Aerosol particles in the atmosphere have recently been found to contain a l
arge number of chemical elements and a high content of organic material. Th
e latter property is explicable by an inverted micelle model. The aerosol s
izes with significant atmospheric lifetimes are the same as those of single
-celled organisms, and they are predicted by the interplay of aerodynamic d
rag, surface tension, and gravity. We propose that large populations of suc
h aerosols could have afforded an environment, by means of their ability to
-concentrate molecules in a wide variety of physical conditions, for key ch
emical transformations in the prebiotic world. We also suggest that aerosol
s could have been precursors to life, since it is generally agreed that the
common ancestor of terrestrial life Was a single-celled organism, The earl
y steps in some of these initial transformations should be accessible to ex
perimental investigation.