Apaza Alccayhuaman Karol Ali, Heimel Patrick, Tangl Stefan, Lettner Stefan, Kampleitner Carina, Panahipour Layla, Kuchler Ulrike, Gruber Reinhard
Department of Oral Biology, University Clinic of Dentistry, Medical University of Vienna, 1090 Vienna, Austria.
Karl Donath Laboratory for Hard Tissue and Biomaterial Research, University Clinic of Dentistry, Medical University of Vienna, 1090 Vienna, Austria.
J Funct Biomater. 2024 Feb 21;15(3):54. doi: 10.3390/jfb15030054.
Bio-Gide is a collagen membrane routinely used in guided bone regeneration. Recent studies have shown that this collagen membrane has osteoconductive properties, meaning that it can support the growth of new bone. However, it has also been observed that the collagen membrane has areas of mineralized fibers which can occur spontaneously and independently of osteoblasts. To better understand how this works, we established a model using minced collagen membranes to reduce the active mineralization of intact collagen membranes in favor of passive mineralization. We thus compared the original intact membrane with a minced collagen membrane in a 5 mm calvarial defect model in Sprague Dawley rats. After three weeks of healing, histology and microcomputed tomography (μCT) were performed. Histological analysis confirmed the osteoconductive properties, with new bone growing inside the intact collagen membrane. However, in minced collagen membranes, the osteoconductive properties were restricted to the defect margins. Interestingly, histology revealed large mineralized areas indicating passive mineralization with no signs of bone formation. In the μCT analysis, the intact collagen membranes caused a higher median mineralized volume (1.5 mm) compared with the minced group (0.4 mm), but this lacked significance ( = 0.09). The μCT analysis needs to be interpreted carefully, particularly in defects filled with minced membranes, considering that the mineralized tissue may not necessarily be bone but also the result of passive mineralization. Taken together, the findings suggest that Bio-Gide collagen membranes support bone formation while also exhibiting potential for passive mineralization.
Bio-Gide是一种常用于引导骨再生的胶原膜。最近的研究表明,这种胶原膜具有骨传导特性,即它能够支持新骨生长。然而,也有人观察到胶原膜存在矿化纤维区域,这些区域可能自发形成且独立于成骨细胞。为了更好地理解其作用机制,我们建立了一个模型,使用切碎的胶原膜来减少完整胶原膜的活性矿化,以利于被动矿化。因此,我们在Sprague Dawley大鼠的5毫米颅骨缺损模型中,将原始完整膜与切碎的胶原膜进行了比较。愈合三周后,进行了组织学和显微计算机断层扫描(μCT)检查。组织学分析证实了骨传导特性,完整胶原膜内有新骨生长。然而,在切碎的胶原膜中,骨传导特性仅限于缺损边缘。有趣的是,组织学显示有大片矿化区域,表明存在被动矿化且无骨形成迹象。在μCT分析中,完整胶原膜的中位矿化体积(1.5毫米)高于切碎组(0.4毫米),但差异无统计学意义( = 0.09)。考虑到矿化组织不一定是骨,也可能是被动矿化的结果,μCT分析结果需要谨慎解读。综上所述,这些发现表明Bio-Gide胶原膜在支持骨形成的同时,也展现出被动矿化的潜力。