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New study reveals surprising clues about the beginning of subduction on Earth

Unlocking Earth's deep past
Olivine cumulate from the Weltevreden Formation showing that although these cumulates are significantly altered, they still contain preserved unaltered olivine cores (microscopic image taken in plane-polarized light). Credit: Nature Communications (2025). DOI: 10.1038/s41467-025-59024-6

Subduction, a crucial geological process on Earth, may have begun hundreds of millions of years earlier than traditionally believed.

This surprising discovery comes from a new study by researchers from GFZ Helmholtz Centre for Geosciences, along with international colleagues, in Nature Communications. The team from Potsdam (Germany), Grenoble (France), and Madison (USA) presents groundbreaking evidence that subduction and continental crust formation during the so-called Hadean Eon were already active and more vigorous than previously thought.

The Hadean Eon, spanning from 4.6 to 4.0 billion years ago, remains the most enigmatic chapter in Earth's history. It began with the planet's formation, followed by a massive collision with a Mars-sized body that led to the creation of the moon and the complete melting of Earth's interior. Solidification of Earth's crust began around 4.5 billion years ago, but what happened next has long been debated.

The prevailing theory suggests that until at least the end of the Hadean, Earth was locked in a "stagnant lid" tectonic regime. In this , our planet was covered by a rigid, immobile outer shell, with convection processes occurring beneath it in Earth's mantle—lacking the subduction, i.e. the downward sinking of crust into Earth's interior, and continental crust formation seen in modern plate tectonics.

Now, researchers are challenging that view.

In their new study, the team presents evidence that subduction and continental formation were already active and more vigorous in the Hadean than previously thought. Using an innovative analytical technique, the Grenoble team measured strontium isotopes and in melt inclusions preserved within 3.3-billion-year-old olivine crystals. Meanwhile, the GFZ team used cutting-edge geodynamic simulations to interpret these geochemical signals in terms of early Earth processes.

Their combined findings suggest a much more active early Earth, indicating that extensive and continent formation may have started hundreds of millions of years earlier than previously believed.

More information: Adrien Vezinet et al, Growth of continental crust and lithosphere subduction in the Hadean revealed by geochemistry and geodynamics, Nature Communications (2025).

Journal information: Nature Communications

Citation: New study reveals surprising clues about the beginning of subduction on Earth (2025, August 7) retrieved 13 October 2025 from /news/2025-08-reveals-clues-subduction-earth.html
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