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9 - Palaeoenvironmental and limnological reconstruction of Lake Lisan and the Dead Sea

from Part II - The palaeoenvironmental record

Published online by Cambridge University Press:  26 April 2011

Stuart Black
Affiliation:
University of Reading
Stuart Robinson
Affiliation:
University College London
Richard Fitton
Affiliation:
Talisman Energy Inc.
Rachel Goodship
Affiliation:
University of Reading
Claire Rambeau
Affiliation:
University of Reading
Bruce Sellwood
Affiliation:
University of Reading
Steven Mithen
Affiliation:
University of Reading
Emily Black
Affiliation:
University of Reading
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Summary

ABSTRACT

Lake Lisan existed between 75 and 14 ka BP and provides a unique opportunity for investigating climate change for the southern Levant region. The exposures of Lake Lisan deposits on the eastern shores of the current Dead Sea have received limited study in comparison to the western shores. Here we present new U-series and elevation data for a sequence of Lisan deposits ranging between 25 and 8 ka BP. The data show an elevation–age record consistent with previously published data while providing new information about the extent of decrease in lake levels in the Late Pleistocene and early Holocene. All dates cited in this chapter are calibrated; those that were uncalibrated in their original publications were calibrated using the online OxCAL program.

INTRODUCTION

Lake Lisan existed from approximately 70 to 15 cal ka BP (see Kaufman, 1971, Kaufman et al., 1992, Schramm et al., 2000; Hasse-Schramm et al., 2004 and references therein) and extended up to 200 km along the Dead Sea Transform at its highest levels (Hazan et al., 2005; Chapter 6, this volume; Figures 9.1, 9.2). During its history, the lake fluctuated between highstands of 165–180 mbsl (metres below sea level) and lowstands of perhaps as much as 700 mbsl (Chapter 6, this volume; Begin et al., 1985, Bartov et al., 2002).

Type
Chapter
Information
Water, Life and Civilisation
Climate, Environment and Society in the Jordan Valley
, pp. 113 - 128
Publisher: Cambridge University Press
Print publication year: 2011

