Microbial life has adapted to various individual extreme conditions; yet, organisms simultaneously adapted to low pH, high salt and high temperature are unknown. We combined environmental 16S/18S rRNA-gene metabarcoding, cultural approaches, fluorescence-activated cell sorting, scanning electron microscopy and chemical analyses to study samples along such 25 unique polyextreme gradients in the Dallol-Danakil area (Ethiopia). We identify two physicochemical barriers to life in the presence of surface liquid water defined by high chaotropicity-low water activity in Mg 2+ /Ca 2+ -dominated brines and hyperacidity-salt combinations. When detected, life was dominated by highly diverse ultrasmall archaea widely distributed across phyla with and without previously known hyperhalophilic members. We detect 30 active silica encrustment/fossilization of cells but also abiotic biomorphs of varied chemistry, raising warnings for the interpretation of morphological biosignatures on Earth and beyond.
One Sentence Summary:The absence of life from some polyextreme sites in the presence of liquid surface water on Earth 35 helps to circumscribe habitability Belilla et al.
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Main Text:Microbial life has adapted to so-called extreme values of temperature, pH or salinity, but also to 5 several polyextreme, e.g. hot acidic or salty alkaline, ecosystems (1, 2). However, organisms adapted simultaneously to low pH and high salt, and eventually also high temperature, are not known (1). Are molecular adaptations to those combinations incompatible or (hot) acidic hypersaline environments simply rare and unexplored? The Dallol geothermal dome and its surroundings (Danakil Depression, Afar, Ethiopia) allow to address this question by offering 10 unique polyextreme gradients combining high salt content (20 to >50%; either Mg 2+ /Ca 2+ or Na + (/Fe 2+/3+ )-rich), high temperature (25-110°C) and low pH (≤-1.5 to 6). Dallol is an up-lifted (~40 m) dome structure located in the North of the Danakil depression (~120 m below-sea-level), a 200 km-long basin within the Afar rift, at the triple junction between the Nubian, Somalian and Arabian Plates (3). Lying only 30 km north of the hypersaline, hydrothermally-influenced, Lake 15 Assale (Karum) and the Erta Ale volcanic range, Dallol does not display volcanic outcrops but intense degassing and hydrothermal activity. These activities are observed on the salt dome and the adjacent Black Mountain and Yellow Lake (Gaet'Ale) areas (3, 4) ( Fig. 1a-b). Gas and fluid isotopic measurements indicate that meteoritic waters, notably infiltrating from the high Ethiopian plateau (>2,500 m), interact with an underlying geothermal reservoir (280-370°C) (4, 20 5). Further interaction of those fluids with the km-thick marine evaporites filling the Danakil depression results in unique combinations of polyextreme conditions and salt chemistries (3,4,6, 7), which have led some authors consider Dallol as a Mars analog (8).Here, we use environmental 16S/18S rRNA-gene metabarcoding, cultural approaches, fluorescence-activa...