Rb and Sr variability within plagioclase from the 3.73 Ga Manfred Complex. Credit: Nature Communications (2025). DOI: 10.1038/s41467-025-64641-2
An analysis of feldspar crystals within the oldest magmatic rocks in Australia has provided a unique insight into Earth’s ancient mantle and continents, and the early beginnings of the moon.
Lead author and Ph.D. student Matilda Boyce collaborated with researchers from UWA’s School of Earth and Oceans, the University of Bristol, the Geological Survey of Wes…
Rb and Sr variability within plagioclase from the 3.73 Ga Manfred Complex. Credit: Nature Communications (2025). DOI: 10.1038/s41467-025-64641-2
An analysis of feldspar crystals within the oldest magmatic rocks in Australia has provided a unique insight into Earth’s ancient mantle and continents, and the early beginnings of the moon.
Lead author and Ph.D. student Matilda Boyce collaborated with researchers from UWA’s School of Earth and Oceans, the University of Bristol, the Geological Survey of Western Australia and Curtin University on the study published in Nature Communications.
Researchers examined 3.7-billion-year-old anorthosites from the Murchison region of Western Australia—the oldest rocks on the Australian continent and some of the oldest rocks on Earth.
“The timing and rate of early crustal growth on Earth remains contentious due to the scarcity of very ancient rocks,” Boyce said. “We used fine-scale analytical methods to isolate the fresh areas of plagioclase feldspar crystals, which record the isotopic ‘fingerprint’ of the ancient mantle.”
The results suggested the continents began to grow relatively late in Earth’s history, from around 3.5 billion years ago, which is 1 billion years after the planet formed. The study also compared the results with measurements of lunar anorthosites collected during NASA’s Apollo program.
“Anorthosites are rare rocks on Earth but very common on the moon,” Boyce said. “Our comparison was consistent with Earth and the 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.”
More information: Matilda Boyce et al, Coupled strontium-calcium isotopes in Archean anorthosites reveal a late start for mantle depletion, Nature Communications (2025). DOI: 10.1038/s41467-025-64641-2
Citation: Oldest rocks on Australian continent offer insight into origins of Earth and the moon (2025, November 3) retrieved 3 November 2025 from https://phys.org/news/2025-11-oldest-australian-continent-insight-earth.html
This document is subject to copyright. Apart from any fair dealing for the purpose of private study or research, no part may be reproduced without the written permission. The content is provided for information purposes only.