Sedimentary processes and records of the Holocene mud area off Shandong Peninsula
Gu Yu1, Liu Xi-Ting1,2, Wu Xiao1,2, Wang Ai-Mei1,2, Bi Nai-Shuang1,2, Wang Hou-Jie1,2
1 College of Marine Geosciences, Key Laboratory of Submarine Geosciences and Prospecting Technology, Ocean University of China, Shandong Qingdao 266100,China; 2 Laboratory for Marine Geology,Qingdao National Laboratory for Marine Science and Technology, Shandong Qingdao 266237,China
Abstract：The Holocene mud areas on the eastern continental shelf of China are an ideal area for studying paleoceanography and paleoclimate. From the perspective of modern sedimentary processes and Holocene sedimentary records,previous research results of the Holocene mud area off Shandong Peninsula are summarized to provide references for further studies. The mud area off Shandong Peninsula is located along the coast of Shandong Peninsula. It is mainly formed by the sediment from the Yellow River and deposited under the interaction of coastal,upwelling and tide currents,exhibiting a unique “Ω” shape. The mud area off Shandong Peninsula was formed by the last deglacial transgression in the Holocene. The Yellow River sediments are thought to be the main source of the mud area,while the nearshore erosion and local small rivers along the Shandong Peninsula coast also contributed sediments to the mud area. The formation and evolution of mud area record rich environmental information and are related to multi-factors,such as paleoceanography,sea-level changes and inland paleoclimatic evolution. The sedimentation of the mud area off Shandong Peninsula can respond to the evolution of East Asian Monsoon rapidly,and its high sedimentation rate can provide high resolution archive for the evolution of paleoclimate in the Yellow River Basin,which provide references for predicting the Yellow River Basin evolution under global climatic changes in future. Although a great deal of work has been done on modern sedimentary processes,modern observation and numerical simulation are still needed to provide data and theoretical support for better reconstruction of sedimentary dynamic processes in the study area. In addition,the response of the depositional processes of clastic sediment and organic matter to the paleoceanography and paleoclimate in the long-time scale need to be better understood.
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