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Arctic zircon U-Pb ages reveal multiphase glaciations in East Siberia during the late Quaternary

Author

Listed:
  • Han Feng

    (Ministry of Natural Resources)

  • Zhengquan Yao

    (Ministry of Natural Resources
    Qingdao Marine Science and Technology Center
    Shandong (preparatory))

  • Xuefa Shi

    (Ministry of Natural Resources
    Qingdao Marine Science and Technology Center
    Shandong (preparatory))

  • Zhongshi Zhang

    (Peking University)

  • Huayu Lu

    (Nanjing University)

  • Hanzhi Zhang

    (Nanjing University)

  • Yanguang Liu

    (Ministry of Natural Resources
    Qingdao Marine Science and Technology Center
    Shandong University of Science and Technology)

  • Xin Shan

    (Ministry of Natural Resources
    Qingdao Marine Science and Technology Center)

  • Jiang Dong

    (Ministry of Natural Resources
    Qingdao Marine Science and Technology Center)

  • Linsen Dong

    (Ministry of Natural Resources
    Qingdao Marine Science and Technology Center)

  • Gongxu Yang

    (Ministry of Natural Resources)

  • Limin Hu

    (Qingdao Marine Science and Technology Center
    Ocean University of China)

  • Yuri Vasilenko

    (Far Eastern Branch of Russian Academy of Sciences)

  • Anatolii Astakhov

    (Far Eastern Branch of Russian Academy of Sciences)

  • Alexander Bosin

    (Far Eastern Branch of Russian Academy of Sciences)

Abstract

Tracing ice-rafted debris (IRD) in Arctic Ocean sediments is crucial for understanding the evolution of Northern Hemisphere ice cover. However, uncertainties in identifying the provenance of IRD across circum-Arctic shelves have complicated reconstructions of the East Siberian Ice Sheet (ESIS). Here, we present a provenance study using 10,111 detrital zircon U-Pb ages from circum-Arctic shelf sediments and central Arctic IRD. Our results reveal that a prominent ~90–110 Ma zircon peak serves as a distinctive fingerprint for East Siberian-sourced sediments. Central Arctic IRD from at least four glacial periods contains this signature, indicating repeated ESIS glaciation, likely within the past three glacial cycles. This multiphase glaciation of East Siberia exerted significant, though poorly understood, influences on both polar and global climates during the late Quaternary. Our findings provide valuable insights into the history of Northern Hemisphere glaciation and offer an effective approach for reconstructing ice sheet evolution.

Suggested Citation

  • Han Feng & Zhengquan Yao & Xuefa Shi & Zhongshi Zhang & Huayu Lu & Hanzhi Zhang & Yanguang Liu & Xin Shan & Jiang Dong & Linsen Dong & Gongxu Yang & Limin Hu & Yuri Vasilenko & Anatolii Astakhov & Ale, 2025. "Arctic zircon U-Pb ages reveal multiphase glaciations in East Siberia during the late Quaternary," Nature Communications, Nature, vol. 16(1), pages 1-12, December.
  • Handle: RePEc:nat:natcom:v:16:y:2025:i:1:d:10.1038_s41467-025-62499-y
    DOI: 10.1038/s41467-025-62499-y
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    References listed on IDEAS

    as
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