Community shifts and carbon translocation within metabolically-active rhizosphere microorganisms in grasslands under elevated CO2

被引:143
作者
Denef, K.
Bubenheim, H.
Lenhart, K.
Vermeulen, J.
Van Cleemput, O.
Boeckx, P.
Mueller, C.
机构
[1] Univ Ghent, Lab Appl Phys Chem, B-9000 Ghent, Belgium
[2] Univ Giessen, D-35392 Giessen, Germany
[3] Univ Coll Dublin Belfield, Sch Biol & Environm Sci, Dublin 4, Ireland
关键词
D O I
10.5194/bg-4-769-2007
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
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.
引用
收藏
页码:769 / 779
页数:11
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