Oxic Fe(III) reduction could have generated Fe(II) in the photic zone of Precambrian seawater

Swanner, E.D.; Maisch, M.; Wu, W.; Kappler, A.

doi:/10.1038/s41598-018-22694-y

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Oxic Fe(III) reduction could have generated Fe(II) in the photic zone of Precambrian seawater

Swanner, E.D.; Maisch, M.; Wu, W.; Kappler, A. (2018). Oxic Fe(III) reduction could have generated Fe(II) in the photic zone of Precambrian seawater. NPG Scientific Reports 8(1): 9 pp. https://dx.doi.org/10.1038/s41598-018-22694-y

In: Scientific Reports (Nature Publishing Group). Nature Publishing Group: London. ISSN 2045-2322; e-ISSN 2045-2322, more

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Swanner, E.D. Maisch, M. Wu, W. Kappler, A.

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