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Sökning: id:"swepub:oai:DiVA.org:nrm-3395" > Paleo-rock-hosted l...

Paleo-rock-hosted life on Earth and the search on Mars: a review and strategy for exploration

Onstott, T.C. (författare)
Princeton Univ, Dept Geosci, Princeton, NJ 08544 USA
Ehlmann, Bethany (författare)
CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA;CALTECH, Jet Prop Lab, Pasadena, CA USA
Sapers, Haley (författare)
CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA;CALTECH, Jet Prop Lab, Pasadena, CA USA;Univ Southern Calif, Dept Earth Sci, Los Angeles, CA USA
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Coleman, Max (författare)
CALTECH, Jet Prop Lab, Pasadena, CA USA;NASA, Astrobiol Inst, Pasadena, CA USA
Ivarsson, Magnus, 1975- (författare)
Naturhistoriska riksmuseet,Enheten för paleobiologi,Univ Southern Denmark, Dept Biol, Odense, Denmark
Marlow, J.J. (författare)
Harvard Univ, Dept Organism & Evolutionary Biol, Cambridge, MA 02138 USA
Neubeck, Anna (författare)
Uppsala universitet,Paleobiologi
Niles, P (författare)
NASA, Astromat Res & Explorat Sci Div, Johnson Space Ctr, Houston, TX USA
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 (creator_code:org_t)
Mary Ann Liebert Inc, Publishers, 2019
2019
Engelska.
Ingår i: Astrobiology. - : Mary Ann Liebert Inc, Publishers. - 1531-1074 .- 1557-8070. ; 19:10, s. 1230-1262
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • Here we review published studies on the abundance and diversity of terrestrial rock-hosted life, the environments it inhabits, the evolution of its metabolisms, and its fossil biomarkers to provide guidance in the search for life on Mars. Key findings are (1) much terrestrial deep subsurface metabolic activity relies on abiotic energy-yielding fluxes and in situ abiotic and biotic recycling of metabolic waste products rather than on buried organic products of photosynthesis; (2) subsurface microbial cell concentrations are highest at interfaces with pronounced chemical redox gradients or permeability variations and do not correlate with bulk host rock organic carbon; (3) metabolic pathways for chemolithoautotrophic microorganisms evolved earlier in Earth's history than those of surface-dwelling phototrophic microorganisms; (4) the emergence of the former occurred at a time when Mars was habitable, whereas the emergence of the latter occurred at a time when the martian surface was not continually habitable; (5) the terrestrial rock record has biomarkers of subsurface life at least back hundreds of millions of years and likely to 3.45 Ga with several examples of excellent preservation in rock types that are quite different from those preserving the photosphere-supported biosphere. These findings suggest that rock-hosted life would have been more likely to emerge and be preserved in a martian context. Consequently, we outline a Mars exploration strategy that targets subsurface life and scales spatially, focusing initially on identifying rocks with evidence for groundwater flow and low-temperature mineralization, then identifying redox and permeability interfaces preserved within rock outcrops, and finally focusing on finding minerals associated with redox reactions and associated traces of carbon and diagnostic chemical and isotopic biosignatures. Using this strategy on Earth yields ancient rock-hosted life, preserved in the fossil record and confirmable via a suite of morphologic, organic, mineralogical, and isotopic fingerprints at micrometer scale. We expect an emphasis on rock-hosted life and this scale-dependent strategy to be crucial in the search for life on Mars.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Multidisciplinär geovetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geosciences, Multidisciplinary (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Annan geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Other Earth and Related Environmental Sciences (hsv//eng)

Nyckelord

subsurface life
microbial diversity
biosignitures
search for life
Mars
Diversity of life
Livets mångfald

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