资源环境科技发展态势分析平台

Subaerial continental crust plays a fundamental role in modulating the composition of the ocean, atmosphere, and biosphere, but the timing and rate of continental emergence above sea level remain unclear. Here we use the zircon oxygen isotopic compositions of early Paleoproterozoic metasediment-derived granitoids from the southwestern Yangtze Craton to constrain the rapidity of continental emergence. Statistical analyses of compiled igneous and detrital zircon oxygen isotopic database show a rapid increase in zircon δ¹⁸O at ∼2.36 Ga. We suggest that this isotopic shift is best explained by a significant increase of continental freeboard between ∼2.43 Ga and ∼2.36 Ga due to the increasing strength of the continental lithosphere since the late Archean, concomitantly yielding a high-δ¹⁸O sedimentary reservoir. Subsequent melting of these high-δ¹⁸O sediments in a variety of tectonic regimes results in high zircon δ¹⁸O.