Strata sequence and paleochannel response to tectonic, sea-level, and Asian monsoon variability since the late Pleistocene in the South Yellow Sea
Wang, Liyan1,2; Li, Guangxue1,2; Xu, Jishang1,2; Liu, Yong1,2; Qiao, Lulu1,2; Ding, Dong1,2; Yang, Jichao3; Dada, Olusegun A.4; Li, Qian1,2
刊名QUATERNARY RESEARCH
2019-09
卷号92期号:2页码:450-468
关键词South Yellow Sea Stratigraphic sequence Paleochannel Sea-level changes Asian summer monsoon
ISSN号0033-5894
DOI10.1017/qua.2019.29
英文摘要The continental shelf strata provide information regarding sea-level fluctuation and climate changes in the Quaternary period. A 5831.47-km-long high-resolution seismic profile and borehole core (YS01) were acquired to reconstruct the evolutionary history of the strata in South Yellow Sea (SYS) during the late Pleistocene. The strata recorded three transgression events (HI, HII, and HIII) and three stages of paleochannel development (LI, LII, and LIII). Based on the distribution, thickness, and volume of the strata formed in the three transgressions, we concluded that the scale of the three transgressions during the late Pleistocene was HIII, HI, and HII, in descending order. In addition, our data show that the Yellow River extended to the Yellow Sea Trough during the last glacial maximum. The influence of the tectonic framework on sedimentation in the SYS was completely concealed by sea-level changes and sediment supply in the late Pleistocene (similar to Marine Isotope Stage 5). Since then, the accommodation space, a crucial prerequisite for sedimentation, has been controlled solely by sea-level changes in the SYS. Furthermore, two "source to sink" models of the neritic shelf in the marine and terrestrial environments were established, including high sea-level and shelf-exposure models.
资助项目National Key Research and Development Program of China[DD20160147] ; National Key Research and Development Program of China[GZH201100202] ; National Key Research and Development Program of China[GASI-02-PAC-CJ15] ; National Key Research and Development Program of China[SQ2017YFGH001475]
WOS关键词LATE QUATERNARY DEPOSITS ; CONTINENTAL-SHELF ; PROVENANCE DISCRIMINATION ; SEDIMENT DISTRIBUTION ; SEISMIC STRATIGRAPHY ; SYSTEMS TRACTS ; MUD DEPOSIT ; CHINA ; EVOLUTION ; MAGNETOSTRATIGRAPHY
WOS研究方向Physical Geography ; Geology
语种英语
出版者CAMBRIDGE UNIV PRESS
WOS记录号WOS:000487316500013
内容类型期刊论文
源URL[http://ir.fio.com.cn:8080/handle/2SI8HI0U/30146]  
专题自然资源部第一海洋研究所
通讯作者Li, Guangxue; Xu, Jishang
作者单位1.Ocean Univ China, Key Lab Submarine Sci & Prospecting Tech, MOE, Qingdao 266100, Shandong, Peoples R China
2.Ocean Univ China, Coll Marine Geosci, Qingdao 266100, Shandong, Peoples R China
3.State Ocean Adm, Natl Deep Sea Ctr, Qingdao 266237, Shandong, Peoples R China
4.Fed Univ Technol Akure, Dept Marine Sci & Technol, Akure 340252, Nigeria
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Wang, Liyan,Li, Guangxue,Xu, Jishang,et al. Strata sequence and paleochannel response to tectonic, sea-level, and Asian monsoon variability since the late Pleistocene in the South Yellow Sea[J]. QUATERNARY RESEARCH,2019,92(2):450-468.
APA Wang, Liyan.,Li, Guangxue.,Xu, Jishang.,Liu, Yong.,Qiao, Lulu.,...&Li, Qian.(2019).Strata sequence and paleochannel response to tectonic, sea-level, and Asian monsoon variability since the late Pleistocene in the South Yellow Sea.QUATERNARY RESEARCH,92(2),450-468.
MLA Wang, Liyan,et al."Strata sequence and paleochannel response to tectonic, sea-level, and Asian monsoon variability since the late Pleistocene in the South Yellow Sea".QUATERNARY RESEARCH 92.2(2019):450-468.
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