Millennial‐Scale Temperature Evolution in East Asia During the Last Glacial: Constraints from Speleothem Δ <sub>47</sub> Thermometry

Abstract Millennial‐scale events of the last glaciation profoundly reorganized global climate, yet the terrestrial temperature response in East Asia remains debated due to the seasonal biases and calibration uncertainties inherent in biological proxies. To address this, we present a carbonate clumped isotope (Δ 47 ) record from a central Chinese speleothem spanning the Last Glacial Maximum (LGM) and Heinrich Stadial 1 (HS1). Supported by petrographic and trace element evidence for negligible kinetic effects, our temperature record from the thermally buffered cave provides a robust reconstruction of mean annual temperature. We identify a ∼6°C cooling compared to the present during the LGM, intensified by an additional ∼2°C cooling during HS1. These results contradict warming signals found in precious study but align with iTraCE simulations, which attribute HS1 cooling to severe winter temperature drops partially offset by insolation‐driven summer warming. Our findings reconcile current proxy–model temperature discrepancies and improve the climatic interpretation of speleothem δ 18 O during Heinrich stadials.

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Journal
Journal of Geophysical Research Atmospheres
Published
2026-04-11
DOI
https://doi.org/10.1029/2025jd046164
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00

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article

Millennial‐Scale Temperature Evolution in East Asia During the Last Glacial: Constraints from Speleothem Δ 47 Thermometry

Biao Chang, Michael L. Griffiths, William F. Defliese, Shufang Yuan et al.
Journal of Geophysical Research Atmospheres
Geology and Paleoclimatology Research
article

Millennial‐Scale Temperature Evolution in East Asia During the Last Glacial: Constraints from Speleothem Δ 47 Thermometry

Biao Chang, Michael L. Griffiths, William F. Defliese, Shufang Yuan, Yitao Liu, Genming Luo, Shucheng Xie, Xinzhu Ning, Tianyu Zhou, Shuyu Xue, Junhua Huang, Ke Lin, Zhen Xu, Wei Guo, Xianfeng Wang, Shitou Wu
article en

Abstract

Abstract Millennial‐scale events of the last glaciation profoundly reorganized global climate, yet the terrestrial temperature response in East Asia remains debated due to the seasonal biases and calibration uncertainties inherent in biological proxies. To address this, we present a carbonate clumped isotope (Δ 47 ) record from a central Chinese speleothem spanning the Last Glacial Maximum (LGM) and Heinrich Stadial 1 (HS1). Supported by petrographic and trace element evidence for negligible kinetic effects, our temperature record from the thermally buffered cave provides a robust reconstruction of mean annual temperature. We identify a ∼6°C cooling compared to the present during the LGM, intensified by an additional ∼2°C cooling during HS1. These results contradict warming signals found in precious study but align with iTraCE simulations, which attribute HS1 cooling to severe winter temperature drops partially offset by insolation‐driven summer warming. Our findings reconcile current proxy–model temperature discrepancies and improve the climatic interpretation of speleothem δ 18 O during Heinrich stadials.

Journal of Geophysical Research AtmospheresVol. 131(8)
William Paterson University (US), The University of Queensland (AU), Nanyang Technological University (SG), Chinese Academy of Sciences (CN), China University of Geosciences (CN), Earth Observatory of Singapore (SG), Institute of Geology and Geophysics (CN), Institute of Earth Environment (CN), Xi'an Jiaotong University (CN)
National Natural Science Foundation of China, China Scholarship Council
Climate action
Openalex Percentile: Top 17%
Geology and Paleoclimatology Research
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