Hartlev Louise Brøndt, Klose-Jensen Rasmus, Thomsen Jesper Skovhus, Nyengaard Jens Randel, Boel Lene Warner Thorup, Laursen Mogens Berg, Laurberg Trine Bay, Nielsen Andreas Wiggers, Steengaard-Pedersen Kristian, Hauge Ellen-Margrethe
Department of Rheumatology, Aarhus University Hospital, Aarhus, Denmark.
Department of Biomedicine - Anatomy, Aarhus University, Aarhus, Denmark.
RMD Open. 2018 Sep 21;4(2):e000747. doi: 10.1136/rmdopen-2018-000747. eCollection 2018.
Bone formation is a hallmark of osteoarthritis (OA). It has been speculated that bone formation may occur because of ossification at the bone-cartilage unit, that is, bone formation directly involving the calcified cartilage (CC). This study aimed to investigate the thickness of the CC and subchondral bone (SCB) in relation to the severity of the overlying articular cartilage (AC) degeneration.
We investigated femoral heads from 20 patients with OA and 15 healthy subjects with design-based stereology using systematic uniform random sampling of the entire joint surface. This was combined with the Osteoarthritis Research Society International (OARSI) OA cartilage histopathology assessment system, thus obtaining focal OARSI grades paired with thickness measurements of AC, CC and the SCB.
The patients with OA had thicker CC (mean 159; 95% CI 144 to 177 µm) compared with the healthy subjects (mean 132; 95% CI 113 to 1550 µm; p=0.036), and this difference was even higher in areas without loss of AC thickness (OARSI grade ≤3); 187 (95% CI 164 to 214) µm vs 132 (95% CI 113 to 155) µm (p=0.001). In the patients with OA, a thicker SCB was observed in areas with loss of AC thickness (OARSI grade ≥4), but not in areas without loss of AC thickness (OARSI grade ≤3).
The study showed that thicker CC is present in early stages of OA, suggesting that bone formation by endochondral ossification is an early phenomenon of OA. Thickening of the SCB was present, but only in areas with denuded bone. Suggesting that also appositional bone growth occurs and that it may be a consequence of changed biomechanics.
骨形成是骨关节炎(OA)的一个标志。据推测,骨形成可能是由于骨 - 软骨单元处的骨化,即骨形成直接涉及钙化软骨(CC)。本研究旨在调查CC和软骨下骨(SCB)的厚度与上方关节软骨(AC)退变严重程度的关系。
我们使用基于设计的体视学方法,通过对整个关节表面进行系统均匀随机抽样,研究了20例OA患者和15名健康受试者的股骨头。这与国际骨关节炎研究学会(OARSI)的OA软骨组织病理学评估系统相结合,从而获得与AC、CC和SCB厚度测量值配对的局灶性OARSI分级。
与健康受试者相比,OA患者的CC更厚(平均值159;95%可信区间144至177μm),健康受试者的CC平均值为132(95%可信区间113至1550μm;p = 0.036),在AC厚度未丧失的区域(OARSI分级≤3)这种差异甚至更大;187(95%可信区间164至214)μm对132(95%可信区间113至155)μm(p = 0.001)。在OA患者中,在AC厚度丧失的区域(OARSI分级≥4)观察到SCB更厚,但在AC厚度未丧失的区域(OARSI分级≤3)未观察到。
该研究表明,OA早期存在较厚的CC,提示软骨内成骨是OA的早期现象。SCB存在增厚,但仅在骨裸露区域。提示也发生了表面骨生长,并且这可能是生物力学改变的结果。