A new analysis of the metstones of magmatic iron challenges traditional theories about why Earth and Mars are depleted with moderately volatile elements.
Medium volatile elements (MVEs) such as copper and zinc play an important role in planetary chemistry with essential elements of life, such as water, carbon, and nitrogen.
Understanding its origins provides important clues as to why the Earth has become a habitable world.
Earth and Mars contain significantly fewer MVEs than primitive metstones (chondrites), raising basic questions about the planetary layer.
This new study employs a new approach by analyzing iron meteorites (the metal core remnants of the earliest planetary building blocks) to reveal new insights.
“We’ve seen a lot of experience in the world,” said Dr. Damanveer Grewal, a researcher at Arizona State University.
“This discovery reconstructs our understanding of how the planet acquired its components.”
Until now, scientists believed that MVE was lost because they were not completely condensed in the early solar system or escaped during planetary differentiation.
However, new research reveals a different story. It is held by many MVEs on the first planet, suggesting that the building blocks of Earth and Mars later lost theirs.
Surprisingly, the authors discovered that many inner solar system planets retain abundance of MVEs like chondrites, and accretion continues despite being differentiated. It indicates that it has been saved.
This was not because Earth and Mars ancestors began to deplete with these elements, but instead occurred in the long history of collision growth, rather than incomplete condensation of solar nebulae or planet differentiation. Suggests that.
“Our work redefines how we understand the chemical evolution of planets,” Dr. Grewal said.
“It shows that the components of Earth and Mars were originally rich in these vital elements, but the intense collisions during the planet’s growth caused depletion.”
study Published in the journal Advances in Science.
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Damanveer S. Grewal et al. 2025. Enrichment of moderate volatile elements in first-generation planets of the inner solar system. Advances in Science 11 (6); doi:10.1126/sciadv.adq7848
Source: www.sci.news