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New Dates from Submerged Late Pleistocene Sediments in the Southern Sea of Galilee, Israel

Published online by Cambridge University Press:  18 July 2016

D Nadel ,
S Belitzky ,
E Boaretto ,
I Carmi ,
J Heinemeier ,
E Werker  and
S Marco
D Nadel
Affiliation:
Zinman Institute of Archaeology, Haifa University.
S Belitzky
Affiliation:
Department of Archaeology, The Hebrew University of Jerusalem
E Boaretto
Affiliation:
Environmental Science and Energy Research, Weizmann Institute
J Heinemeier
Affiliation:
14C AMS Laboratory, Aarhus University
E Werker
Affiliation:
Department of Botany, The Hebrew University of Jerusalem
S Marco
Affiliation:
Department of Geophysics and Planetary Sciences, Tel Aviv University, Ramat Aviv, Tel Aviv 96978, Israel
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Abstract

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Unusual 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.

Type
Near East Chronology: Archaeology and Environment
Information
Radiocarbon , Volume 43 , Issue 3: Proceedings of the 17th International Radiocarbon Conference (Part 3 of 3) , 2001 , pp. 1167 - 1178
Copyright
Copyright © 2001 The Arizona Board of Regents on behalf of the University of Arizona 

References

Bard, E, Rostek, F, Turon, JL, Gendreau, S. 2000. Hydrological impact of Heinrich events in the subtropical northeast Atlantic. Science 289:1321–24.CrossRefGoogle ScholarPubMed
Bar-Mathews, M, Ayalon, A, Kaufman, A. 1997. Late Quaternary paleoclimate in the eastern Mediterranean region from stable isotope analysis of speleothems at Soreq Cave, Israel. Quaternary Research 47:155–68.Google Scholar
Bar-Mathews, M, Ayalon, A, Kaufman, A, Wasserburg, GJ. 1999. The eastern Mediterranean paleoclimate as a reflection of regional events: Soreq Cave, Israel. Earth and Planetary Science Letters 166:85–95.Google Scholar
Bar-Yosef, O, Nadel, D. 1988. Ohalo—a prehistoric site in the Sea of Galilee. Mitekufat Haeven, Journal of the Israel Prehistoric Society 21:87–94.Google Scholar
Begin, ZB, Ehrlich, A, Nathan, Y. 1974. Lake Lisan, the Pleistocene precursor of the Dead Sea. Ministry of Commerce and Industry, Geological Survey, Bulletin nr 63, Jerusalem.Google Scholar
Ben-Arieh, Y. 1965. The shift of the outlet of the Jordan at the southern shore of Lake Tiberias. Palestine Exploration Quarterly: 54–65.Google Scholar
Ben-Avraham, Z, Ten Brink, U, Bell, R, Reznikov, M. 1996. Gravity field over the Sea of Galilee: evidence for a composite basin along a transform fault. Journal of Geophysical Research 101(B1):533–44.Google Scholar
Bottema, S, van Zeist, W. 1981. Palynological evidence for the climatic history of the Near East 50,000–6,000 BP. In: Cauvin, J, Sanlaville, P, editors. Prehistoire du Levant. Paris: CNRS. p 111–32.Google Scholar
Garfunkel, Z. 1981. Internal structure of the Dead Sea transform (rift) in relation to plate kinematics. Tectonophysics 80:80–108.Google Scholar
Horowitz, A. 1978. The Quaternary evolution of the Jordan Valley: In: Serruya, C, editor. Lake Kinneret, monografiae biologicae 32:33–43.Google Scholar
Horowitz, A. 1979. The Quaternary of Israel. New York: Academic Press.Google Scholar
