Cited by 215Paleontology and Stratigraphy of FossilsGeochemistry and Elemental AnalysisGeological and Geochemical Analysis

Petrography and geochemistry of the Dales Gorge banded iron formation: paragenetic sequence, source and implications for palaeo-ocean chemistry

Pecoits, E., Gingras, M.K., Barley, M.E., Kappler, A., Posth, N.R., Konhauser, K.O.·2009·Precambrian Research

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Crossref · 10.1016/j.precamres.2009.03.014

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121 of 121 references verified0 citation errors · 0 not checkable

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  • The Dales Gorge Member is composed of relatively pure chemical precipitates, as supported by low Al, Ti, Th, Zr, Hf, and Sc concentrations.

    “The Dales Gorge Member is also composed of relatively pure chemical precipitates, as supported by low Al, Ti, Th, Zr, Hf, and Sc concentrations (Pecoits et al., 2009)”
  • Compared to the underlying Dales Gorge Member, the Joffre Member has significantly higher REE concentrations.

    “Compared to the underlying Dales Gorge Member, the Joffre Member has significantly higher REE concentrations (Pecoits et al., 2009; Haugaard et al., 2016b)”
  • The Dales Gorge Member displays typical seawater REE+Y patterns, including low Pr/YbSN (0.08-0.3), low Sm/YbSN (0.1-0.4), positive La anomalies, positive Eu anomalies, and superchondritic Y/Ho ratios.

    “Typical seawater REE+Y patterns are displayed by the Dales Gorge Member, including low Pr/YbSN (0.08-0.3), low Sm/YbSN (0.1-0.4), positive La anomalies, positive Eu anomalies, and superchondritic Y/Ho ratios (Pecoits et al., 2009)”
  • The Dales Gorge Member lacks a true negative Ce anomaly, suggesting low-oxygen conditions at the time of deposition.

    “the Dales Gorge Member lacks a true negative Ce anomaly, suggesting low-oxygen conditions at the time of deposition”
  • Iron isotope compositions in both the Joffre and Dales Gorge members show a wide range in δ56Fe values, indicating multiple Fe sources and pathways, with average δ56Fe values in the Joffre Member heavier than those of the Dales Gorge Member.

    “Iron isotope compositions in both the Joffre and the Dales Gorge members show a wide range in d 56 Fe values, indicating multiple Fe sources and pathways (Fig. 6), where average d 56 Fe values in the Joffre Member are heavier than those of the Dales Gorge Member (Johnson et al., 2008b; Pecoits et al., 2009; W Li et al., 2013a; Haugaard et al., 2016b)”

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Authors
Pecoits, E., Gingras, M. K., Barley, M. E., Kappler, A., Posth, N. R., & Konhauser, K. O.
Affiliations
  • University of Alberta (CA)
  • The University of Western Australia (AU)
  • University of Tübingen (DE)
Venue
Precambrian Research
Publisher
Elsevier BV
Published
2009-07
Volume
172
Issue
1-2
Pages
163-187
ISSN
0301-9268 (ISSN-L)
OpenAlex
W2171500660
Cited by
215
References
121
Citations by year
2026: 9 · 2025: 10 · 2024: 22 · 2023: 16 · 2022: 13 · 2021: 14 · 2020: 12 · 2019: 12 · 2018: 11 · 2017: 18 · 2016: 15 · 2015: 16 · 2014: 14 · 2013: 8 · 2012: 6
FWCI
6.53
Type
journal article
Language
en
Open access
closed
Locations
  • Precambrian Research (publishedVersion)
  • UWA Profiles and Research Repository (UWA) (submittedVersion)
  • Research at the University of Copenhagen (University of Copenhagen) (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 › Geological and Geochemical Analysis
Keywords
banded iron formations, paragenetic sequence, siderite, siderite dissolution, siderite precipitation, greenalite, magnetite, hematite, trace element partitioning, hydrothermal alteration, upper continental crust, Fe(III) reduction

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