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      A Low-Diversity Microbiota Inhabits Extreme Terrestrial Basaltic Terrains and Their Fumaroles: Implications for the Exploration of Mars

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          Abstract

          A major objective in the exploration of Mars is to test the hypothesis that the planet hosted life. Even in the absence of life, the mapping of habitable and uninhabitable environments is an essential task in developing a complete understanding of the geological and aqueous history of Mars and, as a consequence, understanding what factors caused Earth to take a different trajectory of biological potential. We carried out the aseptic collection of samples and comparison of the bacterial and archaeal communities associated with basaltic fumaroles and rocks of varying weathering states in Hawai‘i to test four hypotheses concerning the diversity of life in these environments. Using high-throughput sequencing, we found that all these materials are inhabited by a low-diversity biota. Multivariate analyses of bacterial community data showed a clear separation between sites that have active fumaroles and other sites that comprised relict fumaroles, unaltered, and syn-emplacement basalts. Contrary to our hypothesis that high water flow environments, such as fumaroles with active mineral leaching, would be sites of high biological diversity, alpha diversity was lower in active fumaroles compared to relict or nonfumarolic sites, potentially due to high-temperature constraints on microbial diversity in fumarolic sites. A comparison of these data with communities inhabiting unaltered and weathered basaltic rocks in Idaho suggests that bacterial taxon composition of basaltic materials varies between sites, although the archaeal communities were similar in Hawai‘i and Idaho. The taxa present in both sites suggest that most of them obtain organic carbon compounds from the atmosphere and from phototrophs and that some of them, including archaeal taxa, cycle fixed nitrogen. The low diversity shows that, on Earth, extreme basaltic terrains are environments on the edge of sustaining life with implications for the biological potential of similar environments on Mars and their exploration by robots and humans.

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          Controlling the False Discovery Rate: A Practical and Powerful Approach to Multiple Testing

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            Global mineralogical and aqueous mars history derived from OMEGA/Mars Express data.

            Global mineralogical mapping of Mars by the Observatoire pour la Mineralogie, l'Eau, les Glaces et l'Activité (OMEGA) instrument on the European Space Agency's Mars Express spacecraft provides new information on Mars' geological and climatic history. Phyllosilicates formed by aqueous alteration very early in the planet's history (the "phyllocian" era) are found in the oldest terrains; sulfates were formed in a second era (the "theiikian" era) in an acidic environment. Beginning about 3.5 billion years ago, the last era (the "siderikian") is dominated by the formation of anhydrous ferric oxides in a slow superficial weathering, without liquid water playing a major role across the planet.
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              A habitable fluvio-lacustrine environment at Yellowknife Bay, Gale crater, Mars.

              The Curiosity rover discovered fine-grained sedimentary rocks, which are inferred to represent an ancient lake and preserve evidence of an environment that would have been suited to support a martian biosphere founded on chemolithoautotrophy. This aqueous environment was characterized by neutral pH, low salinity, and variable redox states of both iron and sulfur species. Carbon, hydrogen, oxygen, sulfur, nitrogen, and phosphorus were measured directly as key biogenic elements; by inference, phosphorus is assumed to have been available. The environment probably had a minimum duration of hundreds to tens of thousands of years. These results highlight the biological viability of fluvial-lacustrine environments in the post-Noachian history of Mars.
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                Author and article information

                Journal
                Astrobiology
                Astrobiology
                ast
                Astrobiology
                Mary Ann Liebert, Inc., publishers (140 Huguenot Street, 3rd FloorNew Rochelle, NY 10801USA )
                1531-1074
                1557-8070
                01 March 2019
                06 March 2019
                06 March 2019
                : 19
                : 3
                : 284-299
                Affiliations
                [ 1 ]UK Centre for Astrobiology, School of Physics and Astronomy, University of Edinburgh, Edinburgh, UK.
                [ 2 ]Aquatic Biogeochemistry Research Unit, Ecosystems and Environment Research Programme, Faculty of Biological and Environmental Sciences, University of Helsinki, Helsinki, Finland.
                [ 3 ]Turku Centre for Biotechnology, University of Turku and Åbo Akademi University, Turku, Finland.
                [ 4 ]Department of Geosciences, Idaho State University, Pocatello, Idaho, USA.
                [ 5 ]School of Geography and Earth Sciences, McMaster University, Hamilton, Canada.
                [ 6 ]NASA Ames Research Center, Mountain View, California, USA.
                [ 7 ]Mars Space Flight Facility, Arizona State University, Tempe, Arizona, USA.
                [ 8 ]KBRwyle, NASA Johnson Space Center, Houston, Texas, USA.
                [ 9 ]Biomedical Research & Environmental Sciences Division (SK), NASA Johnson Space Center, Houston, Texas, USA.
                [ 10 ]Bay Area Environmental Research Institute (BAERI), Moffett Field, California, USA.
                Author notes
                [*]Address correspondence to: Charles S. Cockell, School of Physics and Astronomy, University of Edinburgh, King's Buildings, Edinburgh EH9 3JZ, UK c.s.cockell@ 123456ed.ac.uk
                Article
                10.1089/ast.2018.1870
                10.1089/ast.2018.1870
                6442273
                30840501
                b4523c8e-c88c-4f08-98e3-961f4e0cf05e
                © Charles S. Cockell et al., 2018; Published by Mary Ann Liebert, Inc.

                This Open Access article is distributed under the terms of the Creative Commons License ( http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited.

                History
                : 23 March 2018
                : 28 October 2018
                Page count
                Figures: 8, Tables: 2, References: 78, Pages: 16
                Categories
                Research Articles

                mars,life,basalts,bacteria,weathering,human exploration
                mars, life, basalts, bacteria, weathering, human exploration

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