末次冰消期以来长江口沉积环境演化及沿岸流变化

战庆; 王张华; 赵宝成; 王寒梅; 史玉金; 何中发; 谢建磊

doi:10.3799/dqkx.2020.073

Volume 45 Issue 7

Jul. 2020

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Article Navigation > Earth Science > 2020 > 45(7): 2697-2708

Zhan Qing, Wang Zhanghua, Zhao Baocheng, Wang Hanmei, Shi Yujin, He Zhongfa, Xie Jianlei, 2020. Sedimentary Evolution and Coastal Currents Variations of the Yangtze River Mouth(East China Sea) since Last Deglaciation. Earth Science, 45(7): 2697-2708. doi: 10.3799/dqkx.2020.073

Citation:

Zhan Qing, Wang Zhanghua, Zhao Baocheng, Wang Hanmei, Shi Yujin, He Zhongfa, Xie Jianlei, 2020. Sedimentary Evolution and Coastal Currents Variations of the Yangtze River Mouth(East China Sea) since Last Deglaciation. Earth Science, 45(7): 2697-2708. doi: 10.3799/dqkx.2020.073

Citation:

Zhan Qing, Wang Zhanghua, Zhao Baocheng, Wang Hanmei, Shi Yujin, He Zhongfa, Xie Jianlei, 2020. Sedimentary Evolution and Coastal Currents Variations of the Yangtze River Mouth(East China Sea) since Last Deglaciation. Earth Science, 45(7): 2697-2708. doi: 10.3799/dqkx.2020.073

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Sedimentary Evolution and Coastal Currents Variations of the Yangtze River Mouth(East China Sea) since Last Deglaciation

doi: 10.3799/dqkx.2020.073

1.
Shanghai Institute of Geological Survey, Shanghai 200072, China
2.
State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China

Received Date: 2020-04-09
Publish Date: 2020-07-15

Abstract

Abstract

The study of coastal currents variations in the Yangtze River mouth has significance for the understanding of riverine sediment 'source to sink' processes in this region. The post-glacial core sediments from the northern Yangtze River mouth, along with sedimentary structures and distributions of grain size and benthic foraminifera, show an estuarine depositional system characterized by tidal sand ridge in Early Holocene and a deltaic system consists of prodelta, delta front slope and delta front. Based on changes in the dominant microfauna species, two main current patterns prevailed in this region during most of the Holocene:one is the Yellow Sea coastal current (YSCC) and the other is the Yangtze dilute water (YDW). in Early Holocene, the YSCC dominated this area and the effect of YDW gradually strengthened. The YDW clearly weakened due to the sea level rise in early Middle Holocene. Then the East China Sea water mass (ESWM) penetrated the area dominated by mixed water mass consists of YDW, YSCC, Zhe-Min coastal current (ZMCC) and Yellow Sea cold water (YSCW), yet the Yangtze plume prevailed due to the rapid seaward migration of the Yangtze mouth.The YDW dominated this area again in Late Holocene.
- last deglaciation,
- Yangtze Estuary,
- sedimentary evolution,
- coastal current,
- foraminifera,
- sedimentology

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References(52)

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