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DOI	10.1016/j.quascirev.2019.02.015
	Sedimentary; geochemical and hydrological history of Lake Kinneret during the past 28;000 years
	Lev L.; Stein M.; Ito E.; Fruchter N.; Ben-Avraham Z.; Almogi-Labin A.
发表日期	2019
ISSN	0277-3791
起始页码	114
结束页码	128
卷号	209
英文摘要	The sedimentary, geochemical and hydrological history of Lake Kinneret (Sea of Galilee) is reconstructed for the past ∼28 kyrs, based on three sedimentary cores drilled at the lake and a trench dug at the shore of the prehistorical Ohalo–II site. During the past 28 kyrs either laminated or massive fine-grained sediments were deposited in the lake comprising primary calcites and fine-grain detritus. Sr/Ca, Mg/Ca, 87 Sr/ 86 Sr ratios and δ 18 O values of live and fossil ostracod shells (Cyprideis torosa) and primary calcites together with XRD, grain-size, and carbonate content analyses indicate contribution of the following types of waters to the lake: (1) Jordan River; (2) Regional runoff; and (3) Ca-chloride brines (currently comprises the Tiberias Spa brine). During the last glacial period (∼28-24 ka) the lake rose to its highest stand of ∼170 m below sea level (bsl), expanding over the Kinnarot Basin and converging with the southern hypersaline Lake Lisan. At that time, waters were mainly supplied to the lake by the Jordan River and regional runoff with enhanced contribution of the Dead Sea Ca-chloride brine. Primary calcites were precipitated from the lake's solution forming sequences of laminated sediments on the lake's floor. At ∼24-22 ka (coinciding with Heinrich event H2 at the North Atlantic) the lake retreated below the modern level (of ∼214 m bsl), depositing mainly flood-related sediments at its margins. The lake slightly rose during the Younger Dryas and subsequently declined towards the modern level with decreasing contributions of the Jordan River waters, brines and regional runoff, reflecting a continuous aridification of the region during the Holocene. © 2019 Elsevier Ltd
英文关键词	East Mediterranean; Geochemistry; Lake Kinneret; Late Quaternary; Levant; Ostracods; Paleo-limnology; Sr and O isotopes
语种	英语
scopus关键词	Animals; Calcite; Chlorine compounds; Geochemistry; Rivers; Runoff; Sea level; Sedimentology; Sediments; East Mediterranean; Lake Kinneret; Late quaternary; Levant; Ostracods; Lakes; aridification; fossil record; geochemistry; Heinrich event; Holocene; lacustrine deposit; Last Glacial; ostracod; oxygen isotope; paleolimnology; Quaternary; river water; runoff; sea level change; shell; strontium isotope; Younger Dryas; Atlantic Ocean; Atlantic Ocean (North); Dead Sea; Israel; Jordan Basin; Kinnarot Basin; Levantine Sea; Mediterranean Sea; Mediterranean Sea (East); Northern District; Sea of Galilee; Cyprideis torosa; Ostracoda
来源期刊	Quaternary Science Reviews
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/151991
作者单位	Geological Survey of Israel, 30 Malkhe Israel St, Jerusalem, 9550161, Israel; Department of Geophysical and Planetary Sciences, Tel Aviv University, P.O. Box 39040, Tel Aviv, 6997801, Israel; Institute of Earth Sciences, The Hebrew University, Givat Ram, Jerusalem, Israel; Department of Earth Sciences and the Limnological Research Center, University of Minnesota, 310 Pillsbury Drive SE, Minneapolis, MN 55455, United States
推荐引用方式 GB/T 7714	Lev L.,Stein M.,Ito E.,et al. Sedimentary; geochemical and hydrological history of Lake Kinneret during the past 28;000 years[J],2019,209.
APA	Lev L.,Stein M.,Ito E.,Fruchter N.,Ben-Avraham Z.,&Almogi-Labin A..(2019).Sedimentary; geochemical and hydrological history of Lake Kinneret during the past 28;000 years.Quaternary Science Reviews,209.
MLA	Lev L.,et al."Sedimentary; geochemical and hydrological history of Lake Kinneret during the past 28;000 years".Quaternary Science Reviews 209(2019).