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Mid-latitudinal habitable environment for marine eukaryotes during the waning stage of the Marinoan snowball glaciation

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  • Huyue Song

    (China University of Geosciences)

  • Zhihui An

    (Wuhan Center of China Geological Survey)

  • Qin Ye

    (China University of Geosciences)

  • Eva E. Stüeken

    (University of St. Andrews)

  • Jing Li

    (China University of Geosciences)

  • Jun Hu

    (China University of Geosciences)

  • Thomas J. Algeo

    (China University of Geosciences
    China University of Geosciences
    University of Cincinnati)

  • Li Tian

    (China University of Geosciences)

  • Daoliang Chu

    (China University of Geosciences)

  • Haijun Song

    (China University of Geosciences)

  • Shuhai Xiao

    (Virginia Tech)

  • Jinnan Tong

    (China University of Geosciences)

Abstract

During the Marinoan Ice Age (ca. 654–635 Ma), one of the ‘Snowball Earth’ events in the Cryogenian Period, continental icesheets reached the tropical oceans. Oceanic refugia must have existed for aerobic marine eukaryotes to survive this event, as evidenced by benthic phototrophic macroalgae of the Songluo Biota preserved in black shales interbedded with glacial diamictites of the late Cryogenian Nantuo Formation in South China. However, the environmental conditions that allowed these organisms to thrive are poorly known. Here, we report carbon-nitrogen-iron geochemical data from the fossiliferous black shales and adjacent diamictites of the Nantuo Formation. Iron-speciation data document dysoxic-anoxic conditions in bottom waters, whereas nitrogen isotopes record aerobic nitrogen cycling perhaps in surface waters. These findings indicate that habitable open-ocean conditions were more extensive than previously thought, extending into mid-latitude coastal oceans and providing refugia for eukaryotic organisms during the waning stage of the Marinoan Ice Age.

Suggested Citation

  • Huyue Song & Zhihui An & Qin Ye & Eva E. Stüeken & Jing Li & Jun Hu & Thomas J. Algeo & Li Tian & Daoliang Chu & Haijun Song & Shuhai Xiao & Jinnan Tong, 2023. "Mid-latitudinal habitable environment for marine eukaryotes during the waning stage of the Marinoan snowball glaciation," Nature Communications, Nature, vol. 14(1), pages 1-9, December.
  • Handle: RePEc:nat:natcom:v:14:y:2023:i:1:d:10.1038_s41467-023-37172-x
    DOI: 10.1038/s41467-023-37172-x
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    References listed on IDEAS

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    1. Xianguo Lang & Bing Shen & Yongbo Peng & Shuhai Xiao & Chuanming Zhou & Huiming Bao & Alan Jay Kaufman & Kangjun Huang & Peter W. Crockford & Yonggang Liu & Wenbo Tang & Haoran Ma, 2018. "Transient marine euxinia at the end of the terminal Cryogenian glaciation," Nature Communications, Nature, vol. 9(1), pages 1-8, December.
    2. Jochen J. Brocks & Amber J. M. Jarrett & Eva Sirantoine & Christian Hallmann & Yosuke Hoshino & Tharika Liyanage, 2017. "The rise of algae in Cryogenian oceans and the emergence of animals," Nature, Nature, vol. 548(7669), pages 578-581, August.
    3. Benjamin W. Johnson & Simon W. Poulton & Colin Goldblatt, 2017. "Marine oxygen production and open water supported an active nitrogen cycle during the Marinoan Snowball Earth," Nature Communications, Nature, vol. 8(1), pages 1-10, December.
    4. Charles H. Wellman & Peter L. Osterloff & Uzma Mohiuddin, 2003. "Fragments of the earliest land plants," Nature, Nature, vol. 425(6955), pages 282-285, September.
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    Cited by:

    1. Trent B. Thomas & David C. Catling, 2024. "Three-stage formation of cap carbonates after Marinoan snowball glaciation consistent with depositional timescales and geochemistry," Nature Communications, Nature, vol. 15(1), pages 1-15, December.

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