GOOD-BYE OCEAN? Scientists have long
searched Mars for carbonate minerals, a common by-product of weathering. But despite ample evidence for
lots of water at the surface, massive carbonate deposits - relics of
a possible ancient ocean - have proved elusive. Spectral data from the orbiting Thermal
Emission Spectrometer (TES) came to the rescue - sort of. TES showed
that Martian carbonate minerals do exist, but they are not primarily in the
rocks. Instead, carbonate minerals dwell mainly in the dust that's everywhere
on Mars. These carbonates
probably did not form in any large bodies of water, but rather as
atmospheric moisture combined with airborne dust. Click on the
image to download a larger version (660 kB). NASA/JPL/Arizona State
University
Bandfield, J. L., T. D. Glotch, and P. R. Christensen, Spectroscopic identification of carbonates in the Martian dust, Science, 301, 1084:1987, 2003.