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Late Quaternary Geological History of the Dead Sea Area, Israel

Published online by Cambridge University Press:  20 January 2017

Y. Yechieli ,
M. Magaritz ,
Y. Levy ,
U. Weber ,
U. Kafri ,
W. Woelfli  and
G. Bonani
Y. Yechieli
Affiliation:
Department of Environmental Science and Energy Research, Weizmann Institute of Science, Rehovot 76100, Israel
M. Magaritz
Affiliation:
Department of Environmental Science and Energy Research, Weizmann Institute of Science, Rehovot 76100, Israel
Y. Levy
Affiliation:
Geological Study of Israel, 30 Malkhei Israel, Jerusalem 95501, Israel
U. Weber
Affiliation:
Department of Environmental Science and Energy Research, Weizmann Institute of Science, Rehovot 76100, Israel
U. Kafri
Affiliation:
Geological Survey of Israel, 30 Malkhei Israel, Jerusalem 95501 Israel
W. Woelfli
Affiliation:
Institut fur Mittelenergiephysik, ETH-Honggerberg, 8093 Zurich, Switzerland
G. Bonani
Affiliation:
Institut fur Mittelenergiephysik, ETH-Honggerberg, 8093 Zurich, Switzerland
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Abstract

A 34.5 m borehole, which was drilled near the Dead Sea coast (altitude -394 m) in the southern part of the fan delta of Wadi Zeelim, reveals the geological history of that area from the latest Pleistocene to present. The depositional time frame is based on six 14C dates and two U-Th dates. An erosional (or nondepositional) period is implied by the hiatus between 21,100 yr B.P. (U-Th age, depth 33 m) and 11,315 yr B.P. (14C age, depth 32 m). A subsequent arid phase is recorded by a 6.5-m-thick layer of halite; based on 14C dates this phase relates to the abrupt Younger Dryas cold period reported in temperate to polar regions. The fragility of the environment in this region is indicated by the fact that the region experienced such a severe, short aridification phase (less than 1000 yr), evidence of which is found widely in the desert fringes of the Middle East and North Africa. The aragonite found in most of the Holocene section indicates that the well site was covered by the lake for most of the Holocene. Exceptions are the intervals at 0-3 and 10-14 m depths which represent low stands of the lake.

Type
Articles
Information
Quaternary Research , Volume 39 , Issue 1 , January 1993 , pp. 59 - 67
Copyright
University of Washington

