Coupled Fe(II)−Fe(III) Electron and Atom Exchange as a Mechanism for Fe Isotope Fractionation during Dissimilatory Iron Oxide Reduction-Reference-Cited by-同舟云学术

Coupled Fe(II)−Fe(III) Electron and Atom Exchange as a Mechanism for Fe Isotope Fractionation during Dissimilatory Iron Oxide Reduction

Published:2005-07-23 Issue:17 Volume:39 Page:6698-6704
ISSN:0013-936X
Container-title:Environmental Science & Technology
language:en
Short-container-title:Environ. Sci. Technol.

Author:

Crosby Heidi A.¹,Johnson Clark M.¹,Roden Eric E.¹,Beard Brian L.¹

Affiliation:

1. Department of Geology and Geophysics, University of Wisconsin-Madison, 1215 West Dayton Street, Madison, Wisconsin 53706

Publisher

American Chemical Society (ACS)

Subject

Environmental Chemistry,General Chemistry

Link

https://pubs.acs.org/doi/pdf/10.1021/es0505346

Reference64 articles.

1. IRON AND MANGANESE IN ANAEROBIC RESPIRATION: Environmental Significance, Physiology, and Regulation

2. Microbiological evidence for Fe(III) reduction on early Earth

3. Lovley, D. R. Fe(III) and Mn(IV) Reduction. InEnvironmental Microbe-Metal Interactions; Lovley, D. R., Ed.; ASM Press: Washington, DC, 2000; pp 3−30.

4. Iron Isotope Biosignatures

5. Application of Fe isotopes to tracing the geochemical and biological cycling of Fe

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