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Deep Earth’s Oxygen recycling at subduction Zones

Project description

Unravelling the mystery of Earth’s oxygen-breathing interior

Scientists have long marvelled at the Earth’s oxygen-breathing interior. It has puzzled them. To shed new light on this phenomenon, the OZ project, funded by the European Research Council, will address this issue. Unlike other planets, the Earth’s interior is oxygenated through the sink of oxidised tectonic plates at convergent margins. However, recent estimates suggest that some key subducting chemical elements are not balanced on geological time scales by global magmatism and volcanism. OZ will determine the effectiveness of subduction slab fluids to oxidise the mantle wedge and generate the most oxidised magmatism on Earth: arc magmatism. The project aims to achieve four specific goals through innovative techniques, including characterising sulfide-oxide mineral associations in natural samples and upscaling these processes to subduction zones.

Objective

In contrast to other known terrestrial planets, the Earth's interior is oxygen-breathing through the sink of oxidised tectonic plates at convergent margins since the late Archean to Paleoproterozoic. Recent estimates suggest that the redox capacity of some key subducting chemical elements is not balanced on geological time scales by global magmatism and volcanism, thus implying a puzzling deep oxygenation of our planet. Although current models presume that the redox state of subducting slabs is irreversible, my most recent results demonstrate that mixing of fluids from different slab lithologies can dramatically change the redox capacity of such fluids and the deeply subducted residues. The OZ project will provide an unprecedented quantitative framework to account for such interactions in order to determine the effectiveness of subduction slab fluids to oxidise the mantle wedge and generate the most oxidised magmatism on Earth: arc magmatism. To achieve this ambitious goal, OZ will address four specific goals: (1) the experimental determination of the effect of oxygen (fO2) and sulphur (fS2) fugacity on the stability of critical mineral assemblages during the prograde metamorphic evolution of serpentinites by using a novel triple capsule buffering technique in high pressure experiments; (2) the determination of sulphur mobility at high pressure due to gradients in fO2 and fS2 by means of an original experimental capsule design with interconnected reservoirs representative of the heterogeneity of the slab; (3) the characterization of sulphide-oxide mineral associations in natural samples from exhumed paleo-subduction terranes to demonstrate the scales of fluid mixing in nature; and (4) the upscaling of these processes to subduction zones by using two types of equilibrium reactive transport models at the scale of the slab and the mantle wedge.

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HORIZON-ERC - HORIZON ERC Grants

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Call for proposal

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(opens in new window) ERC-2022-COG

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Host institution

AGENCIA ESTATAL CONSEJO SUPERIOR DE INVESTIGACIONES CIENTIFICAS
Net EU contribution

Net EU financial contribution. The sum of money that the participant receives, deducted by the EU contribution to its linked third party. It considers the distribution of the EU financial contribution between direct beneficiaries of the project and other types of participants, like third-party participants.

€ 2 000 000,00
Address
CALLE SERRANO 117
28006 MADRID
Spain

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Region
Comunidad de Madrid Comunidad de Madrid Madrid
Activity type
Research Organisations
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Total cost

The total costs incurred by this organisation to participate in the project, including direct and indirect costs. This amount is a subset of the overall project budget.

€ 2 000 000,00

Beneficiaries (1)

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