Reconstruction of ice conditions in the northern Chukchi Sea during recent centuries: Geochemical proxy compared with observed data

doi:10.1016/j.quaint.2019.05.009

	Reconstruction of ice conditions in the northern Chukchi Sea during recent centuries: Geochemical proxy compared with observed data
	Astakhov, A. S.1; Bosin, A. A.1; Liu, Y. G.2; Darin, A., V 3; Kalugin, I. A.3; Artemova, A., V 1; Babich, V. V.3; Melgunov, M. S.3; Vasilenko, Yu P.1; Vologina, E. G.4
刊名	QUATERNARY INTERNATIONAL
	2019-07-10
卷号	522 页码:23-37
关键词	Arctic shelf XRF-SR Sedimentation rate Reconstruction Transfer function Little Ice Age
ISSN号	1040-6182
DOI	10.1016/j.quaint.2019.05.009
英文摘要	This paper presents the first results of the quantitative reconstruction of ice conditions in the Arctic based on a comparison of the data for periods of meteorological observations with variations in the chemical compositions of the sediments accumulated during the same times. The biogenic elements (Br, Ca, and Sr) and some redox-sensitive (As and Fe) elements are the most informative for the reconstruction of changes in ice conditions with positive correlations, and the lithogenic elements (K and Ti) are predominantly negatively correlated. The reconstruction results for the last 300-400 years of average annual air temperature anomalies for all cores in general terms coincide with the reconstruction for the Northern Hemisphere. The common features of all reconstructions are low temperatures during the Little Ice Age (LIA) and a rapid warming in the middle of the 19th century and in the last decades of the 20th and first decades of the 21st centuries. The results of the reconstruction of the duration of the ice-free period generally coincide with the temperature changes for the last two centuries, although for LIA there is an inverse correlation between the variations in temperature and the duration of the ice-free period. A possible reason for this may be changes in the structure of the surface currents in the Chukchi Sea and the northern part of the Bering Sea, because of which the inflow of warm and freshened waters through the Bering Strait to the Arctic increased occasionally.
资助项目	National Natural Science Foundation of China[U1606401] ; National Natural Science Foundation of China[41876070]
WOS关键词	ARCTIC-OCEAN SEDIMENTS ; LATE HOLOCENE SEDIMENTATION ; BOTTOM SEDIMENTS ; DIATOM DISTRIBUTION ; ORGANIC-MATTER ; OKHOTSK SEA ; BERING-SEA ; LAST ; VARIABILITY ; CLIMATE
WOS研究方向	Physical Geography ; Geology
语种	英语
出版者	PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号	WOS:000485032800003
内容类型	期刊论文
源URL	[http://ir.fio.com.cn:8080/handle/2SI8HI0U/30178]
专题	自然资源部第一海洋研究所
通讯作者	Bosin, A. A.
作者单位	1.Russian Acad Sci, Far Eastern Branch, VI Ilichey Pacific Oceanol Inst, Vladivostok, Russia 2.Minist Nat Resources, Inst Oceanog 1, Beijing, Peoples R China 3.Russian Acad Sci, Siberian Branch, VS Sobolev Inst Geol & Mineral, Novosibirsk, Russia 4.Russian Acad Sci, Siberian Branch, Inst Earths Crust, Novosibirsk, Russia
推荐引用方式 GB/T 7714	Astakhov, A. S.,Bosin, A. A.,Liu, Y. G.,et al. Reconstruction of ice conditions in the northern Chukchi Sea during recent centuries: Geochemical proxy compared with observed data[J]. QUATERNARY INTERNATIONAL,2019,522:23-37.
APA	Astakhov, A. S..,Bosin, A. A..,Liu, Y. G..,Darin, A., V.,Kalugin, I. A..,...&Vologina, E. G..(2019).Reconstruction of ice conditions in the northern Chukchi Sea during recent centuries: Geochemical proxy compared with observed data.QUATERNARY INTERNATIONAL,522,23-37.
MLA	Astakhov, A. S.,et al."Reconstruction of ice conditions in the northern Chukchi Sea during recent centuries: Geochemical proxy compared with observed data".QUATERNARY INTERNATIONAL 522(2019):23-37.