A change in the geodynamics of continental growth 3 billion years ago

Bruno Dhuime, Chris J. Hawkesworth, Peter A. Cawood, Craig D. Storey

Research output: Contribution to journalArticleResearchpeer-review

641 Citations (Scopus)


Models for the growth of continental crust rely on knowing the balance between the generation of new crust and the reworking of old crust throughout Earth's history. The oxygen isotopic composition of zircons, for which uranium-lead and hafnium isotopic data provide age constraints, is a key archive of crustal reworking. We identified systematic variations in hafnium and oxygen isotopes in zircons of different ages that reveal the relative proportions of reworked crust and of new crust through time. Growth of continental crust appears to have been a continuous process, albeit at variable rates. A marked decrease in the rate of crustal growth at ∼3 billion years ago may be linked to the onset of subduction-driven plate tectonics.

Original languageEnglish
Pages (from-to)1334-1336
Number of pages3
Issue number6074
Publication statusPublished - 16 Mar 2012
Externally publishedYes

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