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Biologically recycled continental iron is a major component in banded iron formations

Proceedings of the National Academy of Sciences - PNAS, 2015-07, Vol.112 (27), p.8193-8198

2015

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Fe(II)-Catalyzed Recrystallization of Goethite Revisited

Environmental science & technology, 2014-10, Vol.48 (19), p.11302-11311

2014

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Atom Exchange between Aqueous Fe(II) and Goethite: An Fe Isotope Tracer Study

Environmental science & technology, 2009-02, Vol.43 (4), p.1102-1107

2009

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The Iron Isotope Fingerprints of Redox and Biogeochemical Cycling in Modern and Ancient Earth

Annual review of earth and planetary sciences, 2008-01, Vol.36 (1), p.457-493

2008

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Determination of the Fe(II)aq–magnetite equilibrium iron isotope fractionation factor using the three-isotope method and a multi-direction approach to equilibrium

Earth and planetary science letters, 2014-04, Vol.391, p.77-86

2014

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Magnesium isotope fractionation during precipitation of inorganic calcite under laboratory conditions

Earth and planetary science letters, 2012-06, Vol.333-334, p.304-316

2012

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Iron Geochemistry: An Isotopic Perspective

1st ed. 2020., 2020

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Fe Atom Exchange between Aqueous Fe2+ and Magnetite

Environmental science & technology, 2012-11, Vol.46 (22), p.12399-12407

2012

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Iron isotope fractionation between aqueous Fe(II) and goethite revisited: New insights based on a multi-direction approach to equilibrium and isotopic exchange rate modification

Geochimica et cosmochimica acta, 2014-08, Vol.139, p.383-398

2014

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Iron isotope fractionation between aqueous ferrous iron and goethite

Earth and planetary science letters, 2010-06, Vol.295 (1-2), p.241-250

2010

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Stable Iron Isotope Fractionation Between Aqueous Fe(II) and Hydrous Ferric Oxide

Environmental science & technology, 2011-03, Vol.45 (5), p.1847-1852

2011

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Biological Fe oxidation controlled deposition of banded iron formation in the ca. 3770Ma Isua Supracrustal Belt (West Greenland)

Earth and planetary science letters, 2013-02, Vol.363, p.192-203

2013

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An anoxic, Fe(II)-rich, U-poor ocean 3.46 billion years ago

Geochimica et cosmochimica acta, 2013-11, Vol.120, p.65-79

2013

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Iron isotopes constrain biologic and abiologic processes in banded iron formation genesis

Geochimica et cosmochimica acta, 2008, Vol.72 (1), p.151-169

2008

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Evidence for free oxygen in the Neoarchean ocean based on coupled iron–molybdenum isotope fractionation

Geochimica et cosmochimica acta, 2012-06, Vol.86, p.118-137

2012

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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

Earth and planetary science letters, 2010-05, Vol.294 (1-2), p.8-18

2010

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The effect of early diagenesis on the Fe isotope compositions of porewaters and authigenic minerals in continental margin sediments

Geochimica et cosmochimica acta, 2006-01, Vol.70 (8), p.2006-2022

2006

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The mechanisms of iron isotope fractionation produced during dissimilatory Fe(III) reduction by Shewanella putrefaciens and Geobacter sulfurreducens

Geobiology, 2007-06, Vol.5 (2), p.169-189

2007

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Life on a Mesoarchean marine shelf – insights from the world’s oldest known granular iron formation

Scientific reports, 2020-06, Vol.10 (1), p.10519-10519, Article 10519

2020

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

Environmental science & technology, 2005-09, Vol.39 (17), p.6698-6704

2005

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Iron isotope constraints on Fe cycling and mass balance in oxygenated Earth oceans

Geology (Boulder), 2003-07, Vol.31 (7), p.629

2003

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Experimental constraints on Fe isotope fractionation during magnetite and Fe carbonate formation coupled to dissimilatory hydrous ferric oxide reduction

Geochimica et cosmochimica acta, 2005-02, Vol.69 (4), p.963-993

2005

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Volcanic biotite-sanidine 40Ar/39Ar age discordances reflect Ar partitioning and pre-eruption closure in biotite

Geology (Boulder), 2010-10, Vol.38 (10), p.923-926

2010

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Ancient geochemical cycling in the Earth as inferred from Fe isotope studies of banded iron formations from the Transvaal Craton

Contributions to mineralogy and petrology, 2003-02, Vol.144 (5), p.523-547

2003

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Pre-4.0 billion year weathering on Mars constrained by Rb–Sr geochronology on meteorite ALH84001

Earth and planetary science letters, 2013-01, Vol.361, p.173-182

2013

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Biologically recycled continental iron is a major component in banded iron formations

Fe(II)-Catalyzed Recrystallization of Goethite Revisited

Atom Exchange between Aqueous Fe(II) and Goethite: An Fe Isotope Tracer Study

The Iron Isotope Fingerprints of Redox and Biogeochemical Cycling in Modern and Ancient Earth

Determination of the Fe(II)aq–magnetite equilibrium iron isotope fractionation factor using the three-isotope method and a multi-direction approach to equilibrium

Magnesium isotope fractionation during precipitation of inorganic calcite under laboratory conditions

Iron Geochemistry: An Isotopic Perspective

Fe Atom Exchange between Aqueous Fe2+ and Magnetite

Iron isotope fractionation between aqueous Fe(II) and goethite revisited: New insights based on a multi-direction approach to equilibrium and isotopic exchange rate modification

Iron isotope fractionation between aqueous ferrous iron and goethite

Stable Iron Isotope Fractionation Between Aqueous Fe(II) and Hydrous Ferric Oxide

Biological Fe oxidation controlled deposition of banded iron formation in the ca. 3770Ma Isua Supracrustal Belt (West Greenland)

An anoxic, Fe(II)-rich, U-poor ocean 3.46 billion years ago

Iron isotopes constrain biologic and abiologic processes in banded iron formation genesis

Evidence for free oxygen in the Neoarchean ocean based on coupled iron–molybdenum isotope fractionation

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

The effect of early diagenesis on the Fe isotope compositions of porewaters and authigenic minerals in continental margin sediments

The mechanisms of iron isotope fractionation produced during dissimilatory Fe(III) reduction by Shewanella putrefaciens and Geobacter sulfurreducens

Life on a Mesoarchean marine shelf – insights from the world’s oldest known granular iron formation

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

Iron isotope constraints on Fe cycling and mass balance in oxygenated Earth oceans

Experimental constraints on Fe isotope fractionation during magnetite and Fe carbonate formation coupled to dissimilatory hydrous ferric oxide reduction

Volcanic biotite-sanidine 40Ar/39Ar age discordances reflect Ar partitioning and pre-eruption closure in biotite

Ancient geochemical cycling in the Earth as inferred from Fe isotope studies of banded iron formations from the Transvaal Craton

Pre-4.0 billion year weathering on Mars constrained by Rb–Sr geochronology on meteorite ALH84001

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