IOCAS-IR  > 海洋地质与环境重点实验室
Sea-level oscillations in the East China Sea and their implications for global seawater redistribution during 14.0-10.0 kyr BP
Dong, Jiang1,3; Li, Anchun1,2; Liu, Xiting1,2,4; Wan, Shiming1,2; Feng, Xuguang1,3; Lu, Jian1; Pei, Wenqiang1,3; Wang, Hongli1
2018-12-15
Source PublicationPALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN0031-0182
Volume511Pages:298-308
Corresponding AuthorLi, Anchun(acli@qdio.ac.cn)
AbstractThe sea-level curve during the last deglaciation is characterized by two episodes of rapid sea-level rise, termed Meltwater Pulses (MWPs) 1A (14.6-14.3 kyr BP) and 1B (11.45-11.1 kyr BP), as well as an episode of relatively slow sea-level rise during the Younger Dryas stadial (YD; 12.85-11.65 kyr BP). However, the relative sea-level changes during the YD and MWP-1B periods are still not well defined. Here, we use precisely dated intertidal sediments derived from 6 sediment cores on the tectonically stable continental shelf of the East China Sea (ECS) to reconstruct a high-resolution sea-level curve between 14.0 kyr BP and 10.0 kyr BP. Although linear regression analysis suggests that the sea level rose continuously, with an average rate of 10.6 +/- 0.6 mm/yr (r = -0.87, p (a) < 0.01, n = 95), the mode of sea-level rise differs before, during, and after the YD stadial. A rapid sea-level rise of 30.5 +/- 4.9 mm/yr (r = 0.79, p(a) < 0.05, n = 25) occurred during 14.0-12.85 kyr BP. Subsequently, the rate of sea-level rise decreased significantly in response to the YD stadial, and it increased smoothly to 12.0 +/- 1.4 mm/yr (r = -0.86, p(a) < 0.01, n = 29) from 11.65-10.0 kyr BP, indicating that MWP-1B was absent on the ECS shelf. Furthermore, based on comparisons of these data with other high-resolution curves of sea level or elevation at different latitudes, we suggest that the poleward seawater migration from intertropical broad oceans occurred because glacial isostatic adjustment could have generated a relatively consistent global sea-level height during the last deglaciation, especially during the YD, when the rate of sea-level rise was slowed.
KeywordYounger Dryas Meltwater pulse 1B Sedimentary environment Isostatic adjustment Continental shelf
DOI10.1016/j.palaeo.2018.08.015
Indexed BySCI
Language英语
Funding ProjectNational Natural Science Foundation of China[41430965] ; National Natural Science Foundation of China[41606062]
WOS Research AreaPhysical Geography ; Geology ; Paleontology
WOS SubjectGeography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS IDWOS:000452583600017
PublisherELSEVIER SCIENCE BV
Citation statistics
Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.qdio.ac.cn/handle/337002/155794
Collection海洋地质与环境重点实验室
Corresponding AuthorLi, Anchun
Affiliation1.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.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Ocean Univ China, Coll Marine Geosci, Key Lab Submarine Geosci & Prospecting Tech, Qingdao 266100, Peoples R China
First Author AffilicationInstitute of Oceanology, Chinese Academy of Sciences
Corresponding Author AffilicationInstitute of Oceanology, Chinese Academy of Sciences
Recommended Citation
GB/T 7714
Dong, Jiang,Li, Anchun,Liu, Xiting,et al. Sea-level oscillations in the East China Sea and their implications for global seawater redistribution during 14.0-10.0 kyr BP[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2018,511:298-308.
APA Dong, Jiang.,Li, Anchun.,Liu, Xiting.,Wan, Shiming.,Feng, Xuguang.,...&Wang, Hongli.(2018).Sea-level oscillations in the East China Sea and their implications for global seawater redistribution during 14.0-10.0 kyr BP.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,511,298-308.
MLA Dong, Jiang,et al."Sea-level oscillations in the East China Sea and their implications for global seawater redistribution during 14.0-10.0 kyr BP".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 511(2018):298-308.
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