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As for Onstott's group, they are trying to expand the subsurface life panoply even more.
An analogous fossil record of subsurface life is nearly missing on Earth.
"It gives us a quantum change in our understanding of how much of the Earth's crust might indeed be habitable and have enough energy to sustain subsurface life.
The establishment of this high surface biomass represented a crucial shift from a planet dominated by subsurface life to one in which surface life became proportionately significant.
There is an implication for other rocky planets, which may similarly contain a subsurface reservoir of hydrogen derived from radiolysis, and thereby could support subsurface life.
If coal beds occur near the limiting zone of deep subsurface life, the nature of survival strategy of microbes may be explored, and 3.
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However, if subsurface microbial life had evolved by this point, it would have survived the bombardment.
Heat transfer between the interior and upper layers would be critical in sustaining any subsurface oceanic life.
Another limiting factor for subsurface martian life is the availability of fixed nitrogen as an essential nutrient, although, as noted above, nitric oxide was found in the eolian deposits of Gale Crater (Stern et al., 2015).
A damp subsurface is where life is most likely to be found today on Mars, notes McEwen.
They also assume, from studies of modern deep subsurface microbes, that life could have thrived in the rock down to a depth of 4 kilometers, putting it out of the reach of impact heating.
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