Soil microbial responses to experimental warming and clipping in a tallgrass prairie

被引:364
作者
Zhang, W
Parker, KM
Luo, Y
Wan, S
Wallace, LL
Hu, S
机构
[1] N Carolina State Univ, Dept Plant Pathol, Raleigh, NC 27695 USA
[2] Nanjing Agr Univ, Dept Agron, Nanjing 210095, Peoples R China
[3] Univ Oklahoma, Dept Bot & Microbiol, Norman, OK 73019 USA
关键词
bacteria; experimental warming; fungi; microbial activity; microbial biomass; microbial community; soil microbes; tallgrass prairie; temperature acclimatization;
D O I
10.1111/j.1365-2486.2005.00902.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Global surface temperature is predicted to increase by 1.4-5.8degreesC by the end of this century. However, the impacts of this projected warming on soil C balance and the C budget of terrestrial ecosystems are not clear. One major source of uncertainty stems from warming effects on soil microbes, which exert a dominant influence on the net C balance of terrestrial ecosystems by controlling organic matter decomposition and plant nutrient availability. We, therefore, conducted an experiment in a tallgrass prairie ecosystem at the Great Plain Apiaries (near Norman, OK) to study soil microbial responses to temperature elevation of about 2degreesC through artificial heating in clipped and unclipped field plots. While warming did not induce significant changes in net N mineralization, soil microbial biomass and respiration rate, it tended to reduce extractable inorganic N during the second and third warming years, likely through increasing plant uptake. In addition, microbial substrate utilization patterns and the profiles of microbial phospholipid fatty acids (PLFAs) showed that warming caused a shift in the soil microbial community structure in unclipped subplots, leading to the relative dominance of fungi as evidenced by the increased ratio of fungal to bacterial PLFAs. However, no warming effect on soil microbial community structure was found in clipped subplots where a similar scale of temperature increase occurred. Clipping also significantly reduced soil microbial biomass and respiration rate in both warmed and unwarmed plots. These results indicated that warming-led enhancement of plant growth rather than the temperature increase itself may primarily regulate soil microbial response. Our observations show that warming may increase the relative contribution of fungi to the soil microbial community, suggesting that shifts in the microbial community structure may constitute a major mechanism underlying warming acclimatization of soil respiration.
引用
收藏
页码:266 / 277
页数:12
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