Ancient Australian rocks reveal clues to Earth and Moon formation

Scientists have analyzed 3.7-billion-year-old rocks from Western Australia to uncover details about the early Earth and the Moon's origins. The study indicates that Earth's continents began forming around 3.5 billion years ago, long after the planet itself emerged. Comparisons with Apollo mission samples support the theory of a massive cosmic collision birthing the Moon.

In a new study published in Nature Communications, researchers led by PhD student Matilda Boyce from the University of Western Australia examined tiny feldspar crystals within anorthosites collected from the Murchison region. These rocks, dating back 3.7 billion years, are among the oldest known on the Australian continent and provide a preserved record of Earth's ancient mantle.

"The timing and rate of early crustal growth on Earth remains contentious due to the scarcity of very ancient rocks," Boyce noted. Using high-precision isotopic analysis on untouched parts of plagioclase feldspar crystals, the team found that significant continental growth did not start until approximately 3.5 billion years ago—about one billion years after Earth's formation around 4.5 billion years ago. This delay challenges previous assumptions about the rapid development of the planet's crust.

The findings also connect Earth's history to the Moon's. By comparing the Australian samples with lunar anorthosites returned by NASA's Apollo missions, the researchers observed a striking chemical similarity. "Anorthosites are rare rocks on Earth but very common on the Moon," Boyce explained. "Our comparison was consistent with the Earth and Moon having the same starting composition of around 4.5 billion years ago. This supports the theory that a planet collided with early Earth and the high-energy impact resulted in the formation of the Moon."

The research involved collaborators from the University of Bristol, the Geological Survey of Western Australia, and Curtin University, with funding from the Australian Research Council. These insights offer a clearer timeline for planetary evolution, highlighting how a catastrophic event shaped both worlds.

Articoli correlati

Harvard geoscientists have found the oldest direct evidence of plate tectonics on Earth, dating back 3.5 billion years. Analysis of ancient rocks from western Australia reveals early crustal drift and rotation. The discovery, published in Science, challenges notions of a rigid early planetary surface.

Riportato dall'IA

Researchers at Curtin University have developed a technique using krypton gas in microscopic zircon crystals to track the history of Earth's landscapes over millions of years. The method, which relies on cosmic rays striking surface minerals, reveals how erosion and sediment movement have shaped terrains in response to climate and tectonic changes. This approach could also aid in locating mineral deposits in Australia.

A new study suggests that Earth's early molten phase preserved water deep in its mantle through bridgmanite, preventing loss to space. Led by researchers at the Chinese Academy of Sciences, the findings explain how this hidden reservoir contributed to the planet's evolution into a water-rich world. Published in Science, the research challenges previous views on the mantle's dryness.

Riportato dall'IA

A recent analysis of clay pebbles from Mars' Jezero crater suggests the planet experienced a warm and wet climate during the Noachian epoch billions of years ago. This finding challenges the prevailing view of a cold and icy environment at that time. The evidence comes from NASA's Perseverance rover and points to conditions potentially suitable for life.

 

 

 

Questo sito web utilizza i cookie

Utilizziamo i cookie per l'analisi per migliorare il nostro sito. Leggi la nostra politica sulla privacy per ulteriori informazioni.
Rifiuta