Long-term global sea-level change due to dynamic topography since 410 Ma

doi:10.1016/j.dsr.2022.103944

IOCAS-IR > 海洋地质与环境重点实验室

	Long-term global sea-level change due to dynamic topography since 410 Ma
	Yang, An 1,2,3,4
	2023
发表期刊	DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
ISSN	0967-0637
卷号	191 页码:9
通讯作者	Yang, An([email protected])
摘要	Sedimentary studies at continental boundary show that the global sea level has hundreds of meters of change since the late Paleozoic. Long-term global sea-level change is closely related to the mantle convection. The deflection of the ocean basins caused by dynamic topography can change the container volume of the basin, thus inducing global sea-level change. However, the influence of dynamic topography on the global sea-level change during supercontinent cycles is not well understood. Based on dynamic topography from mantle convection models and past seafloor age from plate reconstructions, I studied the influence of dynamic topography on global sea-level change since 410 Ma. Model results show that the present-day dynamic topography contributes to similar to 120 m of positive global sea level. Dynamic topography raises the sea level during the dispersal, assembly, and transition phases, and drops the sea level during period of supercontinent stability. Global sea-level change caused by the seafloor age distribution is the main factor that controls the long-term global sea-level change. Different methods to define the ocean basin have only a small influence on global sea level change due to the combined effects of seafloor age and dynamic topography. The combined effects of dynamic topography and seafloor age uplift the sea-level during Pangea dispersal and assembly phases, and decrease sea-level during stability and the transition phases.
关键词	Dynamic topography Sea level Mantle convection Plate tectonics Mantle structure
DOI	10.1016/j.dsr.2022.103944
收录类别	SCI
语种	英语
资助项目	NSFC; Special Funds of Shandong Province for Qingdao National Laboratory for Marine Science and Technology; [41804086]; [2022QNLM050201-2]
WOS研究方向	Oceanography
WOS类目	Oceanography
WOS记录号	WOS:000901438300003
出版者	PERGAMON-ELSEVIER SCIENCE LTD
引用统计	被引频次：2[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/181406
专题	海洋地质与环境重点实验室
通讯作者	Yang, An
作者单位	1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China 3.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China 4.7 Nanhai Rd, Qingdao 266071, Peoples R China
第一作者单位	中国科学院海洋研究所
通讯作者单位	中国科学院海洋研究所
推荐引用方式 GB/T 7714	Yang, An. Long-term global sea-level change due to dynamic topography since 410 Ma[J]. DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS,2023,191:9.
APA	Yang, An.(2023).Long-term global sea-level change due to dynamic topography since 410 Ma.DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS,191,9.
MLA	Yang, An."Long-term global sea-level change due to dynamic topography since 410 Ma".DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS 191(2023):9.