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Brine pool
Accumulation of brine in a seafloor depression
A brine pool, sometimes called an underwater lake, deepwater or brine lake, is a volume of brine collected in a seafloor depression. These pools are dense bodies of water that have a salinity that is typically three to eight times greater than the surrounding ocean. Brine pools are commonly found below polar sea ice and in the deep ocean. This below-sea ice forms through a process called brine rejection.[1] For deep-sea brine pools, salt is necessary to increase the salinity gradient. The salt can come from one of two processes: the dissolution of large salt deposits through salt tectonics[2] or geothermally-heated brine issued from tectonic spreading centers.[3]
The brine often contains high concentrations of hydrogen sulfide and methane, which provide energy to chemosynthetic organisms that live near the pool. These creatures are often extremophiles and symbionts.[4][5] Deep-sea and polar brine pools are toxic to marine animals due to their high salinity and anoxic properties,[1] which can ultimately lead to toxic shock and possibly death.