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Rates and potential mechanism of anaerobic nitrate-dependent microbial pyrite oxidation.

Biochem. Soc. Trans. 40, 1280-1283 (2012)
DOI PMC
Open Access Green möglich sobald Postprint bei der ZB eingereicht worden ist.
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
Korrespondenzautor
Schlagwörter autolithotrophy; denitrification; ferrous sulfide; microbial iron oxidation; pyrite; Thiobacillus denitrificans
ISSN (print) / ISBN 0300-5127
e-ISSN 1470-8752
Quellenangaben Band: 40, Heft: 6, Seiten: 1280-1283 Artikelnummer: , Supplement: ,
Verlag Portland Press
Nichtpatentliteratur Publikationen
Begutachtungsstatus Peer reviewed