Middle Holocene Organic Carbon and Biomarker Records from the South Yellow Sea: Relationship to the East Asian Monsoon

2018 ◽  
Vol 17 (4) ◽  
pp. 823-834
Author(s):  
Liang Zou ◽  
Bangqi Hu ◽  
Jun Li ◽  
Yanguang Dou ◽  
Luhua Xie ◽  
...  
Keyword(s):  
Organic Carbon ◽  
Yellow Sea ◽  
Asian Monsoon ◽  
East Asian Monsoon ◽  
East Asian ◽  
South Yellow Sea ◽  
The South ◽  
Middle Holocene ◽  
The South Yellow Sea

Centennial-scale records of total organic carbon in sediment cores from the South Yellow Sea, China

2018 ◽  
Vol 36 (1) ◽  
pp. 128-138 ◽  
Author(s):  
Qing Zhu ◽  
Jia Lin ◽  
Yuehui Hong ◽  
Lirong Yuan ◽  
Jinzhong Liu ◽  
...  
Keyword(s):  
Organic Carbon ◽  
Total Organic Carbon ◽  
Yellow Sea ◽  
Sediment Cores ◽  
South Yellow Sea ◽  
The South ◽  
The South Yellow Sea

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

2020 ◽  
pp. 1-18
Author(s):  
Liyan Wang ◽  
Guangxue Li ◽  
Linmiao Wang ◽  
Wenchao Zhang ◽  
Yang Zhang ◽  
...  
Keyword(s):  
Yellow Sea ◽  
Time Scale ◽  
East Asian ◽  
Phase Correlation ◽  
South Yellow Sea ◽  
The South ◽  
The Past ◽  
Stable Conditions ◽  
Asian Summer ◽  
The South Yellow Sea

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.

CLASSIFICATION AND TECTONIC CHARACTERISTICS OF BURIED HILLS IN THE SOUTH YELLOW SEA BASIN

2012 ◽  
Vol 32 (2) ◽  
pp. 85-92 ◽  
Author(s):  
Fanghui HOU ◽  
Xunhua ZHANG ◽  
Zhixun ZHANG ◽  
Zhenhe WEN ◽  
Rihui LI ◽  
...  
Keyword(s):  
Yellow Sea ◽  
South Yellow Sea ◽  
The South ◽  
South Yellow Sea Basin ◽  
The South Yellow Sea

Evolution of radiative sand ridge field of the South Yellow Sea and its sedimentary characteristics

1999 ◽  
Vol 42 (1) ◽  
pp. 97-112 ◽  
Author(s):  
Ying Wang ◽  
Dakui Zhu ◽  
Kunyuan You ◽  
Shaoming Pan ◽  
Xiaodong Zhu ◽  
...  
Keyword(s):  
Yellow Sea ◽  
Sand Ridge ◽  
South Yellow Sea ◽  
The South ◽  
Sedimentary Characteristics ◽  
The South Yellow Sea

Characterization of microbial communities in sediments of the South Yellow Sea

2020 ◽  
Author(s):  
Ye Chen ◽  
Siqi Li ◽  
Xiaoqing Xu ◽  
Manman Ma ◽  
Tiezhu Mi ◽  
...  
Keyword(s):  
Microbial Communities ◽  
Yellow Sea ◽  
South Yellow Sea ◽  
The South ◽  
The South Yellow Sea

Late Quaternary coccolith records in the South China Sea and East Asian monsoon dynamics

2013 ◽  
Vol 111 ◽  
pp. 88-96 ◽  
Author(s):  
Xiang Su ◽  
Chuanlian Liu ◽  
Luc Beaufort ◽  
Jun Tian ◽  
Enqing Huang
Keyword(s):  
South China Sea ◽  
South China ◽  
Asian Monsoon ◽  
East Asian Monsoon ◽  
Late Quaternary ◽  
East Asian ◽  
The South China Sea ◽  
The South ◽  
China Sea ◽  
Monsoon Dynamics
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