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

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planets <strong>and</strong> <strong>for</strong> underst<strong>and</strong><strong>in</strong>g subsequent processes such as accretion, magma oceans, differentiation,<br />

core convection, dynamo generation, partial melt<strong>in</strong>g <strong>and</strong> volcanism. Mars, <strong>the</strong> Moon, Venus, <strong>and</strong><br />

Mercury are l<strong>in</strong>ked by similar bombardment histories, <strong>and</strong> all conta<strong>in</strong> evidence <strong>for</strong> volcanism,<br />

differentiation <strong>and</strong> early crustal growth. Of <strong>the</strong>se <strong>in</strong>ner planets, Mars has evidence of an early dynamo<br />

process, absent on Venus <strong>and</strong> <strong>the</strong> Moon. Thus, Mars provides <strong>in</strong><strong>for</strong>mation on <strong>the</strong> early stages of planet<br />

<strong>for</strong>mation <strong>and</strong> heat-loss mechanisms that are crucial <strong>for</strong> putt<strong>in</strong>g <strong>the</strong> differentiation history, bulk chemistry<br />

<strong>and</strong> geophysical properties of all of <strong>the</strong> <strong>in</strong>ner planets, <strong>in</strong>clud<strong>in</strong>g Earth, <strong>in</strong> context.<br />

To Extrasolar Planets<br />

Mars provides a unique alternative to Earth as a lead<strong>in</strong>g potential example of a planet that has<br />

been habitable <strong>in</strong> <strong>the</strong> past, at least episodically. There<strong>for</strong>e, it is especially <strong>in</strong>terest<strong>in</strong>g with regard to our<br />

underst<strong>and</strong><strong>in</strong>g of <strong>the</strong> habitability of extrasolar terrestrial planets <strong>and</strong> <strong>the</strong> likel<strong>in</strong>ess of life elsewhere. In<br />

particular:<br />

• Mars has a low mass/radius relative to Earth <strong>and</strong> <strong>the</strong>re<strong>for</strong>e exp<strong>and</strong>s <strong>the</strong> possible range of<br />

silicate extrasolar planet mass/radius values that may be targeted <strong>for</strong> habitability;<br />

• The potential discovery of habitable regions on Mars <strong>for</strong>ces us to exp<strong>and</strong> <strong>the</strong> concept of <strong>the</strong><br />

classic “habitable zone” 75 with<strong>in</strong> planetary systems;<br />

• Ancient Mars was probably a case of a relatively dry planet (no global oceans) with an<br />

environmental regime fundamentally different than that of our planet, <strong>and</strong> which we can study through <strong>the</strong><br />

geological records; <strong>and</strong><br />

• The fact that Mars has lost its ability to susta<strong>in</strong> liquid water teaches us lessons about possible<br />

processes that may prevent many extrasolar planets from rema<strong>in</strong><strong>in</strong>g habitable.<br />

To Human Exploration<br />

Mars is <strong>the</strong> only planet <strong>in</strong> <strong>the</strong> solar system that is realistically accessible to human exploration,<br />

<strong>and</strong> has been proposed as a target <strong>for</strong> orbital flybys <strong>and</strong> future l<strong>and</strong><strong>in</strong>g by human explorers. To reduce <strong>the</strong><br />

cost <strong>and</strong> risk <strong>for</strong> future human exploration, robotic precursor missions would be needed to acquire<br />

<strong>in</strong><strong>for</strong>mation concern<strong>in</strong>g potential resources <strong>and</strong> hazards, per<strong>for</strong>m technology <strong>and</strong> flight system<br />

demonstrations, <strong>and</strong> deploy <strong>in</strong>frastructure to support future human exploration activities. The elements of<br />

<strong>the</strong> Mars Sample Return campaign, beg<strong>in</strong>n<strong>in</strong>g with MSL, will provide crucial data <strong>for</strong> l<strong>and</strong><strong>in</strong>g significant<br />

mass, execut<strong>in</strong>g surface ascent <strong>and</strong> return to Earth, <strong>and</strong> identify<strong>in</strong>g potential hazards <strong>and</strong> resources. 76<br />

IMPORTANCE OF MARS SAMPLE RETURN<br />

For <strong>the</strong> past three decades, <strong>the</strong> scientific community has consistently advocated <strong>the</strong> return of<br />

geological samples from Mars. Summaries of <strong>the</strong> literature on this topic appear <strong>in</strong> <strong>the</strong> extensive writ<strong>in</strong>gs<br />

of <strong>the</strong> NRC, 77 several major recent reports by MEPAG, 78 <strong>and</strong> a significant recent contribution by <strong>the</strong><br />

International Mars Exploration Work<strong>in</strong>g Group. 79 Numerous white papers submitted to <strong>the</strong> NRC Decadal<br />

Survey <strong>in</strong>dicated substantial community support via signatories <strong>and</strong> addressed <strong>the</strong> importance <strong>and</strong><br />

significance of Mars Sample Return as <strong>the</strong> keystone of future Mars exploration. 80<br />

The committee, build<strong>in</strong>g on numerous community assessment groups, open discussions, <strong>and</strong><br />

white papers, places as <strong>the</strong> highest priority Mars science goal to address <strong>in</strong> detail <strong>the</strong> questions of<br />

habitability <strong>and</strong> <strong>the</strong> potential orig<strong>in</strong> <strong>and</strong> evolution of life on Mars. The committee carefully considered<br />

<strong>the</strong> alternative of several rover missions <strong>in</strong>stead of sample return. It is our op<strong>in</strong>ion that sample return<br />

would have significantly higher science return <strong>and</strong> a much higher science-to-dollar ratio. Thus, a critical<br />

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

6-21

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