Fact
|
Assumption
|
Experiment
|
Life on Earth requires water
- Water is located near
the Martian poles
- Water is located
beneath the Martian surface
|
-Life will only exist on Mars near water
-Look underground or near poles
|
Drill below the surface and test for water.
|
-Mars probably has an oxidizing surface due to the
presence of superoxides
-Mars has very little atmospheric pressure
-The atmosphere is mostly CO2
-The surface is unshielded from UV radiation
|
Martian life, if it exists, will not exist on the surface;
rather, it will exist deep underground or below the surface of large rocks
|
-Examine the surfaces of rocks for evidence of life just
below the rock surface
-Drill
|
-Life on Earth is carbon-based
-Carbon has by far the most diverse chemistry of any
element
|
Martian life will also be carbon based
|
Test for the presence of complex organic molecules
|
Earth life is based on four particular organic compounds:
nucleic acids, proteins, carbohydrates, and lipids
|
Martian life will also use these classes of compounds
|
Test for the presence of these compounds
|
Life on Earth is associated with energetic simple
molecules
|
Martian life will also use these energy sources
|
Look for energetic simple molecules, such as CH4,
H2, CO, H2S, and FeS, as well as evidence of past
carbon and nitrogen cycles
|
Life on Earth is attracted to sources of thermal and light
energy
|
The surface is inhospitable, so Martian life will be
attracted to geothermal heat sources.
|
Look for geothermal heat sources [will be done by
satellite not part of mission]
|
-Earth life metabolizes organic molecules
-Earth life produces gaseous products of such metabolism
|
Mars life will also metabolize organic molecules to
gaseous products
|
Look for evidence of metabolic gas products, and confirm
that they are not caused by abiotic chemical reactions (labeled-release)
|
Some forms of Earth life are photosynthetic and
chemosynthetic, and able to convert CO and CO2 to complex
molecules
|
There will also be photosynthetic or chemosynthetic Mars
life
|
Look for evidence of CO2 uptake and retention
(pyrolytic release)
|
No Mars missions have examined the subsurface structure of
Mars
|
It would be helpful to have such information in order to
drill
|
Conduct a geological survey
|
Earth life is occasionally preserved in rocks as visible
organic structures
|
Mars life would be similarly preserved
|
Examine rocks for visible fossil evidence
|
Metabolism in Earth life discriminates between different
isotopes
|
Mars life will discriminate similarly
|
Look for differences in isotope ratios between organic
carbon and inorganic carbon
|