, tidemark count and tidemark linear accretion rate by site in the equine third metacarpal distal condyle. To determine the effects of exercise during early life on articular calcified cartilage.
Six of 12 pasture-raised Thoroughbred horses were exercised from 10 days old. Calcein labels were given 19 and 8 days prior to euthanasia at 18 months old. Osteochondral specimens were cut from the distal third metacarpal condyle and imaged using confocal scanning light microscopy (CSLM) and quantitative backscattered electron scanning electron microscopy (qBSE). Articular calcified cartilage thickness and total thickness mineralisation density were measured on montaged qBSE image sets, and inter-label mineralisation density, tidemark count and linear accretion rate measured on registered CSLM-qBSE image pairs.
Calcified cartilage thickness, mineralisation density, tidemark count and linear accretion rate varied significantly between sites. Regions with thinner calcified cartilage had greater linear accretion rates, hence rapid chondroclastic resorption. Mineralisation density was positively correlated with linear accretion rate. Fewer multiple tidemarks were counted in regions with greater linear accretion rates. Lag time between the tidemark and cement line was estimated (180 days; in the range of 0-648 days). Exercise had little effect on measured parameters.
The major determinant of articular calcified cartilage thickness is the rate of chondroclastic resorption, not tidemark linear accretion rate. Our evidence supports coupled, mechanosensitive regulation of chondroclastic resorption and linear accretion rate in articular calcified cartilage. Exercising pasture-reared foals causes little additional adaptation in distal third metacarpal articular calcified cartilage.
研究马第三掌骨远端髁不同部位的关节钙化软骨厚度、矿化密度、潮标计数及潮标线性生长速率之间的相互关系。确定早期生活中的运动对关节钙化软骨的影响。
12匹在牧场饲养的纯种马中有6匹从10日龄开始运动。在18月龄处死后,分别于安乐死19天和8天前给予钙黄绿素标记。从第三掌骨远端髁切取骨软骨标本,使用共聚焦扫描光学显微镜(CSLM)和定量背散射电子扫描电子显微镜(qBSE)成像。在拼接的qBSE图像集上测量关节钙化软骨厚度和总厚度矿化密度,并在配准的CSLM-qBSE图像对上测量标记间矿化密度、潮标计数和线性生长速率。
钙化软骨厚度、矿化密度、潮标计数和线性生长速率在不同部位间差异显著。钙化软骨较薄的区域线性生长速率较高,因此软骨细胞吸收迅速。矿化密度与线性生长速率呈正相关。线性生长速率较高的区域计数到的多条潮标较少。估计潮标与黏合线之间的延迟时间为180天(范围为0 - 648天)。运动对测量参数影响不大。
关节钙化软骨厚度的主要决定因素是软骨细胞吸收速率,而非潮标线性生长速率。我们的证据支持关节钙化软骨中软骨细胞吸收和线性生长速率的耦合、机械敏感调节。对在牧场饲养的幼驹进行运动,第三掌骨远端关节钙化软骨几乎不会产生额外适应性变化。