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References

Abed, A. M. and Yaghan, R. (2000) On the paleoclimate of Jordan during the last glacial maximum. Palaeogeography Palaeoclimatology Palaeoecology 160: 23–33.CrossRefGoogle Scholar
Bar-Matthews, M., Ayalon, A., Gilmour, M., Matthews, A. and Hawkesworth, C. J. (2003) Sea–land oxygen isotopic relationships from planktonic foraminifera and speleothems in the Eastern Mediterranean region and their implication for paleorainfall during interglacial intervals. Geochimica et Cosmochimica Acta 67: 3181–3199.CrossRefGoogle Scholar
Bartov, Y., Stein, M., Enzel, Y., Agnon, A. and Reches, Z. (2002) Lake levels and sequence stratigraphy of Lake Lisan, the late Pleistocene precursor of the Dead Sea. Quaternary Research 57: 9–21.CrossRefGoogle Scholar
Bartov, Y., Goldstein, S. L., Stein, M. and Enzel, Y. (2003) Catastrophic arid episodes in the Eastern Mediterranean linked with the North Atlantic Heinrich events. Geology 31: 439–442.2.0.CO;2>CrossRefGoogle Scholar
Begin, Z. B. (2002) Computer simulation of salinity in the Quaternary Lake Lisan. Israel Journal of Earth Sciences 51: 225–232.CrossRefGoogle 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
Begin, Z. B., Broecker, W., Buchbinder, B.et al. (1985) Dead Sea and Lake Lisan levels in the last 30,000 years: a preliminary report. Israel Geological Survey Report 29/85.
Begin, Z. B., Stein, M., Katz, A.et al. (2004) Southward migration of rain tracks during the last glacial, revealed by salinity gradient in Lake Lisan (Dead Sea rift). Quaternary Science 23: 1627–1636.Google Scholar
Bischoff, J. L. and Fitzpatrick, J. A. (1991) U-series dating of impure carbonates – an isochron technique using total-sample dissolution. Geochimica et Cosmochimica Acta 55: 543–554.CrossRefGoogle Scholar
Bookman, R., Enzel, Y., Agnon, A. and Stein, M. (2004) Late Holocene lake levels of the Dead Sea. Geological Society of America Bulletin 116: 555–571.CrossRefGoogle Scholar
Bourdon, B., Turner, S., Henderson, G. M. and Lundstrom, C. C. (2003) Introduction to U series geochemistry. In Uranium-Series Geochemistry, Reviews in Mineralogy and Geochemistry, ed. Bourdon, B., Turner, S., Henderson, G. M. and Lundstrom, C. C.. Washington DC: Mineralogical Society of America.Google Scholar
Candy, I. and Black, S. (2009) The timing of Quaternary calcrete development in semi-arid southeast Spain: investigating the role of climate on calcrete genesis. Sedimentary Geology 218: 6–15.CrossRefGoogle Scholar
Candy, I., Black, S. and Sellwood, B. (2005) U-series isochron dating of immature and mature calcretes as a basis for constructing Quaternary landform chronologies for the Sorbas basin, southeast Spain. Quaternary Research 64: 100–111.CrossRefGoogle Scholar
Druckman, Y., Magaritz, M. and Sneh, A. (1987) The shrinking of Lake Lisan, as reflected by the diagenesis of its marginal oolitic deposits. Israel Journal of Earth Sciences 36: 101–106.Google Scholar
Edwards, R. L., Gallup, C. D. and Cheng, H. (2003) Uranium-series dating of marine and lacustrine carbonates. In Uranium-Series Geochemistry, Reviews in Mineralogy and Geochemistry, ed. Bourdon, B., Turner, S., Henderson, G. M. and Lundstrom, C. C.. Washington DC: Mineralogical Society of America.Google Scholar
Emeis, K. C., Struck, U., Schulz, H. M.et al. (2000) Temperature and salinity variations of Mediterranean Sea surface waters over the last 16,000 years from records of planktonic stable oxygen isotopes and alkenone unsaturation ratios. Palaeogeography Palaeoclimatology Palaeoecology 158: 259–280.CrossRefGoogle Scholar
Enzel, Y., Bookman, R., Sharon, D.et al. (2003) Late Holocene climates of the Near East deduced from Dead Sea level variations and modern regional winter rainfall. Quaternary Research 60: 263–273.CrossRefGoogle Scholar
Freund, R., Garfunkel, Z., Zak, I., Goldberg, M., Weissbrod, T. and Derin, B. (1970) The shear along the Dead Sea rift. Philosophical Transactions of the Royal Society of London A. 267: 107–130.CrossRefGoogle Scholar
Garfunkel, Z. (1981) Internal structure of the Dead-Sea leaky transform (rift) in relation to plate kinematics. Tectonophysics 80: 81–108.CrossRefGoogle Scholar
Garfunkel, Z. and BenAvraham, Z. (1996) The structure of the Dead Sea basin. Tectonophysics 266: 155–176.CrossRefGoogle Scholar
Gvirtzman, G. and Wieder, M. (2001) Climate of the last 53,000 years in the eastern Mediterranean, based on soil-sequence stratigraphy in the coastal plain of Israel. Quaternary Science Reviews 20: 1827–1849.CrossRefGoogle Scholar
Hasse-Schramm, A., Goldstein, S. L. and Stein, M. (2004) U-Th dating of Lake Lisan (late Pleistocene Dead Sea) aragonite and implication for glacial East Mediterranean climate change. Geochimica et Cosmochimica Acta 68: 985–1005.CrossRefGoogle Scholar
Hazan, N., Stein, M., Agnon, A.et al. (2005) The late quaternary limnological history of Lake Kinneret (Sea of Galilee), Israel. Quaternary Research 63: 60–77.CrossRefGoogle 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
