Geochemistry and Holocene Sedimentary Environment Evolution of Subaqueous Clinoform off Shandong Peninsula (Yellow Sea)

Yingtao Zhu,Yongchen Xu,Mingyang Liu,Longhai Zhu,Zhaobin Lin

doi:10.3390/min11111209

Abstract

As a key sedimentary body connecting the north and South Yellow Sea, the subaqueous clinoform off Shandong Peninsula plays an important role in the sedimentary system of China seas, and it is also a studied example in the study among the major “source to sink” systems. Based on AMS 14C dating, sediment grain size, major and trace element contents from core WH-05 located at the edge of the clinoform, we discuss changes in the deposition rate, analyze sediment provenance and controlling factors, and reveal the environmental evolution of the source area since the Holocene. Results from core WH-05 show that marine sedimentation began at about 8.5 ka B.P. The deposition rate decreased from the initial 28.37 m/ka to 0.52 m/ka. Sediment provenance suggests that the Huanghe river sediments have been the main source for the study area since the Holocene. The As/Al, V/Sc indicators show that the environmental oxidation environment was gradually weakened and then increased slightly starting from 7.0 ka B.P. The change in redox is consistent with the change in sea level, the deposition rate, and depositional depth.

Highlights

IntroductionOwing to a large number of preserved sedimentary records from the continent to the ocean contained in the marine sediments, the Quaternary paleoceanography of marginal seas [1] once became a research hotspot
Based on the characteristics of sediment grain size, major and trace element contents, we reveal the changes in the sedimentation rate, sediment provenance, and sedimentary environment evolution since the Holocene
Based on the characteristics of sediment grain size, major and trace element contents, we reveal the changes in the sedimentation rate, of 18 sediment provenance, and sedimentary environment evolution since the Holocene

Summary

Introduction

Owing to a large number of preserved sedimentary records from the continent to the ocean contained in the marine sediments, the Quaternary paleoceanography of marginal seas [1] once became a research hotspot. The Yellow Sea, where a large number of terrigenous materials of the Eurasian plate were deposited, became a research hotspot in the recent decades [2,3,4,5,6,7,8]. In the early Holocene, the global sea level was about 58 m lower [9], and the whole Bohai Sea, located to the west of the study area (Figure 2), was exposed to the land surface [10]. Between 11.6 and 11.3 ka B.P., the sea level rose from −58 m to

Methods

Results

Discussion

Conclusion