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轮藻节间细胞中的胞质环流与重力感应

Cytoplasmic streaming and gravity sensing in Chara internodal cells.

作者信息

Staves M P

机构信息

Department of Biology, Grand Valley State University, Allendale, MI 49401, USA.

出版信息

Planta. 1997 Sep;203(Suppl 1):S79-84. doi: 10.1007/pl00008119.

Abstract

Since the nineteenth century, the merits of two alternate models for explaining the mechanism of plant gravity perception have been discussed. The gravitational pressure model states that plant cells perceive gravity by sensing their relative buoyancy to that of the surrounding medium, whereas the more popular starch-statolith model states that intracellular sedimenting particles act as gravity sensors. Vertically-oriented Chara internodal cells exhibit a gravity dependent polarity of cytoplasmic streaming such that the downwardly-directed stream moves ca. 10% faster than the upwardly-directed stream. This polarity of cytoplasmic streaming is not simply a consequence of gravity acting directly on the cytoplasm but is rather under physiological control. When Chara internodal cells are placed in a medium more dense than themselves, the gravity-induced polarity of cytoplasmic streaming is reversed. This phenomenon cannot be explained by a model which relies on intracellular sedimenting particles as gravity sensors but is consistent with the gravitational pressure model for gravity sensing. We propose that gravity causes the internodal cells to settle within the confines of the extracellular matrix resulting in a tension between the plasma membrane and the extracellular matrix at the top of the cell and a compression between the plasma membrane and the extracellular matrix at the bottom of the cell. These stresses are proposed to act upon peptides which span the plasma membrane/extracellular matrix interface at the ends of the cells and which subsequently activate Ca2+ channels which in turn may induce a polarity of cytoplasmic streaming.

摘要

自19世纪以来,人们一直在讨论两种用于解释植物重力感知机制的交替模型的优点。重力压力模型指出,植物细胞通过感知自身相对于周围介质的相对浮力来感知重力,而更流行的淀粉平衡石模型则认为细胞内沉降颗粒充当重力传感器。垂直取向的轮藻节间细胞表现出依赖重力的细胞质流动极性,使得向下流动的速度比向上流动的速度快约10%。这种细胞质流动的极性不仅仅是重力直接作用于细胞质的结果,而是受生理控制的。当轮藻节间细胞置于比自身密度更大的介质中时,重力诱导的细胞质流动极性会反转。这种现象不能用依赖细胞内沉降颗粒作为重力传感器的模型来解释,但与重力感知的重力压力模型一致。我们提出,重力导致节间细胞在细胞外基质范围内沉降,从而在细胞顶部的质膜和细胞外基质之间产生张力,在细胞底部的质膜和细胞外基质之间产生压缩。这些应力作用于跨越细胞末端质膜/细胞外基质界面的肽,随后激活Ca2+通道,进而可能诱导细胞质流动的极性。

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