Kaufman, A. (1971) U-series dating of Dead Sea Basin carbonates. Geochimica et Cosmochimica Acta 35: 1269–1281.CrossRefGoogle Scholar
Kaufman, A., Yechieli, Y. and Gardosh, M. (1992) Reevaluation of the lake-sediment chronology in the Dead Sea Basin, Israel, based on new 230Th/U dates. Quaternary Research 38: 292–304.CrossRefGoogle Scholar
Klein-BenDavid, O., Sass, E. and Katz, A. (2004) The evolution of marine evaporitic brines in inland basins: the Jordan–Dead Sea Rift valley. Geochimica et Cosmochimica Acta 68: 1763–1775.CrossRefGoogle Scholar
Klinger, Y., Avouac, J. P., Bourles, D. and Tisnerat, N. (2003) Alluvial deposition and lake-level fluctuations forced by Late Quaternary climate change: the Dead Sea case example. Sedimentary Geology 162: 119–139.CrossRefGoogle Scholar
Kolodny, Y., Stein, M. and Machlus, M. (2007) Sea-rain-lake relation in the Last Glacial East Mediterranean revealed by δ18O-δ13C in Lake Lisan aragonites. Geochimica et Cosmochimica Acta 71: 3926–3927.CrossRefGoogle Scholar
Landmann, G., Abu Qudaira, G. M., Shawabkeh, K., Wrede, V. and Kempe, S. (2002) Geochemistry of the Lisan and Damya Formations in Jordan, and implications for palaeoclimate. Quaternary International 89: 45–57.CrossRefGoogle Scholar
Luo, S. and Ku, T. L. (1991) U-series isochron dating: a generalized method employing total-sample dissolution. Geochimica et Cosmochimica Acta 55: 555–564.CrossRefGoogle Scholar
Machlus, M., Enzel, Y., Goldstein, S. L., Marco, S. and Stein, M. (2000) Reconstructing low levels of Lake Lisan by correlating fan-delta and lacustrine deposits. Quaternary International 73–4: 137–144.CrossRefGoogle 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 Palaeoecology 84: 163–173.CrossRefGoogle Scholar
Marco, S. and Agnon, A. (2005) High-resolution stratigraphy reveals repeated earthquake faulting in the Masada Fault Zone, Dead Sea Transform. Tectonophysics 408: 101–112.CrossRefGoogle Scholar
McLaren, S. J., Gilbertson, D. D., Grattan, J. P.et al. (2004) Quaternary palaeogeomorphologic evolution of the Wadi Faynan area, southern Jordan. Palaeogeography Palaeoclimatology Palaeoecology 205: 131–154.CrossRefGoogle Scholar
Migowski, C., Agnon, A., Bookman, R., Negendank, J. F. W. and Stein, M. (2004) Recurrence pattern of Holocene earthquakes along the Dead Sea transform revealed by varve-counting and radiocarbon dating of lacustrine sediments. Earth and Planetary Science Letters 222: 301–314.CrossRefGoogle Scholar
Neev, D. and Emery, K. O. (1967) The Dead Sea. Geological Society of Israel Bulletin 41: 1–147.Google Scholar
Neev, D. and Emery, K. O. (1995) The Destruction of Sodom, Gomorragh, and Jericho. New York: Oxford University Press.Google Scholar
Prasad, S., Vos, H., Negendank, J. F. W.et al. (2004) Evidence from Lake Lisan of solar influence on decadal- to centennial-scale climate variability during marine oxygen isotope stage 2. Geology 32: 581–584.CrossRefGoogle Scholar
Robinson, S. A., Black, S., Sellwood, B. and Valdes, P. J. (2006) A review of palaeoclimates and palaeoenvironments in the Levant and Eastern Mediterranean from 25,000 to 5000 years BP: setting the environmental background for the evolution of human civilisation. Quaternary Science Reviews 25: 1517–1541.CrossRefGoogle Scholar
Schramm, A., Stein, M. and Goldstein, S. L. (2000) Calibration of the C-14 time scale to > 40 ka by 234U-230Th dating of Lake Lisan sediments (last glacial Dead Sea). Earth and Planetary Science Letters 175: 27–40.CrossRefGoogle Scholar
Sneh, A. (1979) Late Pleistocene fan-deltas along the Dead Sea rift. Journal of Sedimentary Petrology 49: 541–552.Google Scholar
Stein, M. (2001) The sedimentary and geochemical record of Neogene–Quaternary water bodies in the Dead Sea Basin – inferences for the regional paleoclimatic history. Journal of Paleolimnology 26: 271–282.CrossRefGoogle Scholar
Stein, M., Starinsky, A., Katz, A.et al. (1997) Strontium isotopic, chemical, and sedimentological evidence for the evolution of Lake Lisan and the Dead Sea. Geochimica et Cosmochimica Acta 61: 3975–3992.CrossRefGoogle Scholar
Stein, M., Starinsky, A., Agnon, A.et al. (2000) The impact of brine–rock interaction during marine evaporite formation on the isotopic Sr record in the oceans: evidence from Mt. Sedom, Israel. Geochimica et Cosmochimica Acta 64: 2039–2053.CrossRefGoogle Scholar
Stein, M., Torfstein, A., Gavrieli, I. and Yechieli, Y. (2010) Abrupt aridities and salt deposition in the post-glacial Dead Sea and their North Atlantic connection. Quaternary Science Reviews 29: 567–575.CrossRefGoogle Scholar
Torfstein, A., Gavrieli, I. and Stein, M. (2005) The sources and evolution of sulfur in the hypersaline Lake Lisan (paleo-Dead Sea). Earth and Planetary Science Letters 236: 61–77.CrossRefGoogle Scholar
Yechieli, Y., Magaritz, M., Levy, Y.et al. (1993) Late Quaternary geological history of the Dead Sea area, Israel. Quaternary Research 39: 59–67.CrossRefGoogle Scholar

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