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54 - Isotopic Tracers of Dust and Loess in the Levant

from Part V: - Quaternary Geomorphology

Published online by Cambridge University Press:  04 May 2017

Yehouda Enzel
Hebrew University of Jerusalem
Ofer Bar-Yosef
Harvard University, Massachusetts
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At the northern edge of Sahara-Arabia, dust settles in water-bodies or forms widespread loess. Sr, Pb, and Nd isotopic ratios determine sources of atmospheric dust to the Levant in these vast deserts. Combining results of contemporary storms, Sr-Nd isotopes and Mg/Al of Negev loess, fine-grained deposits in the Red Sea and from the Dead Sea indicate shifts in delivery synoptic systems. The samples Nd-Sr results are in-between the fields of (mostly) Proterozoic Sahara Shields, late Proterozoic Arabian Nubian Shield (ANS) and Nile sediments containing Neogene-Quaternary basaltic derived material. The relative fraction of each of the source end members in the final sinks reflects configurations of atmospheric-synoptic patterns and their delivery efficiencies, which in turn, are related to regional changes in climate. Easttern Mediterranean cold frontal depressions and Sharav cyclones deliver most of the dust from the Sahara; Red Sea trough delivers fine-grain material from the Red Sea region and is responsible for bringing dust from ANS rock sources. During intervals of more frequent occurrences of Red Sea trough, the isotopic composition of the dust shifted accordingly.
Quaternary of the Levant
Environments, Climate Change, and Humans
, pp. 483 - 492
Publisher: Cambridge University Press
Print publication year: 2017

