Triple oxygen isotopic composition of the high-3He/4He mantle

Starkey, N.A., Jackson, C.R.M., Greenwood, R.C., Parman, S., Franchi, I.A., Jackson, M., Fitton, J.E., Stuart, F.M. , Kurz, M. and Larsen, L.M. (2016) Triple oxygen isotopic composition of the high-3He/4He mantle. Geochimica et Cosmochimica Acta, 176, pp. 227-238. (doi:10.1016/j.gca.2015.12.027)

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Abstract

Measurements of Xe isotope ratios in ocean island basalts (OIB) suggest that Earth’s mantle accreted heterogeneously, and that compositional remnants of accretion are sampled by modern, high-3He/4He OIB associated with the Icelandic and Samoan plumes. If so, the high-3He/4He source may also have a distinct oxygen isotopic composition from the rest of the mantle. Here, we test if the major elements of the high-3He/4He source preserve any evidence of heterogeneous accretion using measurements of three oxygen isotopes on olivine from a variety of high-3He/4He OIB locations. To high precision, the Δ17O value of high-3He/4He olivines from Hawaii, Pitcairn, Baffin Island and Samoa, are indistinguishable from bulk mantle olivine (Δ17OBulk Mantle − Δ17OHigh 3He/4He olivine = −0.002 ± 0.004 (2 × SEM)‰). Thus, there is no resolvable oxygen isotope evidence for heterogeneous accretion in the high-3He/4He source. Modelling of mixing processes indicates that if an early-forming, oxygen-isotope distinct mantle did exist, either the anomaly was extremely small, or the anomaly was homogenised away by later mantle convection. The δ18O values of olivine with the highest 3He/4He ratios from a variety of OIB locations have a relatively uniform composition (∼5‰). This composition is intermediate to values associated with the depleted MORB mantle and the average mantle. Similarly, δ18O values of olivine from high-3He/4He OIB correlate with radiogenic isotope ratios of He, Sr, and Nd. Combined, this suggests that magmatic oxygen is sourced from the same mantle as other, more incompatible elements and that the intermediate δ18O value is a feature of the high-3He/4He mantle source. The processes responsible for the δ18O signature of high-3He/4He mantle are not certain, but δ18O–87Sr/86Sr correlations indicate that it may be connected to a predominance of a HIMU-like (high U/Pb) component or other moderate δ18O components recycled into the high-3He/4He source.

Item Type:Articles
Additional Information:Open Access funded by Science and Technology Facilities Council.
Status:Published
Refereed:Yes
Glasgow Author(s) Enlighten ID:Fitton, Mr James and Stuart, Professor Finlay
Authors: Starkey, N.A., Jackson, C.R.M., Greenwood, R.C., Parman, S., Franchi, I.A., Jackson, M., Fitton, J.E., Stuart, F.M., Kurz, M., and Larsen, L.M.
College/School:College of Science and Engineering > School of Geographical and Earth Sciences
College of Science and Engineering > Scottish Universities Environmental Research Centre
Journal Name:Geochimica et Cosmochimica Acta
Publisher:Elsevier
ISSN:0016-7037
ISSN (Online):1872-9533
Published Online:02 January 2016
Copyright Holders:Copyright © 2016 Crown Copyright
First Published:First published in Geochimica et Cosmochimica Acta 176:227-238
Publisher Policy:Reproduced under a creative commons license

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