Fe-XANES analyses of Reykjanes Ridge basalts: implications for oceanic crust’s role in the solid Earth oxygen cycle

• Published in: Earth and Planetary Science Letters
• Main Authors: Shorttle, Oliver, Moussallam, Yves, Hartley, Margaret, Maclennan, John, Edmonds, Marie, Murton, Bramley
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2015
• Subjects: Reykjanes; Iceland
• Online Access: https://eprints.soton.ac.uk/379555/; https://eprints.soton.ac.uk/379555/1/Shorttle_os_fo2015-preprint.pdf; https://eprints.soton.ac.uk/379555/2/1-s2.0-S0012821X15004446-main.pdf

The cycling of material from Earth’s surface environment into its interior can couple mantle oxidation state to the evolution of the oceans and atmosphere. A major uncertainty in this exchange is whether altered oceanic crust entering subduction zones can carry the oxidised signal it inherits during alteration at the ridge axis, past the arc front and into the deep mantle for long-term storage. However, recycled oceanic crust may eventually be entrained into mantle upwellings and undergo melting at ocean islands, creating the potential for basalt chemistry to constrain the nature of past solid Earth–hydrosphere redox coupling. Numerous independent observations suggest that Iceland contains a significant recycled oceanic crustal component, making it an ideal locality to investigate links between redox proxies and geochemical indices of enrichment. We have interrogated the elemental, isotope and redox geochemistry of basalts from the Reykjanes Ridge, which forms a 700 km transect of the Iceland plume. Over this distance, geophysical and geochemical tracers of plume influence increase dramatically, with the basalts recording both longand short-wavelength heterogeneity in the Iceland plume. We present new high-precision Fe-XANES measurements of Fe3+=P Fe on a suite of 64 basalt glasses from the Reykjanes Ridge. These basalts exhibit positive correlations between Fe3+=P Fe and trace element and isotopic signals of enrichment, and become progressively oxidised towards Iceland: fractionation-corrected Fe3+=P Fe increases by ? 0:015 and ?QFM by ? 0:2 log units. We carefully rule out a role for sulfur degassing in creating this trend, and by considering various redox melting processes and metasomatic source enrichment mechanisms, conclude that an intrinsically oxidised component within the Icelandic mantle is required. Given the previous evidence for entrained oceanic crustal material within the Iceland plume, we consider this the most plausible carrier of the oxidised signal. To determine the ferric iron content of the ...