Open AccessMicrobial community changes at a terrestrial volcanic CO 2 vent induced by soil acidification and anaerobic microhabitats within the soil column
Author(s) -
Frerichs Janin,
Oppermann Birte I.,
Gwosdz Simone,
Möller Ingo,
Herrmann Martina,
Krüger Martin
Publication year - 2013
Publication title -
fems microbiology ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.377
H-Index - 155
eISSN - 1574-6941
pISSN - 0168-6496
DOI - 10.1111/1574-6941.12040
Subject(s) - thaumarchaeota , biology , archaea , soil water , microbial population biology , ecosystem , ecology , environmental chemistry , microbial ecology , geomicrobiology , terrestrial ecosystem , soil microbiology , environmental biotechnology , bacteria , chemistry , genetics
CO 2 capture and storage ( CCS ) in deep geological formations is one option currently evaluated to reduce greenhouse gas emissions. Consequently, the impact of a possible CO 2 leakage from a storage site into surface environments has to be evaluated. During such a hypothetical leakage event, the CO 2 migrates upwards along fractures entering surface soils, a scenario similar to naturally occurring CO 2 vents. Therefore, such a natural analogue site at the Laacher See was chosen for an ecosystem study on the effects of high CO 2 concentrations on soil chemistry and microbiology. The microbial activities revealed differences in their spatial distribution and temporal variability for CO 2 ‐rich and reference soils. Furthermore, the abundance of several functional and group‐specific gene markers revealed further differences, for example, a decrease in Geobacteraceae and an increase in sulphate‐reducing prokaryotes in the vent centre. Molecular–biological fingerprinting of the microbial communities with DGGE indicated a shift in the environmental conditions within the Laacher See soil column leading to anaerobic and potentially acidic microenvironments. Furthermore, the distribution and phylogenetic affiliation of the archaeal 16S rRNA genes, the presence of ammonia‐oxidizing Archaea and the biomarker analysis revealed a predominance of Thaumarchaeota as possible indicator organisms for elevated CO 2 concentrations in soils.