New Study Of Earth’s Crust Shows Global Growth Spurt Three Billion Years Ago

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A melt water stream in Greenland carrying ancient zircon crystals.
Credit; Curtin University

The findings not only advance an understanding of the production of the Earth’s crust through deep time, along with its structure and composition, but reveal a planet-wide crustal growth spurt three billion years ago when mantle temperatures peaked.

Lead author Professor Chris Kirkland, from Curtin University’s Timescales of Mineral Systems Group, said the research used the chemistry of old crystals preserved within stream sediments in arctic Greenland to test the idea that portions of ancient crust served as seeds for later growth of continents.

“We found there was a widespread bloom in crust production three billion years ago, during a peak in mantle temperatures,” Professor Kirkland said.

“Three-billion-year-old magmas from the mantle had penetrated even more ancient four-billion-year-old crust to create rocks of mixed composition.

“Old crust appeared to be critical in continent production as it acted much like a life raft to preserve crust through later stages of earth history.

“The spike in the age of crust production in Greenland matches other regions across the globe and points to a significant widespread event that formed crust relatively early in the history of our planet.”

Professor Kirkland said understanding the production of crust improved the understanding of its structure and composition.

“The Earth’s crust hosts concentrations of economically valuable ores and minerals but finding them is becoming increasingly challenging as more near-surface deposits are exhausted,” Professor Kirkland said.

“Understanding that later crust is ‘seeded’ on older pre-existing crust refines our understanding of the generation of where certain metals are hosted and ultimately explains the habitable part of our planet.”

Funded by the Greenland Ministry of Mineral Resources, the full research paper, ‘Widespread reworking of Hadean-to-Eoarchean continents during Earth’s thermal peak,’ was published in Nature Communications and can be found online here.

Contacts and sources:
Lucien Wilkinson