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Biogenic Fe(III) minerals: From formation to diagenesis and preservation in the rock record
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“Despite the consensus amongst workers that the precursor phase during the sedimentation of IF was most likely Fe(III)-oxyhydroxides (e.g., Konhauser et al., 2002; Kappler et al., 2005; Posth et al., 2014; Sun et al., 2015) or an Fe(III)-Si gel (e.g., Percak-Dennett et al., 2011; Zheng et al., 2016)”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Posth et al., 2014
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Metadata
- Authors
- Posth, N. R., Canfield, D. E., & Kappler, A.
- Affiliations
- University of Southern Denmark (DK)
- University of Tübingen (DE)
- Corresponding author
- Posth, N.R.
- Venue
- Earth-Science Reviews
- Publisher
- Elsevier BV
- Published
- 2014-08
- Volume
- 135
- Pages
- 103-121
- ISSN
- 0012-8252 (ISSN-L)
- OpenAlex
- W1873850631
- Cited by
- 153
- References
- 261
- Citations by year
- 2026: 7 · 2025: 18 · 2024: 10 · 2023: 8 · 2022: 14 · 2021: 20 · 2020: 9 · 2019: 16 · 2018: 10 · 2017: 9 · 2016: 14 · 2015: 14 · 2014: 2
- FWCI
- 8.71
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth-Science Reviews (publishedVersion)
- University of Southern Denmark Research Portal (University of Southern Denmark) (submittedVersion)
- 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 › Geophysics › Geomagnetism and Paleomagnetism Studies
- Keywords
- iron oxidation, Fe(II)-oxidizing bacteria, banded iron formations, diagenesis, iron cycling, iron isotopes, biomarkers, early Earth, sedimentary iron
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