Velocity distribution of the anterograde and retrograde transport of extracellular particles byAmoeba proteus

Summary

The transverse velocity profiles of the anterograde flow of particles on the cell surface and around it are approximately parabolic. The peak velocity is recorded close to the membrane and the descendent arm of the profile is viscosity-dependent. It indicates that the extracellular forward flow is probably generated by a forward movement of the fluid fraction of the membrane itself. The retrograde component of extracellular movements is manifested by particles kept on the cell surface by adhesion, which behave exactly as the ectoplasmic layer on the opposite side of the membrane,i.e., they probably reflect the movement of that fraction of the surface material which is attached to the cortical microfilaments. In the longitudinal profile, the velocity of anterograde flow rises from the tail to the front of amoeba, but is generally related to the effective cell locomotion rate and not to the movements of any intracellular layer. Around the cells deprived of any attachment to the substratum, which cannot locomote but manifest vigorous intracellular movements, the anterograde flow ceases at least along 2/3 of their lenght. It persists, however, around the frontal fountain zone, where other particles still move backwards together with the retracted ectoplasmic layer. This indicates that the role of the forward flow of and on the cell surface is to compensate for: (1) the increase of the surface area in the frontal regions due to locomotion, (2) the withdrawal of a part of material which is hauled back by the retracting cortical layer. A comprehensive scheme of the velocity distribution within the different layers of a moving amoeba and around it has been constructed on the basis of present and earlier data.