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Nitrate-Dependent Iron Oxidation: A Potential Mars Metabolism
This work considers the hypothetical viability of microbial nitrate-dependent Fe(2+) oxidation (NDFO) for supporting simple life in the context of the early Mars environment. This draws on knowledge built up over several decades of remote and in situ observation, as well as recent discoveries that h...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Frontiers Media S.A.
2018
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5869265/ https://www.ncbi.nlm.nih.gov/pubmed/29616015 http://dx.doi.org/10.3389/fmicb.2018.00513 |
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author | Price, Alex Pearson, Victoria K. Schwenzer, Susanne P. Miot, Jennyfer Olsson-Francis, Karen |
author_facet | Price, Alex Pearson, Victoria K. Schwenzer, Susanne P. Miot, Jennyfer Olsson-Francis, Karen |
author_sort | Price, Alex |
collection | PubMed |
description | This work considers the hypothetical viability of microbial nitrate-dependent Fe(2+) oxidation (NDFO) for supporting simple life in the context of the early Mars environment. This draws on knowledge built up over several decades of remote and in situ observation, as well as recent discoveries that have shaped current understanding of early Mars. Our current understanding is that certain early martian environments fulfill several of the key requirements for microbes with NDFO metabolism. First, abundant Fe(2+) has been identified on Mars and provides evidence of an accessible electron donor; evidence of anoxia suggests that abiotic Fe(2+) oxidation by molecular oxygen would not have interfered and competed with microbial iron metabolism in these environments. Second, nitrate, which can be used by some iron oxidizing microorganisms as an electron acceptor, has also been confirmed in modern aeolian and ancient sediment deposits on Mars. In addition to redox substrates, reservoirs of both organic and inorganic carbon are available for biosynthesis, and geochemical evidence suggests that lacustrine systems during the hydrologically active Noachian period (4.1–3.7 Ga) match the circumneutral pH requirements of nitrate-dependent iron-oxidizing microorganisms. As well as potentially acting as a primary producer in early martian lakes and fluvial systems, the light-independent nature of NDFO suggests that such microbes could have persisted in sub-surface aquifers long after the desiccation of the surface, provided that adequate carbon and nitrates sources were prevalent. Traces of NDFO microorganisms may be preserved in the rock record by biomineralization and cellular encrustation in zones of high Fe(2+) concentrations. These processes could produce morphological biosignatures, preserve distinctive Fe-isotope variation patterns, and enhance preservation of biological organic compounds. Such biosignatures could be detectable by future missions to Mars with appropriate instrumentation. |
format | Online Article Text |
id | pubmed-5869265 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2018 |
publisher | Frontiers Media S.A. |
record_format | MEDLINE/PubMed |
spelling | pubmed-58692652018-04-03 Nitrate-Dependent Iron Oxidation: A Potential Mars Metabolism Price, Alex Pearson, Victoria K. Schwenzer, Susanne P. Miot, Jennyfer Olsson-Francis, Karen Front Microbiol Microbiology This work considers the hypothetical viability of microbial nitrate-dependent Fe(2+) oxidation (NDFO) for supporting simple life in the context of the early Mars environment. This draws on knowledge built up over several decades of remote and in situ observation, as well as recent discoveries that have shaped current understanding of early Mars. Our current understanding is that certain early martian environments fulfill several of the key requirements for microbes with NDFO metabolism. First, abundant Fe(2+) has been identified on Mars and provides evidence of an accessible electron donor; evidence of anoxia suggests that abiotic Fe(2+) oxidation by molecular oxygen would not have interfered and competed with microbial iron metabolism in these environments. Second, nitrate, which can be used by some iron oxidizing microorganisms as an electron acceptor, has also been confirmed in modern aeolian and ancient sediment deposits on Mars. In addition to redox substrates, reservoirs of both organic and inorganic carbon are available for biosynthesis, and geochemical evidence suggests that lacustrine systems during the hydrologically active Noachian period (4.1–3.7 Ga) match the circumneutral pH requirements of nitrate-dependent iron-oxidizing microorganisms. As well as potentially acting as a primary producer in early martian lakes and fluvial systems, the light-independent nature of NDFO suggests that such microbes could have persisted in sub-surface aquifers long after the desiccation of the surface, provided that adequate carbon and nitrates sources were prevalent. Traces of NDFO microorganisms may be preserved in the rock record by biomineralization and cellular encrustation in zones of high Fe(2+) concentrations. These processes could produce morphological biosignatures, preserve distinctive Fe-isotope variation patterns, and enhance preservation of biological organic compounds. Such biosignatures could be detectable by future missions to Mars with appropriate instrumentation. Frontiers Media S.A. 2018-03-20 /pmc/articles/PMC5869265/ /pubmed/29616015 http://dx.doi.org/10.3389/fmicb.2018.00513 Text en Copyright © 2018 Price, Pearson, Schwenzer, Miot and Olsson-Francis. http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms. |
spellingShingle | Microbiology Price, Alex Pearson, Victoria K. Schwenzer, Susanne P. Miot, Jennyfer Olsson-Francis, Karen Nitrate-Dependent Iron Oxidation: A Potential Mars Metabolism |
title | Nitrate-Dependent Iron Oxidation: A Potential Mars Metabolism |
title_full | Nitrate-Dependent Iron Oxidation: A Potential Mars Metabolism |
title_fullStr | Nitrate-Dependent Iron Oxidation: A Potential Mars Metabolism |
title_full_unstemmed | Nitrate-Dependent Iron Oxidation: A Potential Mars Metabolism |
title_short | Nitrate-Dependent Iron Oxidation: A Potential Mars Metabolism |
title_sort | nitrate-dependent iron oxidation: a potential mars metabolism |
topic | Microbiology |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5869265/ https://www.ncbi.nlm.nih.gov/pubmed/29616015 http://dx.doi.org/10.3389/fmicb.2018.00513 |
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