Articles | Volume 23, issue 21
https://doi.org/10.5194/bg-23-7893-2026
https://doi.org/10.5194/bg-23-7893-2026
Research article
 | 
06 Nov 2026
Research article |  | 06 Nov 2026

Microscale C-O-S isotope signatures record microbial sulfate reduction in ancient deep subsurface pyrite–calcite–barite assemblages

Eric Runge, Vanessa Fichtner, Mikael Tillberg, Martin Whitehouse, and Henrik Drake

Viewed

Total article views: 797 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
562 190 45 797 51 40 36
  • HTML: 562
  • PDF: 190
  • XML: 45
  • Total: 797
  • Supplement: 51
  • BibTeX: 40
  • EndNote: 36
Views and downloads (calculated since 23 Apr 2026)
Cumulative views and downloads (calculated since 23 Apr 2026)

Viewed (geographical distribution)

Total article views: 797 (including HTML, PDF, and XML) Thereof 776 with geography defined and 21 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 06 Nov 2026
Download
Short summary
We investigated past microbial processes in the deep continental subsurface by stable C-O-S isotope analyses of fracture-hosted pyrite-calcite-barite assemblages. These minerals show signatures of two different pathways of microbial sulfate reduction, linked to local hydrogeochemical conditions. We further suggest that these local conditions are also crucial in controlling the preservation of microbial biosignatures in deep subsurface mineral assemblages.
Share
Altmetrics
Final-revised paper
Preprint