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References

Almogi-Labin, A. Hemleben, C Meischner, D., and Erlenkeuser, H. (1991). Paleoenvironmental events during (he last 13,000 years in the central Red Sea as recorded by Pteropoda. Paleoceanography 6(1), 83–98.CrossRefGoogle Scholar
Banin, A., and Amiel, A. (1969). A correlative study of the chemical and physical properties of a group of natural soils of Israel. Geo-dermal, 185–198.Google Scholar
Bard, E. Hamelin, B. Fairbanks, R. G., and Zindler, A. (1990). Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U-Th ages from Barbados corals. Nature 345, 405–410.CrossRefGoogle Scholar
Bar-Yosef, O. (1987). Prehistory of the Jordan rift. Israel Journal of Earth Science 36, 107–119.Google Scholar
Begin, Z. B. Broecker, W. Buchbinder, B. Druckman, Y. Kaufman, A. Magaritz, M., and Neev, D. (1985). Dead Sea and Lake Lisan levels in the last 30,000 years: A preliminary report. Israel Geological Survey Report 29/85, 1–18.Google Scholar
Begin, Z. B. Ehrlich, A., and Nathan, Y. (1974). Lake Lisan, the Pleistocene precursor of the Dead Sea. Geological Survey of Israel Bulletin 63, 30.Google Scholar
Berger, W. H. (1990). The Younger Dryas cold spell — A quest for causes. Palaeogeography, Paiaeocltmatology, Palaeoecology (Global and Planetary Change Section), 89, 219–237.CrossRefGoogle Scholar
Broecker, W. S. Kennett, J. P. Flower, B. P. Teller, J. T. Trumbore, S. Bonani, G., and Wolfli, W. (1989). Routing of meltwater from the Laurentide Ice Sheet during the Younger Dryas cold episode. Nature 341, 318–321.CrossRefGoogle Scholar
Druckman, Y. Magaritz, M., and Sneh, A. (1987). The shrinking of Lake Lisan, as reflected by the diagenesis of its marginal oolithic deposits. Israel Journal of Earth Science 36, I0I–I06.Google Scholar
Engstrom, D. R. Hansen, B. C. S., and Wright, H. E. Jr. (1990). A possible Younger Dryas record in southeastern Alaska. Science 250, 1383–1385.CrossRefGoogle ScholarPubMed
Frumkin, A. Magaritz, M. Carmi, I., and Zak, I. (1991). The Holocene climatic record of the salt caves of Mount Sedom, Israel. Holocene, 1, 191–200.CrossRefGoogle Scholar
Garber, R. A. Levy, Y., and Friedman, G. M. (1987). The sedimentol-Ogyof the Dead Sea. Carbonates and Evaporites 2(1), 43–57.CrossRefGoogle Scholar
Gardosh, M., and Mor, U. (1988). “Tectonic and Stratigraphic Phases in the Northeastern Margins of the Dead Sea Basin.” Israel Geological Society Meeting, En Bokek. Field trip guide., pp. 83–110.Google Scholar
Gat, J. R., and Magaritz, M. (1980). Climatic variations in the eastern Mediterranean Sea area. Naturwissenschaften 67, 80–87.CrossRefGoogle Scholar
Gillespie, R. Street-Perrott, F. A., and Switsur, R. (1983). Post-glacial arid episodes in Ethiopia have implications for climatic prediction. Nature 306, 680–683.CrossRefGoogle Scholar
Goldberg, P. (1977). Late Quaternary stratigraphy of Gebel Maghara. Qedem, 7, 11–31.Google Scholar
Goldberg, P., and Bar-Yosef, O. (1982). Environmental and archaeological evidence for climatic changes in the southern Levant. British Archaeological Reports, International Series 133, 399–414.Google Scholar
Goodfriend, G. A., and Magaritz, M. (1988). Paleosols and late Pleis– tocene rainfall fluctuations in the Negev Desert. Nature 332, 144–146.CrossRefGoogle Scholar
Heusser, C. J., and Rabassa, J. (1987). Cold climatic episode of Younger Dryas age in Tierra del Fuego. Nature 328, 609–611.CrossRefGoogle Scholar
Horowitz, A. (1979). “The Quaternary of Israel.” Academic Press, New York.Google Scholar
Katz, A., and Kolodny, N. (1989). Hypersaline brine diagenesis and evolution in the Dead Sea-Lake Lisan system (Israel). Geochimica et Cosmochimica Acta 53, 59–67.CrossRefGoogle Scholar
Katz, A. Kolodny, Y., and Nissenbaum, A. (1977). The geochemical evolution of the Pleistocene Lake Lisan-Dead Sea system. Geochi-mica et Cosmochimica Acta 41, 1609–1626.CrossRefGoogle Scholar
Kaufman, A. (1971). U-series dating of Dead Sea basin carbonates. Geochimica et Cosmochimica Acta 35, 1269–1281.CrossRefGoogle Scholar
Klein, C. (1985). “Fluctuation of the Levels of the Dead Sea and Climatic Fluctuation in the Country during Historical Times.’” International Association of Hydrological Science. International Symposium on Scientific Basis for Water Resources Management, Jerusalem, September 19–23. Additional Paper and Posters Summaries, Vol. 2, pp. 197–224.Google Scholar
Kudrass, H. R. Erlenkeuser, H. Vollbrecht, R., and Weiss, W. (1991). Global nature of the Younger Dryas cooling event inferred from oxygen isotope data from Sulu Sea cores. Nature 349, 406–409.CrossRefGoogle Scholar
Leroi-Gourhan, A. (1981). Diagrammes polliniques de sites arche-ologiques au Moyen-Orient. In “Beitrage zur Umweltgeschichte des Vorderen Orients” (Frey, W. and Uerpmann, H. P., Eds.), Vol. 8, pp. 121–133. Beihefte zum Tubinger Atlas des Vorderen Orients, Reihe A (Naturwissenschaften). Google Scholar
Leroi-Gourhan, A., and Darmon, F. (1987). Analyses palynologiques de sites archeologiques de Pleistocene final dans la Vallee du Jourdain. Israel Journal of Earth Science 36, 65–72.Google Scholar
