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

Journal Article · · Science Advances
 [1];  [2];  [3]; ORCiD logo [4];  [5];  [6];  [7];  [8];  [3];  [1];  [9];  [10];  [10];  [9];  [11]
  1. Universita di Bologna
  2. Universite Claude Bernard Lyon 1
  3. University Grenoble Alpes
  4. BATTELLE (PACIFIC NW LAB)
  5. University of Turin
  6. WITec GmbH
  7. Fondazione Bruno Kessler
  8. Istituto Nazionale di Ricerca Metrologica
  9. European Synchrotron Research Facility
  10. Universite de Lorraine
  11. University of Johannesburg

Subsurface habitats on Earth host an extensive extant biosphere and likely provided one of Earth’s earliest microbial habitats. Though the site of life’s emergence continues to be debated, evidence of early life provides insights into its early evolution1. Here we present our discovery of exceptionally well-preserved ~3.40-billion-years-old carbonaceous filamentous microfossils that inhabited a paleo-subseafloor hydrothermal vein system of the Barberton greenstone belt (BGB) in South Africa. The distribution of the microfossils in growth position on the walls of the initial conduits created by low- temperature hydrothermal fluid and their morphological and chemical characteristics as investigated over a range of scales, are consistent with an assemblage of methanogens that thrived in an ultramafic volcanic substrate.

Research Organization:
Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
Sponsoring Organization:
USDOE
DOE Contract Number:
AC05-76RL01830
OSTI ID:
1819941
Report Number(s):
PNNL-SA-158859
Journal Information:
Science Advances, Vol. 7, Issue 29; ISSN 2375-2548
Publisher:
AAAS
Country of Publication:
United States
Language:
English

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