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Sigmoid plate dehiscence: Congenital or acquired condition?

Authors :
Liu, Zhaohui
Li, Jing
Zhao, Pengfei
Lv, Han
Dong, Cheng
Liu, Wenjuan
Wang, Zhenchang
Source :
European Journal of Radiology. May2015, Vol. 84 Issue 5, p862-864. 3p.
Publication Year :
2015

Abstract

Background and purpose The imaging features of sigmoid plate dehiscence-induced pulsatile tinnitus have been presented. The origin of the sigmoid plate dehiscence, however, remains unclear. Our aim was to assess the prevalence and extent of sigmoid plate dehiscence on computed tomography (CT) images in multiple age groups to determine whether this condition is more likely to be congenital or acquired. Materials and methods We retrospectively reviewed contrast-enhanced CT images of sigmoid plates of temporal bones in 504 patients. Each temporal bone was characterized as normal or dehiscent. Patients were then subcategorized into four age groups, and the prevalence and extent of dehiscent sigmoid plates in each group were calculated and compared. Results Overall, 80 patients had sigmoid plate dehiscence, nine of whom had it bilaterally. In successively older age groups, the prevalences of sigmoid plate dehiscence were 18.9%, 20.1%, 14.5%, and 12.7%, respectively. Respective average anteroposterior bony defect diameters were 3.7 ± 1.7, 3.0 ± 1.3, 3.1 ± 1.5, and 3.0 ± 1.1 mm. Respective average vertical bony defect diameters were 3.6 ± 2.3, 2.6 ± 1.2, 3.2 ± 1.5, and 3.0 ± 1.7 mm. The prevalence and extent of sigmoid plate dehiscence were not statistically different among the four age groups. Conclusions The similar radiologic prevalence and extent of dehiscent sigmoid plates among the age groups suggest that the dehiscence is more commonly a congenital than an acquired condition. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
0720048X
Volume :
84
Issue :
5
Database :
Academic Search Index
Journal :
European Journal of Radiology
Publication Type :
Academic Journal
Accession number :
102099604
Full Text :
https://doi.org/10.1016/j.ejrad.2014.12.024