image: 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: A. Vezinet et al., Nature Communications 2025
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 model, 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 the Earth’s interior, and continental crust formation seen in modern plate tectonics.
Now, researchers from the ERC Synergy Grant Project “Monitoring Earth Evolution through Time” (MEET)—a collaboration between geochemists from Grenoble (France) and Madison (USA), and geodynamic modelers from GFZ Helmholtz Centre for Geosciences in Potsdam (Germany)—are challenging that view.
In their new study, published in Nature Communications, the MEET team presents evidence that subduction and continental crust 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 trace elements 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 subduction and continent formation may have started hundreds of millions of years earlier than previously believed.
Scientific contact: Prof Dr. Stephan Sobolev, stephan.sobolev@gfz-potsdam.de
Original study: A. Vezinet, A. V. Chugunov, A. V. Sobolev, C. Jain, S. V. Sobolev, V. G. Batanova, E. V. Asafov, A. N. Koshlaykova, N. T. Arndt, L. V. Danyushevsky, and J. W. Valley, Growth of continental crust and lithosphere subduction in the Hadean revealed by geochemistry and geodynamics, Nature Communications 2025, https://doi.org/10.1038/s41467-025-59024-6
Journal
Nature Communications
Method of Research
Experimental study
Subject of Research
Not applicable
Article Title
Growth of continental crust and lithosphere subduction in the Hadean revealed by geochemistry and geodynamics
Article Publication Date
25-Apr-2025
COI Statement
No conflicts of interested were declared