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Novel mode of microbial energy metabolism: organic carbon oxidation coupled to dissimilatory reduction of iron or manganese.新型微生物能量代谢模式:有机碳的氧化与铁或锰的异化还原相偶联。
Appl Environ Microbiol. 1988 Jun;54(6):1472-80. doi: 10.1128/aem.54.6.1472-1480.1988.
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Availability of ferric iron for microbial reduction in bottom sediments of the freshwater tidal potomac river.铁在淡水潮汐波托马克河底沉积物中微生物还原的可用性。
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Reduction of ferric iron in anaerobic, marine sediment and interaction with reduction of nitrate and sulfate.在厌氧海洋沉积物中还原三价铁及其与硝酸盐和硫酸盐还原的相互作用。
Appl Environ Microbiol. 1982 Feb;43(2):319-24. doi: 10.1128/aem.43.2.319-324.1982.
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Dissimilatory Fe(III) and Mn(IV) reduction.异化铁(III)和锰(IV)还原
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5
Microbial reduction of manganese and iron: new approaches to carbon cycling.微生物对锰和铁的还原作用:碳循环的新途径。
Appl Environ Microbiol. 1992 Feb;58(2):439-43. doi: 10.1128/aem.58.2.439-443.1992.

丹麦韦杰恩一处受垃圾渗滤液污染的含水层中微生物铁还原的证据。

Evidence for microbial iron reduction in a landfill leachate-polluted aquifer (Vejen, Denmark).

作者信息

Albrechtsen H J, Christensen T H

机构信息

Institute of Environmental Science and Engineering, Technical University of Denmark, Lyngby.

出版信息

Appl Environ Microbiol. 1994 Nov;60(11):3920-5. doi: 10.1128/aem.60.11.3920-3925.1994.

DOI:10.1128/aem.60.11.3920-3925.1994
PMID:7993081
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC201916/
Abstract

Aquifer sediment samples obtained from the anaerobic part of a landfill leachate plume in Vejen, Denmark, were suspended in groundwater or in an artificial medium and incubated. The strictly anaerobic suspensions were tested for reduction of ferric iron [Fe(III)] oxides, which was measured as an increase in the concentration of dissolved Fe(II). Iron reduction did not occur when the medium was inoculated with inactive sediment and when the organisms in the inoculated medium were killed by formaldehyde, by chloroform, or by pasteurization, whereas the level of iron reduction was significant when living bacteria were present. Mixed cultures were obtained from the sediment samples, and differences in apparent iron reduction rates among the different cultures were maintained during several transfers. In addition, iron reduction was observed in unamended incubation mixtures containing whole sediment and groundwater. Synthetic amorphous Fe(III) oxides, as well as naturally occurring sediment-bound Fe(III) oxides, could be reduced by the cultures. Together, our results provide evidence that iron-reducing bacteria are present and microbial iron reduction occurs in the polluted aquifer sediments which we studied.

摘要

从丹麦韦杰恩一个垃圾渗滤液羽流的厌氧部分采集的含水层沉积物样本,被悬浮于地下水或人工培养基中并进行培养。对严格厌氧的悬浮液进行了三价铁[Fe(III)]氧化物还原测试,以溶解态Fe(II)浓度的增加来衡量。当培养基接种无活性沉积物以及接种培养基中的生物体被甲醛、氯仿或巴氏灭菌法杀死时,未发生铁还原现象,而当存在活细菌时,铁还原水平显著。从沉积物样本中获得了混合培养物,不同培养物之间明显的铁还原率差异在多次传代过程中得以保持。此外,在含有完整沉积物和地下水的未改良培养混合物中也观察到了铁还原现象。合成无定形Fe(III)氧化物以及天然存在的沉积物结合态Fe(III)氧化物均可被这些培养物还原。总之,我们的结果证明我们所研究的受污染含水层沉积物中存在铁还原细菌且发生了微生物铁还原作用。