Journal article

Publication year: 2007

Pages: 769-779

Journal: Biogeosciences

Volume number: 4

Issue number: 5

ISSN: 1726-4170

eISSN: 1726-4189

Open access status: Gold

DOI Link: https://doi.org/10.5194/bg-4-769-2007

Publisher: Copernicus Publications

Abstract: 
The aim of this study was to identify the microbial communities that are actively involved in the assimilation of rhizosphere-C and are most sensitive in their activity to elevated atmospheric CO2 in a temperate semi-natural low-input grassland ecosystem. For this, we analyzed C-13 signatures in microbial biomarker phospholipid fatty acids (PLFA) from an in-situ (CO2)-C-13 pulse-labeling experiment in the Giessen Free Air Carbon dioxide Enrichment grasslands (GiFACE, Germany) exposed to ambient and elevated (i.e. 50% above ambient) CO2 concentrations. Short-term C-13 PLFA measurements at 3 h and 10 h after the pulse-labeling revealed very little to no C-13 enrichment after 3 h in biomarker PLFAs and a much greater incorporation of new plant-C into fungal compared to bacterial PLFAs after 10 h. After a period of 11 months following the pulse-labeling experiment, the C-13 enrichment of fungal PLFAs was still largely present but had decreased, while bacterial PLFAs were much more enriched in C-13 compared to a few hours after the pulse-labeling. These results imply that new rhizodeposit-C is rapidly processed by fungal communities and only much later by the bacterial communities, which we attributed to either a fungal-mediated translocation of rhizosphere-C from the fungal to bacterial biomass or a preferential bacterial use of dead root or fungal necromass materials as C source over the direct utilization of fresh root-exudate C in these N-limited grassland ecosystems. Elevated CO2 caused an increase in the proportional C-13 enrichment (relative to the universal biomarker 16:0) of the arbuscular mycorrhizal fungal biomarker PLFA 16:1 omega 5 and one gram-positive bacterial biomarker PLFA i16:0, but a decrease in the proportional C-13 enrichment of 18:1 omega 9c, a commonly used though questionable fungal biomarker PLFA. This suggests enhanced fungal rhizodeposit-C assimilation only by arbuscular mycorrhizal fungal species under elevated CO2.

Harvard Citation style: Denef, K., Bubenheim, H., Lenhart, K., Vermeulen, J., Van Cleemput, O., Boeckx, P., et al. (2007) Community shifts and carbon translocation within metabolically-active rhizosphere microorganisms in grasslands under elevated CO2, Biogeosciences, 4(5), pp. 769-779. https://doi.org/10.5194/bg-4-769-2007

APA Citation style: Denef, K., Bubenheim, H., Lenhart, K., Vermeulen, J., Van Cleemput, O., Boeckx, P., & Müller, C. (2007). Community shifts and carbon translocation within metabolically-active rhizosphere microorganisms in grasslands under elevated CO2. Biogeosciences. 4(5), 769-779. https://doi.org/10.5194/bg-4-769-2007