Responses of Bioconvection of Tetrahymena thermophila to Partial Gravity Created by Aircraft Flight

Bioconvection is a form of collective pattern formation driven by negative gravitaxis of swimming microorganisms. In bioconvection, the interaction between individual swimmers results in self-organization leading to the development of a macroscopic structure typically 100-1000 times greater than an individual microorganism. To gain insight into the role of gravity in this self-organization phenomenon, we investigated the bioconvective behavior of the ciliate Tetrahymena thermophila under short-term partial gravity, i.e., gravitational acceleration < 1 g, achieved by quasiparabolic flight maneuvers of an aircraft. The bioconvective responses of T. thermophila were assessed by observing the collective motion simultaneously in two separate scales, which we call macroscale and microscale, using a newly designed "dual-objective" device with two different magnifications. Microscale analysis revealed that the magnitude of gravikinesis, i.e., active regulation of the propulsive thrust, decreased almost linearly with changes in gravitational acceleration, while gravitactic characteristics, assessed by the distribution of the swimming direction, did not change significantly during partial gravity. Macroscale analysis demonstrated that downward plumes of convection pattern gradually shortened from the lower end, and disappeared under partial gravity. The sustained time of the plumes decreased almost linearly with changes in gravitational acceleration. The response of downward plumes to partial gravity may be attributable to the accumulation of cells into blobs in downward migration, which increases the rate of downward migration enough to exceed the rate of upward movement, which is enhanced due to gravikinesis. This suggests that gravity may act on cells involved in collective pattern formation differently than on free-swimming cells.