Diatom Gliding Motility. Группа авторов

Diatom Gliding Motility - Группа авторов


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the plausible assumption that the inertia force can be neglected in the equation of motion, and Stokes’ law holds, the velocity is proportional to the force. In Figure 1.27 the speed of a diatom, which is proportional to the force, is plotted versus the distance between two approaching diatoms. It was determined from a video recorded at 30 fps. This is not sufficient to measure the high speeds shortly before the collision. The fluctuations in velocity at longer distances are probably due to the different drift velocities of the diatoms. This image is primarily intended to illustrate the method.

Schematic illustration of two adjacent Nitzschia sigmoidea on the water surface seen from the horizontal direction. Photo depicts very regular structure of a diatom cluster on the water surface.

      A remarkable aspect is the dynamics of movement. Different forms of movement occur, which indicate different mechanisms. Single floating diatoms are able to move slowly in the direction of the apical axis. This is similar to the movement on substrate, but hardly any longer distances are covered. Adhering lumps of EPS are typically not visible. Since no axenic cultures are used, bacteria can usually be seen on the water surface in phase contrast, making water movement observable. One recognizes changing currents of the water along the raphes, which run opposite to the movement of the diatoms. Apparently, the activity of the raphes can couple to a liquid medium. I do not want to exclude the possibility that the bacteria have an influence on the movement by mechanically coupling to the raphes, but in view of their small size and their lack of mutual contact, I consider their influence to be small. Theories of motility that require adhesion to a solid substrate cannot adequately explain this phenomenon. The movement of diatoms in hanging drops at the interface to air was interpreted by Nultsch in 1957 on the basis of the since disproved cytoplasmic streaming theory. Wavelike movements of microfibrils, as suggested by Bertrand [1.4] in 2008 (translation in Chapter 12 of this book), could cause the observed water transport along the raphe. They strengthen this hypothesis. I could not observe this form of movement with certainty in clusters of several connected diatoms, possibly because they contribute little to movement compared to the other forces acting there.

      In nature, the currents in the water are also likely to whirl up diatoms that do not have a high adhesion to the ground. They may occasionally reach the water surface. The ability to stay there for a longer period of time could lead to dispersal by drifting, i.e., hydrochory.

Schematic illustration of energetically favorable patterns of three diatoms on the water surface: all diatoms parallel (a) and diatoms form a triangle (b). Schematic illustration of the temporal development of seven connected diatoms. Schematic illustration of Pinnularia gentilis.
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