Variation of the Asian summer monsoon during the MIS 5a/5b period inferred from a new high-resolution stalagmite record

ZHANG Taotao; LI Tingyong; HAN Liyin; CHENG Hai; LI Junyun; ZHAO Xin; ZHOU Jingli

doi:10.11932/karst20170202

Volume 36 Issue 2

Apr. 2017

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Article Navigation > CARSOLOGICA SINICA > 2017 > 36(2): 162-170

ZHANG Taotao, LI Tingyong, HAN Liyin, CHENG Hai, LI Junyun, ZHAO Xin, ZHOU Jingli. Variation of the Asian summer monsoon during the MIS 5a/5b period inferred from a new high-resolution stalagmite record[J]. CARSOLOGICA SINICA, 2017, 36(2): 162-170. doi: 10.11932/karst20170202

Citation:

ZHANG Taotao, LI Tingyong, HAN Liyin, CHENG Hai, LI Junyun, ZHAO Xin, ZHOU Jingli. Variation of the Asian summer monsoon during the MIS 5a/5b period inferred from a new high-resolution stalagmite record[J]. CARSOLOGICA SINICA, 2017, 36(2): 162-170. doi: 10.11932/karst20170202

Citation:

ZHANG Taotao, LI Tingyong, HAN Liyin, CHENG Hai, LI Junyun, ZHAO Xin, ZHOU Jingli. Variation of the Asian summer monsoon during the MIS 5a/5b period inferred from a new high-resolution stalagmite record[J]. CARSOLOGICA SINICA, 2017, 36(2): 162-170. doi: 10.11932/karst20170202

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Variation of the Asian summer monsoon during the MIS 5a/5b period inferred from a new high-resolution stalagmite record

doi: 10.11932/karst20170202

1.
Chongqing Key Laboratory of Karst Environment, School of Geographical Sciences, Southwest University/Field Scientific Observation & Research Base of Karst Eco-environments at Nanchuan in Chongqing, Ministry of Land and Resources of China/Institute of Karst Geology, CAGS/Key Laboratory of Karst Dynamics,MLR & GZAR
2.
Chongqing Key Laboratory of Karst Environment, School of Geographical Sciences, Southwest University
3.
Institute of Global Environmental Change, Xi’an Jiaotong University

Publish Date: 2017-04-25

Abstract

Abstract

Due to the paucity of the high-resolution records of the Asian summer monsoon (ASM) during the marine isotope stage (MIS) 5, our understanding about the ASM in this period is limited. In this study, a 38-yr resolution stalagmite oxygen isotope record from the Yangkou Cave, Chongqing, southwestern China, is used to reconstruct the detailed evolution of the ASM during the period of MIS 5a/5b. The Yangkou record exhibits a close correlation between the ASM and the climate of the North Atlantic at a centennial-millennial-scale. In terms of the precise 230Th dating with error less than 0.4%, the onset and termination of Chinese Interstadial (CIS) 22 are constrained to 91.2±0.3 ka BP and 88.9±0.3 ka BP, respectively, and the beginning of the CIS 21 is defined at 84.6±0.3 ka BP. In addition, the evolution pattern of CIS 22 and CIS 21 recorded in the stalagmite from the Yangkou Cave is slightly different from those recorded in NGRIP,which is anti-phased with the trend of temperature change in the Antarctica. We speculate that the ASM during MIS 5a/5b may be affected by climate variation in the southern hemisphere.
- Asian summer monsoon,
- stalagmite δ18O,
- marine isotope stage 5a/5b,
- 230Th dating,
- climate change in the southern hemisphere

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References

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