Perforation of the temporomandibular joint disc: cadaveric anatomical study

被引:0
作者
Iwanaga, J. [1 ,2 ,3 ,8 ]
Kitagawa, N. [1 ]
Fukino, K. [1 ]
Kikuta, S. [4 ]
Tubbs, R. Shane [2 ,5 ,6 ]
Yoda, T. [7 ]
机构
[1] Tokyo Med & Dent Univ, Grad Sch Med & Dent Sci, Dept Oral & Maxillofacial Anat, Tokyo, Japan
[2] Tulane Univ, Sch Med, Tulane Ctr Clin Neurosci, Dept Neurosurg, New Orleans, LA USA
[3] Kurume Univ, Sch Med, Dept Anat, Div Gross & Clin Anat, Kurume, Fukuoka, Japan
[4] Kurume Univ, Sch Med, Dent & Oral Med Ctr, Kurume, Fukuoka, Japan
[5] Tulane Univ, Sch Med, Dept Struct & Cellular Biol, New Orleans, LA USA
[6] St Georges Univ, Dept Anat Sci, St Georges, Grenada
[7] Tokyo Med & Dent Univ, Grad Sch Med & Dent Sci, Dept Maxillofacial Surg, Tokyo, Japan
[8] Tulane Univ, Sch Med, Neurosurg, 131 S Robertson St, Suite 1300, New Orleans, LA 70112 USA
关键词
Anatomy; Cadaver; Temporomandibular joint disc; Temporomandibular joint disorders; Magnetic resonance imaging; DIAGNOSIS;
D O I
10.1016/j.ijom.2023.10.033
中图分类号
R78 [口腔科学];
学科分类号
1003 ;
摘要
The aim of this human cadaveric study was to investigate the relationship between temporomandibular joint disc perforation and bony changes of the mandibular condyle. Overall, 135 cadaveric mandibles were used (69 male, 66 female; all White). Mean age at death was 78.7 years. Perforation of the disc was investigated. Differences in the area of the perforation according to the different types of bony change (erosion, flattening, osteophyte) were evaluated. Perforation of the disc was observed in 34.8% of all mandibles, occurring unilaterally in 53.2% of cases and bilaterally in 46.8%. The prevalence of perforation was 16.4% in cadavers < 80 years old (67 heads) and 52.9% in those >= 80 years old (68 heads) ( P < 0.001). Osteophyte formation was always identified along with other bony changes (21.7%) and never in isolation. The area of the perforation was significantly larger in the groups with bony changes (one, two, or three changes) than in the 'no bony change' group. The group with osteophyte formation showed a significantly larger perforated area than the group without osteophyte formation; likewise, the group with flattening showed a significantly larger perforated area than the group without flattening. Osteophytes and flattening are probably secondary bony changes that occur following disc perforation. Based on this study, disc perforation should be suspected when these findings are identified on imaging.
引用
收藏
页码:422 / 429
页数:8
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