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天然生长植物根际微生物种群在 V-Ti 磁铁矿尾矿自然衰减过程中的变化。

Changes of root microbial populations of natively grown plants during natural attenuation of V-Ti magnetite tailings.

机构信息

College of Resources, Sichuan Agricultural University, Chengdu, 611130, China; Geomicrobiology Group, School of Life Sciences, University of Dundee, Dundee, DD1 5EH, UK.

Sichuan Provincial Academy of Natural Resource and Sciences, Chengdu, 610015, China.

出版信息

Ecotoxicol Environ Saf. 2020 Sep 15;201:110816. doi: 10.1016/j.ecoenv.2020.110816. Epub 2020 Jun 7.

Abstract

Mine tailings contain dangerously high levels of toxic metals which pose a constant threat to local ecosystems. Few naturally grown native plants can colonize tailings site and the existence of their root-associated microbial populations is poorly understood. The objective of this study was to give further insights into the interactions between native plants and their microbiota during natural attenuation of abandoned V-Ti magnetite mine tailings. In the present work, we first examined the native plants' potential for phytoremediation using plant/soil analytical methods and then investigated the root microbial communities and their inferred functions using 16 S rRNA-based metagenomics. It was found that in V-Ti magnetite mine tailings the two dominant plants Bothriochloa ischaemum and Typha angustifolia were able to increase available nitrogen in the rhizosphere soil by 23.3% and 53.7% respectively. The translocation factors (TF) for both plants indicated that B. ischaemum was able to accumulate Pb (TF = 1.212), while T. angustifolia was an accumulator of Mn (TF = 2.502). The microbial community structure was more complex in the soil associated with T. angustifolia than with B. ischaemum. The presence of both plants significantly reduced the population of Acinetobacter. Specifically, B. ischaemum enriched Massilia, Opitutus and Hydrogenophaga species while T. angustifolia significantly increased rhizobia species. Multivariate analyses revealed that among all tested soil variables Fe and total organic carbon (TOC) could be the key factors in shaping the microbial structure. The putative functional analysis indicated that soil sample of B. ischaemum was abundant with nitrate/nitrite reduction-related functions while that of T. angustifolia was rich in nitrogen fixing functions. The results indicate that these native plants host a diverse range of soil microbes, whose community structure can be shaped by plant types and soil variables. It is also possible that these plants can be used to improve soil nitrogen content and serve as bioaccumulators for Pb or Mn for phytoremediation purposes.

摘要

矿山尾矿中含有高浓度的有毒金属,对当地生态系统构成持续威胁。很少有天然生长的本地植物能够在尾矿场定殖,而其根相关微生物种群的存在则知之甚少。本研究的目的是进一步了解废弃 V-Ti 磁铁矿尾矿自然衰减过程中本地植物与其微生物群之间的相互作用。在本工作中,我们首先使用植物/土壤分析方法研究了本地植物的植物修复潜力,然后使用 16S rRNA 宏基因组学研究了根微生物群落及其推断的功能。结果发现,在 V-Ti 磁铁矿尾矿中,两种主要植物扭黄茅和香蒲能够分别将根际土壤中的有效氮增加 23.3%和 53.7%。两种植物的转移因子(TF)表明,扭黄茅能够积累 Pb(TF=1.212),而香蒲是 Mn 的积累者(TF=2.502)。与扭黄茅相比,与香蒲相关的土壤微生物群落结构更为复杂。两种植物的存在显著降低了不动杆菌的种群。具体而言,扭黄茅富集了马塞利亚菌、卵形菌和噬氢菌,而香蒲则显著增加了根瘤菌的数量。多元分析表明,在所有测试的土壤变量中,Fe 和总有机碳(TOC)可能是塑造微生物结构的关键因素。推测功能分析表明,扭黄茅土壤样本富含硝酸盐/亚硝酸盐还原相关功能,而香蒲土壤样本富含固氮功能。结果表明,这些本地植物拥有丰富多样的土壤微生物,其群落结构可以通过植物类型和土壤变量来塑造。这些植物也有可能被用于提高土壤氮含量,并作为 Pb 或 Mn 的生物积累者用于植物修复。

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