The Holocene climatic evolution in Eastern China and its bearing on climatic events

WANG Jiangyue; BAI Weiming; WANG Zhaobo; WANG Minghui; LI Baojie

doi:10.16562/j.cnki.0256-1492.2021122001

2022 Vol. 42, No. 2

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Article navigation > Marine Geology & Quaternary Geology > 2022 > 42(2): 167-177

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WANG Jiangyue, BAI Weiming, WANG Zhaobo, WANG Minghui, LI Baojie. The Holocene climatic evolution in Eastern China and its bearing on climatic events[J]. Marine Geology & Quaternary Geology, 2022, 42(2): 167-177. doi: 10.16562/j.cnki.0256-1492.2021122001

Citation:

WANG Jiangyue, BAI Weiming, WANG Zhaobo, WANG Minghui, LI Baojie. The Holocene climatic evolution in Eastern China and its bearing on climatic events[J]. Marine Geology & Quaternary Geology, 2022, 42(2): 167-177. doi: 10.16562/j.cnki.0256-1492.2021122001

The Holocene climatic evolution in Eastern China and its bearing on climatic events

1.
Key Laboratory of Gold Mineralization Processes and Resource Utilization, MNR; Shandong Provincial Key Laboratory of Metallogenic Geological Process and Resource Utilization, Jinan 250013, China
2.
The University of Sheffield, Sheffield S10 2TN, UK, England
3.
Qingdao Institute of Marine Geology, CGS,Qingdao 266237, China
4.
Yimeng National Geological Park Management Office, Linyi 273304, China
5.
Shandong Compass Mineral Exploration co., Ltd, Linyi 276006, China

More Information

Corresponding author: BAI Weiming, qdbwm@163.com

Received Date: 20 December 2021

Revised Date: 14 February 2022

Accepted Date: 14 February 2022

Publish Date: 28 April 2022

Abstract

Abstract

Based on the Holocene climate evolution curve constructed with the Greenland ice core GISP2 and the integrated climate curves at the latitude of 30°～90°N, as well as the climate evolutionary curves recently acquired from the Holocene cave stalagmites, loess and lake sediments, the Holocene climatic rhythm stages has been established by this paper for Eastern China, which consists of 11 warm periods (numbered W1-W11) and 10 cold periods (numbered C1-C10). Correspondingly, the analysis of Holocene climatic events, such as floods, transgressions, regressions, glaciers, freezing and other climate events in the eastern China is conducted. Evidence confirms that there is a millennium scale rhythmical climate evolution in China during the Holocene. The cooling periods numbered C2, C4 and C6 have showed the considerable cooling and may correspond to the cooling events in 10, 8.2 and 5.3 kaBP, respectively. The warming period numbered W5 is corresponding to the Megathermal around 7 kaBP. It indicates that the Holocene climate change in eastern China is obviously influenced by land-sea interactions.
- climate rhythm stages /
- millennial scale /
- cycle of cooling and warm periods /
- megathermal /
- Holocene

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References

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