中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Phylogenetic diversity of dissimilatory ferric iron reducers in paddy soil of hunan, south china

文献类型:期刊论文

作者Wang, Xin-Jun1,2; Yang, Jing1; Chen, Xue-Ping1; Sun, Guo-Xin1; Zhu, Yong-Guan1,3
刊名Journal of soils and sediments
出版日期2009-12-01
卷号9期号:6页码:568-577
关键词Arsenic Dissimilatory iron-reducing bacteria Enrichment cultures Paddy soil Terminal restriction fragment length polymorphism (t-rflp)
ISSN号1439-0108
DOI10.1007/s11368-009-0113-x
通讯作者Zhu, yong-guan(ygzhu@rcees.ac.cn)
英文摘要Dissimilatory iron-reducing bacteria have been described by both culture-dependent and -independent methods in various environments, including freshwater, marine sediments, natural wetlands, and contaminated aquifers. however, little is known about iron-reducing microbial communities in paddy soils. the goal of this study was to characterize iron-reducing microbial communities in paddy soil. moreover, the effect of dissolved and solid-phase iron (iii) species on the iron-reducing microbial communities was also investigated by enrichment cultures. ferric citrate and ferrihydrite were used respectively to set up enrichment cultures of dissimilatory iron-reducing microorganisms using 1% inoculum of soil samples, and the iron reduction was measured. moreover, bacterial dna was extracted and 16s rrna genes were pcr-amplified, and subsequently analyzed by the clone library and terminal restriction fragment length polymorphism (t-rflp). phylogenetic analysis of 16s rrna gene sequences extracted from the enrichment cultures revealed that bradyrhizobium, bacteroides, clostridium and ralstonia species were the dominant bacteria in the ferric citrate enrichment. however, members of the genera clostridium, bacteroides, and geobacter were the dominant microorganisms in the ferrihydrite enrichment. analysis of enrichment cultures by t-rflp strongly supported the cloning and sequencing results. the present study demonstrated that dissimilatory iron-reducing consortia in as-contaminated paddy soil are phylogenetically diverse. moreover, iron (iii) sources as a key factor have a strong effect on the iron (iii)-reducing microbial community structure and relative abundance in the enrichments. in addition, geobacter species are selectively enriched by ferrihydrite enrichment cultures.
WOS关键词RICE-FIELD SOIL ; ANAEROBIC AMMONIUM OXIDATION ; SP-NOV. ; PLANT RESIDUE ; FE(III)-REDUCING BACTERIA ; RALSTONIA-METALLIDURANS ; REDUCING BACTERIA ; GEN. NOV. ; REDUCTION ; SEDIMENTS
WOS研究方向Geology ; Agriculture
WOS类目Geosciences, Multidisciplinary ; Soil Science
语种英语
WOS记录号WOS:000271643900007
出版者SPRINGER HEIDELBERG
URI标识http://www.irgrid.ac.cn/handle/1471x/2404900
专题中国科学院大学
通讯作者Zhu, Yong-Guan
作者单位1.Chinese Acad Sci, Sate Key Lab Urban & Reg Ecol, Ecoenvironm Sci Res Ctr, Beijing 10085, Peoples R China
2.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Key Lab Urban Environm & Hlth, Inst Urban Environm, Xiamen 361021, Peoples R China
推荐引用方式
GB/T 7714
Wang, Xin-Jun,Yang, Jing,Chen, Xue-Ping,et al. Phylogenetic diversity of dissimilatory ferric iron reducers in paddy soil of hunan, south china[J]. Journal of soils and sediments,2009,9(6):568-577.
APA Wang, Xin-Jun,Yang, Jing,Chen, Xue-Ping,Sun, Guo-Xin,&Zhu, Yong-Guan.(2009).Phylogenetic diversity of dissimilatory ferric iron reducers in paddy soil of hunan, south china.Journal of soils and sediments,9(6),568-577.
MLA Wang, Xin-Jun,et al."Phylogenetic diversity of dissimilatory ferric iron reducers in paddy soil of hunan, south china".Journal of soils and sediments 9.6(2009):568-577.

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