Department of Radiology, Gaziosmanpasa Training and Research Hospital, University of Health Sciences Turkey, 34255, Istanbul, Turkey.
Department of Neurology, Gaziosmanpasa Training and Research Hospital, University of Health Sciences Turkey, Istanbul, Turkey.
Neuroradiology. 2020 Aug;62(8):947-953. doi: 10.1007/s00234-020-02398-9. Epub 2020 Mar 19.
Despite considerable published information about the clinical-radiological correlation of medullary infarcts, no study has determined whether topographic evaluations are performed accurately among researchers. Our purpose in this study was twofold: to evaluate the topographic pattern of medullary infarcts on diffusion-weighted imaging by their radiological aspect, and to assess interobserver agreement on the topographic pattern.
We retrospectively reviewed our imaging and clinical database for patients admitted to our radiology department between January 2014 and September 2019. Two radiologists evaluated the imaging studies independently. Consensus data were used in the analysis.
The retrospective review yielded 92 patients with medullary infarction. The affected vascular territories were lateral (n = 58), anteromedial (n = 28), posterior (n = 3), and anterolateral (n = 1). Two patients had hemimedullary infarction. The rostrocaudal levels of the medullary infarct were superior (n = 34), middle (n = 31), inferior (n = 4), superior-middle (n = 13), and middle-inferior (n = 10). The medullary infarcts were divided into two types: lateral (n = 62) and medial (n = 28). The affected vascular territories differed with rostrocaudal topography of medullary infarct (p = 0.003). Excellent interobserver agreement was found for type of medullary infarct, compared with moderate for vascular territory and fair for rostrocaudal topography. The anterolateral and posterior territories were the most often misdiagnosed, while the level with the most disagreements in rostrocaudal topography was middle.
The accurate topographic evaluation of a medullary infarct can be an important basis for investigating stroke etiology. However, correct topographic evaluation may not always be available and smaller territories such as anterolateral and posterior should be assessed carefully.
尽管已有大量关于脑髓质梗死的临床-放射学相关性的文献报道,但尚无研究确定研究人员是否准确地进行了脑髓质梗死的地形学评估。本研究的目的有两个:通过放射学特征评估弥散加权成像上脑髓质梗死的地形模式,并评估在脑髓质梗死地形模式方面的观察者间一致性。
我们回顾性地审查了 2014 年 1 月至 2019 年 9 月期间在我院放射科就诊的患者的影像学和临床数据库。两名放射科医生独立评估影像学研究。分析中使用了共识数据。
回顾性审查得出 92 例脑髓质梗死患者。受累的血管区域为外侧(n=58)、前内侧(n=28)、后(n=3)和前外侧(n=1)。2 例患者为半侧脑髓质梗死。脑髓质梗死的颅尾水平为上(n=34)、中(n=31)、下(n=4)、中上(n=13)和中下部(n=10)。脑髓质梗死分为两种类型:外侧(n=62)和内侧(n=28)。受累的血管区域与脑髓质梗死的颅尾位置有关(p=0.003)。脑髓质梗死类型的观察者间一致性极好,而血管区域和颅尾位置的观察者间一致性为中度和一般。前外侧和后区域最常被误诊,而颅尾位置的差异最大。
脑髓质梗死的准确地形学评估可为研究卒中病因提供重要依据。然而,并非总是能进行正确的地形学评估,并且应仔细评估较小的区域,如前外侧和后区域。