Distribution of paramagnetic and diamagnetic cortical substrates following mild Traumatic Brain Injury: A depth- and curvature-based quantitative susceptibility mapping study

Christi A. Essex, Jenna L. Merenstein, Devon K. Overson, Trong-Kha Truong, David J. Madden, Mayan J. Bedggood, Helen Murray, Samantha J. Holdsworth, Ashley W. Stewart, Catherine Morgan, Richard L. M. Faull, Patria Hume, Alice Theadom, Mangor Pedersen
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Abstract

Evidence has linked head trauma to increased risk factors for neuropathology, including acute mechanical deformation of the cortical sulcal fundus and, later, perivascular accumulation of hyperphosphorylated tau (p-tau) adjacent to these spaces related to chronic traumatic encephalopathy (CTE). Despite this, little is known about microstructural abnormalities and cellular dyshomeostasis at the acute stage of mild traumatic brain injury (mTBI) in humans, particularly in the cortex. To address this gap in the literature, we designed the first architectonically-motivated quantitative susceptibility mapping (QSM) study to assess regional patterns of positive (iron-related) and negative (myelin-, calcium-, and protein-related) magnetic susceptibility in cortical regions of interest (ROI) following mTBI. Depth- and curvature-specific positive and negative QSM values were compared between 25 males with acute (< 14 days) sports-related mTBI (sr-mTBI) and 25 age-matched male controls across 34 cortical ROIs. Bilateral between-group analyses were conducted on specific ROI curvature bins (crown, bank, and fundus) as well as a combined curvature measure, across 21 cortical depths, for each ROI. Correlations between positive and negative susceptibility were analysed for age, brain injury severity, and the number of days since injury. We observed significant group differences in magnetic susceptibility for depth, curvature, and ROIs. Our results suggest a trauma-induced pattern of iron deposition preferential to superficial, perivascular-adjacent spaces in the sulci of the parahippocampal gyrus. Co-localised decreases in diamagnetism in the same region suggest dual pathology of neural substrates, the biological mechanisms behind which remain speculative. Significant correlations were found between magnetic susceptibility and age, both in ROIs and cortical depths distinct from those showing sr-mTBI-related differences. Little to no relationship was observed between magnetic susceptibility and subjective markers of injury or injury latency. The coherence between our findings and pathognomonic patterns of misfolded proteins in trauma-related neurodegeneration is interesting, which may have implications for the role of brain iron in microstructural cortical tissue damage after a mild brain injury. Further longitudinal research is needed to elucidate the long-term implications of our findings.
轻度脑外伤后顺磁性和二磁性皮层基质的分布:基于深度和曲率的定量电感图谱研究
有证据表明,头部创伤与神经病理学风险因素的增加有关,包括皮质沟底的急性机械变形,以及随后与慢性创伤性脑病(CTE)相关的高磷酸化 tau(p-tau)在这些空间附近的血管周围积聚。尽管如此,人们对人类轻度创伤性脑损伤(mTBI)急性期的微结构异常和细胞失衡知之甚少,尤其是在大脑皮层。为了填补这一文献空白,我们设计了第一项以建筑学为动机的定量磁感应强度绘图(QSM)研究,以评估轻微脑损伤后皮层感兴趣区(ROI)中正磁感应强度(铁相关)和负磁感应强度(髓鞘、钙和蛋白质相关)的区域模式。25 名急性(14 天)运动相关 mTBI(sr-mTBI)男性患者和 25 名年龄匹配的男性对照组患者在 34 个皮层 ROI 中比较了特定深度和曲率的正负 QSM 值。对每个 ROI 的特定 ROI 曲度分段(冠状面、基底面和基底面)以及 21 个皮层深度的综合曲度测量进行了双侧组间分析。分析了年龄、脑损伤严重程度和受伤后天数与正负磁感应强度之间的相关性。我们观察到磁感应强度在深度、曲率和 ROI 方面存在明显的组间差异。我们的研究结果表明,创伤诱导的铁沉积模式偏好于海马旁回沟内浅表、血管周围邻近的空间。同一区域的二磁性同时下降,表明神经基质出现了双重病理变化,其背后的生物机制仍有待推测。在与 sr-mTBI 相关差异不同的区域和皮层深度中,磁感应强度与年龄之间存在显著相关性。磁感应强度与损伤的主观指标或损伤潜伏期之间几乎没有关系。我们的研究结果与创伤相关神经变性中错误折叠蛋白的病理模式之间的一致性非常有趣,这可能对轻度脑损伤后脑铁在皮质组织微结构损伤中的作用有影响。要阐明我们研究结果的长期影响,还需要进一步的纵向研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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