{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,10,6]],"date-time":"2026-10-06T10:47:09Z","timestamp":1791283629805,"version":"4.1.0"},"reference-count":37,"publisher":"Portland Press Ltd.","issue":"6","content-domain":{"domain":["portlandpress.com"],"crossmark-restriction":true},"short-container-title":[],"published-print":{"date-parts":[[2012,12,1]]},"abstract":"<jats:p>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.<\/jats:p>","DOI":"10.1042\/bst20120102","type":"journal-article","created":{"date-parts":[[2012,11,23]],"date-time":"2012-11-23T17:09:55Z","timestamp":1353690595000},"page":"1280-1283","update-policy":"https:\/\/doi.org\/10.1042\/crossmark_policy","source":"Crossref","is-referenced-by-count":28,"title":["Rates and potential mechanism of anaerobic nitrate-dependent microbial pyrite oxidation"],"prefix":"10.1042","volume":"40","author":[{"given":"Julian","family":"Bosch","sequence":"first","affiliation":[{"name":"Institute of Groundwater Ecology, Helmholtz Zentrum M\u00fcnchen, 85764 Neuherberg, Germany"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Rainer\u00a0U.","family":"Meckenstock","sequence":"additional","affiliation":[{"name":"Institute of Groundwater Ecology, Helmholtz Zentrum M\u00fcnchen, 85764 Neuherberg, Germany"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"288","published-online":{"date-parts":[[2012,11,21]]},"reference":[{"key":"2021111720514867700_B1","doi-asserted-by":"crossref","first-page":"49","DOI":"10.1126\/science.203.4375.49","article-title":"Pyrite: its rapid formation in a salt marsh and its importance in ecosystem metabolism","volume":"203","author":"Howarth","year":"1979","journal-title":"Science"},{"key":"2021111720514867700_B2","doi-asserted-by":"crossref","first-page":"1426","DOI":"10.1126\/science.282.5393.1426","article-title":"Paleoclimate: the sulfur cycle and atmospheric oxygen","volume":"282","author":"Berner","year":"1998","journal-title":"Science"},{"key":"2021111720514867700_B3","doi-asserted-by":"crossref","first-page":"417","DOI":"10.1007\/978-0-387-73563-4_9","article-title":"Microbiological controls on geochemical kinetics. 2. 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