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Fe, C, and O isotope compositions of banded iron formation carbonates demonstrate a major role for dissimilatory iron reduction in ~2.5Ga marine environments

Heimann, Adriana, Johnson, Clark M., Beard, Brian L., Valley, John W., Roden, Eric E., Spicuzza, Michael J., Beukes, Nicolas J.·2010·Earth and Planetary Science Letters

DOI 10.1016/j.epsl.2010.02.015

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Miyano, 1984, Phase relations of stilpnomelane, ferriannite and riebeckite in very low-grade metamorphosed iron-formations, Geol. Soc. South Africa Trans., 87, 111
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Authors: Heimann, A., Johnson, C. M., Beard, B. L., Valley, J. W., Roden, E. E., Spicuzza, M. J., & Beukes, N. J.
Affiliations: University of Wisconsin–Madison (US)
University of Johannesburg (ZA)
Corresponding author: Heimann, Adriana
ORCID: Valley, John W.
Roden, Eric E.
Spicuzza, Michael J.
Beukes, Nicolas J.
Venue: Earth and Planetary Science Letters
Publisher: Elsevier BV
Published: 2010-05
Volume: 294
Issue: 1-2
Pages: 8-18
ISSN: 0012-821X (ISSN-L)
DOI: 10.1016/j.epsl.2010.02.015
OpenAlex: W2148984976
Cited by: 283
References: 93
Citations by year: 2026: 15 · 2025: 20 · 2024: 27 · 2023: 28 · 2022: 18 · 2021: 22 · 2020: 16 · 2019: 17 · 2018: 15 · 2017: 23 · 2016: 14 · 2015: 13 · 2014: 13 · 2013: 16 · 2012: 11
FWCI: 9.09
Type: journal article
Language: en
Open access: closed
Licence: www.elsevier.com/tdm/userlicense/1.0/ (tdm)
Locations: Earth and Planetary Science Letters (publishedVersion)
Funders: National Science Foundation
NASA Astrobiology Institute
Topics: Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
Keywords: banded iron formations, siderite, dissimilatory iron reduction, δ13C, oxygen isotope composition, iron oxide inclusions, iron remobilization, microbial iron reduction, Precambrian geochemistry

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Fe, C, and O isotope compositions of banded iron formation carbonates demonstrate a major role for dissimilatory iron reduction in ~2.5Ga marine environments

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