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In-phase and out-of-phase behavior of the East Asian summer and winter monsoons recorded in the South Yellow Sea sediment over the past 9.5 ka

Published online by Cambridge University Press:  01 September 2020

Liyan Wang
Affiliation:
Key Laboratory of Submarine Sciences and Prospecting Techniques, MOE, and College of Marine Geosciences, Ocean University of China, Qingdao266100, China College of Ocean Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China
Guangxue Li*
Affiliation:
Key Laboratory of Submarine Sciences and Prospecting Techniques, MOE, and College of Marine Geosciences, Ocean University of China, Qingdao266100, China
Linmiao Wang
Affiliation:
Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, SOA, Qingdao266061, China
Wenchao Zhang
Affiliation:
Key Laboratory of Submarine Sciences and Prospecting Techniques, MOE, and College of Marine Geosciences, Ocean University of China, Qingdao266100, China
Yang Zhang
Affiliation:
Key Laboratory of Submarine Sciences and Prospecting Techniques, MOE, and College of Marine Geosciences, Ocean University of China, Qingdao266100, China
Yong Liu
Affiliation:
Key Laboratory of Submarine Sciences and Prospecting Techniques, MOE, and College of Marine Geosciences, Ocean University of China, Qingdao266100, China
Xiangdong Wang
Affiliation:
Qingdao Blue Earth Big Data Technology Co., Ltd, Qingdao266400, China
Haoyin Wang
Affiliation:
Key Laboratory of Ocean and Marginal Sea Geology, Chinese Academy of Sciences, Guangzhou510301, China
*
*Corresponding author at: Key Laboratory of Submarine Sciences and Prospecting Techniques, MOE, and College of Marine Geosciences, Ocean University of China, Qingdao266100, China. E-mail address: [email protected] (G. Li).

Abstract

The variability of the East Asian monsoon (EAM) during the Holocene exhibits significant regional response, and its evolution needs further discussion. A well-dated, high-resolution sea-surface temperature record based on long-chain unsaturated alkenones, grain-size data, and clay mineral assemblages from the South Yellow Sea sediment is presented to investigate the sedimentary provenance and reconstruct the EAM over the past 9.5 ka. The results show that the sediments are most likely supplied by the Huanghe. The evolution of the East Asian summer monsoon (EASM) can be divided into three periods: strong and relatively stable conditions during 9.5–7.0 ka, weakened conditions during 7.0–1.5 ka, and strengthened conditions during 1.5–0 ka. The East Asian winter monsoon (EAWM) has experienced five periods: weakened conditions during 9.5–6.7 ka, weak and relatively stable conditions during 6.7–5.6 ka, strong and relatively stable conditions during 5.6–2.6 ka, strengthened conditions during 2.6–1.5 ka, and weak and stable conditions during 1.5–0 ka. Moreover, in-phase correlation was found between the EAWM and EASM at the orbital time scale in response to orbital-driven solar insolation, but out-of-phase correlation at a centennial time scale is predominantly associated with solar activity.

Type
Research Article
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2020

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