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<p>Voluminous felsic continental crust is, as far as we know, unique to Earth, yet the timescales of its earliest growth remain debated. Archean mantle evolution is complementary to crustal growth but is largely unconstrained for strontium isotopes due widespread Rb-Sr disturbance. Here, we perform high spatial resolution radiogenic Sr and Ca isotope measurements in magmatic plagioclase megacrysts from 3.7–2.8 Ga Archean anorthosites and leucogabbros. We report mantle-like Ca isotope signatures and the most unradiogenic terrestrial <sup>87</sup>Sr/<sup>86</sup>Sr ratio yet measured on Earth, in plagioclase (<sup>87</sup>Sr/<sup>86</sup>Sr<sub>initial</sub> = 0.700050 ± 0.000017, 95% confidence interval) from the 3.73 Ga Manfred Complex of the Narryer Terrane, Western Australia. These data are consistent with <sup>87</sup>Sr/<sup>86</sup>Sr homogenisation between the Earth and Moon (<sup>87</sup>Sr/<sup>86</sup>Sr<sub>initial</sub> ≈ 0.699061) at ca. 4.515 Ga during the Moon-forming giant impact. The appearance of a depleted mantle signature in the terrestrial strontium record post-3.5 Ga suggests that extensive continental growth began relatively late.</p>

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Coupled strontium-calcium isotopes in Archean anorthosites reveal a late start for mantle depletion

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  • 发表日期：

    2025年10月31日

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  • Matilda Boyce,
  • Anthony Kemp,
  • Chris Fisher,
  • Dan Bevan,
  • Aleksey Sadekov,
  • Jamie Lewis,
  • Simon Wilde,
  • Tim Ivanic,
  • Tim Elliott

摘要

Voluminous felsic continental crust is, as far as we know, unique to Earth, yet the timescales of its earliest growth remain debated. Archean mantle evolution is complementary to crustal growth but is largely unconstrained for strontium isotopes due widespread Rb-Sr disturbance. Here, we perform high spatial resolution radiogenic Sr and Ca isotope measurements in magmatic plagioclase megacrysts from 3.7–2.8 Ga Archean anorthosites and leucogabbros. We report mantle-like Ca isotope signatures and the most unradiogenic terrestrial 87Sr/86Sr ratio yet measured on Earth, in plagioclase (87Sr/86Srinitial = 0.700050 ± 0.000017, 95% confidence interval) from the 3.73 Ga Manfred Complex of the Narryer Terrane, Western Australia. These data are consistent with 87Sr/86Sr homogenisation between the Earth and Moon (87Sr/86Srinitial ≈ 0.699061) at ca. 4.515 Ga during the Moon-forming giant impact. The appearance of a depleted mantle signature in the terrestrial strontium record post-3.5 Ga suggests that extensive continental growth began relatively late.