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Paleoclimate reconstruction based on the timing of speleothem growth and oxygen and carbon isotope composition in a cave located in the rain shadow in Israel

Published online by Cambridge University Press:  20 January 2017

Anton Vaks
Affiliation:
Geological Survey of Israel, 30 Malchei Israel Street, Jerusalem 95501, Israel
Miryam Bar-Matthews
Affiliation:
Geological Survey of Israel, 30 Malchei Israel Street, Jerusalem 95501, Israel
Avner Ayalon
Affiliation:
Geological Survey of Israel, 30 Malchei Israel Street, Jerusalem 95501, Israel
Bettina Schilman
Affiliation:
Geological Survey of Israel, 30 Malchei Israel Street, Jerusalem 95501, Israel
Mabs Gilmour
Affiliation:
Department of Earth Sciences, The Open University, Walton Hall, Milton Keynes, MK7 6AA, UK
Chris J Hawkesworth
Affiliation:
Department of Earth Sciences, The University of Bristol, Bristol, UK
Amos Frumkin
Affiliation:
Department of Physical Geography, The Hebrew University of Jerusalem, Jerusalem 91905, Israel
Aaron Kaufman
Affiliation:
Department of Environmental Sciences, The Weizmann Institute of Science, Rehovot 76100, Israel
Alan Matthews
Affiliation:
Department of Earth Sciences, The Hebrew University of Jerusalem, Jerusalem 91905, Israel
Corresponding
E-mail address:

Abstract

High-resolution 230Th/234U ages and δ18O and δ13C compositions of speleothems in Ma’ale Efrayim Cave located to the east of the central mountain ridge of Israel enable us to examine the nature of the rain shadow aridity during glacial and interglacial intervals. Speleothem growth occurred during marine glacial isotopic periods, with no growth during the two last marine isotope interglacial intervals and during the peak of the Last Glacial Maximum. This contrasts with speleothem growth in caves located on the western flank of the central mountain ridge, in the Eastern Mediterranean semiarid climatic zone, which continued throughout the last 240,000 yr. Thus, during glacial periods water reached both sides of the central mountain ridge. A comparison of the present-day rain and cave water isotopic compositions and amounts at the Ma’ale Efrayim Cave site with those on the western flank shows that evaporation and higher temperatures on the eastern flank are major influences on isotopic composition and the lack of rainfall. The δ18O and δ13C profiles of the speleothems deposited between 67,000 and 25,000 yr B.P. match the general trends of the isotopic profiles of Soreq Cave speleothems, suggesting a similar source (eastern Mediterranean Sea) and similar climatic conditions. Thus, during glacial periods the desert boundary effectively migrated further south or east from its present-day location on the eastern flank, whereas interglacial periods appear to have been similar to the present, with the desert boundary at the same position. The decrease in overall temperature and a consequent reduction in the evaporation to precipitation ratios on the eastern flank are viewed as the major factors controlling the decay of the rain shadow effect during glacial periods.

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Articles
Copyright
Elsevier Science (USA)

