Transient O₂ pulses direct Fe crystallinity and Fe(III)-reducer gene expression within a soil microbiome.

ABSTRACT:

Background

Many environments contain redox transition zones, where transient oxygenation events can modulate anaerobic reactions that influence the cycling of iron (Fe) and carbon (C) on a global scale. In predominantly anoxic soils, this biogeochemical cycling depends on Fe mineral composition and the activity of mixed Fe(III)-reducer populations that may be altered by periodic pulses of molecular oxygen (O₂).

Methods

We repeatedly exposed anoxic (4% H₂:96% N₂) suspensions of soil from the Luquillo Critical Zone Observatory to 1.05 × 10², 1.05 × 10³, and 1.05 × 10⁴ mmol O₂ kg^-1 soil h^-1 during pulsed oxygenation treatments. Metatranscriptomic analysis and ⁵⁷Fe Mössb

SUBMITTER: Wilmoth JL 

PROVIDER: S-EPMC6199725 | biostudies-literature | 2018 Oct

REPOSITORIES: biostudies-literature