Mike
Engel and Randall S. Perry
There
is no compelling evidence that life, as we know it, presently exists elsewhere
in our solar system or beyond. Even
Mars, the most obvious extraterrestrial planetary candidate for life, is
unlikely to have had surface (or near surface) conditions conducive for life
during the past 3 to 4 billion years (e.g. Shuster and Weiss, 2005). Fossil and geochemical data indicate that
life may have existed on Earth for as far back in time as the rock record
extends (approximately 3.5 Ga). If this
is true, then it will not be possible to search the Earth's rock record for
evidence of life's origin unless older rocks of appropriate type and thermal
history are discovered. Alternatively,
this evidence may be sought from meteorites and planetary materials that were
formed during the solar system's first 500 million years. Criteria are presented
that can be used to determine if life's building blocks (e.g. amino acids) in
these ancient materials are relicts of early life or if they were formed by
non-biological processes. Additional
criteria are presented for distinguishing indigenous organic compounds in
ancient rocks from more recent contaminants.
D.L.
Shuster and B.P. Weiss (2005) Martian surface paleotemperature from
thermochronology of meteorites, Science 309, 594-600.