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References

Almogi-Labin, A., Luz, B., and Duplessy, J. Quaternary paleo-oceanography, pteropod preservation and stable isotope record of the Red Sea. Palaeogeography, Palaeoclimatology, Palaeoecology 57, (1986). 195 211.CrossRefGoogle Scholar
Ayalon, A., Bar-Matthews, M., and Sass, E. Rainfall-recharge relationships within a karstic terrain in the Eastern Mediterranean semi-arid region, Israel, δ18O and δD characteristics. Journal of Hydrology 207, (1998). 18 31.CrossRefGoogle Scholar
Ayalon, A., Bar-Matthews, M., and Kaufman, A. Climatic conditions during marine oxygen isotope stage 6 in the eastern Mediterranean region from the isotopic composition of speleothems of Soreq Cave, Israel. Geology 30, (2002). 303 306.2.0.CO;2>CrossRefGoogle Scholar
Ayliffe, L.K., Marianelli, P.C., Moriarty, K.C., Wells, R.T., McCulloch, M.T., Mortimer, G.E., and Hellstrom, J.C. 500 ka precipitation record from southeastern Australia. evidence for interglacial relative aridity. Geology 26, (1998). 147 150.2.3.CO;2>CrossRefGoogle Scholar
Bar-Matthews, M., Ayalon, A., (2001). Eastern Mediterranean paleoclimate during the last 250,000 years as derived from the petrography, mineralogy, trace element and isotopic composition of cave deposits (speleothems), Israel. Geological Survey of Israel Report GSI/41/01, 44 ppGoogle Scholar
Bar-Matthews, M., Ayalon, A., (2003). Speleothems as paleoclimate indicators, a case study from Soreq cave located in the Eastern Mediterranean region, Israel. in: Battarbee, R.W., Gasse, F., Stickly, C.E. (Eds.), Past Climate Variability through Europe and Africa, Kluwer Academic Publisher, (in press) Google Scholar
Bar-Matthews, M., Ayalon, A., Matthews, A., Sass, E., and Halicz, L. Carbon and oxygen isotope study of the active water-carbonate system in the karstic Mediterranean cave. implications for paleoclimate research in semiarid regions. Geochimica et Cosmochimica Acta 60, (1996). 337 347.CrossRefGoogle Scholar
Bar-Mattews, M., Ayalon, A., and Kaufman, A. Late Quaternary paleoclimate in the Eastern Mediterranean Region from stable isotope analysis of speleothems in Soreq cave, Israel. Quaternary Research 47, (1997). 155 168.CrossRefGoogle Scholar
Bar-Matthews, M., Ayalon, A., Kaufman, A., and Wasserburg, G.J. The Eastern Mediterranean paleoclimate as a reflection of regional events. Soreq cave, Israel. Earth Planetary Science Letters 166, (1999). 85 95.CrossRefGoogle Scholar
Bar-Matthews, M., Ayalon, A., and Kaufman, A. Timing and hydrological conditions of Sapropel events in the Eastern Mediterranean, as evident from speleothems, Soreq cave, Israel. Chemical Geology 169, (2000). 145 156.CrossRefGoogle Scholar
Bar-Matthews, M., Ayalon, A., Gilmour, M., Matthews, A., 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 (in press) CrossRefGoogle Scholar
Bartov, Y., Stein, M., Enzel, Y., Agnon, A., and Reches, Z. Lake levels and sequence stratigraphy of Lake Lisan, the late Pleistocene precursor of the Dead Sea. Quaternary Research 57, (2002). 9 21.CrossRefGoogle Scholar
Begin, Z.B., Ehrlich, A., and Nathan, Y. Lake Lisan, the Pleistocene precursor of the Dead Sea. Geological Survey of Israel Bulletin 63, (1974). 30 Google Scholar
Coleman, M.L., Shepherd, T.J., Durham, J.J., Rouse, J.E., and Moore, G.R. Reduction of water with zinc for hydrogen isotope analysis. Analytical Chemistry 54, (1982). 993 995.CrossRefGoogle Scholar
Craig, G. Isotopic variations in meteoric waters. Science 133, (1961). 1702 1703.CrossRefGoogle ScholarPubMed
Dansgaard, W. Stable isotopes in precipitation. Tellus 16, (1964). 438 468.CrossRefGoogle Scholar
Emeis, K.C., Struck, U., Schulz, H.M., Rosenberg, R., Bernasconi, S., Erlenkeuser, H., Sakamoto, T., and Martinez-Ruiz, F. 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, (2000). 259 280.CrossRefGoogle Scholar
Epstein, S., and Mayeda, T.K. Variations of 18O of waters from natural sources. Geochimica et Cosmochimica Acta 4, (1953). 213 224.CrossRefGoogle Scholar
Frumkin, A., Ford, D.C., and Schwarcz, H.P. Continental oxygen isotopic record of the last 170,000 years in Jerusalem. Quaternary Research 51, (1999). 317 327.CrossRefGoogle Scholar
Frumkin, A., Ford, D.C., and Schwarcz, H.P. Paleoclimate and vegetation of the last glacial cycles in Jerusalem from a speleothem record. Global Biochemical Cycles 14, (2000). 863 870.CrossRefGoogle Scholar
Gascoyne, M., Schwarcz, H.P., and Ford, D.C. Uranium series ages of speleothem from Northwest England. correlation with Quaternary climate. Philosophical Transactions Royal Society of London B-301, (1982). 143 164.Google Scholar
