Sedimentary environment and paleo-tidal evolution of the eastern Bohai Sea, China since the last glaciation. (8th June 2017)

• Record Type: Journal Article
• Authors: Yao, Zhengquan; Shi, Xuefa; Li, Xiaoyan; Liu, Yanguang; Liu, Jian; Qiao, Shuqing; Bai, Yazhi; Wang, Xin; Zhu, Aimei; Wang, Xuchen
• Is Part Of: Quaternary international. Volume 440(2017)Part A
• Page Start: 129
• Page End: 138
• Publication Date: 2017-06-08
• Subjects: Bohai Sea -- Tidal current -- The deglacial period -- Sea-level; Geology, Stratigraphic -- Quaternary -- Periodicals; Stratigraphie -- Quaternaire -- Périodiques; 551.79
• DOI: 10.1016/j.quaint.2016.04.010
• Languages: English
• ISSNs: 1040-6182

Abstract

Abstract: Numerical simulation suggests that the Holocene sediments re-suspension and distribution in the Bohai Sea was mainly controlled by tidal current regime, which was closely related with sea-level change. Study on sediments in the Bohai Sea thus can provide insights into the evolution of tidal-influenced sedimentary environment and its links with sea-level change. Our understanding of this issue remains incomplete, however, owing to the lack of comprehensive study on sediment core with high-resolution proxies to test such inference. In this study, analyses of sedimentary facies, proxies (grain size, total organic carbon and total nitrogen, X-ray fluorescence scanning Sulfur and Chlorine ratio) and accelerator mass spectrometry 14 C dates of a sediment core recovered from the eastern Bohai Sea were carried out to clarify the Holocene sedimentary environment, tidal current change and its relation to the sea-level. The results indicate that the eastern Bohai Sea was dominated by fluvial-coastal environment prior to 12, 400 cal a BP due to the sea-level lowstand and changed to tidal-influenced environment from 12, 400 to 6700 cal a BP following the rapid sea-level rising. Thereafter shelf environment with minor tidal influence dominated the eastern Bohai Sea under the condition of a deceleration of sea-level rise. The significant change at ∼6700 cal a BP both in sedimentary environment and sediment proxies, indicating an environmental transition from strong tidal-influenced to less tidal-influenced setting. With the sea-level rising from the early Holocene to the mid-Holocene, tidal-current was much strong due to the low sea-level stand and became weak after the maximum transgression at ∼6700 cal a BP. These results are consistent with the numerical simulation, which suggested that less strong tidal current were the consequence of the most highstand sea-level since the mid-Holocene. Our study thus provides a sedimentary record to support the interpretation of numerical simulation-based tidal-influenced depositional process in the eastern Bohai Sea since the deglacial period.