Production of carbon-containing pyrite spherules induced by hyperthermophilic Thermococcales: a biosignature?
GUYOT, François
Biominéralogie : histoire, mécanismes et applications [IMPMC] [IMPMC_BIOMIN]
Institut universitaire de France [IUF]
< Réduire
Biominéralogie : histoire, mécanismes et applications [IMPMC] [IMPMC_BIOMIN]
Institut universitaire de France [IUF]
Langue
EN
Article de revue
Ce document a été publié dans
Frontiers in Microbiology. 2023-05-25, vol. 14
Résumé en anglais
Thermococcales, a major order of hyperthermophilic archaea inhabiting iron- and sulfur-rich anaerobic parts of hydrothermal deep-sea vents, are known to induce the formation of iron phosphates, greigite (Fe 3 S 4 ) and ...Lire la suite >
Thermococcales, a major order of hyperthermophilic archaea inhabiting iron- and sulfur-rich anaerobic parts of hydrothermal deep-sea vents, are known to induce the formation of iron phosphates, greigite (Fe 3 S 4 ) and abundant quantities of pyrite (FeS 2 ), including pyrite spherules. In the present study, we report the characterization of the sulfide and phosphate minerals produced in the presence of Thermococcales using X-ray diffraction, synchrotron-based X ray absorption spectroscopy and scanning and transmission electron microscopies. Mixed valence Fe(II)-Fe(III) phosphates are interpreted as resulting from the activity of Thermococcales controlling phosphorus–iron–sulfur dynamics. The pyrite spherules (absent in abiotic control) consist of an assemblage of ultra-small nanocrystals of a few ten nanometers in size, showing coherently diffracting domain sizes of few nanometers. The production of these spherules occurs via a sulfur redox swing from S 0 to S –2 and then to S –1 , involving a comproportionation of (-II) and (0) oxidation states of sulfur, as supported by S-XANES data. Importantly, these pyrite spherules sequester biogenic organic compounds in small but detectable quantities, possibly making them good biosignatures to be searched for in extreme environments.< Réduire
Mots clés en anglais
archaea biosignatures hydrothermal vents pyrite greigite
archaea
biosignatures
hydrothermal vents
pyrite
greigite
Project ANR
Les HYPERthermophiles et leur mécanisme de BIOMINeralisation - ANR-20-CE02-0001