Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831-6038, USA.
Appl Environ Microbiol. 2010 Feb;76(4):999-1007. doi: 10.1128/AEM.02874-09. Epub 2009 Dec 18.
Researchers agree that climate change factors such as rising atmospheric [CO2] and warming will likely interact to modify ecosystem properties and processes. However, the response of the microbial communities that regulate ecosystem processes is less predictable. We measured the direct and interactive effects of climatic change on soil fungal and bacterial communities (abundance and composition) in a multifactor climate change experiment that exposed a constructed old-field ecosystem to different atmospheric CO2 concentration (ambient, +300 ppm), temperature (ambient, +3 degrees C), and precipitation (wet and dry) might interact to alter soil bacterial and fungal abundance and community structure in an old-field ecosystem. We found that (i) fungal abundance increased in warmed treatments; (ii) bacterial abundance increased in warmed plots with elevated atmospheric [CO2] but decreased in warmed plots under ambient atmospheric [CO2]; (iii) the phylogenetic distribution of bacterial and fungal clones and their relative abundance varied among treatments, as indicated by changes in 16S rRNA and 28S rRNA genes; (iv) changes in precipitation altered the relative abundance of Proteobacteria and Acidobacteria, where Acidobacteria decreased with a concomitant increase in the Proteobacteria in wet relative to dry treatments; and (v) changes in precipitation altered fungal community composition, primarily through lineage specific changes within a recently discovered group known as soil clone group I. Taken together, our results indicate that climate change drivers and their interactions may cause changes in bacterial and fungal overall abundance; however, changes in precipitation tended to have a much greater effect on the community composition. These results illustrate the potential for complex community changes in terrestrial ecosystems under climate change scenarios that alter multiple factors simultaneously.
研究人员一致认为,气候变化因素(如大气中[CO2]的上升和变暖)可能会相互作用,从而改变生态系统的特性和过程。然而,调节生态系统过程的微生物群落的反应则不太容易预测。我们在一个多因素气候变化实验中测量了气候变化对土壤真菌和细菌群落(丰度和组成)的直接和交互影响,该实验使构建的旧农田生态系统暴露于不同的大气 CO2 浓度(环境、+300ppm)、温度(环境、+3°C)和降水(湿润和干燥)下,这些因素可能会相互作用,改变旧农田生态系统中的土壤细菌和真菌丰度和群落结构。我们发现:(i)在变暖处理中真菌丰度增加;(ii)在大气[CO2]升高的变暖斑块中细菌丰度增加,但在环境大气[CO2]下的变暖斑块中减少;(iii)细菌和真菌克隆的系统发育分布及其相对丰度因处理而异,这表明 16S rRNA 和 28S rRNA 基因发生了变化;(iv)降水的变化改变了变形菌门和酸杆菌门的相对丰度,其中在湿润处理中与干燥处理相比,酸杆菌门减少,而变形菌门增加;(v)降水的变化改变了真菌群落的组成,主要是通过最近发现的一个被称为土壤克隆组 I 的群体中的谱系特异性变化。总的来说,我们的结果表明,气候变化驱动因素及其相互作用可能导致细菌和真菌总丰度的变化;然而,降水的变化往往对群落组成有更大的影响。这些结果说明了在同时改变多个因素的气候变化情景下,陆地生态系统中复杂群落变化的潜力。