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dc.contributor.authorNadel, D.
dc.contributor.authorBelitzky, S.
dc.contributor.authorBoaretto, E.
dc.contributor.authorCarmi, I.
dc.contributor.authorHeinemeier, J.
dc.contributor.authorWerker, E.
dc.contributor.authorMarco, S.
dc.date.accessioned2021-02-11T21:32:32Z
dc.date.available2021-02-11T21:32:32Z
dc.date.issued2001-01-01
dc.identifier.citationNadel, D., Belitzky, S., Boaretto, E., Carmi, I., Heinemeier, J., Werker, E., & Marco, S. (2001). New dates from submerged late Pleistocene sediments in the southern Sea of Galilee, Israel. Radiocarbon, 43(3), 1167-1178.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200038467
dc.identifier.urihttp://hdl.handle.net/10150/654540
dc.descriptionFrom the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000.
dc.description.abstractUnusual low water levels in the Sea of Galilee (Dead Sea Fault, Israel) have caused the recent exposure of submerged Late Pleistocene prehistoric sites and lacustrine sediments along the southern shores of the lake. The Ohalo II site is a large fisher-hunter-gatherers camp with in-situ brush hut floors, hearths, and a human grave. The site is radiometrically dated by 25 charcoal dates to 19,430 BP (average, uncalibrated). The archaeological remains include quantities of excellently preserved organic remains. These would not have been preserved without a rapid rise of lake level immediately after the occupation, covering the remains with silts and sand. Recently a concentration of eight tree trunks were found about 1.5 km south of Ohalo II, of which five trunks were identified as Salix species and dated as a single accumulation at about 16,100 BP. The trunks, too, had to be submerged quickly together to ensure excellent preservation. The camp and the trunks were found at –212/–213 m, almost 4 m below modern high water levels. We suggest that the finds represent two separate episodes of deposition during low lake levels, almost 3,000 radiocarbon years apart, each followed by an abrupt water rise. It is possible that climatic changes caused the observed fluctuations, though earthquakes (blocking or lowering the Jordan outlet, for example) cannot be ruled out.
dc.language.isoen
dc.publisherDepartment of Geosciences, The University of Arizona
dc.relation.urlhttp://radiocarbon.webhost.uits.arizona.edu/
dc.rightsCopyright © by the Arizona Board of Regents on behalf of the University of Arizona. All rights reserved.
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.titleNew Dates from Submerged Late Pleistocene Sediments in the Southern Sea of Galilee, Israel
dc.typeProceedings
dc.typetext
dc.identifier.journalRadiocarbon
dc.description.collectioninformationThe Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information.
dc.eprint.versionFinal published version
dc.description.admin-noteMigrated from OJS platform February 2021
dc.source.volume43
dc.source.issue3
dc.source.beginpage1167
dc.source.endpage1178
refterms.dateFOA2021-02-11T21:32:32Z


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