Department of Physiology, McGill University, Montréal, Quebec, Canada.
Department of Cell Biology, School of Medicine, Emory University, Atlanta, Georgia.
Biophys J. 2022 Dec 6;121(23):4419-4432. doi: 10.1016/j.bpj.2022.11.007. Epub 2022 Nov 8.
Spontaneous Ca local transients (SCaLTs) in isolated oligodendrocyte precursor cells are largely regulated by the following fluxes: store-operated Ca entry (SOCE), Na/Ca exchange, Ca pumping through Ca-ATPases, and Ca-induced Ca-release through ryanodine receptors and inositol-trisphosphate receptors. However, the relative contributions of these fluxes in mediating fast spiking and the slow baseline oscillations seen in SCaLTs remain incompletely understood. Here, we developed a stochastic spatiotemporal computational model to simulate SCaLTs in a homogeneous medium with ionic flow between the extracellular, cytoplasmic, and endoplasmic-reticulum compartments. By simulating the model and plotting both the histograms of SCaLTs obtained experimentally and from the model as well as the standard deviation of inter-SCaLT intervals against inter-SCaLT interval averages of multiple model and experimental realizations, we revealed the following: (1) SCaLTs exhibit very similar characteristics between the two data sets, (2) they are mostly random, (3) they encode information in their frequency, and (4) their slow baseline oscillations could be due to the stochastic slow clustering of inositol-trisphosphate receptors (modeled as an Ornstein-Uhlenbeck noise process). Bifurcation analysis of a deterministic temporal version of the model showed that the contribution of fluxes to SCaLTs depends on the parameter regime and that the combination of excitability, stochasticity, and mixed-mode oscillations are responsible for irregular spiking and doublets in SCaLTs. Additionally, our results demonstrated that blocking each flux reduces SCaLTs' frequency and that the reverse (forward) mode of Na/Ca exchange decreases (increases) SCaLTs. Taken together, these results provide a quantitative framework for SCaLT formation in oligodendrocyte precursor cells.
孤立少突胶质前体细胞中的自发性 Ca 局部瞬变 (SCaLT) 主要受以下流驱动:储存操作的 Ca 内流 (SOCE)、Na/Ca 交换、通过 Ca-ATP 酶的 Ca 泵送以及通过 Ryanodine 受体和肌醇三磷酸受体的 Ca 诱导的 Ca 释放。然而,这些流在介导 SCaLT 中观察到的快速尖峰和缓慢基线振荡中的相对贡献仍不完全清楚。在这里,我们开发了一个随机时空计算模型,以模拟同质介质中的 SCaLT,其中细胞外、细胞质和内质网隔室之间存在离子流动。通过模拟模型并绘制从实验和模型获得的 SCaLT 直方图以及多个模型和实验实现的跨 SCaLT 间隔的标准偏差与跨 SCaLT 间隔平均值的关系,我们揭示了以下几点:(1)两个数据集之间的 SCaLT 表现出非常相似的特征;(2)它们主要是随机的;(3)它们在频率中编码信息;(4)它们的缓慢基线振荡可能是由于肌醇三磷酸受体的随机缓慢聚类(建模为 Ornstein-Uhlenbeck 噪声过程)。模型的确定性时间版本的分岔分析表明,流对 SCaLT 的贡献取决于参数范围,并且兴奋性、随机性和混合模式振荡的组合是导致 SCaLT 不规则尖峰和双脉冲的原因。此外,我们的结果表明,阻断每种流都会降低 SCaLT 的频率,而 Na/Ca 交换的反向(正向)模式会降低(增加)SCaLT。总之,这些结果为少突胶质前体细胞中 SCaLT 的形成提供了一个定量框架。