Growth of continental crust and lithosphere subduction in the Hadean revealed by geochemistry and geodynamics

The rates of continental crust growth and recycling on early Earth remain unclear due to the lack of information resulting from the extensive alteration of ancient rocks. Melt inclusions trapped and shielded from alteration in Archean high-Mg olivine crystals offer a solution to this problem. We report an unprecedented unradiogenic Sr mantle source component (<sup>87</sup>Sr/<sup>86</sup>Sr = 0.69932 ± 0.00024, 95% confidence interval) of melts included in olivine from 3.27 Ga komatiitic lava flows in the Barberton Greenstone Belt, South Africa. This component indicates a model age of 4.31 ± 0.19 Ga and significant chemical fractionation (Nb/U = 36.9 ± 1.5, Ce/Pb=16.7 ± 1.1), suggesting up to 80% ± 16% of the present-day continental crust's mass was extracted by the late Hadean from the whole mantle. Geodynamic models support this finding, explaining geochemical data by producing 40% to 70% of the present-day continental crust mass during the Hadean in a variable tectonic regime with tens of millions of years-long periods of massive impulsive subduction induced by mantle plumes.

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Publication Details

Journal
Nature Communications
Published
2025-04-25
DOI
https://doi.org/10.1038/s41467-025-59024-6
Citations
9
Primary Topic
Geological and Geochemical Analysis
Type
article
Field-Weighted Citation Impact
16.80
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article

Growth of continental crust and lithosphere subduction in the Hadean revealed by geochemistry and geodynamics

Nicholas Arndt, Valentina Batanova, Evgeny Asafov, А В Чугунов et al.
9 citations
Nature Communications
Geological and Geochemical Analysis
16.80
article

Growth of continental crust and lithosphere subduction in the Hadean revealed by geochemistry and geodynamics

Nicholas Arndt, Valentina Batanova, Evgeny Asafov, А В Чугунов, A. N. Koshlyakova, Charitra Jain, S. V. Sobolev, А. В. Соболев, Adrien Vezinet, John W. Valley, Leonid V. Danyushevsky
article en
9 citations

Abstract

The rates of continental crust growth and recycling on early Earth remain unclear due to the lack of information resulting from the extensive alteration of ancient rocks. Melt inclusions trapped and shielded from alteration in Archean high-Mg olivine crystals offer a solution to this problem. We report an unprecedented unradiogenic Sr mantle source component (<sup>87</sup>Sr/<sup>86</sup>Sr = 0.69932 ± 0.00024, 95% confidence interval) of melts included in olivine from 3.27 Ga komatiitic lava flows in the Barberton Greenstone Belt, South Africa. This component indicates a model age of 4.31 ± 0.19 Ga and significant chemical fractionation (Nb/U = 36.9 ± 1.5, Ce/Pb=16.7 ± 1.1), suggesting up to 80% ± 16% of the present-day continental crust's mass was extracted by the late Hadean from the whole mantle. Geodynamic models support this finding, explaining geochemical data by producing 40% to 70% of the present-day continental crust mass during the Hadean in a variable tectonic regime with tens of millions of years-long periods of massive impulsive subduction induced by mantle plumes.

Nature CommunicationsVol. 16(1)
Centre National de la Recherche Scientifique (FR), University of Wisconsin System (US), Russian Academy of Sciences (RU), University of Wisconsin–Madison (US), University of Potsdam (DE), Friends United (US), Institut des Sciences de la Terre (FR), GFZ Helmholtz Centre for Geosciences (DE), Université Gustave Eiffel (FR), V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry (RU), Institut de Recherche pour le Développement (FR), Université Savoie Mont Blanc (FR), Université Grenoble Alpes (FR)
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Openalex Percentile: Top 1%
Geological and Geochemical Analysis
16.80
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