If early Mars was as barren and cold as it is today, massive asteroid and comet impacts would have produced enough heat to melt subsurface ice, said Stephen Mojzsis, a professor at University of Colorado Boulder in US.
The impacts would have produced regional hydrothermal systems on Mars similar to those in the Yellowstone National Park in US, which today harbour chemically powered microbes, some of which can survive boiling in hot springs or inhabiting water acidic enough to dissolve nails.
In addition to producing hydrothermal regions in portions of Mars' fractured and melted crust, a massive impact could have temporarily increased the planet's atmospheric pressure, periodically heating Mars up enough to "re-start" a dormant water cycle.
"This study shows the ancient bombardment of Mars by comets and asteroids would have been greatly beneficial to life there, if life was present," said Mojzsis.
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"But up to now we have no convincing evidence life ever existed there, so we don't know if early Mars was a crucible of life or a haven for life," he said.
Unlike Earth, which has been "resurfaced" time and again by erosion and plate tectonics, heavy cratering is still evident on Mercury, Earth's moon and Mars, Mojzsis said.
Researchers used a supercomputer cluster for some of the 3D modelling used in the study.
They looked at temperatures beneath millions of individual craters in their computer simulations to assess heating and cooling, as well as the effects of impacts on Mars from different angles and velocities.
"None of the models we ran could keep Mars consistently warm over long periods," said Mojzsis.
While Mars is believed to have spent most of its history in a cold state, Earth was likely habitable over almost its entire existence.
An earlier study showed that the Late Heavy Bombardment period in the inner solar system nearly 4 billion years ago did not have the firepower to extinguish potential early life on Earth and may have even given it a boost if it was present.