The samples were collected during a field trip to the Dallol volcano and the Danakil Depression in northern Ethiopia in January 2017, which was funded by the Europlanet 2020 Research Infrastructure (RI). The results are published in the journal Scientific Reports.
"This is an exotic, multi-extreme environment, with organisms that need to love high temperature, high salt content and very low pH in order to survive," said Dr. Gomez.
Precipitation by superheated water saturated with various salts, including silver chloride, zinc iron sulphide, manganese dioxide and normal rock-salt, creates Dallol's technicoloured landscape of yellows, reds, greens and blues. The team collected samples of the thin layers of salt deposits from the wall of a yellow chimney stack and a blue pool of water surrounding the outcrop.
The samples were transported in sterile, sealed vials to state-of-the-art facilities in Spain, where they were analysed using a range of techniques, including electron microscopy, chemical analysis and DNA sequencing. The team identified tiny, spherical structures within the salt samples that had a high carbon content, demonstrating an unambiguously biological origin.
The microorganisms are 50-500 nanometers in diameter - up to 20 times smaller than the average bacteria. In several cases, the microorganisms are surrounded by needle-shaped crystals, which suggests that the nanobacteria may play an active role in the salt deposits and the geochemical cycle at Dallol.
The Dallol volcano and geothermal area is one of the hottest places on Earth, with average annual temperatures of 36 to 38 degrees Celsius. It is located at the northern end of the Danakil Depression, which lies around 125m below sea level at the junction of three of the Earth's lithospheric plates (Arabian, Nubian and Somalian) that are moving apart.
Hydrothermal activity is fueled by water that has been heated and enriched in gases by a shallow magma reservoir beneath the volcano. Dallol is surrounded by the wide Assale salt plain. The interaction between evaporated deposits and volcanism creates a unique and complex physical and chemical environment.
The unusual geochemistry of Dallol has close parallels to hydrothermal environments found on Mars, including the Gusev Crater, where NASA's Spirit Mars Exploration Rover landed. Last month, the same international team published a review in the journal Astrobiology highlighting the importance of Dallol as a field analogue for Mars and for astrobiological studies. The paper is the culmination of a two-year process supported by Europlanet 2020 RI to characterise the Dallol site's geology, mineralogy and biology in preparation for further study by planetary researchers.
"Deep investigation of the characteristics of this amazing site will improve our understanding of the limits of life on Earth and inform our search for life on Mars and elsewhere in the universe," said Barbara Cavalazzi of the University of Bologna, lead author of the review.
* F. Gomez, B. Cavalazzi, N. Rodriguez, R. Amils, G. G. Ori, K. Olsson-Francis, C. Escudero, J. M. Martinez and H. Miruts, "Ultra-Small Microorganisms in the Polyextreme Conditions of the Dallol Volcano, Northern Afar, Ethiopia," Scientific Reports, 2019 May 27
* B. Cavalazzi, R. Barbieri, F. Gomez, B. Capaccioni, K. Olsson-Francis, M. Pondrelli, A.P. Rossi, K. Hickman-Lewis, A. Agangi, G. Gasparotto, M. Glamoclija, G.G. Ori, N. Rodriguez, and M. Hagos, "The Dallol Geothermal Area, Northern Afar (Ethiopia) - An Exceptional Planetary Field Analog on Earth," 2019 March 27, Astrobiology.
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