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In deep ocean ecosystems, bacteria primarily derive their energy from chemosynthesis, a process that converts inorganic compounds into organic matter. They utilize chemicals such as hydrogen sulfide, methane, or ammonia, often found near hydrothermal vents or cold seeps, as energy sources. This unique form of energy production supports diverse ecosystems, including communities of organisms that rely on these bacteria for sustenance. Through this process, deep-sea bacteria play a crucial role in the nutrient cycling and overall functioning of these environments.

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