18th International Symposium on Microbial Ecology, Lausanne, İsviçre, 14 - 19 Ağustos 2022, ss.1, (Özet Bildiri)
The continental deep subsurface environment is one of the largest ecosystems in terms of microbial abundance1, where cells are exposed to large changes in
concentrations of dissolved inorganic carbon (DIC) as they are transported through aquifers with potential to affect the deep carbon cycle via
chemoautotrophy2-6. However, direct links between HCO3
- concentrations and carbon fixation by specific microbial primary producers is lacking. Here, we use
quantitative 13C DNA stable isotope probing (qSIP) to provide the first quantitative measurements of microbial carbon fixation at different H13CO3
-
concentrations (1 – 10 mM) by specific operational taxonomic units in alkaline hydrothermal fluids from a deep (750 m below surface) subsurface carbonate
aquifer in Biga Peninsula, Turkey.