蕨类苔藓的茎部向地性和淀粉体沉积。

J. Schwuchow, D. Kim, F. Sack
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引用次数: 26

摘要

对蕨类苔藓的茎部进行了检查,以确定它们是否向地性。此外,还对Funaria和Physcomitrella进行了评价,以比较角齿兽的淀粉体沉积。原体要么被化学固定在原位,要么被红外延时视频显微镜活体检查。龙葵呈负向地性生长,即在黑暗中向上生长。在藻属的细胞分裂之前,向上弯曲暂时逆转,这一现象已经在角角兽和小立小藻中为人所知。大多数水平和向上弯曲的蕨菜尖细胞包含一个广泛的近顶区,在那里发生了质体沉积。在黑暗生长的锅状小立藻中,通过在细胞顶部出现一薄的无淀粉体的细胞质条来检测沉积。这些结果表明,向地性和顶端下淀粉体沉积可能在苔藓中相对普遍。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Caulonemal gravitropism and amyloplast sedimentation in the moss Funaria.
Caulonemata of the moss Funaria were examined to determine whether they are gravitropic. Funaria and Physcomitrella were also evaluated to compare amyloplast sedimentation with that of Ceratodon. Protonemata were either chemically fixed in place or examined alive using infrared timelapse videomicroscopy. Funaria caulonemata were found to be negatively gravitropic, i.e., they grew upwards in the dark. Upward curvature reversed temporarily before cytokinesis in Funaria, a phenomenon already known for Ceratodon and Physcomitrella. Most horizontal and upward-curving Funaria tip cells contained a broad subapical zone where plastid sedimentation occurred. In dark-grown Physcomitrella caulonemata, sedimentation was detected by the presence of a thin, amyloplast-free strip of cytoplasm at the top of the cell. These results suggest that gravitropism and subapical amyloplast sedimentation may be relatively common in moss caulonemata.
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