The Fe and Zn isotope composition of deep mantle source regions: Insights from Baffin Island picrites

• Published in: Geochimica et Cosmochimica Acta
• Main Authors: Mccoy-West, Alex, Fitton, J. Godfrey, Pons, Marie-Laure, Inglis, Edward, Williams, Helen
• Other Authors: Department of Earth Sciences Durham, Durham University, Monash University Clayton, School of Geosciences Edinburgh, University of Edinburgh (Edin.), Eberhard Karls Universität Tübingen = University of Tübingen, Institut de Physique du Globe de Paris (IPGP (UMR_7154)), Institut national des sciences de l'Univers (INSU - CNRS)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Department of Earth Sciences Cambridge, UK, University of Cambridge UK (CAM), Laidlaw-Hall Trust European Research Council (ERC)306655NERC Natural Environment Research CouncilNE/M0003/1, European Project: 306655,EC:FP7:ERC,ERC-2012-StG_20111012,HABITABLEPLANET(2013)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2018
• Subjects: Iron; Zinc; Stable isotopes; Picrites; Komatiites; Olivine; Sulfide; [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry; Baffin Island; Canada; Baffin; North Atlantic
• Online Access: https://insu.hal.science/insu-02915540; https://insu.hal.science/insu-02915540/document; https://insu.hal.science/insu-02915540/file/25743.pdf; https://doi.org/10.1016/j.gca.2018.07.021

International audience Young (61 Ma) unaltered picrites from Baffin Island, northeast Canada, possess some of the highest 3He/4He (up to 50 Ra) seen on Earth, and provide a unique opportunity to study primordial mantle that has escaped subsequent chemical modification. These high-degree partial melts also record anomalously high 182W/184W ratios, but their Sr-Nd-Hf-Pb isotopic compositions (including 142Nd) are indistinguishable from those of North Atlantic mid-ocean ridge basalts. New high precision Fe and Zn stable isotope analyses of Baffin Island picrites show limited variability with δ56Fe ranging from −0.03‰ to 0.13‰ and δ66Zn varying from 0.18‰ to 0.28‰. However, a clear inflection is seen in both sets of isotope data around the composition of the parental melt (MgO = 21 wt%; δ56Fe = 0.08 ± 0.04‰; and δ66Zn = 0.24 ± 0.03‰), with two diverging trends interpreted to reflect the crystallisation of olivine and spinel in low-MgO samples and the accumulation of olivine at higher MgO. Olivine mineral separates are significantly isotopically lighter than their corresponding whole rocks (δ56Fe ≥ −0.62‰ and δ66Zn ≥ −0.22‰), with analyses of individual olivine phenocrysts having extremely variable Fe isotope compositions (δ56Fe = −0.01‰ to −0.80‰). By carrying out modelling in three-isotope space, we show that the very negative Fe isotope compositions of olivine phenocryst are the result of kinetic isotope fractionation from disequilibrium diffusional processes. An excellent correlation is observed between δ56Fe and δ66Zn, demonstrating that Zn isotopes are fractionated by the same processes as Fe in simple systems dominated by magmatic olivine. The incompatible behaviour of Cu during magmatic evolution is consistent with the sulfide-undersaturated nature of these melts. Consequently Zn behaves as a purely lithophile element, and estimates of the bulk Earth Zn isotope composition based on Baffin Island should therefore be robust. The ancient undegassed lower mantle sampled at Baffin Island possesses a δ56Fe value ...