Chemoautotrophic carbon fixation in thermokarst lakes on the Tibetan Plateau.
Ontology highlight
ABSTRACT: Dissolved organic carbon (DOC) derived from thermokarst lakes is usually considered to be prone to microbial degradation and releases substantial carbon dioxide to the atmosphere, potentially enhancing the positive permafrost carbon (C)-climate feedback. In contrast to this long-term standing view, here we show that dark C fixation exceeds DOC degradation in ~1/3 of the investigated thermokarst lakes on the Tibetan Plateau, based on the combination of large-scale water and sediment sampling across seasons and years, biodegradable DOC experiments and 14C-labeling bicarbonate (NaH14CO3) assimilation incubation experiment. By employing qPCR, amplicon sequencing and metagenomic analyses, we find that microbial C fixation is mainly driven by nitrifying microorga
SUBMITTER: Liu F
PROVIDER: S-EPMC12824148 | biostudies-literature | 2025 Dec
REPOSITORIES: biostudies-literature
ACCESS DATA