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Statistical geochemistry reveals disruption in secular lithospheric evolution about 2.5 Gyr ago

Author

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  • C. Brenhin Keller

    (Princeton University)

  • Blair Schoene

    (Princeton University)

Abstract

Statistical sampling of a large geochemical database reveals a pervasive discontinuity about 2.5 billion years ago, indicating marked changes in mantle and deep-crustal melting, and providing a link between deep Earth processes and the rise of atmospheric oxygen on the Earth.

Suggested Citation

  • C. Brenhin Keller & Blair Schoene, 2012. "Statistical geochemistry reveals disruption in secular lithospheric evolution about 2.5 Gyr ago," Nature, Nature, vol. 485(7399), pages 490-493, May.
    • Handle: RePEc:nat:nature:v:485:y:2012:i:7399:d:10.1038_nature11024
    DOI: 10.1038/nature11024
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    Cited by:

    1. Di-Cheng Zhu & Qing Wang & Roberto F. Weinberg & Peter A. Cawood & Sun-Lin Chung & Yong-Fei Zheng & Zhidan Zhao & Zeng-Qian Hou & Xuan-Xue Mo, 2022. "Interplay between oceanic subduction and continental collision in building continental crust," Nature Communications, Nature, vol. 13(1), pages 1-10, December.
    2. Guoxiong Chen & Qiuming Cheng & Timothy W. Lyons & Jun Shen & Frits Agterberg & Ning Huang & Molei Zhao, 2022. "Reconstructing Earth’s atmospheric oxygenation history using machine learning," Nature Communications, Nature, vol. 13(1), pages 1-13, December.
    3. Pitcher, Bradley W & Kent, Adam J.R., 2018. "Statistics and segmentation: Using Big Data to assess Cascades Arc compositional variability," Earth Arxiv 6xq3w, Center for Open Science.
    4. Bo Huang & Man Liu & Timothy M. Kusky & Tim E. Johnson & Simon A. Wilde & Dong Fu & Hao Deng & Qunye Qian, 2023. "Changes in orogenic style and surface environment recorded in Paleoproterozoic foreland successions," Nature Communications, Nature, vol. 14(1), pages 1-14, December.

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