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Spatial patterns of Holocene temperature changes over mid-latitude Eurasia

Author

Listed:
  • Jiawei Jiang

    (The University of Hong Kong)

  • Bowen Meng

    (The University of Hong Kong
    Research Institute of Petroleum Exploration and Development, PetroChina)

  • Huanye Wang

    (State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Center for Excellence in Quaternary Science and Global Change, Chinese Academy of Sciences)

  • Hu Liu

    (State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Center for Excellence in Quaternary Science and Global Change, Chinese Academy of Sciences)

  • Mu Song

    (The University of Hong Kong)

  • Yuxin He

    (Zhejiang University)

  • Cheng Zhao

    (Nanjing University)

  • Jun Cheng

    (Nanjing University of Information Science and Technology)

  • Guoqiang Chu

    (Institute of Geology and Geophysics, Chinese Academy of Sciences)

  • Sergey Krivonogov

    (Southwest Jiaotong University)

  • Weiguo Liu

    (State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Center for Excellence in Quaternary Science and Global Change, Chinese Academy of Sciences)

  • Zhonghui Liu

    (The University of Hong Kong
    The University of Hong Kong)

Abstract

The Holocene temperature conundrum, the discrepancy between proxy-based Holocene global cooling and simulated global annual warming trends, remains controversial. Meanwhile, reconstructions and simulations show inconsistent spatial patterns of terrestrial temperature changes. Here we report Holocene alkenone records to address spatial patterns over mid-latitude Eurasia. In contrast with long-term cooling trends in warm season temperatures in northeastern China, records from southwestern Siberia are characterized by colder conditions before ~6,000 years ago, thus long-term warming trends. Together with existing records from surrounding regions, we infer that colder airmass might have prevailed in the interior of mid-latitude Eurasian continent during the early to mid-Holocene, perhaps associated with atmospheric response to remnant ice sheets. Our results challenge the proposed seasonality bias in proxies and modeled spatial patterns in study region, highlighting that spatial patterns of Holocene temperature changes should be re-considered in record integrations and model simulations, with important implications for terrestrial hydroclimate changes.

Suggested Citation

  • Jiawei Jiang & Bowen Meng & Huanye Wang & Hu Liu & Mu Song & Yuxin He & Cheng Zhao & Jun Cheng & Guoqiang Chu & Sergey Krivonogov & Weiguo Liu & Zhonghui Liu, 2024. "Spatial patterns of Holocene temperature changes over mid-latitude Eurasia," Nature Communications, Nature, vol. 15(1), pages 1-10, December.
    • Handle: RePEc:nat:natcom:v:15:y:2024:i:1:d:10.1038_s41467-024-45883-y
    DOI: 10.1038/s41467-024-45883-y
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    References listed on IDEAS

    as
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    2. Jeremiah Marsicek & Bryan N. Shuman & Patrick J. Bartlein & Sarah L. Shafer & Simon Brewer, 2018. "Reconciling divergent trends and millennial variations in Holocene temperatures," Nature, Nature, vol. 554(7690), pages 92-96, February.
    3. Samantha Bova & Yair Rosenthal & Zhengyu Liu & Shital P. Godad & Mi Yan, 2021. "Seasonal origin of the thermal maxima at the Holocene and the last interglacial," Nature, Nature, vol. 589(7843), pages 548-553, January.
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