Beryllium isotopes in maar lake sediments respond to rapid climate change since the last deglaciation

Ye Yang , Zhenping Cao , Zhaoyan Gu , Guoqiang Chu , Hai Xu , Kejun Dong , Cong-Qiang Liu , Sheng Xu

Geoscience Frontiers ›› 2025, Vol. 16 ›› Issue (6) : 102158

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Geoscience Frontiers ›› 2025, Vol. 16 ›› Issue (6) :102158 DOI: 10.1016/j.gsf.2025.102158
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Beryllium isotopes in maar lake sediments respond to rapid climate change since the last deglaciation
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Abstract

The timing, amplitude, and mechanisms of rapid climate changes since the last deglaciation remain elusive in East Asia. In this study, high-resolution beryllium isotope and major element records from the annually laminated sediments of maar lake Xiaolongwan—a small, hydrologically closed basin with homogeneous lithology in northeastern China—offer new insights into East Asian climate variability. Abrupt increases in Al/Mg, Ca/Mg, and Ti/Mg ratios indicate intensified aeolian dust input at the onset of the Bølling-Allerød interstadial and the Early-Mid Holocene, synchronous with enhanced East Asian summer monsoon precipitation. Combined with previous dust provenance analyses, we infer a seasonal pattern of dust transport from the Central Asian deserts by southwesterly winds in spring to early summer, prior to peak monsoon rainfall. The 10 Be/ 9 Be record exhibits sharp declines that correspond closely to the timing of Dansgaard-Oeschger and Bond events in the North Atlantic. Spectral analysis reveals ∼ 1700-yr periodicity in the 10 Be/ 9 Be record, consistent with millennial-scale variability observed in the North Atlantic. These findings highlight a persistent climate teleconnection between East Asia and the North Atlantic and demonstrate that coupled dust and hydroclimate signals in maar lake sediments can reliably track sub-orbital climate variability.

Keywords

East Asian monsoon / 10 Be/9 Be ratio / Rapid climate change / Aeolian dust / Maar lake sediment

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Ye Yang, Zhenping Cao, Zhaoyan Gu, Guoqiang Chu, Hai Xu, Kejun Dong, Cong-Qiang Liu, Sheng Xu. Beryllium isotopes in maar lake sediments respond to rapid climate change since the last deglaciation. Geoscience Frontiers, 2025, 16(6): 102158 DOI:10.1016/j.gsf.2025.102158

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CRediT authorship contribution statement

Ye Yang: Writing - review & editing, Writing - original draft, Visualization, Software, Methodology, Funding acquisition, Data curation. Zhenping Cao: Writing - original draft, Visualization, Methodology, Formal analysis. Zhaoyan Gu: Writing - review & editing, Resources, Investigation. Guoqiang Chu: Writing - review & editing, Resources, Investigation, Funding acquisition. Hai Xu: Writing - review & editing. Kejun Dong: Writing - review & editing, Data curation. Cong-Qiang Liu: Writing - review & editing, Supervision. Sheng Xu: Writing - review & editing, Supervision, Resources, Project administration, Funding acquisition, Conceptualization.

Declaration of competing interest

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Acknowledgements

This work was supported by the National Natural Science Foundation of China (Grant Nos. 42361144879, 42030507, and 42303063), the Tianjin Natural Science Foundation (22JCQNJC00140), and the Postdoctoral Research Foundation of China (2023M732581). Y.Y. was supported by the Science and Technology Innovation Project for Training Leading Talents of the Tianjin University.

Appendix A. Supplementary data

Supplementary data to this article can be found online at https://doi.org/10.1016/j.gsf.2025.102158.

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