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Fluid model of epithelial morphogenesis: Oscillations and structuring

机译:上皮形态发生的流体模型:振动和结构

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摘要

We have revised a mathematical model of epithelial morphogenesis by Belintsev et al. (1987) (BB model) taking into account the oscillatory nature of morphogenesis and stability analysis (Cherdantsev, 2014). Following the BB model in considering the feedback control of cell shape changes by mechanical forces, we modify it to represent epithelial surface movements observed in different types of Metazoan gastrulation. Basing on these observations, we argue that the epithelial surface movement is that of an incompressible fluid supplemented by a positive feedback between the movement and spreading of the surface flow. Dipole interactions between sources and sinks of surface energy provide a single mechanism both of short-ranged and long-ranged regulation of collective cell and surface movements whose basic variables are the space averaged epithelial surface curvature and lateral pressure within the epithelial surface flux negatively related to its velocity. The short-ranged activation means a movement of the surface up to the lateral pressure gradient under non-linear feedback control of the surface flexure. The break of this feedback with equalization of the surface curvature is sufficient for a self restriction of the movement spreading. Owing to bistable interdependence between the lateral pressure and epithelial surface curvature, we get a generic oscillatory contour in which the same region oscillates being alternately a sink and source of the surface flow. The opposite phase oscillations of the lateral pressure and curvature allow for both directional propulsion of the surface through the same region and spatial differentiation based on parametric differences between the large-scaled regions that correspond to sources and sinks of the surface.
机译:我们通过Belintsev等人修正了上皮形态发生的数学模型。 (1987年)(BB模型)考虑到形态发生和稳定性分析的振荡性质(Cherdantsev,2014)。在通过机械力考虑细胞形状的反馈控制之后,我们在通过机械力改变的反馈控制之后,我们将其改变以表示在不同类型的甲卓膜腐蚀性中观察到的上皮表面运动。基于这些观察结果,我们认为上皮表面运动是由表面流动的运动和扩散之间的正反馈补充的不可压缩流体的。来源和表面能量沉积之间的偶极相互作用提供了一种单一机制,包括集体电池的短程和长距离调节,其基本变量是空间平均上皮表面曲率和上皮表面通量内的横向压力呈负相关它的速度。短途激活是指在表面弯曲的非线性反馈控制下的横向压力梯度的表面移动。这种反馈的断裂与表面曲率的均衡足以用于运动扩散的自限制。由于横向压力和上皮表面曲率之间的双稳态相互依赖,我们得到了一个通用振荡轮廓,其中相同区域振荡交替地是表面流的水槽和源极。横向压力和曲率的相反相位振荡允许表面通过相同区域的方向推进和基于与表面的源极和垫地对应的大缩放区域之间的参数差异。

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