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本文引用的文献

1
Microbial links between sulfate reduction and metal retention in uranium- and heavy metal-contaminated soil.硫酸盐还原与铀及重金属污染土壤中金属固定之间的微生物联系。
Appl Environ Microbiol. 2010 May;76(10):3143-52. doi: 10.1128/AEM.00051-10. Epub 2010 Apr 2.
2
Impact of biostimulated redox processes on metal dynamics in an iron-rich creek soil of a former uranium mining area.生物刺激氧化还原过程对铀矿区富铁溪土壤中金属动态的影响。
Environ Sci Technol. 2010 Jan 1;44(1):177-83. doi: 10.1021/es902038e.
3
A Dehalococcoides-containing co-culture that dechlorinates tetrachloroethene to trans-1,2-dichloroethene.一种含有脱氯菌的共培养物，可将四氯乙烯脱氯为反式-1,2-二氯乙烯。
ISME J. 2010 Jan;4(1):88-97. doi: 10.1038/ismej.2009.90. Epub 2009 Aug 6.
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Involvement of siderophores in the reduction of metal-induced inhibition of auxin synthesis in Streptomyces spp.铁载体参与减少金属对链霉菌属中生长素合成的抑制作用
Chemosphere. 2008 Dec;74(1):19-25. doi: 10.1016/j.chemosphere.2008.09.079. Epub 2008 Nov 4.
5
Transcriptome of Geobacter uraniireducens growing in uranium-contaminated subsurface sediments.在受铀污染的地下沉积物中生长的嗜铀地杆菌的转录组。
ISME J. 2009 Feb;3(2):216-30. doi: 10.1038/ismej.2008.89. Epub 2008 Oct 9.
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Depth-resolved quantification of anaerobic toluene degraders and aquifer microbial community patterns in distinct redox zones of a tar oil contaminant plume.对焦油污染羽不同氧化还原带中厌氧甲苯降解菌和含水层微生物群落模式进行深度解析定量分析。
Appl Environ Microbiol. 2008 Feb;74(3):792-801. doi: 10.1128/AEM.01951-07. Epub 2007 Dec 14.
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Phylogenetic and physiological diversity of dissimilatory ferric iron reducers in sediments of the polluted Scheldt estuary, Northwest Europe.西北欧受污染的斯凯尔特河河口沉积物中异化性铁还原菌的系统发育和生理多样性
Environ Microbiol. 2007 Aug;9(8):1956-68. doi: 10.1111/j.1462-2920.2007.01312.x.
8
Desulfosporosinus lacus sp. nov., a sulfate-reducing bacterium isolated from pristine freshwater lake sediments.新种湖泊脱硫芽孢杆菌，一种从原始淡水湖沉积物中分离出的硫酸盐还原菌。
Int J Syst Evol Microbiol. 2006 Dec;56(Pt 12):2729-2736. doi: 10.1099/ijs.0.63610-0.
9
Anaerobic microbial dissolution of transition and heavy metal oxides.厌氧微生物对过渡金属和重金属氧化物的溶解作用。
Appl Environ Microbiol. 1988 Apr;54(4):1009-14. doi: 10.1128/aem.54.4.1009-1014.1988.
10
Organic matter mineralization with reduction of ferric iron in anaerobic sediments.有机物质在厌氧沉积物中伴随着铁离子的还原而矿化。
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受污染溪岸土壤中 Fe(III)还原微生物群落对重金属的耐受性。

Heavy metal tolerance of Fe(III)-reducing microbial communities in contaminated creek bank soils.

机构信息

Institute of Ecology, Friedrich Schiller University Jena, Dornburger-Straße 159, D-07743 Jena, Germany.

出版信息

Appl Environ Microbiol. 2011 May;77(9):3132-6. doi: 10.1128/AEM.02085-10. Epub 2011 Mar 4.

DOI:10.1128/AEM.02085-10
PMID:21378042
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3126387/
Abstract

Fe(III)-reducing soil enrichment cultures can tolerate 100 μM Cu and Cd, 150 μM Co, 600 μM Ni, and 2,500 μM Zn. Metal-tolerant cultures were dominated by Geobacter-related Deltaproteobacteria and Gram-positive Firmicutes spp. (Clostridia and Sedimentibacter). A Cd- and Cu-tolerant Fe(III)-reducing coculture of Desulfosporosinus and Desulfitobacterium indicated the importance of the Firmicutes for Fe(III) reduction in the presence of metals.

摘要

（III）铁还原土壤增菌培养物可耐受 100μM 的铜和镉、150μM 的钴、600μM 的镍和 2500μM 的锌。金属耐受培养物主要由与 Geobacter 相关的 Delta 变形菌门和革兰氏阳性的 Firmicutes 属（梭菌属和 Sedimentibacter）组成。脱硫螺旋菌和脱硫杆菌的耐镉和耐铜的（III）铁还原共培养物表明，在存在金属的情况下，Firmicutes 对铁（III）还原非常重要。