Iron isotope fractionation during sulfide-promoted reductive dissolution of iron (oxyhydr)oxide minerals-Reference-Cited by-同舟云学术

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Iron isotope fractionation during sulfide-promoted reductive dissolution of iron (oxyhydr)oxide minerals

Published:2024-03 Issue: Volume:369 Page:17-34
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

McAnena Alison,Severmann Silke^ORCID,Guilbaud Romain^ORCID,Poulton Simon W.^ORCID

Funder

National Science Foundation

Natural Environment Research Council

Royal Society

Publisher

Elsevier BV

Reference115 articles.

1. Gold accumulation in the Archaean Witwatersrand Basin, South Africa—Evidence from concentrically laminated pyrite;Agangi;Earth Sci. Rev.,2015

2. Mass-dependent and-independent signature of Fe isotopes in magnetotactic bacteria;Amor;Science,2016

3. Iron stable isotopes: beyond biosignatures;Anbar;Earth Planet. Sci. Lett.,2004

4. Coupled Fe and S isotope evidence for Archean microbial Fe(III) and sulfate reduction;Archer;Geology,2006

5. Iron isotope fractionation during microbially stimulated Fe(II) oxidation and Fe(III) precipitation;Balci;Geochim. Cosmochim. Acta,2006

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1. Characteristics of phosphorus transformation from vivianite mediated by sulphide;Journal of Environmental Sciences;2024-08

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