The potential biomass that could have existed on Mars is constrained b
y the total amount of energy available to construct it. From an invent
ory of the available geochemical sources of energy, we estimate that f
rom the time of the onset of the visible geologic record 4 b.y. ago to
the present, as much as 20 g cm(-2) of biota could have been created.
This is the same amount that could have been constructed on the early
Earth in only 100 million years. This indicates that there likely was
sufficient energy available to support an origin of life on Mars but
not sufficient energy to create a ubiquitous and lush biosphere. Simil
ar calculations for Europa suggest that even less geochemical energy w
ould have been available there.