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Divergent responses of soil fungal communities to soil erosion and deposition as evidenced in topsoil and subsoil

机译:土壤真菌社区对土壤侵蚀和沉积的发散反应,如表扬和遗留

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摘要

Despite the pivotal functional roles dominating the pace of nutrient cycles in terrestrial ecosystems, soil fungal communities at erosional and depositional sites have not been comparatively investigated when assessing the ecosystem stability of eroding landscapes. In this study, soil fungal communities in topsoil (0-5 cm) and subsoil (5-10 cm) on simulated eroding slopes of three slope gradients, i.e., 5°, 10°, and 20°, and in the corresponding depositional zones were examined from 2015 to 2017 in the region of the Chinese Loess Plateau. The results showed that, compared with that in the 5° reference slopes, soil fungal richness in the topsoil and subsoil of the 10° and 20° eroding slopes was 11.8-24.9% lower. However, the richness increased by 2.3-22.7% in the subsoil of the depositional zones, yet not in the topsoil. Soil fungal community compositions in both topsoil and subsoil differed between depositional zones and reference slopes but not between eroding slopes and reference slopes. The differentiation of fungal richness and community compositions between eroding slopes and depositional zones increased with slope gradients, regardless of the topsoil and the subsoil. Saprotrophic fungi levels were 22.5-48.0% lower and pathogenic fungi were 45.2-193.3% higher in the subsoil of the depositional zones with 10° and 20° slopes than in the subsoil of the 5° reference slopes. Soil fungal network on the eroding slope was more complex than that in the depositional zone, suggesting more extensive interactions of fungal taxa and higher community stability potential on eroding slopes. The decreasing soil moisture, organic matter, and other properties on the eroding slopes, in contrast with these properties increasing in the depositional zones, were responsible for the variations in fungal richness and community composition. The divergent responses of soil fungal communities to soil erosion and deposition emphasized the complexity and variability of fungal communities during the soil erosion-deposition processes.
机译:尽管在陆地生态系统中营养循环速度的关键功能作用,但在评估侵蚀景观的生态系统稳定性时,侵蚀性和沉积地点的土壤真菌社区尚未相对调查。在本研究中,在三个斜坡梯度的模拟侵蚀斜坡上的裸生莲(0-5cm)和底土(5-10cm)的土壤真菌群落,即5°,10°和20°,以及相应的沉积区从2015年到2017年在中国黄土高原区域审查。结果表明,与5°参考斜坡相比,甲醛和10°和20°侵蚀斜坡的土壤真菌丰富度降低了11.8-24.9%。然而,在沉积区的沉积区的沉积物中,富含性增加了2.3-22.7%,但未在表土中增加。沉积区域和沉积区和参考斜坡之间的土壤真菌群落组合物在沉积区和参考斜坡之间不同,但在侵蚀斜坡和参考斜坡之间。无论表土和底层如何,侵蚀斜坡和沉积区之间的真菌丰富和群落组成的分化增加了坡度梯度。抑制区的沉积区底层含量低于10°和20°的沉积区的沉积物,血管繁殖真菌水平降低45.2-193.3%,而不是5°参考斜面的底层。腐蚀斜坡上的土壤真菌网络比沉积区更复杂,表明真菌分类群和侵蚀斜坡上更高的群落稳定潜力的更广泛的相互作用。与沉积区中增加的这些性质相比,降低土壤湿度,有机物和其他性质,与沉积区中增加的性质相比,对真菌性质和群落组成的变化负责。土壤真菌社区对土壤侵蚀和沉积的发散反应强调了土壤侵蚀沉积过程中真菌社区的复杂性和变异性。

著录项

  • 来源
    《The Science of the Total Environment》 |2021年第2期|142616.1-142616.11|共11页
  • 作者单位

    State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau Institute of Soil and Water Conservation Chinese Academy of Sciences and Ministry of Water Resources Yangling Shaanxi 712100 PR China University of Chinese Academy of Sciences Beijing 100049 PR China;

    State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau Institute of Soil and Water Conservation Chinese Academy of Sciences and Ministry of Water Resources Yangling Shaanxi 712100 PR China University of Chinese Academy of Sciences Beijing 100049 PR China Institute of Soil and Water Conservation Northwest A&F University Yangling Shaanxi 712100 PR China;

    Institute of Soil and Water Conservation Northwest A&F University Yangling Shaanxi 712100 PR China;

    Institute of Soil and Water Conservation Northwest A&F University Yangling Shaanxi 712100 PR China;

    Institute of Soil and Water Conservation Northwest A&F University Yangling Shaanxi 712100 PR China;

    Institute of Soil and Water Conservation Northwest A&F University Yangling Shaanxi 712100 PR China;

    Institute of Soil and Water Conservation Northwest A&F University Yangling Shaanxi 712100 PR China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Eroding slope; Depositional zone; Chinese loess plateau;

    机译:削减斜坡;沉积区;中国黄土高原;

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