Department of Earth and Planetary Sciences, Yale University, P.O. Box 208109, New Haven, CT, USA.
Sci Adv. 2023 Mar 24;9(12):eade2711. doi: 10.1126/sciadv.ade2711.
The onset and rates of continental growth are first-order indicators of early Earth dynamics, and whether substantial crust existed in the Hadean or much later has long been debated. Here, we present a theoretical analysis of published Hf and Nd isotopic data representing the depleted mantle and demonstrate that continental growth must have started in the early Hadean. Whereas the traditional interpretation of depleted mantle signatures in crustal rocks assumes unrealistic instantaneous mantle mixing, our modeling incorporates the effect of a finite mixing time over which these signatures are recorded in rocks produced through mantle melting. This effect is shown to delay, by as much as 0.65 to 0.75 billion years, the appearance of the earliest depleted mantle signatures in continental crust. Our results suggest that published observations of εHf, εNd, and μNd require Hadean growth of continental crust, with a minimum of 50% of today's continental volume already existing by the end of Hadean.
大陆增长的开始和速度是早期地球动力学的首要指标,而大量地壳是否存在于冥古宙或更晚的时期一直存在争议。在这里,我们对代表亏损地幔的已发表的 Hf 和 Nd 同位素数据进行了理论分析,并证明大陆增长必须在冥古宙早期开始。虽然地壳岩石中亏损地幔特征的传统解释假设瞬时地幔混合是不切实际的,但我们的模型考虑了在通过地幔熔融产生的岩石中记录这些特征的有限混合时间的影响。结果表明,这一效应将最早的亏损地幔特征出现在大陆地壳中的时间延迟了 0.65 到 0.75 亿年。我们的结果表明,已发表的 εHf、εNd 和 μNd 观测结果需要冥古宙大陆地壳的生长,到冥古宙末期,至少已经存在今天大陆体积的 50%。