Methanogenic archaea in terrestrial permafrost: a model for probable microbial life in Martian permafrost

Prokaryotic microfossils, found in early Archaean rocks, implies that the earliest life forms on Earth probably date from between 3.5 3.8 Ga ago, when living conditions on Mars were similar to those on early Earth. Therefore it is legitimate to assume that life on Mars emerged as well as on Earth. A...

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Main Authors: Wagner, Dirk, Morozova, Daria
Format: Conference Object
Language:unknown
Published: 2005
Subjects:
Ice
Online Access:https://epic.awi.de/id/eprint/12704/
https://hdl.handle.net/10013/epic.23117
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spelling ftawi:oai:epic.awi.de:12704 2023-09-05T13:20:07+02:00 Methanogenic archaea in terrestrial permafrost: a model for probable microbial life in Martian permafrost Wagner, Dirk Morozova, Daria 2005 https://epic.awi.de/id/eprint/12704/ https://hdl.handle.net/10013/epic.23117 unknown Wagner, D. and Morozova, D. (2005) Methanogenic archaea in terrestrial permafrost: a model for probable microbial life in Martian permafrost , ARCHAEA - The First Generation, Hohenheimer Castle Academy, Munich, June 2-4 . hdl:10013/epic.23117 EPIC3ARCHAEA - The First Generation, Hohenheimer Castle Academy, Munich, June 2-4, 2005 p. Conference notRev 2005 ftawi 2023-08-22T19:50:06Z Prokaryotic microfossils, found in early Archaean rocks, implies that the earliest life forms on Earth probably date from between 3.5 3.8 Ga ago, when living conditions on Mars were similar to those on early Earth. Therefore it is legitimate to assume that life on Mars emerged as well as on Earth. Accepting that first life on both planets was determined by complex microbial communities, the Martian life must have adapted to drastically changing environmental conditions or become again extinct. One possibility for survival of Martian primitive life might be subsurface lithoautotrophic ecosystems. Comparable environments exist in permafrost regions on Earth.The current ESA (European Space Agency) mission Mars Express determined existence of water as ground ice on Mars, which is fundamental requirement for life. Furthermore, Mars Express demonstrated for the first time the presence of CH4 in the Martian atmosphere, which due to the lifetime of CH4 could be only originated from active volcanism or biological sources. This finding may have important implications for the possibility that microbial life could exist on Mars.Methanogenic archaea colonising terrestrial permafrost, are highly specialized organisms from the view point of metabolism. The capability of these organisms to lithoautotrophic growth under strictly anaerobic conditions, tolerance to low temperatures and survival under extreme conditions of permafrost for several millions of years make methanogens one of the most suitable keystone organism for the investigation of possible Martian life.Within the scope of a project in the DFG (German Research Foundation) Priority Program Mars and the Terrestrial Planets we study the tolerances of methanogens under unfavourable life conditions of terrestrial or extraterrestrial permafrost (Mars simulation). The borders of growth influenced by desiccation, temperature extremes, radiation and high salt concentration were analyzed for the organisms in pure cultures obtained from permafrost soils as well as in their ... Conference Object Ice permafrost Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Prokaryotic microfossils, found in early Archaean rocks, implies that the earliest life forms on Earth probably date from between 3.5 3.8 Ga ago, when living conditions on Mars were similar to those on early Earth. Therefore it is legitimate to assume that life on Mars emerged as well as on Earth. Accepting that first life on both planets was determined by complex microbial communities, the Martian life must have adapted to drastically changing environmental conditions or become again extinct. One possibility for survival of Martian primitive life might be subsurface lithoautotrophic ecosystems. Comparable environments exist in permafrost regions on Earth.The current ESA (European Space Agency) mission Mars Express determined existence of water as ground ice on Mars, which is fundamental requirement for life. Furthermore, Mars Express demonstrated for the first time the presence of CH4 in the Martian atmosphere, which due to the lifetime of CH4 could be only originated from active volcanism or biological sources. This finding may have important implications for the possibility that microbial life could exist on Mars.Methanogenic archaea colonising terrestrial permafrost, are highly specialized organisms from the view point of metabolism. The capability of these organisms to lithoautotrophic growth under strictly anaerobic conditions, tolerance to low temperatures and survival under extreme conditions of permafrost for several millions of years make methanogens one of the most suitable keystone organism for the investigation of possible Martian life.Within the scope of a project in the DFG (German Research Foundation) Priority Program Mars and the Terrestrial Planets we study the tolerances of methanogens under unfavourable life conditions of terrestrial or extraterrestrial permafrost (Mars simulation). The borders of growth influenced by desiccation, temperature extremes, radiation and high salt concentration were analyzed for the organisms in pure cultures obtained from permafrost soils as well as in their ...
format Conference Object
author Wagner, Dirk
Morozova, Daria
spellingShingle Wagner, Dirk
Morozova, Daria
Methanogenic archaea in terrestrial permafrost: a model for probable microbial life in Martian permafrost
author_facet Wagner, Dirk
Morozova, Daria
author_sort Wagner, Dirk
title Methanogenic archaea in terrestrial permafrost: a model for probable microbial life in Martian permafrost
title_short Methanogenic archaea in terrestrial permafrost: a model for probable microbial life in Martian permafrost
title_full Methanogenic archaea in terrestrial permafrost: a model for probable microbial life in Martian permafrost
title_fullStr Methanogenic archaea in terrestrial permafrost: a model for probable microbial life in Martian permafrost
title_full_unstemmed Methanogenic archaea in terrestrial permafrost: a model for probable microbial life in Martian permafrost
title_sort methanogenic archaea in terrestrial permafrost: a model for probable microbial life in martian permafrost
publishDate 2005
url https://epic.awi.de/id/eprint/12704/
https://hdl.handle.net/10013/epic.23117
genre Ice
permafrost
genre_facet Ice
permafrost
op_source EPIC3ARCHAEA - The First Generation, Hohenheimer Castle Academy, Munich, June 2-4, 2005 p.
op_relation Wagner, D. and Morozova, D. (2005) Methanogenic archaea in terrestrial permafrost: a model for probable microbial life in Martian permafrost , ARCHAEA - The First Generation, Hohenheimer Castle Academy, Munich, June 2-4 . hdl:10013/epic.23117
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