E published version in the manuscript.J. Mar. Sci. Eng. 2021, 9,14 ofFunding: This study is supported by the National All-natural Science Foundation of China beneath contract Nos 42006020, 41876022, and 41630970; the Guangdong Science and Technologies Project below contract No 2019A1515111044. Institutional Overview Board D-Luciferin potassium salt supplier Statement: Not applicable. Informed Consent Statement: Not applicable. Data Availability Statement: Not applicable. Acknowledgments: Data and samples were collected onboard of R/V Shiyan 1, we thank the crew for their enable in the course of the cruise. Conflicts of Interest: The authors declare no conflict of interest.Journal ofMarine Science and EngineeringArticleSedimentary Environmental Evolution on the Western Taiwan Shoal Region because the Late PleistoceneChipeng He 1 , Longbin Sha 1,2 , Dongbo Zhao 3 , Lu Dai 1,two , Zheng Li 1 , Jiabing Tang 1 , Xianfu Li 1 and Dongling Li 1,two, 2Department of Geography and Spatial Details Technology, Ningbo University, Ningbo 315211, China; [email protected] (C.H.); [email protected] (L.S.); [email protected] (L.D.); [email protected] (Z.L.); [email protected] (J.T.); xianfuli21@hotmail (X.L.) Institute of East China Sea, Ningbo University, Ningbo 315211, China Fujian Provincial Essential Laboratory of Coast and Island Management Technologies Study, Fujian Institute of Oceanography, Xiamen 361013, China; [email protected] Correspondence: [email protected]; Tel.: 86-574-8760-5546; Fax: 86-574-8760-Citation: He, C.; Sha, L.; Zhao, D.; Dai, L.; Li, Z.; Tang, J.; Li, X.; Li, D. Sedimentary Environmental Evolution on the Western Taiwan Shoal Region because the Late Pleistocene. J. Mar. Sci. Eng. 2021, 9, 1150. ten.3390/jmse9101150 Academic Editor: Gemma Aiello Received: 4 September 2021 Accepted: 14 October 2021 Published: 19 OctoberAbstract: A new pollen evaluation and main and trace element contents have been carried out on a 40 m lengthy gravity core recovered in the Taiwan Shoal (sand ridges), south of your Taiwan Strait, starting within the Late Pleistocene. The modifications within the pollen assemblage and concentration represent the climate transform around the Taiwan Shoal and also the strength of your Zhe-Min Coastal Current, whereas variations in important and trace element contents can imply the CGS 21680 Purity & Documentation source on the sediments inside the Taiwan Shoal, that are correlated with all the rise or fall in the sea level with enhanced marine dinoflagellate cysts. The interval of 400 m was characterized by higher pollen and spore concentrations, and evergreen Quercus was dominant taxon, which indicates a warm sedimentary environment, plus the surrounding area from the Taiwan Shoal were covered by a tropical and subtropical broad-leaved forest. There had been no pollen and spores from 304 m, which indicates a robust hydrodynamic sedimentary atmosphere, and most of the Taiwan Shoal may happen to be practical experience subaerial exposure. The interval of 247 m was characterized by the reappearance of pollen and spores, also as marine dinoflagellate cysts and foraminifera, suggesting the climate was warm and wet in the study area and an apparent marine sedimentary atmosphere with relatively high sea level. Deciduous Quercus dominated the interval of 172 m, which indicated that the climate was comparatively cool, corresponding towards the finish of Marine isotope stages3 (MIS3) for the Final Glacial Maximum accompanied by weathering and denudation. Above 12 m, the low pollen concentration with enhanced marine dinoflagellate cysts and foraminifera abundance recommended a marine.