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Organic Acid-Dependent Iron Mineral Formation by a Newly Isolated Iron-Reducing Bacterium,Shewanella sp. HN-41

Lee, Ji-Hoon, Roh, Yul, Kim, Kyoung-Woong, Hur, Hor-Gil·2007·Geomicrobiology Journal
DOI 10.1080/01490450601134291
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Abstract

The influence of organic acids used as substrates for bacterial respiration coupled to dissimilatory Fe(III) reduction on the mineralogy of formed iron minerals was examined. A newly isolated dissimilatory iron-reducing bacterium, Shewanella strain HN-41 exhibited different mineral formation patterns resulting from the reduction of poorly crystalline Fe(III)-oxyhydroxide, akaganeite (β-FeOOH; ∼ 70 mM) depending upon the presence of the different organic acids: lactate, pyruvate, and formate (10 mM) under anaerobic conditions. X-ray diffraction analysis identified the minerals as magnetite, siderite, and a mixture of magnetite and siderite, which were produced by strain HN-41 using lactate, pyruvate, and formate as a sole electron donor, respectively. With the descending order of the amount of Fe(II) in aqueous phase, the pyruvate-, formate-, and lactate-incubations released Fe(II) into aqueous phase from the poorly crystalline akaganeite by the bacterial Fe(III) reduction. The amount of Fe(II) released into aqueous phase was inversely related to the degree of crystallinity. Magnetite produced during lactate-incubation with the least amount of Fe(II) in aqueous phase, and final pH of 8.6 and Eh of –408 mV showed the highest crystallinity, while siderite formed by pyruvate-incubation with the largest release of Fe(II) in aqueous phase, and final pH of 8.1 and Eh of –394 mV showed the lowest crystallinity. When strain HN-41 was incubated with the organic acid substrates at 10 mM…

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Metadata

Authors
Lee, J.-H., Roh, Y., Kim, K.-W., & Hur, H.-G.
Venue
Geomicrobiology Journal
Publisher
Informa UK Limited
Published
2007-01
Volume
24
Issue
1
Pages
31-41
ISSN
  • 0149-0451
  • 1521-0529
DOI
10.1080/01490450601134291
Cited by
53
References
4
Language
en

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