Serpentinization-associated travertines as spatio-temporal archives for lipid biomarkers key for the search for life on Mars.

Biogenicity Lipid biomarkers Mars Preservation Serpentinization

Journal

The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500

Informations de publication

Date de publication:
05 Dec 2023
Historique:
received: 29 09 2023
revised: 28 11 2023
accepted: 30 11 2023
pubmed: 8 12 2023
medline: 8 12 2023
entrez: 7 12 2023
Statut: aheadofprint

Résumé

Serpentinization is a well-known aqueous alteration process that may have played important roles in the origins and early evolution of life on Earth, and perhaps Mars, but there are still aspects related to biomarker distribution, partitioning, and preservation that merit further study. To assess the role that precipitation of carbonate phases in serpentinization settings may have on biomarker preservation, we search for life signs in one of the world's largest outcrops of subcontinental peridotites (Ronda, South Spain). We investigate the organic record of groundwater and associated carbonate deposits (travertines) in seven hyperalkaline springs, and reconstruct the biological activity and metabolic interactions of the serpentinization-hosted ecosystem. We identified lipid biomarkers and isotopic evidences of life, whose concentration and variety were much lower in groundwater than travertine deposits (ppb/ppt versus ppm level). Groundwater carried organics of abiotic (n-alkanes with values of CPI ∼ 1) and/or biotic origin, of fresher (e.g. acids or alcohols) or more diagenetized (mature hopanes and n-alkanes) nature. In contrast, associated travertines held a more prolific record of biomarkers incorporating (molecular and isotopic) fingerprints of surface (mostly phototrophs) and subsurface (chemolithotrophs, methanogens and/or methanotrophs) life. Serpentinization-associated travertines seem to act as biomolecule archives over time fed by autochthonous and allochthonous sources, hence amplifying the dim biological signal of groundwater. These results illustrate the relevance of serpentinization-associated surface mineral deposits in searching for traces of life on analogous environments on Mars. We highlight the diversity of lipids produced in serpentinizing land environments and emphasize the potential of these geostable biomolecules to preserve fingerprints of life.

Identifiants

pubmed: 38061658
pii: S0048-9697(23)07675-1
doi: 10.1016/j.scitotenv.2023.169045
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

169045

Informations de copyright

Copyright © 2023. Published by Elsevier B.V.

Déclaration de conflit d'intérêts

Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

Laura Sánchez-García (L)

Centro de Astrobiología (CAB, CSIC-INTA), 28850 - Torrejón de Ardoz, Madrid, Spain. Electronic address: lsanchez@cab.inta-csic.es.

Daniel Carrizo (D)

Centro de Astrobiología (CAB, CSIC-INTA), 28850 - Torrejón de Ardoz, Madrid, Spain.

Pablo Jiménez-Gavilán (P)

Department of Geology, Faculty of Science, University of Malaga, 29071 Málaga, Spain.

Lucía Ojeda (L)

Department of Geology, Faculty of Science, University of Malaga, 29071 Málaga, Spain.

Víctor Parro (V)

Centro de Astrobiología (CAB, CSIC-INTA), 28850 - Torrejón de Ardoz, Madrid, Spain.

Iñaki Vadillo (I)

Department of Geology, Faculty of Science, University of Malaga, 29071 Málaga, Spain.

Classifications MeSH