Moon’s Origin Tied to Inner Solar System Collision

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A groundbreaking study published in Science confirms that Theia – the ancient planet that collided with Earth to form the Moon – originated much closer to the Sun than previously thought. This research resolves a long-standing mystery surrounding the Moon’s composition, which has long puzzled scientists with its striking similarity to Earth’s. The findings suggest Theia formed within the inner Solar System, sharing a common origin with our planet rather than originating from the outer regions as some earlier theories proposed.

The Mystery of the Moon’s Composition

For decades, the prevailing “giant impact” theory stated that the Moon formed from debris ejected after Theia collided with early Earth. This model predicted significant compositional differences between Earth and the Moon, assuming most of the lunar material came from Theia. However, samples from Apollo missions revealed a surprising truth: the Moon’s chemistry is remarkably similar to Earth’s, far more than expected if it were primarily composed of another planet’s remains. This raised critical questions about Theia’s origin and composition.

Tracing Theia’s Fingerprints

Researchers led by Thorsten Kleine of the Max Planck Institute for Solar System Research tackled this puzzle by analyzing terrestrial and lunar rocks, focusing on isotopes of iron, molybdenum, and zirconium. These elements act as “fingerprints,” revealing where a celestial body formed. The team discovered subtle variations in these isotopes that indicated Theia likely held 5-10% of Earth’s mass and contained higher concentrations of heavy elements, like molybdenum, consistent with formation in the hotter, inner Solar System.

Inner Solar System Origins Confirmed

The team’s analysis of 15 terrestrial and 6 lunar samples, combined with data from 20 meteorites, provided strong evidence for Theia’s inner Solar System origin. The study builds on previous work demonstrating that bodies closer to the Sun accumulate more heavy elements. Earth itself exhibits slightly elevated levels of molybdenum and zirconium, suggesting these were delivered by Theia during the catastrophic collision.

“The authors make new iron isotope measurements at exceptional levels of precision,” notes planetary scientist Sara Russell, reinforcing the study’s rigor and importance.

Implications for Earth’s Evolution

The discovery has implications beyond the Moon’s origin. It helps refine our understanding of Earth’s early formation and the processes that ultimately made it habitable. The impact with Theia wasn’t just a destructive event; it fundamentally reshaped our planet and created the conditions for life as we know it.

The research team plans to further refine their models through simulations and additional isotope analysis of lunar samples. The story of Theia and the Moon remains an ongoing investigation, with each new discovery bringing us closer to understanding the violent, yet ultimately creative, forces that shaped our Solar System.

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