Abstract
The elevational pattern of soil microbial diversity along mountain slopes has received considerable interest over the last decade. An increasing amount of taxonomic data on soil microbial community composition along elevation gradients have been collected, however the trophic patterns and environmental drivers of elevational changes remain largely unclear. Here, we examined the distribution patterns of major soil bacterial and fungal taxa along the northern slope of Changbai Mountain, Northeast China, at five typical vegetation types located between 740 and 2,691 m above sea level. Elevational patterns of the relative abundance of specific microbial taxa could be partially explained by the oligotrophic-copiotrophic theory. Specifically, two dark-coniferous forests, located at mid-elevation sites, were considered to be oligotrophic habitats, with relatively higher soil C/N ratio and -N concentrations. As expected, oligotrophic microbial taxa, belonging to the bacterial phyla Acidobacteria and Gemmatimonadetes, and fungal phylum Basidiomycota, were predominant in the two dark-coniferous forests, exhibiting a mid-elevation maximum pattern. In contrast, the broad leaf-Korean pine mixed forest located at the foot of the mountain, Betula ermanii-dominated forest located below the tree line, and alpine tundra at the highest elevation were considered more copiotrophic habitats, characterized by higher substrate-induced-respiration rates and -N concentrations. Microbial taxa considered to be so called copiotrophic members, such as bacterial phyla Proteobacteria and Actinobacteria, and fungal phylum Ascomycota, were relatively abundant in these locations, resulting in a mid-elevation minimum pattern. At finer taxonomic levels, the two most abundant proteobacterial classes, alpha- and beta-Proteobacteria, along with Acidobacteria Gp1, 2, 3, 15, and the Basidiomycotal class of Tremellomycetes were classified with the copiotrophic group. Gamma- and delta-Proteobacteria, Acidobacteria Gp4, 6, 7, 16, and Basidiomycotal class of Agaricomycetes were classified as oligotrophic taxa. This work uses the oligotrophic-copiotrophic theory to explain the elevational distribution pattern of the relative abundance of specific microbial taxa, confirming some of the existing trophic classifications of microbial taxa and expanding on the theory to include a broader range of taxonomic levels.
Highlights
The oligotrophic-copiotrophic theory has been proposed as an ecological classification scheme for soil bacteria, predicting that copiotrophic taxa are more associated with greater labile carbon (C) pools and flourish in soils with higher net carbon mineralization rate, whereas the oligotrophic taxa dominate soils with lower organic carbon availability (Fierer et al, 2007)
All soil physical and chemical properties measured in this study showed significant variations along the elevational gradient, except TC and TS (Table 1)
The broad leaf-Korean pine mixed forest (BL-KP) forest located at the mountain foot and Alpine tundra (AT) located at the summit contained more soil NO−3 -N than the other vegetation types
Summary
The oligotrophic-copiotrophic theory has been proposed as an ecological classification scheme for soil bacteria, predicting that copiotrophic taxa are more associated with greater labile carbon (C) pools and flourish in soils with higher net carbon mineralization rate, whereas the oligotrophic taxa dominate soils with lower organic carbon availability (Fierer et al, 2007). Ectomycorrhizal (ECM) fungi usually grow under oligotrophic conditions, such as the deeper soil horizons (Lindahl et al, 2007) They typically have a slow growth rate (Hibbett et al, 2000), and have a limited capacity to affect the decomposition of organic materials (Kohler et al, 2015). Based on these previous findings, we proposed that ECM fungal taxa may be characterized as oligotrophic, while saprotrophic fungi may exhibit copiotrophic tendencies
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