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Mercury
Winter 2007 Table of Contents

by
Lisa Kaltenegger
It
is only a matter of time before astronomers find an Earth-sized
planet orbiting a distant star. We will naturally ask whether the
planet is habitable or bears life. But will we be able to tell if
there are bacteria, roaming dinosaurs, or even more advanced life?
While
the first images of any putative exoplanet will be only visual smudges
a single pixel in size, even a low-resolution spectral picture of
the planet will be able to tell us a great deal. For examples: from
spectra we should be able to infer whether the world, like Earth
four billions years ago, was enveloped in a steamy, oxygenless atmosphere
and covered completely by an ocean; or, in a Jurrasic-park-like
epoch, a distant planet’s atmosphere consists of about three-fourths
nitrogen and one-fourth oxygen, with a small percentage of other
gases like carbon dioxide and methane.
In
the past twelve years, scientists have discovered more than two
hundred large planets orbiting other stars, yet finding Earth-like
planets is a fascinating and substantially more technologically
demanding endeavor. And, once we finally do find them, what are
clues to life’s presence on them? Indeed, how do we need to
design our instruments so we don’t miss life’s spectral
signature?
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