Bioconvection occurs when a macroscopic nonuniformity of the concentration
of microbial populations is generated and maintained by the directional swi
mming of the organisms. This study investigated the properties of the patte
rns near the onset of the instability and later during its evolution into a
fully nonlinear convection regime. In suspensions of the bacteria Bacillus
subtilis, which tend to swim upwards in a gradient of oxygen concentration
that they create by consumption, we discovered that the dominant wavelengt
h at the onset of the instability is determined primarily by the cell densi
ty and is influenced only weakly by the fluid depth. This observation contr
asts strongly with previous observations on the gravitactic alga Chlamydomo
nas nivalis, in which the opposite dependence was found. Considerable diffe
rences were also found in the long-term evolution of the convection pattern
s. These results demonstrate the existence of readily distinguishable types
of bioconvection systems, even at early stages of the instability. The obs
erved differences are clearly and causally correlated with disparate reason
s for upward swimming by these microorganisms, leading to different geometr
ic distributions of the density of the suspension.