Summary
Microinjection of DNAase I, which is known to form a specific complex with G-actin, induces characteristic changes in cytoplasmic streaming, locomotion and morphology of the contractile apparatus of A. proteus. Light microscopical studies show pronounced streaming originating from the uroid and/or the retracting pseudopods, which ceases 10–15 min after injection of DNAase I, at a time when ultrastructural studies show that the actin filament system is very much reduced. These results suggest that a controlled reversible equilibrium between soluble and polymerized forms of actin is a necessary requirement for amoeboid movement.
The topographic distribution of contractile filaments beneath the plasma membrane visualized by correlated light- and electron microscopy of DNAase I-injected cells establishes the importance of the membrane-bound filamentous layer for three major aspects of streaming: (1) Streaming originates by local contractions of a cell membrane-associated filament layer at the uroid and/or retracting pseudopods, creating a pressure flow. (2) This flow continues beneath the membrane, which is stabilized by filaments in the lateral regions between the posterior end, with a high hydrostatic pressure, and the anterior end, with a low hydrostatic pressure. (3) Pseudopods or extending areas are created by a local destabilization of the cell periphery caused by the separation of the filamentous layer from the plasma membrane.
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W. Gawlitta was supported by a grant (No. 21619) from the Konrad-Adenauer-Stiftung
The authors wish to thank Dr. Mary Osborn for reading the manuscript
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Wehland, J., Weber, K., Gawlitta, W. et al. Effects of the actin-binding protein DNAase I on cytoplasmic streaming and ultrastructure of Amoeba proteus . Cell Tissue Res. 199, 353–372 (1979). https://doi.org/10.1007/BF00236075
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DOI: https://doi.org/10.1007/BF00236075