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Experimental Laboratory Magma Ocean

Project description

How early planet chemistry shapes habitability

In the early days of our planet, Earth’s surface was a fiery, molten expanse, steaming with gases that would later form the atmosphere. Key elements such as carbon, oxygen, hydrogen, sulfur, and nitrogen shaped the planet from the inside out, driving tectonics and creating conditions for habitability. The ERC-funded ELMO project aims to recreate these early ‘magma oceans’ in the lab to understand how volatile elements control atmospheric chemistry. By combining experiments with data from space missions such as BepiColombo, JWST, and ESA’s Ariel, researchers can link observed exoplanet atmospheres to the interiors of distant worlds. Comparing early Earth with these exoplanets will reveal how common Earth-like planets may be, offering new insights into the building blocks of habitable worlds across the universe.

Objective

Volatile chemical elements such as C, O, H, S, and N, are critical components in the formation and evolution of planets, control physical properties of planet interiors and associated processes such as plate tectonics, largely make up the composition of atmospheres, and determine planet habitability. Telescopic observations of exoplanets provide information about the atmospheres of planets, and the abundances of these volatile elements. However, we lack experimental constraints to reliably interpret atmosphere observations and link them to planet compositions. I propose a novel experimental approach that will provide a quantitative link of atmosphere chemistry and molecular speciation, to magma ocean composition.
All terrestrial planets have experienced a magma ocean stage early in their evolution. With my group I will study the role of volatile elements in this planetary stage, and how composition, and oxidation state of magma oceans control the molecular inventory of their atmospheres. This information is crucial to derive primordial atmosphere compositions of solar system planets and constrain their volatile inventories. The new data will be put in the context of ongoing and future European space missions, such as BepiColombo to Mercury, in which I am directly involved.
On the other hand, with the proposed experimental approach I will build a link from observed volatile species in exoplanet atmospheres to the compositions of the interiors of hot magma ocean worlds. The novel data will be directly integrated with observations from spectroscopic measurements of exoplanet atmospheres by JWST and the planned ESA Ariel mission to constrain planet compositions. By comparing the derived magma ocean atmosphere of Earth with the atmospheres of observed hot exoplanets, I will be able to assess how common systems like the early Earth are, beyond the solar system.

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(opens in new window) ERC-2025-STG

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Host institution

MAX-PLANCK-GESELLSCHAFT ZUR FORDERUNG DER WISSENSCHAFTEN EV
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.

€ 1 495 520,00
Address
HOFGARTENSTRASSE 8
80539 MUNCHEN
Germany

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Region
Bayern Oberbayern München, Kreisfreie Stadt
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.

€ 1 495 520,00

Beneficiaries (1)

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