Cargando…

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...

Descripción completa

Detalles Bibliográficos
Autores principales: Price, Alex, Pearson, Victoria K., Schwenzer, Susanne P., Miot, Jennyfer, Olsson-Francis, Karen
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2018
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
_version_ 1783309254271172608
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
work_keys_str_mv AT pricealex nitratedependentironoxidationapotentialmarsmetabolism
AT pearsonvictoriak nitratedependentironoxidationapotentialmarsmetabolism
AT schwenzersusannep nitratedependentironoxidationapotentialmarsmetabolism
AT miotjennyfer nitratedependentironoxidationapotentialmarsmetabolism
AT olssonfranciskaren nitratedependentironoxidationapotentialmarsmetabolism