A metabolic process that differs drastically
from photosynthesis, the dominant metabolic process on
Earth that relies on energy from the Sun. Chemosynthetic
bacteria use hydrogen sulfide produced at deep seafloor
hydrothermal vents known as black smoker chimneys as an
energy source for their metabolism. The hydrogen sulfide is
produced by water that is heated by magma in the crust and
reacts with the seafloor basalt, converting sulfate in the seawater
to hydrogen sulfide. The primitive bacteria at these
seafloor hydrothermal vents, first discovered in 1977, metabolize
the hydrogen sulfide as an energy source and become
the primary producers in a complex food web around the
vents. Other organisms that in turn depend on the chemosynthetic
bacteria include giant tube worms, giant clams, lobster,
and fish. Some models for the origin of life on Earth suggest
that the earliest life on the planet was probably chemosynthetic
and heat-loving (thermophyllic).
See also BLACK SMOKER CHIMNEYS; LIFE’S ORIGINS AND
EARLY EVOLUTION.














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