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听觉Oddball范式中诱发的P3事件相关电位的颅内地形图。

The intracranial topography of the P3 event-related potential elicited during auditory oddball.

作者信息

Smith M E, Halgren E, Sokolik M, Baudena P, Musolino A, Liegeois-Chauvel C, Chauvel P

机构信息

Unité de Recherches sur l'Epilepsie (INSERM U97), Centre Paul Broca, Paris, France.

出版信息

Electroencephalogr Clin Neurophysiol. 1990 Sep;76(3):235-48. doi: 10.1016/0013-4694(90)90018-f.

Abstract

In order to isolate the anatomical locus of neural activity primarily responsible for generating the scalp-recorded P3 (or P300), the topography of event-related potentials (ERPs) elicited during an auditory oddball task was compared between medial-to-lateral aspects of the frontal, parietal, and temporal lobes in 10 epileptic patients undergoing stereoelectroencephalography for seizure localization. Evidence of local ERP generation was obtained from each of these areas. Small amplitude P3-type potentials were sometimes observed to invert polarity across recording contacts in the frontal lobe. Large amplitude positive polarity P3-type components were observed in the lateral neocortex of the inferior parietal lobule (IPL), that rapidly attenuated in amplitude at more anterior, posterior, superior, inferior, and medial recording contacts. Large amplitude polarity inverting P3-type components were also observed to be highly localized to hippocampal contacts of temporal lobe electrodes. These data are discussed in the context of other recent studies of lesion effects, scalp topography, and intracranial recordings, and it is concluded that activity generated in the IPL is likely to make the major contribution to the scalp-recorded P3, with smaller contributions from these other sources. Finally, salient topographical differences between the intracranial distribution of the P3 and those of the N2 (or N200) and slow wave (SW) suggest that the generators of these components are not identical.

摘要

为了分离出主要负责产生头皮记录的P3(或P300)的神经活动的解剖学部位,我们比较了10名接受立体脑电图检查以进行癫痫灶定位的癫痫患者在听觉oddball任务期间诱发的事件相关电位(ERP)在额叶、顶叶和颞叶从内侧到外侧的地形图。从这些区域中的每一个都获得了局部ERP产生的证据。有时观察到额叶记录电极上小幅度的P3型电位会在记录触点间反转极性。在顶下小叶(IPL)的外侧新皮质中观察到大幅度的正性P3型成分,该成分在更靠前、靠后、靠上、靠下和内侧的记录触点处幅度迅速衰减。还观察到大幅度极性反转的P3型成分高度局限于颞叶电极的海马触点。这些数据在其他近期关于病变影响、头皮地形图和颅内记录的研究背景下进行了讨论,得出的结论是,IPL中产生的活动可能对头皮记录的P3做出主要贡献,其他这些来源的贡献较小。最后,P3的颅内分布与N2(或N200)和慢波(SW)的颅内分布之间显著的地形学差异表明,这些成分的产生源并不相同。

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