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高浓度镉改变了火山区土壤古菌的活性、群落组装及共现网络。

High levels of cadmium altered soil archaeal activity, assembly, and co-occurrence network in volcanic areas.

作者信息

Zhang Zihua, Xu Daolong, Huang Tao, Zhang Qing, Li Yingyue, Zhou Jing, Zou Ruifan, Li Xiaoyu, Chen Jin

机构信息

School of Life Sciences, Anhui Agricultural University, Hefei 230036, China; National Engineering Laboratory of Crop Stress Resistance Breeding, Anhui Agricultural University, Hefei 230036, China; Key Laboratory of Crop Stress Resistance and High Quality Biology of Anhui Province, Anhui Agricultural University, Hefei 230036, China.

Inner Mongolia Academy of Science and Technology, Hohhot 010010, Inner Mongolia, China.

出版信息

Sci Total Environ. 2024 May 10;924:171529. doi: 10.1016/j.scitotenv.2024.171529. Epub 2024 Mar 6.

Abstract

Soil microbial communities are essential to biogeochemical cycles. However, the responses of microorganisms in volcanic soil with high heavy metal levels remain poorly understood. Here, two areas with high levels of cadmium (Cd) from the same volcano were investigated to determine their archaeal composition and assembly. In this study, the Cd concentrations (0.32-0.38 mg/ kg) in the volcanic soils exceeded the standard risk screening values (GB15618-2018) and correlated with archaeal communities strongly (P < 0.05). Moreover, the area with elevated levels of Cd (periphery) exhibited a greater diversity of archaeal species, albeit with reduced archaeal activity, compared to the area with lower levels of Cd (center). Besides, stochastic processes mainly governed the archaeal communities. Furthermore, the co-occurrence network was simplest in the periphery. The proportion of positive links between taxa increased positively with Cd concentration. Moreover, four keystone taxa (all from the family Nitrososphaeraceae) were identified from the archaeal networks. In its entirety, this study has expanded our comprehension of the variations of soil archaeal communities in volcanic areas with elevated cadmium levels and serves as a point of reference for the agricultural development of volcanic soils in China.

摘要

土壤微生物群落对生物地球化学循环至关重要。然而,对于重金属含量高的火山土壤中微生物的反应仍知之甚少。在此,对来自同一火山的两个镉(Cd)含量高的区域进行了调查,以确定它们的古菌组成和组装情况。在本研究中,火山土壤中的镉浓度(0.32 - 0.38毫克/千克)超过了标准风险筛选值(GB15618 - 2018),且与古菌群落密切相关(P < 0.05)。此外,与镉含量较低的区域(中心)相比,镉含量较高的区域(周边)古菌物种多样性更高,尽管古菌活性有所降低。此外,随机过程主要控制着古菌群落。此外,共现网络在周边最为简单。分类单元之间正连接的比例随镉浓度呈正增加。此外,从古菌网络中鉴定出了四个关键分类单元(均来自亚硝化球菌科)。总体而言,本研究扩展了我们对镉含量升高的火山地区土壤古菌群落变化的理解,并为中国火山土壤的农业开发提供了参考依据。

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