Abstract
1 Formation of a sulfate-bearing ocean on Jupiter's satellite Europa
by quenched hydrothermal fluids provides a source of metabolic energy
for low-temperature sulfate-reducing organisms that use dissolved
H-2 as an electron donor. Inhibition of thermodynamically favorable
sulfate reduction in cooled hydrothermal fluids creates the potential
for biologic reduction. Both high temperature and reduced conditions
of ocean-forming hydrothermal solutions favor sulfate reduction in
quenched fluids. The maximum amount of energy available to support
autotrophic sulfate reduction is on the order of a few kilojoules
per kilogram of water and is limited by the low abundances of either
H-2 or sulfate in ocean-forming fluids. Although this irreplaceable
energy source might have supported early life on Europa, maintenance
of biologic sulfate reduction throughout the ocean's history would
require a supply of organic compounds from endogenic sources or from
the satellite's surface.
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