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对 CA1 层和齿状回之间的非线性耦合进行研究。

An investigation into the nonlinear coupling between CA1 layers and the dentate gyrus.

机构信息

Engineering School of Sustainable Infrastructure and Environment.

McKnight Brain Institute.

出版信息

Behav Neurosci. 2020 Dec;134(6):491-515. doi: 10.1037/bne0000366. Epub 2020 Apr 16.

Abstract

Although the activity from the dentate gyrus is known to have strong connections with other hippocampal layers, the functionality of these connections, that is, the degree to which it drives activity in the downstream regions of the hippocampus, is not well understood. This question is particularly relevant for mesoscale localfield potential (LFP) rhythms such as gamma oscillations. Following the hypothesis that fundamental features of the LFP are consistent with turbulent dynamics, we investigate the crosslayer relationship between the CA1 layers and the dentate gyrus as a function of running speed. In agreement with previous studies, same-layer spectral and bispectral analyses show that increasing input (rat speed) results in an increase of power and nonlinearity (phase coupling) between theta and gamma. The effectiveness of the connection between the 2 regions is investigated using cross-bicoherence analysis. Based on the turbulence interpretation of the evolution of spectra and bispectra as a function of the power input rate, we propose a measure for estimating the strength of the cross-frequency, cross-layer nonlinear forcing, that compares the magnitude of bicoherence (same-layer) and cross-bicoherence (cross-layer). Our results suggest that at moderate speeds gamma in CA1 is mainly driven by local theta, while the coupling of the CA1 gamma to the dentate-gyrus gamma becomes significant. Overall, these data are consistent with the hypothesis of theta-to-gamma energy cascade model for the organization of hippocampal LFP, with theta playing the role of a global pacemaker across the entire hippocampus while gamma is a local oscillation generated by through local anatomical connections. (PsycInfo Database Record (c) 2021 APA, all rights reserved).

摘要

尽管已知齿状回的活动与其他海马层有很强的连接,但这些连接的功能,即它在海马下游区域驱动活动的程度,尚不清楚。这个问题对于中尺度局部场电位(LFP)节律(如伽马振荡)尤为重要。根据 LFP 的基本特征与湍流动力学一致的假设,我们研究了 CA1 层和齿状回之间的跨层关系作为跑步速度的函数。与之前的研究一致,同层谱和双谱分析表明,增加输入(大鼠速度)会导致θ和γ之间的功率和非线性(相位耦合)增加。使用跨双相干分析研究了两个区域之间的连接有效性。基于频谱和双谱随功率输入率的演变作为湍流的解释,我们提出了一种用于估计跨频、跨层非线性强迫的强度的度量,该度量比较了双相干(同层)和跨双相干(跨层)的幅度。我们的结果表明,在中等速度下,CA1 中的伽马主要由局部θ驱动,而 CA1 伽马与齿状回伽马的耦合变得显著。总的来说,这些数据与海马 LFP 组织的θ到γ能量级联模型的假设一致,其中θ在整个海马体中起着全局起搏器的作用,而γ是通过局部解剖连接产生的局部振荡。

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