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Linking microbial co‐occurrences to soil ecological processes across a woodland‐grassland ecotone

机译:将微生物共生与林地-草地交错带中的土壤生态过程联系起来

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Ecotones between distinct ecosystems have been the focus of many studies as they offer valuable insights into key drivers of community structure and ecological processes that underpin function. While previous studies have examined a wide range of above‐ground parameters in ecotones, soil microbial communities have received little attention. Here we investigated spatial patterns, composition, and co‐occurrences of archaea, bacteria, and fungi, and their relationships with soil ecological processes across a woodland‐grassland ecotone. Geostatistical kriging and network analysis revealed that the community structure and spatial patterns of soil microbiota varied considerably between three habitat components across the ecotone. Woodland samples had significantly higher diversity of archaea while the grassland samples had significantly higher diversity of bacteria. Microbial co‐occurrences reflected differences in soil properties and ecological processes. While microbial networks were dominated by bacterial nodes, different ecological processes were linked to specific microbial guilds. For example, soil phosphorus and phosphatase activity formed the largest clusters in their respective networks, and two lignolytic enzymes formed joined clusters. Bacterial ammonia oxidizers were dominant over archaeal oxidizers and showed a significant association ( p ??0.001) with potential nitrification (PNR), with the PNR subnetwork being dominated by Betaproteobacteria . The top ten keystone taxa comprised six bacterial and four fungal OTUs, with Random Forest Analysis revealing soil carbon and nitrogen as the determinants of the abundance of keystone taxa. Our results highlight the importance of assessing interkingdom associations in soil microbial networks. Overall, this study shows how ecotones can be used as a model to delineate microbial structural patterns and ecological processes across adjoining land‐uses within a landscape.
机译:独特的生态系统之间的生态过渡一直是许多研究的重点,因为它们提供了宝贵的见解,深入了解了支撑功能的社区结构和生态过程的关键驱动因素。尽管先前的研究已经检查了过渡带中的各种地上参数,但土壤微生物群落却鲜有关注。在这里,我们调查了古林,草地和草原交错带中古细菌,细菌和真菌的空间格局,组成和共生关系,以及它们与土壤生态过程的关系。地统计学克里金法和网络分析表明,生态交错带中三个生境成分之间的土壤微生物群落结构和空间格局差异很大。林地样品具有较高的古细菌多样性,而草原样品具有较高的细菌多样性。微生物共生反映了土壤性质和生态过程的差异。虽然微生物网络以细菌节点为主,但不同的生态过程却与特定的微生物协会有关。例如,土壤磷和磷酸酶活性在它们各自的网络中形成最大的簇,而两种木质素分解酶形成连接的簇。细菌氨氧化剂比古细菌氧化剂占主导地位,并且与潜在的硝化作用(PNR)呈显着关联(p 0.001),PNR子网由Beta变形杆菌占主导。排名前十的梯形分类群包括六个细菌和四个真菌OTU,随机森林分析显示土壤碳和氮是梯形分类群丰富度的决定因素。我们的结果凸显了评估土壤微生物网络中相互联系的重要性。总体而言,这项研究表明,生态交错带如何可以用作描述景观中相邻土地利用的微生物结构模式和生态过程的模型。

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