Chemosynthesis
Some microbes oxidize hydrogen sulfide, methane or hydrogen to power the fixation of carbon into organic molecules.
Where sunlight ends,
another world begins.
Descend into a luminous sanctuary of volcanic chimneys, glass jellies and creatures powered by the chemistry of the Earth.
Change the conditions. Watch the living landscape respond in real time.
A volcanic mineral tower releasing superheated, mineral-rich fluid. Its dark plume is tiny particles of metal sulfides.
Microbes can harvest energy from chemical reactions instead of sunlight.
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Hydrothermal vents form where seawater descends into fractured seafloor rock, heats near magma, dissolves minerals, and rushes back into cold ocean water. Within these chemical gradients, microbes use chemosynthesis to create organic matter. They are the foundation of astonishing animal communities.
Some microbes oxidize hydrogen sulfide, methane or hydrogen to power the fixation of carbon into organic molecules.
When hot fluid mixes with cold seawater, dissolved metals precipitate as dark mineral-rich particles, while deposits build chimneys.
Some tube worms rely on internal bacteria for nutrition rather than an ordinary digestive system.
Scientific note: The exhibit combines vent organisms, deep-sea corals and jellies in a stylized educational scene. Not all species shown necessarily coexist at one real vent site. Slider responses are illustrative.