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Magmatic Triggering of Cenozoic Climate Changes

Project description

Decoding the Earth’s secrets

The Earth’s geological carbon cycle acts as a long-term thermostat, controlling climate and life’s evolution through plate tectonics. However, a major knowledge gap remains: the uncertainty of CO2 emissions from continental magmatic arcs, which are a key natural source of carbon in the atmosphere and oceans. In this context, the ERC-funded MATRICs project aims to fill this gap by reconstructing the history of magmatic CO2 emissions from the Neo-Tethyan convergent plate margin. Using melt inclusions, trace element analyses, and advanced numerical modelling, MATRICs will shed light on the role of these emissions in early Cenozoic climate shifts. This research will enhance our understanding of natural climate drivers, offering valuable insights for comparing them with today’s anthropogenic emissions.

Objective

By preventing all the Earth’s carbon to be released into the oceans and atmosphere or to be stored within rocks, the geological carbon cycle acts as a global long term thermostat, linking the evolution of climate and life to plate tectonics. The uncertainty regarding CO2 emissions from continental magmatic arcs, a primary natural input of carbon into the ocean and atmosphere, is currently the greatest limitation to our quantitative understanding of the geological carbon cycle. The high-gain target of MATRICs is to reconstruct the time history of magmatic CO2 emissions from the Neo-Tethyan convergent plate margin and its critical contribution to early Cenozoic climate changes. This ambitious goal will be achieved by iterative geologic data acquisition and state-of-the-art numerical modeling.

I propose to couple three established techniques to assess temporal changes in the source and amount of CO2 emissions from the Neo-Tethyan magmatic arc and assess their effects on early Cenozoic climate: (1) studies of melt inclusions, pockets of melts preserved within magmatic rocks, (2) analyses of trace elements concentrations (e.g. Hg, Te) within the sedimentary record, and (3) numerical petro-thermo-mechanical geodynamic and climate carbon cycle modeling. Undertaking this multi-disciplinary and ground-breaking project is now possible, owing to my success in using numerical modeling and diverse geological data to unravel the interactions between tectonics and climate accounting for magmatism.

Engaging in a high-gain win-win challenge, MATRICs will either overturn or finally validate untested paradigms about the tectonic forcing of Cenozoic climate. In either case, the knowledge produced about the geological carbon cycle will allow us to better assess the drivers of natural climate variability and, by comparison, the climatic consequences of current anthropic emissions.

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Topic(s)

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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-2024-COG

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Host institution

UNIVERSITA' DEGLI STUDI DI MILANO-BICOCCA
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.

€ 1 999 968,75
Address
PIAZZA DELL'ATENEO NUOVO 1
20126 Milano
Italy

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Region
Nord-Ovest Lombardia Milano
Activity type
Higher or Secondary Education Establishments
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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.

€ 1 999 968,75

Beneficiaries (1)

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