Cellular remains in a ~3.42-billion-year-old subseafloor hydrothermal environment

Author:

Cavalazzi Barbara12ORCID,Lemelle Laurence3ORCID,Simionovici Alexandre45ORCID,Cady Sherry L.6ORCID,Russell Michael J.7,Bailo Elena8ORCID,Canteri Roberto9ORCID,Enrico Emanuele10ORCID,Manceau Alain4ORCID,Maris Assimo11ORCID,Salomé Murielle12,Thomassot Emilie13ORCID,Bouden Nordine13ORCID,Tucoulou Rémi12,Hofmann Axel2ORCID

Affiliation:

1. Dipartimento di Scienze Biologiche, Geologiche e Ambientali, Università di Bologna, Bologna, Italy.

2. Department of Geology, University of Johannesburg, Johannesburg, South Africa.

3. LGL-TPE, ENS de Lyon, Université de Lyon, CNRS, Lyon, France.

4. ISTerre, University of Grenoble-Alpes, CNRS, Grenoble, France.

5. Institut Universitaire de France, Paris, France.

6. Pacific Northwest National Laboratory, EMSL, Richland, WA, USA.

7. Dipartimento di Chimica, Università degli Studi di Torino, Torino, Italy.

8. WITec GmbH, Ulm, Germany.

9. FBK—Fondazione Bruno Kessler, Trento, Italy.

10. INRiM, Istituto Nazionale di Ricerca Metrologica, Torino, Italy.

11. Dipartimento di Chimica “Giacomo Ciamician,” Università di Bologna, Bologna, Italy.

12. European Synchrotron Radiation Facility, Grenoble, France.

13. Université de Lorraine, CNRS, CRPG, Nancy, France.

Abstract

Oldest microfossils with methane-based metabolism in a subsurface environment expand the frontiers of early Earth habitability.

Funder

Horizon 2020 Framework Programme

FP7-PEOPLE-2013-CIG

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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