Gat, J.R., (1982). Precipitation, groundwater and surface waters, in: Paleoclimates and Paleowaters. International Atomic Energy Agency, Vienna., pp. 312.Google Scholar
Gat, J.R. Oxygen and hydrogen isotopes in the hydrologic cycle. Annual Reviews Earth Planetary Science 24, (1996). 225 262.CrossRefGoogle Scholar
Gat, J.R., and Carmi, I. Evolution in the isotopic composition of atmospheric waters in the Mediterranean Sea area. Journal Geophysical Research 75, (1970). 3039 3048.CrossRefGoogle Scholar
Gat, J.R., Carmi, I., (1987). Effect of climate changes on the precipitation patterns and isotopic composition of water in climatic transition zone: case of Eastern Mediterranean sea area. in: The influence of Climatic Change Climatic Variability on the Hydrologic Regime and Water Resources, IANS 168 Symp. Proc. pp. 513523.Google Scholar
Goodfriend, G.A. Holocene trends in 18O in land snail shells from the Negev Desert and their implications for changes in rainfall source areas. Quaternary Research 35, (1991). 417 426.CrossRefGoogle Scholar
Goodfriend, G.A. Terrestrial stable isotope records of Late Quaternary paleoclimates in the eastern Mediterranean region. Quaternary Science Reviews 18, (1999). 501 513.CrossRefGoogle Scholar
Goodfriend, G.A., and Magaritz, M. Palaeosols and late Pleistocene rainfall fluctuations in the Negev Desert. Nature 332, (1988). 144 146.CrossRefGoogle Scholar
Gordon, D., Smart, P.I., Ford, D.C., Andrew, J.N., Atkinson, T.C., Rowe, P.J., and Christopher, N.S.J. Dating of Late Pleistocene interglacial and interstadial periods in the United Kingdom from speleothem growth frequency. Quaternary Research 31, (1989). 14 26.CrossRefGoogle Scholar
Hendy, C.H. The isotopic composition of the speleothems I. The calculation of the effects of different modes of formation on the isotopic composition of speleothems and their applicability as paleoclimatic indicators. Geochimica et Cosmochimica Acta 35, (1971). 801 824.CrossRefGoogle Scholar
Kallel, N., Paterne, M., Duplessy, J.-C., Vergnaud-Grazzini, C., Pujol, C., Labeyrie, L., Arnold, M., Fontugne, M., and Pierre, C. Enhanced rainfall in the Mediterranean region during the last sapropel event. Oceanologica Acta 20, (1997). 697 712.Google Scholar
Kaufman, A., Wasserburg, G.J., Porcelli, D., Bar-Matthews, M., Ayalon, A., and Halicz, L. U-Th isotope systematics from the Soreq Cave Israel and climatic correlations. Earth Planetary Science Letters 156, (1998). 141 155.CrossRefGoogle Scholar
Lauritzen, S.E. High-resolution paleotemperature proxy record for the last interglaciation based on the Norwegian speleothems. Quaternary Research 43, (1995). 133 146.CrossRefGoogle Scholar
McDermott, F., Frisia, S., Huang, Y., Longinelli, A., Spiro, B., Heaton, T.H.E., Hawkesworth, C.J., Borsato, A., Keppens, E., Fairchild, I.J., Borg, K., Verheyden, S., and Selmo, E. Holocene climate variability in Europe. evidence from δ18O, textural and extension rate variations in three speleothems. Quaternary Science Reviews 18, (1999). 1021 1038.CrossRefGoogle Scholar
Neev, D., Emery, K.O., (1967). The Dead-Sea; depositional processes and environments of evaporites. Geological Survey of Israel Bulletin 41, 147 ppGoogle Scholar
O’Neil, J.R., Clayton, R.N., and Mayeda, T.K. Oxygen isotope fractionation of divalent metal carbonates. Journal of Chemical Physics 30, (1969). 5547 5558.CrossRefGoogle Scholar
Rindsberger, M., Jaffe, S.h., Rahamin, S.h., and Gat, J.R. Patterns of the isotopic composition of precipitation in time and space. data from the Israeli storm water collection program. Tellus 42B, (1990). 263 271.CrossRefGoogle Scholar
Rozanski, K., Araguás-Araguás, L., Gonfiantini, R. (1993). Isotopic patterns in modern global precipitation. Climate Change in Continental Isotopic Records, Geophysical Monograph 78, American Geophysical Union, 1–36Google Scholar
Schwarcz, H.P. Geochronology and isotopic geochemistry of speleothems. Fritz, P., and Fontes, J.C. Handbook of Enviromental Isotope Geochemistry, Vol. 2. (1986). Elsevier, Amsterdam. 271 300.Google Scholar
Tanweer, A., Hut, G., and Burgman, J.O. Optimal conditions for the reduction of water to hydrogen by zinc for mass spectrometric analysis of the deuterium content. Chemical Geology (Isotope Geoscience Section) 73, (1988). 199 203.CrossRefGoogle Scholar
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Paleoclimate reconstruction based on the timing of speleothem growth and oxygen and carbon isotope composition in a cave located in the rain shadow in Israel
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