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Hydrothermal iron from the earth’s interior as fertiliser of photosynthesis in the ocean

Project description

The role of submarine volcanoes in ocean fertilisation

Plankton require iron to grow but this essential nutrient is scarce in many ocean regions and is traditionally thought to be delivered mainly by atmospheric dust. However, hydrothermal iron released from underwater volcanoes may represent a major, overlooked source of phytoplankton fertilisation. The ERC-funded HARVEST project investigates how iron emitted by shallow submarine volcanoes influences phytoplankton production and ocean ecosystems. Focusing on the Tonga volcanic arc, where large phytoplankton blooms occur within an iron-limited ocean, HARVEST will track how hydrothermal iron is released, transported and reaches surface waters. By combining field observations and modelling, the project will upscale these findings to assess the global role of submarine volcanic iron in ocean productivity and the carbon cycle.

Objective

HARVEST investigates how iron released from submarine volcanoes stimulates the growth of phytoplankton, especially in nutrient-poor ocean regions. Iron is known to be a limiting nutrient for photosynthesizing plankton, but research has mostly focused on iron delivery via atmospheric dust. The contribution of iron from hydrothermal sources – leached out of hot rock along the volcanically active plate boundaries – has been largely overlooked. This process, however, may drive a significant component of primary production in iron-limited ocean areas.

HARVEST addresses this critical knowledge gap through a holistic investigation of hydrothermal iron sources on the seafloor, and the mechanisms by which iron is transported to the ocean’s sunlit surface layer. A focus is on shallow seamounts in volcanic arcs and hotspots, which are hypothesised to have the most direct hydrothermal impact on surface waters, but remain the least studied. Measuring, modelling and comparing iron fluxes from shallow versus deep submarine sources, HARVEST advances from local through regional to global scales. Its main fieldwork area around Tonga-Lau features large and recurrent phytoplankton blooms, and the range of tectonically relevant settings. HARVEST will track iron-laden hydrothermal plumes, their dispersal, and their effects on phytoplankton, using ship-based surveys, autonomous vehicles and long-term moorings.

Dedicated ocean models with a biogeochemical compartment will simulate the transport of hydrothermal plumes on regional and global scales, away from their hydrothermal sources, and into the sunlit ocean layer. This will clarify the role of hydrothermal iron on primary production and on the carbon cycle in present and future climate scenarios. Thus HARVEST will reveal the overlooked contribution of submarine volcanism to ocean fertilisation, opening up new views into the interconnectedness of solid earth, oceans, and marine life.

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HORIZON-ERC-SYG - HORIZON ERC Synergy Grants

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Call for proposal

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(opens in new window) ERC-2025-SyG

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Host institution

CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE CNRS
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.

€ 10 892 132,50
Address
RUE MICHEL ANGE 3
75794 PARIS
France

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Region
Ile-de-France Ile-de-France Paris
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.

€ 11 089 727,00

Beneficiaries (3)

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