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Physics News Update
Number 283, August 27, 1996 by Phillip F. Schewe and Ben Stein

POSSIBLE EVIDENCE FOR LIFE ON MARS has been reported by a team of scientists studying an ancient rock found in Antarctica in 1984. Minerals in the rock suggest that it came from Mars, where it was probably ejected by a giant meteor impact event some millions of years ago. The rock itself, referred to as ALH84001, was formed billions of years earlier, at a time when Mars was warmer, wetter, and presumably more hospitable to life. What does the rock tell us? Team leader, NASA scientist David McKay, says that several strands of evidence, none of which is conclusive by itself, together point toward the existence of ancient life forms on Mars. Microscopic inspection of the rock shows, for example, the presence of organic molecules called polycyclic aromatic hydrocarbons, which can come from the breakdown of biological or non-biological sources. Also present in the sample were minerals sometimes (but not always) associated with bacteria, namely carbonate granules, magnetite, and pyrrhotite. Finally, sample images show 100-nm-sized ovoid shapes which, McKay suggests, might be the fossilized creatures themselves. Various outside scientists have been impressed by the data but skeptical of a biological interpretation; they argue that non-biological causes could account for all of the new findings. Meanwhile, government officials, including President Clinton and NASA administrator Daniel Goldin, have expressed great interest in this research, and proposals for new Mars-oriented projects will doubtless receive great attention. (David S. McKay et al., Science, 16 August 1996.)

A TRANS-SOLAR SPACE CRAFT , one sallying forth beyond the outer planets, would probably need the help of some novel propulsion system, such as the use of sails which would enable the craft to reach high speeds by patiently but effectively reflecting sunlight. Under study at NASA, the Thousand Astronomical Unit mission would have a number of goals. One would be the closeup study of the Kuiper Belt of asteroids (at a distance of about 40 AU). A second goal would be to locate the heliopause, the zone (at around 110-160 AU) where the outgoing solar wind is halted by the incoming interstellar wind. Third, at a distance of several hundred AU, a 1-m telescope on the craft could by triangulation accurately measure distances to stars across much of the Milky Way. (Currently parallax measurements of distances are limited by the baseline of the Earth's orbit to stars out to about 200 light years.) Another goal would be the use of the sun as a gravitational lens for imaging distant objects behind the sun. Moreover, tiny modulations in the return signal from the craft (3 days' transit for light over a path of 500 AU) might encode information about passing gravity waves. (Astronomy, August 1996.)