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首页> 外文期刊>Microbial Ecology: An International Journal >Fungal Communities and Functional Guilds Shift Along an Elevational Gradient in the Southern Appalachian Mountains
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Fungal Communities and Functional Guilds Shift Along an Elevational Gradient in the Southern Appalachian Mountains

机译:真菌社区和功能公会沿着阿巴拉契亚山脉南部的高度梯度转移

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摘要

Nitrogen deposition alters forest ecosystems particularly in high elevation, montane habitats where nitrogen deposition is greatest and continues to increase. We collected soils across an elevational (788-1940 m) gradient, encompassing both abiotic (soil chemistry) and biotic (vegetation community) gradients, at eight locations in the southern Appalachian Mountains of southwestern North Carolina and eastern Tennessee. We measured soil chemistry (total N, C, extractable PO4, soil pH, cation exchange capacity [ECEC], percent base saturation [% BS]) and dissected soil fungal communities using ITS2 metabarcode Illumina MiSeq sequencing. Total soil N, C, PO4, % BS, and pH increased with elevation and plateaued at approximately 1400 m, whereas ECEC linearly increased and C/N decreased with elevation. Fungal communities differed among locations and were correlated with all chemical variables, except PO4, whereas OTU richness increased with total N. Several ecological guilds (i.e., ectomycorrhizae, saprotrophs, plant pathogens) differed in abundance among locations; specifically, saprotroph abundance, primarily attributable to genus Mortierella, was positively correlated with elevation. Ectomycorrhizae declined with total N and soil pH and increased with total C and PO4 where plant pathogens increased with total N and decreased with total C. Our results demonstrate significant turnover in taxonomic and functional fungal groups across elevational gradients which facilitate future predictions on forest ecosystem change in the southern Appalachians as nitrogen deposition rates increase and regional temperature and precipitation regimes shift.
机译:氮沉积改变了森林生态系统,特别是在高升高,氮沉积最大的山麦栖息地,并继续增加。我们在南部卡罗莱纳州和东田纳西州南部阿巴拉契亚山脉的八个地点收集了跨非生物学(土壤化学)和生物(植被群落)梯度的土壤,包括非生物(土壤化学)和生物(植被群落)梯度。我们测量了土壤化学(总N,C,可提取的PO4,土壤pH,阳离子交换能力[eCEC],百分比基础饱和度[%BS],使用ITS2 Metabarcode Illumina Miseq测序解剖土壤真菌社区。全土壤N,C,PO4,%BS和pH增加,升高增加,并在大约1400米处柔韧,而ECEC线性增加,C / N随着升高而降低。真菌社区不同的地方不同,除了PO4之外的所有化学变量都与所有化学变量相关联,而OTU Richness总共增加了几个生态公会(即ectomycorrhizae,植物病原体)在地点之间的丰富不同;具体而言,主要归因于Martierella的皂细胞丰度,与升高呈正相关。 Ececyycorrhizae总共下降和土壤pH值,总C和PO4增加,植物病原体总共增加,总计C,我们的结果表明了跨越森林生态系统变革的未来预测的分类学和功能性真菌群体的显着成交在南方阿巴拉契亚人作为氮气沉积率增加和区域温度和降水制度变化。

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