Brine pool

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These craters mark the formation of brine pools, from which salt has seeped through the seafloor and encrusted the nearby substrate.
NOAA rendering of a brine pool in the Gulf of Mexico.
Chimaeridae fish and seep mussels at edge of brine pool.

A brine pool is a large area of brine on the ocean basin. These pools are bodies of water that have a salinity three to five times greater than the surrounding ocean. For deep-sea brine pools, the source of the salt is the dissolution of large salt deposits through salt tectonics. The brine often contains high concentrations of methane, providing energy to chemosynthetic animals that live near the pool. These creatures are often extremophiles.[1][2] Brine pools are also known to exist on the Antarctic Shelf where the source of brine is salt excluded during formation of sea ice. Deep-sea and Antarctic brine pools can be toxic to marine animals.


Brine pools are sometimes called seafloor "lakes" because the dense brine does not easily mix with overlying seawater. The high salinity raises the density of the brine, which creates a distinct surface and shoreline for the pool.[3] When submarines dive into brine pools, they float on the brine surface due to the high density. The motion of a submarine can create waves across the brine-seawater interface that wash over the surrounding "shoreline".[4]

Support of life[edit]

Deep sea brine pools often coincide with cold seep activity. Methane released by the seep is processed by bacteria, which have a symbiotic relationship with seep mussels living at the edge of the pool. This ecosystem is dependent on chemical energy, and unlike almost all other life on Earth, has little dependence on energy from the Sun.[5]