Membrane movements and fluidity during rotational motility of a termite flagellate. A freeze-fracture study

Abstract

Freeze-fracture electron microscopy was used to examine the structure of a region of plasma membrane that undergoes continual, unidirectional shear. Membrane shear arises from the continual clockwise rotation of one part (head) of a termite flagellate relative to the rest of the cell. Freeze-fracture replicas show that the lipid bilayer is continuous across the shear zone. Thus, the relative movements of adjacent membrane regions are visible evidence of membrane fluidity. The distribution and density of intramembrane particles within the membrane of the shear zone is not different from that in other regions of the cell membrane. Also, an additional membrane shear zone arises when body membrane becomes closely applied to the rotating axostyle as cells change shape in vitro. This suggests that the entire membrane is potentially as fluid as the membrane between head and body but that this fluidity is only expressed at certain locations for geometrical and/or mechanical reasons. Membrane movements may be explained solely by cell shape and proximity to rotating structures, although specific membrane-cytoskeletal connections cannot be ruled out. The membrane of this cell may thus be viewed as a fluid which adheres to the underlying cytoplasm/cytoskeleton and passively follows its movements.