PX282 - M2 - possible environments for life
mars
- it lies in the habitable zone around the sun. where liquid water can exist on the surface of a planet, and the atmospheric pressure is just enough
- imaging and sampling show that surface water was abundant in the past
- enhanced deuterium-hydrogen ratio (D/H) provides evidence of past water lost to evaporation
- there is radar evidence of liquid water lakes below ice caps
venus
- it has no surface water, and has an extreme D/H implying extreme water loss
- possible detection of phosphine PH
might be a biomarker - liquid water droplets (in the form of sulphuric acid) do exist in clouds
icy moons of the giants
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europa, which is resurfaced with liquid water from a tidally-heated subsurface ocean
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it has relatively low water content
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thin ocean and maybe hydrothermal vents providing nutrients
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deeper oceans on ganymede will have ice at the bottom, and probably no hydrothermal vents
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enceladus has water geysers with organic chemistry, and molecular hydrogen
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titan may have exotic life in its methane lakes