The traditional view of the dependency of subsurface environments on surface-derived allochthonous carbon inputs is challenged by increasing evidence for the role of lithoautotrophy in aquifer carbon flow. We linked information on autotrophy (Calvin-Benson-Bassham cycle) with that from total microbial community analysis in groundwater at two superimposed-upper and lower-limestone groundwater reservoirs (aquifers). Quantitative PCR revealed that up to 17% of the microbial population had the genetic potential to fix CO 2 via the Calvin cycle, with abundances of cbbM and cbbL genes, encoding RubisCO (ribulose-1,5-bisphosphate carboxylase/oxygenase) forms I and II, ranging from 1.14 ؋ 10 3 to 6 ؋ 10 6 genes liter ؊1 over a 2-year period. The structure of the active microbial communities based on 16S rRNA transcripts differed between the two aquifers, with a larger fraction of heterotrophic, facultative anaerobic, soil-related groups in the oxygen-deficient upper aquifer. Most identified CO 2 -assimilating phylogenetic groups appeared to be involved in the oxidation of sulfur or nitrogen compounds and harbored both RubisCO forms I and II, allowing efficient CO 2 fixation in environments with strong oxygen and CO 2 fluctuations. The genera Sulfuricella and Nitrosomonas were represented by read fractions of up to 78 and 33%, respectively, within the cbbM and cbbL transcript pool and accounted for 5.6 and 3.8% of 16S rRNA sequence reads, respectively, in the lower aquifer. Our results indicate that a large fraction of bacteria in pristine limestone aquifers has the genetic potential for autotrophic CO 2 fixation, with energy most likely provided by the oxidation of reduced sulfur and nitrogen compounds.
Due to the lack of light-driven primary production, groundwater ecosystems were originally believed to be controlled by surface-derived allochthonous organic matter input (1-3) and to be dominated by heterotrophic prokaryotes adapted to nutrient limitation. However, there is increasing evidence of the important role of lithoautotrophy for carbon flow in aquifers (4-7). A large proportion of drinking water originates from groundwater resources (8), with karstic aquifers providing ϳ25% of the drinking water sources on a global scale (9). Despite the crucial role of microbial activity in shaping groundwater geochemistry (10-12), the links between microbial diversity and function in groundwater ecosystems, especially with regard to chemolithoautotrophy, are still poorly understood (7). Recent studies suggest that microbial CO 2 assimilation in aquifers could be fueled by energy conserved by nitrification, oxidation of ferrous iron and reduced sulfur compounds (6, 7), or oxidation of H 2 or methane (13, 14). Oxidation of electron donors present as solid minerals such as pyrite can even yield highly reactive dissolved ions that might affect other minerals and dissolved ions in the aquifer, leading to changes to the makeup of rocks and groundwater.Today, there are six known autotrophic CO 2 fixation pathways (reviewed in refere...