Fine structure of dark layers in the central Japan Sea and their relationship with the abrupt climate and sea level changes over the last 75 ka inferred from lithophysical, geochemical and pollen results

doi:10.1016/j.jseaes.2015.04.040

	Fine structure of dark layers in the central Japan Sea and their relationship with the abrupt climate and sea level changes over the last 75 ka inferred from lithophysical, geochemical and pollen results
	Gorbarenko, S.1; Shi, X.2; Rybiakova, Y.1; Bosin, A.1; Malakhov, M.3; Zou, J.2; Liu, J.2; Velivetskaya, T.4; Ignatiev, A.4; Derkachev, A.1
刊名	JOURNAL OF ASIAN EARTH SCIENCES
	2015-12-15
卷号	114 页码:476-487
关键词	Japan Sea Dark layers Climate changes Interstadial Sea level
ISSN号	1367-9120
DOI	10.1016/j.jseaes.2015.04.040
英文摘要	High resolution of the color lightness, productivity proxies (TOC, chlorin, CaCO3, Ba-bio, Mo and U), and lithological description defined alternation of dark layers (DLs) and light layers in sediment core LV53-23 recovered from the central Japan Sea (west Yamato Rise) over the last 75 ka. Age model was constructed by AMS 14C data, tephrochronology, delta 18o of planktonic foraminifera record, and the correlation of DLs with lightness of Japan Sea core MD01-2407 and with millennial interstadials recorded in the Greenland ice cores and East Asia stalagmites. Regional interstadials were also independently established and dated by vegetation amelioration of the surrounded land, inferred from the pollen results. Correlation of the DLs with millennial scale climate and sea level changes indicate that both interstadial warming and sea level fluctuations influence on its formation providing their individual features. During MIS 3, with sea level above -90 m, DL was formed mostly consistent with the Tada et al. (1999)'s hypotheses. During MIS 2 and 4, when sea level was nearly and below 90 m, sea level descending led to water column stratification, oxygen depletion in bottom water and facilitates the DLs formation. High-resolution lightness and productivity proxies defined the subtle structure of pronounced interstadials 14 and 12. (c) 2015 Elsevier Ltd. All rights reserved.
资助项目	National Natural Science Foundation of China[41420104005] ; National Natural Science Foundation of China[40710069004] ; National Natural Science Foundation of China[40431002]
WOS研究方向	Geology
语种	英语
出版者	PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号	WOS:000367857800005
内容类型	期刊论文
源URL	[http://ir.fio.com.cn/handle/2SI8HI0U/3560]
专题	自然资源部第一海洋研究所
作者单位	1.VI Ilichev Pacific Oceanol Inst, Vladivostok 690041, Russia; 2.SOA, Inst Oceanog 1, Qingdao 266061, Peoples R China; 3.North East Interdisciplinary Sci Res Inst FEB RAS, NEISRI FEB RAS, Magadan 685000, Russia; 4.Far East Geol Inst FEB RAS, Vladivostok 690022, Russia
推荐引用方式 GB/T 7714	Gorbarenko, S.,Shi, X.,Rybiakova, Y.,et al. Fine structure of dark layers in the central Japan Sea and their relationship with the abrupt climate and sea level changes over the last 75 ka inferred from lithophysical, geochemical and pollen results[J]. JOURNAL OF ASIAN EARTH SCIENCES,2015,114:476-487.
APA	Gorbarenko, S..,Shi, X..,Rybiakova, Y..,Bosin, A..,Malakhov, M..,...&Shi, F..(2015).Fine structure of dark layers in the central Japan Sea and their relationship with the abrupt climate and sea level changes over the last 75 ka inferred from lithophysical, geochemical and pollen results.JOURNAL OF ASIAN EARTH SCIENCES,114,476-487.
MLA	Gorbarenko, S.,et al."Fine structure of dark layers in the central Japan Sea and their relationship with the abrupt climate and sea level changes over the last 75 ka inferred from lithophysical, geochemical and pollen results".JOURNAL OF ASIAN EARTH SCIENCES 114(2015):476-487.