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- W2913184755 abstract "Abstract Hydrated, magnesium-rich minerals and subglacial brines exist on the martian surface, so the habitability of high-Mg 2+ environments on Earth has extraterrestrial (as well as terrestrial) implications. Here, we report the discovery of a MgCl 2 -dominated (4.72 M) brine lake on the floor of the Mediterranean Ridge that underlies a 3500-m water column, and name it Lake Hephaestus . Stable isotope analyses indicated that the Hephaestus brine is derived from interactions between ancient bishofite-enriched evaporites and subsurface fluids. Analyses of sediment pore waters indicated that the Hephaestus depression had contained the MgCl 2 brine for a remarkably short period; only 700 years. Lake Hephaestus is, therefore, the youngest among currently known submarine athalassohaline brine lakes on Earth. Due to its biologically hostile properties (low water-activity and extreme chaotropicity), the Hephaestus brine is devoid of life. By contrast, the seawater- Hephaestus brine interface has been shown to act as refuge for extremely halophilic and magnesium-adapted stratified communities of microbes, even at MgCl 2 concentrations that approach the water-activity limit for life (0.653)." @default.
- W2913184755 created "2019-02-21" @default.
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- W2913184755 date "2019-02-08" @default.
- W2913184755 modified "2023-09-26" @default.
- W2913184755 title "The discovery of Lake Hephaestus, the youngest athalassohaline deep-sea formation on Earth" @default.
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- W2913184755 doi "https://doi.org/10.1038/s41598-018-38444-z" @default.
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