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Vision and Voyages for Planetary Science in the - Solar System ...

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DETERMINE IF LIFE EVER AROSE ON MARS<br />

The prime focus of this goal is to determ<strong>in</strong>e if life is or was present on Mars. If life was <strong>the</strong>re we<br />

must underst<strong>and</strong> <strong>the</strong> resources that support or supported it. If life never existed yet conditions appear to<br />

have been suitable <strong>for</strong> <strong>for</strong>mation <strong>and</strong>/or ma<strong>in</strong>tenance of life, a focus would <strong>the</strong>n be to underst<strong>and</strong> why life<br />

did not orig<strong>in</strong>ate. A comprehensive conclusion about <strong>the</strong> question of life on Mars will necessitate<br />

underst<strong>and</strong><strong>in</strong>g <strong>the</strong> planetary evolution of Mars <strong>and</strong> whe<strong>the</strong>r Mars is or could have been habitable, us<strong>in</strong>g<br />

multi-discipl<strong>in</strong>ary scientific exploration at scales rang<strong>in</strong>g from planetary to microscopic. The strategy<br />

adopted to pursue this goal has two sequential science steps: assess <strong>the</strong> habitability of Mars on an<br />

environment-by-environment basis us<strong>in</strong>g global remote sens<strong>in</strong>g observations; <strong>and</strong> <strong>the</strong>n test <strong>for</strong> prebiotic<br />

processes, past life, or present life <strong>in</strong> environments that can be shown to have high habitability potential.<br />

A critical means to achieve both objectives is to characterize martian carbon chemistry <strong>and</strong> carbon<br />

cycl<strong>in</strong>g.<br />

There<strong>for</strong>e, <strong>the</strong> committee’s specific objectives to pursue <strong>the</strong> life goal are to as follows:<br />

• Assess <strong>the</strong> past <strong>and</strong> present habitability of Mars,<br />

• Assess whe<strong>the</strong>r life is or was present on Mars <strong>in</strong> its geochemical context, <strong>and</strong><br />

• Characterize carbon cycl<strong>in</strong>g <strong>and</strong> prebiotic chemistry.<br />

Subsequent sections exam<strong>in</strong>e each of <strong>the</strong>se objectives <strong>in</strong> turn, identifies critical questions to be<br />

addressed <strong>and</strong> future <strong>in</strong>vestigations <strong>and</strong> measurements that could provide answers.<br />

BOX 6.2 Biosignatures<br />

Life can be def<strong>in</strong>ed as essentially a self-susta<strong>in</strong><strong>in</strong>g system capable of evolution. But to guide <strong>the</strong><br />

search <strong>for</strong> signs of life on Mars requires a work<strong>in</strong>g concept of life that helps to identify its key<br />

characteristics <strong>and</strong> its environmental requirements. Biosignatures are features that can be unambiguously<br />

<strong>in</strong>terpreted as evidence of life <strong>and</strong> so provide <strong>the</strong> means to address fundamental questions about <strong>the</strong><br />

orig<strong>in</strong>s <strong>and</strong> evolution of life. Types of biosignatures <strong>in</strong>clude morphologies (e.g., cells, <strong>and</strong> plant or animal<br />

remnants), sedimentary fabrics (e.g., lam<strong>in</strong>ations <strong>for</strong>med by biofilms), organic molecules, biom<strong>in</strong>erals<br />

(e.g., certa<strong>in</strong> <strong>for</strong>ms of magnetite), 4 elemental abundances, <strong>and</strong> stable isotopic patterns. Because some<br />

biosignatures are preserved over geologic time scales <strong>and</strong> <strong>in</strong> environments that are no longer habitable,<br />

<strong>the</strong>y are important targets of exploration. It is not unreasonable to anticipate that any martian life might<br />

differ significantly from life on Earth, though Earth’s environments have been more similar to those on<br />

Mars than to <strong>the</strong> environments of any o<strong>the</strong>r object <strong>in</strong> <strong>the</strong> solar system. Moreover, Mars <strong>and</strong> Earth may<br />

have exchanged life <strong>for</strong>ms through impact ejecta. Any martian life may reasonably be assumed to have<br />

shared at least some of its basic attributes with life as we know it, which implies that any martian life also<br />

requires liquid water, carbon-based chemistry, <strong>and</strong> electron transfer processes. 5,6<br />

Our work<strong>in</strong>g concept of life should also identify environmental conditions that are most<br />

conducive to life. A habitable environment must susta<strong>in</strong> liquid water at least <strong>in</strong>termittently <strong>and</strong> also allow<br />

key biological molecules to survive. The elements carbon, hydrogen, nitrogen, oxygen, phosphorus, <strong>and</strong><br />

sulfur (CHNOPS) must be available, as <strong>the</strong>y are essential <strong>for</strong> <strong>for</strong>m<strong>in</strong>g <strong>the</strong> covalently bonded compounds<br />

of all known life. Organic compounds are <strong>the</strong>re<strong>for</strong>e key targets, with <strong>the</strong> caveat that martian <strong>and</strong> Earthly<br />

life might have employed different compounds. Energy drives metabolism <strong>and</strong> motility, <strong>and</strong> must be<br />

available from, <strong>for</strong> example, light or energy-yield<strong>in</strong>g chemical reactions. 7 F<strong>in</strong>ally, <strong>the</strong> rates of<br />

environmental changes must not exceed rates at which life could adapt. 8<br />

Even if habitable environments supported <strong>the</strong> orig<strong>in</strong>ation <strong>and</strong> evolution of life on Mars, <strong>the</strong> right<br />

set of environmental conditions is required <strong>in</strong> order to preserve biosignatures. The study of fossilization<br />

processes will be as important <strong>for</strong> Mars as it has been <strong>for</strong> Earth. 9 The preservation of biosignatures is<br />

critically sensitive to <strong>the</strong> diagenetic processes that control preservation <strong>and</strong>, paradoxically, <strong>the</strong> very<br />

PREPUBLICATION COPY—SUBJECT TO FURTHER EDITORIAL CORRECTION<br />

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