Holocene Climate Modulates Mud Supply, Transport, and Sedimentation on the East China Sea Shelf | |
Dong, Jiang2,3; Li, Anchun2,5; Liu, Xiting1,5; Wan, Shiming2,5; Xu, Fangjian4; Shi, Xuefa3,5 | |
刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE |
2020-10-01 | |
卷号 | 125期号:10页码:18 |
ISSN号 | 2169-9003 |
DOI | 10.1029/2020JF005731 |
通讯作者 | Li, Anchun(acli@qdio.ac.cn) |
英文摘要 | Shelf mud is an important sink for fluvial sediment, and it is sensitive to variations in river discharge and ocean circulation, which are significantly influenced by climate change. However, the evolution of shelf mud in response to climate change during the Holocene is poorly understood. Here, we present high-resolution sedimentary records of heavy minerals and mass accumulation rates (MARs) from the East China Sea shelf to study the response mechanisms of the Holocene shelf mud supply, transport, and sedimentation to the climate-driven variations in fluvial discharge and ocean currents. The results indicate that the shelf mud primarily originates from the Changjiang (Yangtze) River and has been mainly transported by wind-driven longshore currents in suspension since approximately 8.0 ka. A comparison of the MARs with several shelf mud sedimentation-rate records and climate changes during the Holocene on millennial timescales showed that strong (weak) precipitation in the river basin, which is positively linked with Asian summer monsoon and El Nino-driven storms, could intensify (weaken) the fluvial sediment supply, thereby increasing (decreasing) the shelf mud deposition flux. On multicentennial timescales, changes in the relative intensities of different ocean currents due to climate oscillations during the Holocene could generate frequent migrations of the current shear front (a hydrodynamic barrier), which has trapped an abundance of suspended materials on the shoreward side and resulted in rapid mud sedimentation (similar to 2.3 g/cm(2)/year) at different sites during different periods. Therefore, our study highlights that the Holocene shelf mud evolution responds sensitively to climate changes on different timescales. |
资助项目 | National Natural Science Foundation of China[41430965] ; National Natural Science Foundation of China[41606062] ; National Natural Science Foundation of China[U1606401] ; National Program on Global Change and Air-Sea Interaction[GASI-GEOGE-03] ; Qingdao Postdoctoral Applied Research Project[2019254] |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | AMER GEOPHYSICAL UNION |
WOS记录号 | WOS:000586451100001 |
内容类型 | 期刊论文 |
源URL | [http://ir.qdio.ac.cn/handle/337002/169072] |
专题 | 海洋研究所_海洋地质与环境重点实验室 |
通讯作者 | Li, Anchun |
作者单位 | 1.Ocean Univ China, Coll Marine Geosci, Key Lab Submarine Geosci & Prospecting Tech, Qingdao, Peoples R China 2.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China 3.First Inst Oceanog, Key Lab Marine Geol & Metallogeny, Minist Nat Resources, Qingdao, Peoples R China 4.China Univ Petr, Sch Geosci, Qingdao, Peoples R China 5.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Peoples R China |
推荐引用方式 GB/T 7714 | Dong, Jiang,Li, Anchun,Liu, Xiting,et al. Holocene Climate Modulates Mud Supply, Transport, and Sedimentation on the East China Sea Shelf[J]. JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE,2020,125(10):18. |
APA | Dong, Jiang,Li, Anchun,Liu, Xiting,Wan, Shiming,Xu, Fangjian,&Shi, Xuefa.(2020).Holocene Climate Modulates Mud Supply, Transport, and Sedimentation on the East China Sea Shelf.JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE,125(10),18. |
MLA | Dong, Jiang,et al."Holocene Climate Modulates Mud Supply, Transport, and Sedimentation on the East China Sea Shelf".JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE 125.10(2020):18. |
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