Commenters discussed oxygen-deprived brine pools and layered seas as surprising habitats and possible windows into early life. lproven pointed to subterranean and under-ice lakes like Lake Vostok and the Black Sea’s anoxic lower layer as examples where life persists despite low oxygen. areoform quoted CTD and lab data from NEOM brine pools showing salinity jumping from ~40 to ~160 PSU within centimeters and dissolved oxygen falling to <10 μmol L−1, while temperature rises only modestly, and several participants (aboutplants, nephihaha) emphasized that microbial life is routinely found in extreme niches.
The conversation split over how those sharp interfaces persist. HPsquared and HPsquared (again) proposed geothermal heating, heat-transfer differences, or continual oozing of brine as maintenance mechanisms; yrjrjjrjtjjr suggested molecular turnover with conditions held steady. Others argued physical separation and scale slow mixing: andrewflnr and Lumich compared it to density-driven pyroclastic flows and air-mass behavior, atrus cited stratification in water heaters, zeumo mentioned layered cocktails, and Shitty-kitty pointed to simple density-driven sinking. Opinion divides between proponents of active replenishment/thermal processes and those who attribute longevity to density, scale, and inhibited convection slowing diffusion.
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