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Iron stable isotopes: beyond biosignatures
Earth and Planetary Science Letters, 2004Abstract The stable isotope geochemistry of Fe has attracted intense interest in the past five years. This interest was originally motivated by the possible use of Fe isotopes in biosignature applications, particularly in sediments from the ancient Earth or Mars.
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Iron isotopes as a potential tool for ancient iron metals tracing
Journal of Archaeological Science, 2016J. Milot +3 more
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Fractionation of stable iron isotopes in higher plants.
Environmental Science & Technology, 2007Monika Guelke, F. von Blanckenburg
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Science, 1999
The 56 Fe/ 54 Fe of Fe-bearing phases precipitated in sedimentary environments varies by 2.5 per mil (δ 56 Fe values of +0.9 to −1.6 per mil). In contrast, the 56 Fe/ 54 Fe of Fe-bearing phases in igneous rocks from Earth
B L, Beard +5 more
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The 56 Fe/ 54 Fe of Fe-bearing phases precipitated in sedimentary environments varies by 2.5 per mil (δ 56 Fe values of +0.9 to −1.6 per mil). In contrast, the 56 Fe/ 54 Fe of Fe-bearing phases in igneous rocks from Earth
B L, Beard +5 more
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Analysis of dissolved iron isotopes in seawater
Marine Chemistry, 2010S. John, J. Adkins
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Mass spectrometry and natural variations of iron isotopes.
Mass Spectrometry Reviews, 2006N. Dauphas, O. Rouxel
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