Stimulation of r- vs. K-selected microorganisms by elevated atmospheric CO2 depends on soil aggregate size

被引:87
作者
Dorodnikov, Maxim [2 ,3 ]
Blagodatskaya, Evgenia [1 ,2 ]
Blagodatsky, Sergey [1 ,2 ]
Fangmeier, Andreas [3 ]
Kuzyakov, Yakov [2 ]
机构
[1] RAS, Inst Physicochem & Biol Problems Soil Sci, Pushchino 142290, Russia
[2] Univ Bayreuth, Dept Agroecosyst Res, Bayreuth, Germany
[3] Univ Hohenheim, Inst Landscape & Plant Ecol 320, D-7000 Stuttgart, Germany
关键词
FACE; microaggregates; macroaggregates; SIGR; microbial growth strategies; MICROBIAL BIOMASS; CARBON TURNOVER; RHIZOSPHERE; COMMUNITIES; BACTERIAL; NITROGEN; PLANT; ECOSYSTEMS; DIVERSITY; DIFFUSION;
D O I
10.1111/j.1574-6941.2009.00697.x
中图分类号
Q93 [微生物学];
学科分类号
071005 ; 100705 ;
摘要
Increased root exudation under elevated atmospheric CO2 and the contrasting environments in soil macro- and microaggregates could affect microbial growth strategies. We investigated the effect of elevated CO2 on the contribution of fast- (r-strategists) and slow-growing (K-strategists) microorganisms in soil macro- and microaggregates. We fractionated the bulk soil from the ambient and elevated (for 5 years) CO2 treatments of FACE-Hohenheim (Stuttgart) into large macro- (> 2 mm), small macro- (0.25-2.00 mm), and microaggregates (< 0.25 mm) using 'optimal moist' sieving. Microbial biomass (C-mic), the maximum specific growth rate (mu), growing microbial biomass (GMB) and lag-period (t(lag)) were estimated by the kinetics of CO2 emission from bulk soil and aggregates amended with glucose and nutrients. Although C-org and C-mic were unaffected by elevated CO2, mu values were significantly higher under elevated than ambient CO2 for bulk soil, small macroaggregates, and microaggregates. Substrate-induced respiratory response increased with decreasing aggregate size under both CO2 treatments. Based on changes in mu, GMB and lag period, we conclude that elevated atmospheric CO2 stimulated the r-selected microorganisms, especially in soil microaggregates. Such an increase in r-selected microorganisms indicates acceleration of available C mineralization in soil, which may counterbalance the additional C input by roots in soils in a future elevated atmospheric CO2 environment.
引用
收藏
页码:43 / 52
页数:10
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