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Biology subjects

Demergasso, C.

Publications and source records attributed to Demergasso, C..

3 recordsLinked to original sources

Aridity drives global convergence of desert microbiomes and biogeochemical activities

Deserts cover a third of the worlds surface, supporting unique biomes and ecosystem services. Yet, we lack a comprehensive assessment of what defines and drives the microbial communities that dominate life in these regions. Here, we conducted a standardized field survey in contrasting cold, hot, and polar deserts across the seven continents, and observed geographically distant deserts share similar structure, function, and activities. Desert communities are dominated by genomically streamlined Actinobacteriota and Chloroflexota, and compared with non-desert soils, are significantly enriched with stress tolerance genes, mobile genetic elements, and antiviral strategies, revealing previously unknown ecological and evolutionary dynamics. Metabolically, these communities exhibit reduced capacity for carbohydrate and protein degradation, and instead are enriched for chemosynthetic carbon fixation, continuous energy harvesting using atmospheric trace gases and sunlight, and energy reserve biosynthesis. All sampled soils mediated respiration, trace gas oxidation, and carbon fixation, with detectable activity even in hyper-arid Atacama and Antarctic soils at the margins of life. Driver analyses identified aridity as the primary overriding driver of the microbial communities and biogeochemical activities. Collectively, these findings suggest that aridity selects for metabolically self-sufficient taxa capable of continuously meeting energy and carbon needs independently of vegetation-derived inputs, while enduring physicochemical stressors and potentially elevated viral pressure. These new insights are integral to forecast the future of soils amid increasing desertification. Significance statementDesert soils occupy a vast and expanding portion of Earth, yet what defines and governs their dominant microbial life remains incompletely defined. By assessing the composition, capabilities, and activities of microbial communities across deserts on all seven continents, we identify unifying signatures of life under extreme water limitation. We show microbial communities are highly self-sufficient, capable of acquiring energy and carbon even where plant inputs are minimal. This planetary-scale understanding of the desert microbiome has important ramifications for forecasting potential shifts of microbial communities and the services they provide as desertification intensifies.

microbiology↗

The limit of life at extremely low water activity:Lithium-concentration ponds in a solar saltern(Salar de Atacama, Chile)

Extremely hyper-saline ponds from an industrial lithium-concentration process in solar salterns in the Atacama Desert were studied to determine the limits of life at very low water activity. Water activity (aw) of 0.61 is the lowest aw value for growth of living beings recorded to date. Xerophilic (sometimes called osmophilic) filamentous fungi and yeasts are predominant in high-sugar foods with such low aw values. Some microorganisms are capable of growth at that water activity level. By contrast, high-salt environments are almost exclusively populated by prokaryotes, notably the Halobacteria class and some Bacteroidetes, capable of growing in saturated NaCl (aw 0.75). The lowest aw that can be achieved by the addition of NaCl is 0.75 (saturation point for NaCl). Crystallizer ponds in Li+ concentration plants reach down to water activity levels around 0.1. The aim of this study was to determine how far along the salinity gradient could life be found. Cell counts were attempted by epifluorescence microscopy and qPCR with bacterial and archaeal universal primers. Biomass for DNA extraction was obtained by an optimized protocol involving dialysis of brines previously fixed with ethanol. Prokaryotic diversity was studied by DNA extraction, PCR, qPCR and 16S rRNA amplicon sequencing in different ponds along the salinity gradient. Archaeal DNA was found in the lower salinity ponds, while bacterial DNA was found along the whole gradient. Bacterial cDNA was retrieved from ponds down to an aw of 0.2. Moreover, bacteria could be grown in enriched cultures from most ponds.

microbiology↗

Soil microbial habitats in an extreme desert Mars-analogue environment

Sediments in the hyper-arid core of the Atacama Desert are a terrestrial analogue to Mars regolith. Understanding the distribution and drivers of microbial life in the sediment may give critical clues on how to search for biosignatures on Mars. Here, we identify the spatial distribution of highly specialised bacterial communities in previously unexplored depth horizons of subsurface sediments. We deployed an autonomous rover in a mission-relevant Martian drilling scenario with manual sample validation. Subsurface communities were delineated by depth related to sediment moisture. Geochemical analysis indicated soluble salts and minerology that influenced water bio-availability, particularly in deeper sediments. Colonization was also patchy and uncolonized sediment was associated with indicators of extreme osmotic challenge. The study identifies linkage between biocomplexity, moisture and geochemistry in Mars-like sediments at the limit of habitability and demonstrates feasibility of the rover-mounted drill for future Mars sample recovery.

microbiology↗