铁还原细菌Shewanella oneidensis MR-4诱导水合氧化铁形成蓝铁矿的过程
文献类型:期刊论文
作者 | 王芙仙; 郑世玲; 邱浩; 曹长乾; 唐旭; 郝立凯; 刘芳华![]() |
刊名 | 微生物学报
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出版日期 | 2018-03-16 |
卷号 | 58期号:04页码:573-583 |
关键词 | 铁还原细菌 生物诱导矿化 磁铁矿 蓝铁矿 电子显微学 激光拉曼 X射线衍射 |
ISSN号 | 0001-6209 |
DOI | 10.13343/j.cnki.wsxb.20180029 |
其他题名 | Ferrihydrite reduction and vivianite biomineralization mediated by iron reducing bacterium Shewanella oneidensis MR-4 |
产权排序 | (1)中国科学院地质与地球物理研究所地球与行星物理重点实验室中国科学院地球科学研究院 ; (2)青岛海洋科学与技术国家实验室海洋地质过程与环境功能实验室 ; (3)中国科学院大学 ; (4)中国科学院烟台海岸带研究所海岸带生物学与生物资源保护重点实验室 ; (5)中国科学院地球化学研究所,环境地球化学国家重点实验室 |
英文摘要 | [Objective] To explore the mineralogical,chemical and microscopic properties of extracellular vivianite formation induced by iron-reducing bacteria Shewanella oneidensis MR-4.[Methods] MR-4 cells grown with 30 mmol/L of lactate and 10 mmol/L of amorphous ferrihydrite,which were used as electron donor and electron acceptor,respectively.The medium was buffered with 30 mmol/L [HCO_3~–] and 5 mmol/L [PO_4~(3–)],and the culture was incubated at 30 oC.The headspace of serum bottle flushed with N_2/CO_2 (V/V,80/20).The pH,biomass and [Fe(II)] of the culture were measured by sampling at different time points.Meanwhile,the combination of X-ray diffraction,scanning electron microscope,laser Raman and transmission electron microscope approaches were applied to characterize the mineralogical,chemical and morphological properties of products produced within the culture.[Results] MR-4 could couple the reduction of Fe(III) with the oxidation of lactate for their cell growth and mineral transformation of Ferrihydrite.Specifically,ferrihydrite was initially transformed to nanometer-sized magnetite particles and majorly to micrometer-sized vivianite with bladed and fibrous morphologies finally.[Conclusion] The biomineralization process and products by MR-4 were strongly affected by environmental conditions such as the types and concentration of anions.In this case with relatively high [PO_4~(3–)] within the culture,ferrihydrite was initially converted to nanometer-sized magnetite,and was transformed into vivianite dominantly at the end of the culture.The result of this paper provides a new insight for comprehensive understanding of the microbial induced biomineralization of iron-reducing bacteria and its role in the iron element biogeochemical cycle. |
语种 | 中文 |
CSCD记录号 | CSCD:6214303 |
资助机构 | 国家自然科学基金#41522402,41621004 ; 青岛海洋科学与技术国家实验室海洋地质过程与环境功能实验室开放基金#MGQNLM201704 ; 中国科学院“百人计划”# |
源URL | [http://ir.yic.ac.cn/handle/133337/24715] ![]() |
专题 | 烟台海岸带研究所_近岸生态与环境实验室 烟台海岸带研究所_海岸带生物学与生物资源利用所重点实验室 |
作者单位 | 1.青岛海洋科学与技术国家实验室海洋地质过程与环境功能实验室; 2.中国科学院地质与地球物理研究所地球与行星物理重点实验室中国科学院地球科学研究院; 3.中国科学院大学; 4.中国科学院烟台海岸带研究所海岸带生物学与生物资源保护重点实验室; 5.中国科学院地球化学研究所,环境地球化学国家重点实验室 |
推荐引用方式 GB/T 7714 | 王芙仙,郑世玲,邱浩,等. 铁还原细菌Shewanella oneidensis MR-4诱导水合氧化铁形成蓝铁矿的过程[J]. 微生物学报,2018,58(04):573-583. |
APA | 王芙仙.,郑世玲.,邱浩.,曹长乾.,唐旭.,...&李金华.(2018).铁还原细菌Shewanella oneidensis MR-4诱导水合氧化铁形成蓝铁矿的过程.微生物学报,58(04),573-583. |
MLA | 王芙仙,et al."铁还原细菌Shewanella oneidensis MR-4诱导水合氧化铁形成蓝铁矿的过程".微生物学报 58.04(2018):573-583. |
入库方式: OAI收割
来源:烟台海岸带研究所
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