Kislev, ME, Nadel, D, Carmi, I. 1992. Epipalaeolithic (19,000 BP) cereal and fruit diet at Ohalo II, Sea of Galilee, Israel. Review of Palaeobotany and Palynology 73:161–6.Google Scholar
Kitagawa, H, van der Plicht, J. 1998. Atmospheric radiocarbon calibration to 45,000 BP: late glacial fluctuations and cosmogenic isotope production. Science 279:1187–90.Google Scholar
Marchitto, TM, Curry, WB, Oppo, DW. 1998. Millennial–scale changes in North Atlantic circulation since the last glaciation. Nature 393:557–61.Google Scholar
Marco, S, Rockwell, T, Heimann, A, Agnon, A, Ellenblum, R. 2000. Historical earthquakes deformations revealed by 3-D trenching on Dead Sea Transform. In: Okumura, K, Takada, K, Goto, H, editors. Active fault research for the new millennium. Proceedings of the Hokudan International Symposium and Scholl on Active Faulting. Hokudan Co. Ltd. p 261–3.Google Scholar
Marcus, E, Slager, J. 1985. The sedimentary-magmatic sequence of the Zemah–1 well (Jordan–Dead Sea Rift, Israel) and its emplacement in time and space. Israel Journal of Earth Science 34:1–10.Google Scholar
McCabe, AM, Clark, PU. 1998. Ice–sheet variability around the North Atlantic Ocean during the last deglaciation. Nature 392:373–7.Google Scholar
Nadel, D. 1993. Submerged archaeological sites on the shores of Lake Kinneret, Israel. 'Atiqot (English Series) XXII:1–12.Google Scholar
Nadel, D. 1996. The organization of space in a fisher-hunter-gatherers camp at Ohalo II, Israel. In: Otte, M, editor. Nature et Culture, Colloque de Liege. Liege: E.R.A.U.L. 68. p 373–88.Google Scholar
Nadel, D, Hershkovitz, I. 1991. New subsistence data and human remains from the earliest Levantine Epipalaeolithic. Current Anthropology 32(5):631–5.Google Scholar
Nadel, D, Danin, A, Werker, E, Schick, T, Kislev, ME, Stewart, K. 1994. 19,000-years-old twisted fibers from Ohalo II. Current Anthropology 35(4):451–8.CrossRefGoogle Scholar
Nadel, D, Carmi, I, Segal, D. 1995. Radiocarbon dating of Ohalo II: archaeological and methodological implications. Journal of Archaeological Science 22(6):811–22.Google Scholar
Nadel, D, Werker, E. 1999. The oldest ever brush hut plant remains from Ohalo II, Jordan Valley, Israel (19,000 BP). Antiquity 73 (282):755–64.Google Scholar
Neev, D, Emery, KO. 1967. The Dead Sea. Bulletin of the Geological Survey of Israel 41. Jerusalem.Google Scholar
Neftel, A, Oeschger, H, Staffelbach, T, Stauffer, B. 1988. CO2 record in the Byrd ice core 50,000–5,000 BP. Nature 331:609–11.Google Scholar
Nun, M. 1991. The Sea of Galilee. Water levels, past and present. Kibbutz Ein Gev: Tourist Department and Kinnereth Sailing Co.Google Scholar
Shroder, JF, Bishop, M P, Kornwell, KJ, Inbar, M. 1999. Catastrophic geomorphic processes and Bethsaida archaeology, Israel. In: Arav, R, Freund, RA, editors. Bethsaida, a city by the north shore of the Sea of Galilee. Volume 2. Truman State University Press.Google Scholar
Simchoni, O. 1997. Reconstruction of the landscape and human economy 19,000 BP in the Upper Jordan Valley by the botanical remains found at Ohalo II. [Unpublished PhD Thesis, Bar-Ilan University, Ramat Gan]. In Hebrew.Google Scholar
Weinstein-Evron, M. 1993. Palaeoecological reconstructions of the Upper Palaeolithic in the Levant. In: Pavuk, J, editor. Actes du XIIe Congres International des Sciences Prehistoriques et Protohistoriques. Bratislava. p 259–70.Google Scholar