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The Dallol Geothermal Area, Northern Afar (Ethiopia)—An Exceptional Planetary Field Analog on Earth

The Dallol volcano and its associated hydrothermal field are located in a remote area of the northern Danakil Depression in Ethiopia, a region only recently appraised after decades of inaccessibility due to severe political instability and the absence of infrastructure. The region is notable for hos...

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Autores principales: Cavalazzi, B., Barbieri, R., Gómez, F., Capaccioni, B., Olsson-Francis, K., Pondrelli, M., Rossi, A.P., Hickman-Lewis, K., Agangi, A., Gasparotto, G., Glamoclija, M., Ori, G.G., Rodriguez, N., Hagos, M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Mary Ann Liebert, Inc., publishers 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6459281/
https://www.ncbi.nlm.nih.gov/pubmed/30653331
http://dx.doi.org/10.1089/ast.2018.1926
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author Cavalazzi, B.
Barbieri, R.
Gómez, F.
Capaccioni, B.
Olsson-Francis, K.
Pondrelli, M.
Rossi, A.P.
Hickman-Lewis, K.
Agangi, A.
Gasparotto, G.
Glamoclija, M.
Ori, G.G.
Rodriguez, N.
Hagos, M.
author_facet Cavalazzi, B.
Barbieri, R.
Gómez, F.
Capaccioni, B.
Olsson-Francis, K.
Pondrelli, M.
Rossi, A.P.
Hickman-Lewis, K.
Agangi, A.
Gasparotto, G.
Glamoclija, M.
Ori, G.G.
Rodriguez, N.
Hagos, M.
author_sort Cavalazzi, B.
collection PubMed
description The Dallol volcano and its associated hydrothermal field are located in a remote area of the northern Danakil Depression in Ethiopia, a region only recently appraised after decades of inaccessibility due to severe political instability and the absence of infrastructure. The region is notable for hosting environments at the very edge of natural physical-chemical extremities. It is surrounded by a wide, hyperarid salt plain and is one of the hottest (average annual temperature(Dallol): 36–38°C) and most acidic natural systems (pH(Dallol) ≈0) on Earth. Spectacular geomorphologies and mineral deposits produced by supersaturated hydrothermal waters and brines are the result of complex interactions between active and inactive hydrothermal alteration of the bedrock, sulfuric hot springs and pools, fumaroles and geysers, and recrystallization processes driven by hydrothermal waters, degassing, and rapid evaporation. The study of planetary field analog environments plays a crucial role in characterizing the physical and chemical boundaries within which life can exist on Earth and other planets. It is essential for the definition and assessment of the conditions of habitability on other planets, including the possibility for biosignature preservation and in situ testing of technologies for life detection. The Dallol area represents an excellent Mars analog environment given that the active volcanic environment, the associated diffuse hydrothermalism and hydrothermal alteration, and the vast acidic sulfate deposits are reminiscent of past hydrothermal activity on Mars. The work presented in this paper is an overview of the Dallol volcanic area and its hydrothermal field that integrates previous literature with observations and results obtained from field surveys and monitoring coupled with sample characterization. In so doing, we highlight its exceptional potential as a planetary field analog as well as a site for future astrobiological and exploration programs.
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spelling pubmed-64592812019-04-12 The Dallol Geothermal Area, Northern Afar (Ethiopia)—An Exceptional Planetary Field Analog on Earth Cavalazzi, B. Barbieri, R. Gómez, F. Capaccioni, B. Olsson-Francis, K. Pondrelli, M. Rossi, A.P. Hickman-Lewis, K. Agangi, A. Gasparotto, G. Glamoclija, M. Ori, G.G. Rodriguez, N. Hagos, M. Astrobiology Review Articles The Dallol volcano and its associated hydrothermal field are located in a remote area of the northern Danakil Depression in Ethiopia, a region only recently appraised after decades of inaccessibility due to severe political instability and the absence of infrastructure. The region is notable for hosting environments at the very edge of natural physical-chemical extremities. It is surrounded by a wide, hyperarid salt plain and is one of the hottest (average annual temperature(Dallol): 36–38°C) and most acidic natural systems (pH(Dallol) ≈0) on Earth. Spectacular geomorphologies and mineral deposits produced by supersaturated hydrothermal waters and brines are the result of complex interactions between active and inactive hydrothermal alteration of the bedrock, sulfuric hot springs and pools, fumaroles and geysers, and recrystallization processes driven by hydrothermal waters, degassing, and rapid evaporation. The study of planetary field analog environments plays a crucial role in characterizing the physical and chemical boundaries within which life can exist on Earth and other planets. It is essential for the definition and assessment of the conditions of habitability on other planets, including the possibility for biosignature preservation and in situ testing of technologies for life detection. The Dallol area represents an excellent Mars analog environment given that the active volcanic environment, the associated diffuse hydrothermalism and hydrothermal alteration, and the vast acidic sulfate deposits are reminiscent of past hydrothermal activity on Mars. The work presented in this paper is an overview of the Dallol volcanic area and its hydrothermal field that integrates previous literature with observations and results obtained from field surveys and monitoring coupled with sample characterization. In so doing, we highlight its exceptional potential as a planetary field analog as well as a site for future astrobiological and exploration programs. Mary Ann Liebert, Inc., publishers 2019-04-01 2019-03-27 /pmc/articles/PMC6459281/ /pubmed/30653331 http://dx.doi.org/10.1089/ast.2018.1926 Text en © B. Cavalazzi et al., 2018; Published by Mary Ann Liebert, Inc. This Open Access article is distributed under the terms of the Creative Commons Attribution Noncommercial License (http://creativecommons.org/licenses/by-nc/4.0/) which permits any noncommercial use, distribution, and reproduction in any medium, provided the original author(s) and the source are credited.
spellingShingle Review Articles
Cavalazzi, B.
Barbieri, R.
Gómez, F.
Capaccioni, B.
Olsson-Francis, K.
Pondrelli, M.
Rossi, A.P.
Hickman-Lewis, K.
Agangi, A.
Gasparotto, G.
Glamoclija, M.
Ori, G.G.
Rodriguez, N.
Hagos, M.
The Dallol Geothermal Area, Northern Afar (Ethiopia)—An Exceptional Planetary Field Analog on Earth
title The Dallol Geothermal Area, Northern Afar (Ethiopia)—An Exceptional Planetary Field Analog on Earth
title_full The Dallol Geothermal Area, Northern Afar (Ethiopia)—An Exceptional Planetary Field Analog on Earth
title_fullStr The Dallol Geothermal Area, Northern Afar (Ethiopia)—An Exceptional Planetary Field Analog on Earth
title_full_unstemmed The Dallol Geothermal Area, Northern Afar (Ethiopia)—An Exceptional Planetary Field Analog on Earth
title_short The Dallol Geothermal Area, Northern Afar (Ethiopia)—An Exceptional Planetary Field Analog on Earth
title_sort dallol geothermal area, northern afar (ethiopia)—an exceptional planetary field analog on earth
topic Review Articles
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6459281/
https://www.ncbi.nlm.nih.gov/pubmed/30653331
http://dx.doi.org/10.1089/ast.2018.1926
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