| Qingdao Institute of marine geology, China Geological Survey | Host |
| Citation: |
YAO Zhengquan, LIU Jian, WAN Shiming, LIU Yanguang, YI Liang, LIU Jianxing, SHAN Xin, QIAO Shuqing, ZHAO Debo, XIAO Guoqiao, WANG Kunshan, DOU Yanguang, WANG Zhongbo, XU Qinmian, SHI Xuefa. Progress and prospects of research on the Quaternary sedimentary environment in the eastern shelf of China[J]. Marine Geology & Quaternary Geology, 2022, 42(5): 42-57. doi: 10.16562/j.cnki.0256-1492.2022063001
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Progress and prospects of research on the Quaternary sedimentary environment in the eastern shelf of China
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Abstract
The eastern shelf of China is located in the transitional zone between the Asian continent and the western Pacific Ocean. It is an important link connecting the largest sedimentary source-sink system in the world, and bears many important information on tectonic deformation in East Asia, the formation and evolution of the Asian monsoon system, sea level changes and major water system changes in East Asia. Based on the review of previous studies and the new data obtained from marine projects in China during the last two decades, this paper reviews the Quaternary sedimentary environmental changes in the eastern shelf of China, mainly focusing on changes in marine transgression and regression cycles, and discusses the connection between the Quaternary sedimentary environment in eastern shelf of China and regional tectonic, sea level and East Asian monsoon climate changes. Based on the previous sedimentary source-sink studies in the Yangtze and Yellow River basins and the shelf area, we discuss the timing of penetrating into the sea of the Yangtze and Yellow rivers and controlling factors. We propose that the coupling mechanism of the geological environment evolution in the eastern shelf of China with Asian tectonic deformation, monsoon system evolution, sea-level change, major water system adjustment and carbon burial since the Cenozoic is a key scientific goal for future scientific drilling in the eastern shelf of China.
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References
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YAO Zhengquan, LIU Jian, WAN Shiming, LIU Yanguang, YI Liang, LIU Jianxing, SHAN Xin, QIAO Shuqing, ZHAO Debo, XIAO Guoqiao, WANG Kunshan, DOU Yanguang, WANG Zhongbo, XU Qinmian, SHI Xuefa. Progress and prospects of research on the Quaternary sedimentary environment in the eastern shelf of China[J]. Marine Geology & Quaternary Geology, 2022, 42(5): 42-57. doi: 10.16562/j.cnki.0256-1492.2022063001
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Figure 1.
Location of main cores on the eastern shelf of China mentioned in text
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Figure 2.
The constructed chronology of core BH08 from the Bohai Sea using astronomical tunning methods [34]
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Figure 3.
The constructed age model of core NHH01 from the Yellow Sea using astronomical tunning methods[49]
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Figure 4.
Comparison of sedimentary environmental change in the Bohai Sea and Yellow Sea and coastal area[49]
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Figure 5.
Timing of the integration of the Yangtze River (black bars) and Yellow River (green bars)
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Figure 6.
The sedimentary environmental change at orbital timescale in the Bohai Sea and Yellow Sea[49]
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Figure 7.
Changes in grain size of BH08 sequence and implication for sea level and East Asian summer monsoon[92]