Asian summer monsoon variability across Termination II and implications for ice age terminations

The detailed anatomy of Termination I (TI) is well depicted, but whether changes across Termination II (TII) resemble TI remains controversial. Here we present high-resolution Asian monsoon records covering TII using Shima Cave stalagmites from China. Correlating marine and ice-core records to our U/Th-dated records via millennial-scale variabilities, we find an initial CO<sub>2</sub> rise from 139 ± 1 ka BP concordant with boreal summer insolation increase, which was followed by a major rise phase of CO<sub>2</sub> between 135.7 ± 1 and 129 ± 1 ka BP. The major rise phases of CO<sub>2</sub> were comparable during TI and TII, but the initial CO<sub>2</sub> rise before TII was distinct from CO<sub>2</sub> behavior before TI, likely forced by the Earth's internal variabilities, in particular an ice-sheet collapse event and a 50% reduction in southern hemisphere dust flux. Here, we show that ~4000-5000-year-long gradual changes in CO<sub>2</sub>, along with insolation rise, preconditioned glacial terminations, supporting the "tipping point" theory.

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Publication Details

Journal
Nature Communications
Published
2025-05-30
DOI
https://doi.org/10.1038/s41467-025-60398-w
Citations
2
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
2.60

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article

Asian summer monsoon variability across Termination II and implications for ice age terminations

Zhenqiu Zhang, Hai Cheng, Qingfeng Shao, Yijia Liang et al.
2 citations
Nature Communications
Geology and Paleoclimatology Research
2.60
article

Asian summer monsoon variability across Termination II and implications for ice age terminations

Zhenqiu Zhang, Hai Cheng, Qingfeng Shao, Yijia Liang, Kan Zhao, Tyler E. Huth, Rob Edwards, Quan Wang, Yongjin Wang, Shitao Chen, Bin Zhao
article en
2 citations

Abstract

The detailed anatomy of Termination I (TI) is well depicted, but whether changes across Termination II (TII) resemble TI remains controversial. Here we present high-resolution Asian monsoon records covering TII using Shima Cave stalagmites from China. Correlating marine and ice-core records to our U/Th-dated records via millennial-scale variabilities, we find an initial CO<sub>2</sub> rise from 139 ± 1 ka BP concordant with boreal summer insolation increase, which was followed by a major rise phase of CO<sub>2</sub> between 135.7 ± 1 and 129 ± 1 ka BP. The major rise phases of CO<sub>2</sub> were comparable during TI and TII, but the initial CO<sub>2</sub> rise before TII was distinct from CO<sub>2</sub> behavior before TI, likely forced by the Earth's internal variabilities, in particular an ice-sheet collapse event and a 50% reduction in southern hemisphere dust flux. Here, we show that ~4000-5000-year-long gradual changes in CO<sub>2</sub>, along with insolation rise, preconditioned glacial terminations, supporting the "tipping point" theory.

Nature CommunicationsVol. 16(1)
University of Minnesota (US), Nantong University (CN), Washington University in St. Louis (US), University of Michigan (US), Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application (CN), Ningbo Polytechnic (CN), Xi'an Jiaotong University (CN)
National Natural Science Foundation of China, Jiangxi Normal University, Anhui Normal University
Life below water
Openalex Percentile: Top 12%
Geology and Paleoclimatology Research
2.60
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