Levy, Y. (1988). Sedimentary reflections of the modern (1983/85) halite precipitation from the Dead Sea. Israel Geological Survey Report 12/88.Google Scholar
Macumber, P. G., and Head, M. J. (1991). Implications of the Wadi al-Hammeh sequences for the terminal drying of Lake Lisan, Jordan. Palaeogeography, Palaeoclimatology, Palaecology 84, 163–173.CrossRefGoogle Scholar
Magaritz, M. (1986). Environmental changes recorded in the Upper Pleistocene along the desert boundary, southern Israel. Palaeogeog-raphy, Palaeoclimatology, Paiaeoecoiogy 53, 213–229.CrossRefGoogle Scholar
Magaritz, M., and Enzel, Y. (1990). Standing-water deposits as indicators of late Quaternary dune migration in the northwestern Negev, Israel. Climatic Change 16, 307–318.CrossRefGoogle Scholar
Magaritz, M., and Goodfriend, G. A. (1987). Movement of the desert boundary in the Levant from latest Pleistocene to early Holocene. In “Abrupt Climatic Change—Evidence and Implications,” pp. 173–183. Reidel, Holland.CrossRefGoogle Scholar
Magaritz, M., and Heller, J. (1980). A desert migration indicator-Oxygen isotopic composition of land snail shells. Palaeogeography, Palaeoclimatology, Paiaeoecoiogy 32, 153–162.CrossRefGoogle Scholar
Manspeizer, W. (1985). The Dead Sea rift: Impact of climate and tec-tonism on Pleistocene and Holocene sedimentation. In “Strike Slip Deformation, Basin Formation, and Sedimentation” (Biddle, K. T. and Chritie-Blick, N., Eds.), pp. 143–158. S.E.P.M. Special Publication 37.CrossRefGoogle Scholar
Moore, A, M. T. (1979). A pre-Neolithic farmers’ village on the Euphrates. Scientific American 241, 62–70.CrossRefGoogle Scholar
Neev, D. (1964). “Recent Sedimentary Processes in the Dead Sea.” Unpublished Ph.D. dissertation, Hebrew University.Google Scholar
Neev, D., and Emery, K. O. (1967). The Dead Sea: Depositional processes and environments of evaporites. Israel Geological Survey Bulletin 41, 147.Google Scholar
Neev, D., and Hall, J. (1977). Climatic fluctuations during the Holocene as reflected by the Dead Sea levels. In “Desertic Terminal Lakes” (Greer, D., Ed.), pp. 53–60. Utah State Univ., Logan.Google Scholar
Overpeck, J. T. Peterson, L. C Kipp, N. Inbrie, J., and Rind, D. (1989). Climate change in the circum-North Atlantic region during the last deglaciation. Nature 338, 553–557.CrossRefGoogle Scholar
Roberts, N. (1982). Lake levels as an indicator of Near Eastern palaeo-climates: A preliminary appraisal. In “Palaeoclimates, Palaeoenvi-ronments and Human Communities in the Eastern Mediterranean Region in Later Prehistory” (Bintliff, J. L. and van Zeist, W., Eds.), pp. 235–267. Oxford B.A.R. International Series No. 133, Part 1.Google Scholar
Rossignol-Strick, M. Nesteroff, W. Olive, P., and Vergnaud-Grazzini, E. (1982). After the deluge: Mediterranean stagnation and sapropel formation. Nature 295, 105–110.CrossRefGoogle Scholar
Schuldenrein, J., and Goldberg, P. (1981). Late Quaternary paleoenvi-ronments and prehistoric site distributions in the lower Jordan Valley: A preliminary report. Paleorient 7, 57–71.CrossRefGoogle Scholar
Smith, G. I. (1979). “Subsurface Stratigraphy and Geochemistry of Late Quaternary Evaporites, Searles Lake, California.” U.S. Geo-logical Survey Professional Paper 1043.Google Scholar
Smith, G. I., and Street-Perrott, F. A. (1983). Pluvial lakes of the Western United States. In “Late Quaternary environments of the United States. The Late Pleistocene.” (Porter, S. C., Ed.), Vol. 1. Univ. Minnesota Press.Google Scholar
Sneh, A. (1979). Late Pleistocene fan deltas along the Dead Sea rift. Journal of Sedimentary Petrology 49, 541–552.Google Scholar
Stiller, M. Carmi, I., and Kaufman, A. (1988). Organic and inorganic 14C concentrations in the sediments of Lake Kinneret and the Dead Sea (Israel) and the factors which control them. Chemical Geology (Isotope Geoscience Section) 73, 63–78.CrossRefGoogle Scholar
Street, F. A., and Grove, A. T. (1979). Global maps of lake-level fluctuations since 30,000 yr B.P. Quaternary Research 12, 83–118.CrossRefGoogle Scholar
Street-Perrott, F. A., and Roberts, N. (1983). Fluctuations in the closed-basin lakes as an indicator of past atmospheric circulation patterns. In “Variations in the Global Water Budget” (Street-Perrott, F. A. Beran, M., and Radcliffe, R. A. S., Eds.), pp. 331–345. D. Reidel, Dordrecht.CrossRefGoogle Scholar
Tchemov, E., and Bar-Yosef, O. (1982). Animal exploitation in the Pre-pottery Neolithic B period at Wadi Tbeik, southern Sinai. Pale-orient 8, 17–37.Google Scholar
Yechieli, Y. (1987). “The Geology of the Northern Arava Rift and the Mahmal Anticline, Hazeva Area.” Unpublished M.Sc. thesis, The Geological Survey of Israel, Jerusalem. (In Hebrew, English sum-mary) Google Scholar
Yechieli, Y. Magaritz, M. Levy, Y. Weber, U., and Kafri, U. (1990). “Chemical Processes at the Interface between Dead Sea Water and the Aquifers in Its Vicinity.” Semi-annual report presented to the Ministry of Energy and Infrastructure, January, 1990.Google Scholar
Zak, I. (1967). “The Geology of Mount Sedom.” Unpublished Ph.D. thesis., Hebrew University of Jerusalem. (In Hebrew, English summary) Google Scholar