A sea ice brine pocket is an area of fluid sea water with a high salt concentration trapped in sea ice as it freezes. Due to the nature of their formation, brine pockets are most commonly found in areas below −2 °C (28 °F), where it is sufficiently cold for seawater to freeze and form sea ice. Though the high salinity and low light conditions of brine pockets create a challenging environment for marine mammals, brine pockets serve as a habitat for various microbes. Sampling and studying these pockets requires specialized equipment to accommodate the hypersaline conditions and subzero temperatures.
Formation Brine pockets and channels are formed as seawater freezes, through a process called brine rejection. When sea ice forms, the water molecules form ice crystals, which have a regular lattice structure. The larger salt (NaCl) molecules in the sea water cannot be incorporated into this lattice, resulting in the salt being rejected from the sea ice. As seawater freezes and more pure water ice forms, the salt becomes more highly concentrated in the remaining sea water, forming a brine. As the brine salinity increases it becomes more dense compared to the surrounding sea ice, and the brine sinks downward through the ice, forming brine pockets. As the brine pockets form, they begin to coalesce, forming pockets of dense and saline brine. As these larger pockets of brine become interconnected, the may form a network of brine channels within the ice.
Analysis of structure The internal structure of sea ice can be analyzed using scanning electron microscopy and water-soluble resin. Brine can be drained from the sea ice using centrifugation at sufficiently cold temperatures to prevent melting and to maintain the structural integrity of the sea ice sample. Water-soluble resin is then injected to fill the brine pockets and channels and subsequently polymerized under ultraviolet light at around −12 °C (10 °F). The ice is sublimated by freeze drying, freeing the hardened casts, which can be examined using scanning electron microscopes to determine the structure of the brine pockets and channels and the volume of habitable space available to microbes.
Abiotic conditions
Variability Sea ice brine pockets create diverse and unique microecosystems, with abiotic factors such as chemical composition and physical conditions varying from one pocket to the next. Snow cover and temperature play the most significant role in influencing the variation of conditions present in brine pockets and channels. Sea ice brine pockets in general are extreme environments, due to their subzero temperatures and high salinities, but they harbor a diverse ecosystem of microbial life. Conditions within a brine pocket can vary drastically in a short time with a heavy snowfall or sudden temperature change, which means that microbial life within brine pockets must be flexible to environmental change.
Hypersaline environment As sea ice forms, the water freezes into a lattice structure; this process ejects many of the salts and microbes from the ice, concentrating them in the remaining water. This high-salinity seawater is known as brine, and as more salts accumulate within the brine pockets, the remaining brine becomes more resistant to freezing. This accumulation of salts, producing a liquid environment that can remain liquid in subzero temperatures, provides a harsh-but-suitable environment for microorganisms to survive. These brine pockets maintain a very saline environment, have high concentrations of other dissolved minerals, and have a high density of microbial life. Brine salinity and concentration are directly dependent on the air temperature of the surrounding environment; as temperatures decrease, more salts become rejected from newly-formed ice, causing more salts to accumulate within the brine, and brine pockets decrease in size. This results in a hypersaline environment with dissolved salt contents which can reach up to 200 g/kg, in contrast to open seawater which has a salinity of 33-37 g/kg.
Light limitation Brine pockets can form deep within sea ice where there is very low irradiance. Since snow and ice block and reflect incoming light, with deeper brine pockets experience more light limitation than shallower brine pockets. When salts in seawater become rejected during the ice formation, these salts can precipitate and accumulate within the ice, influencing the ability of light to pass through the ice. Given that more salts will precipitate with colder temperatures as brine becomes more concentrated, colder temperatures can result in a greater change to the optics of the ice as more salts accumulate. Lower light levels in brine pockets can impact the survivability of photosynthetic organisms such as cyanobacteria and diatoms. These organisms have developed adaptations so that they can survive in this extremely light-limited environment.
Microbial diversity and abundance
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