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Rates and potential mechanism of anaerobic nitrate-dependent microbial pyrite oxidation.
Biochem. Soc. Trans. 40, 1280-1283 (2012)
Pyrite (FeS2) is a major iron- and sulfur-containing mineral phase in the environment. Oxidation of pyrite by aerobic micro-organisms has been well investigated. However, the reactivity of pyrite under anoxic conditions is still an open question. In the present paper, we summarize field and laboratory data on this chemolithotrophic respiration process with nitrate as terminal electron acceptor. Geochemical and stable isotope field data indicate that this process is occurring. Laboratory studies are more ambiguous, but recent positive results provide evidence that anaerobic microbial pyrite oxidation can, in fact, occur with nitrate as electron acceptor.
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Publikationstyp
Artikel: Journalartikel
Dokumenttyp
Wissenschaftlicher Artikel
Schlagwörter
autolithotrophy; denitrification; ferrous sulfide; microbial iron oxidation; pyrite; Thiobacillus denitrificans
ISSN (print) / ISBN
0300-5127
e-ISSN
1470-8752
Zeitschrift
Biochemical Society Transactions
Quellenangaben
Band: 40,
Heft: 6,
Seiten: 1280-1283
Verlag
Portland Press
Nichtpatentliteratur
Publikationen
Begutachtungsstatus
Peer reviewed
Institut(e)
Institute of Groundwater Ecology (IGOE)