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Abu Bakr, M., Ghoneim, E., El-Baz, F., Zeneldinc, M. & Zeid, S. 2013. Use of radar data to unveil the paleo-lakes and the ancestral course of Wadi El-Arish, Sinai Peninsula, Egypt. Geomorphology 194: 3445.Google Scholar
Alpert, P. & Ziv, B. 1989. The Sharav cyclone: Observations and some theoretical considerations. Journal of Geophysical Research: Atmos-pheres 94: 18495–514.Google Scholar
Amit, R., Enzel, Y., Porat, N., Gillespie, A.R. & McDonald, V.E. 2009. Significance of primary hilltop loess in reconstructing dust chronology, accretion rates, and sources: An example from the Negev Desert, Israel. Journal of Geophysical Research: Earth Surface 114: F02017.Google Scholar
Amit, R., Enzel, Y., Crouvi, O. et al. 2011. The role of the Nile in initiating a massive dust influx to the Negev late in the middle Pleistocene. Geological Society of America Bulletin 123: 837–89.CrossRefGoogle Scholar
Ben Israel, M., Enzel, Y., Amit, R. & Erel, Y. 2014. Provenance of the Negev loess with implication to changes in major dust sources to the eastern Mediterranean. Quaternary Research 83: 105–15.Google Scholar
Biscaye, P.E., Grousset, F.E., Revel, M. et al. 1997. Asian provenance of last glacial maximum dust in the GISP-2 ice core, Summit, Greenland. Journal of Geophysical Research 102: 26765–81.Google Scholar
Blum, J.D. & Erel, Y. 1997. Rb–Sr isotope systematics of a granitic soil chronosequence: The importance of biotite weathering. Geochimica et Cosmochimica Acta 61: 3193–204.CrossRefGoogle Scholar
Blum, J.D. & Erel, Y. 2003. Radiogenic isotopes in weathering and hydrology. In Surface and Ground Water, Weathering, Erosion and Soils, ed. Drever, J.I.. Treatise on Geochemistry vol. 5. Oxford: Elsevier.Google Scholar
Boher, M., Abouchami, W., Michard, A., Albarede, F. & Arndt, N.T. 1992. Crustal growth in West Africa at 2.1 Ga. Journal of Geophysical Research 97: 345–69.CrossRefGoogle Scholar
Bollhofer, A. & Rosman, K.J.R. 2000. Isotopic source signatures for atmos-pheric lead: The Southern Hemisphere. Geochimica et Cosmochimica Acta 64: 3251–62.Google Scholar
Bollhofer, A. & Rosman, K.J.R. 2001. Isotopic source signatures for atmospheric lead: The Northern Hemisphere. Geochimica et Cosmochimica Acta 65: 1727–37.CrossRefGoogle Scholar
Bory, A., Biscaye, P.E., Grousset, F.E. 2003. Two distinct seasonal Asian source regions for mineral dust deposited in Greenland (NorthGRIP). Geophysical Research Letters 30: 1167.CrossRefGoogle Scholar
Bruins, H.J. 1976. The Origin, Nature and Stratigraphy of Paleosols in the Loessial Deposits of the NW-Negev (Netivot, Israel). Unpublished M.Sc. thesis, Hebrew University of Jerusalem.Google Scholar
Bruins, H. & Yaalon, D. 1979. Stratigraphy of the Netivot section in the desert loess of the Negev (Israel). Acta Geologica Academiae Scientiarum Hungaricae 22: 161–9.Google Scholar
Cole, J.M., Goldstein, S.L., deMenocal, P.B., Hemming, S.R. & Grousset, F.E. 2009. Contrasting compositions of Saharan dust in the eastern Atlantic Ocean during the last deglaciation and African Humid Period. Earth and Planetary Science Letters 278: 257–66.CrossRefGoogle Scholar
Crouvi, O., Amit, R., Enzel, Y., Porat, N., & Sandler, A. 2008. Sand dunes as a major proximal dust source for late Pleistocene loess in the Negev Desert, Israel. Quaternary Research 70: 275–82.Google Scholar
Crouvi, O., Amit, R., Porat, N. et al. 2009. Significance of primary hilltop loess in reconstructing dust chronology, accretion rates, and sources: An example from the Negev Desert, Israel. Journal of Geophysical Research 114: F02017.Google Scholar
Dasch, E.J. 1969. Strontium isotopes in weathering profiles, deep-sea sedi-ments and sedimentary rocks. Geochimica et Cosmochimica Acta 33: 1521–52.CrossRefGoogle Scholar
Dayan, U. 1986. Climatology and back trajectories from Israel based on synoptic analysis. Journal of Applied Meteorology and Climatology 25: 591–5.Google Scholar
Dayan, U. & Levy, I. 2005. The influence of seasonal meteorological conditions and atmospheric circulation types on PM10 and visibility in Tel-Aviv, Israel. Journal of Applied Meteorology 44: 606–19.Google Scholar
Dayan, U., Ziv, B., Shoop, T. & Enzel, Y. 2007. Suspended dust over south-eastern Mediterranean and its relation to atmospheric circulations. International Journal of Climatology 28: 915–24.Google Scholar
Downing, G.E. & Hemming, S.R. 2012. Late glacial and deglacial history of ice rafting in the Labrador Sea: A perspective from radiogenic isotopes in marine sediments. The Geological Society of America Special Paper 487: 113–24.Google Scholar
Enzel, Y., Ken-Tor, R., Sharon, D. et al. 2003. Late Holocene climates of the Near East deduced from Dead Sea level variations and regional winter rainfall. Quaternary Research 60: 26373.CrossRefGoogle Scholar
Erel, Y., Dayan, U., Rabi, R., Rudich, Y. & Stein, M. 2006. Trans boundary transport of pollutants by atmospheric mineral dust. Environmental Science & Technology 40: 29963005.CrossRefGoogle ScholarPubMed
Faure, G. 1986. Principles of Isotope Geology. New York: Wiley.Google Scholar
Frumkin, A. & Stein, M. 2004. The Sahara–east Mediterranean dust and climate connection revealed by strontium and uranium isotopes in a Jerusalem speleothem. Earth and Planetary Science Letters 217: 451–64.Google Scholar
Ganor, E. 1991. The composition of clay minerals transported to Israel as indicators of Saharan dust emission. Atmospheric Environment 25A: 2657–64.Google Scholar
Ganor, E. & Foner, H. 1996. The mineralogical and chemical properties and the behavior of aeolian Saharan dust over Israel. In The Impact of Desert Dust across the Mediterranean, ed. Guerzoni, S. & Chester, R.. Dordrecht: Springer Netherlands, pp. 163–71.Google Scholar
Ganor, E. & Mamane, Y. 1982. Transport of Saharan dust across the eastern Mediterranean. Atmospheric Environment 16: 581–7.Google Scholar
Goldstein, S.L., O'Nions, R.K., Hamilton, P.J. 1984. A Sm–Nd isotopic study of dusts and particulates from major river systems. Earth and Planetary Science Letters 70: 221–36.Google Scholar
Grousset, F.E. & Biscaye, P.E. 1989. Nd and Sr isotopes as tracers of wind transport in Atlantic aerosols and surface sediments. In NATO Advanced Research Workshop: Paleoclimatology and Paleometeor-ology: Modern and Past Patterns of Global Atmospheric Transport, vol. 282, ed. Leinen, M. & Sarnthein, M.. Dordrecht: Kluwer Academic Publishers, pp. 385400.Google Scholar
Grousset, F.E. & Biscaye, P.E. 2005. Tracing dust sources and transport patterns using Sr, Nd and Pb isotopes. Chemical Geology 222: 149–67.Google Scholar
Grousset, F.E., Biscaye, P.E., Zindler, A., Prospero, J. & Chester, R. 1988. Neodymium isotopes as tracers in marine sediments and aerosols: North Atlantic. Earth and Planetary Science Letters 87: 367–78.CrossRefGoogle Scholar
Grousset, F.E., Rognon, P., Coudé-Gaussen, G. & Pédemay, Ph. 1992. Origins of peri-Saharan dust deposits traced by their Nd and Sr isotopic composition. Paleogeography, Paleoclimatology, Paleoecology 93: 203–12.Google Scholar
Grousset, F.E., Parra, M., Bory, A. et al. 1998. Saharan wind regimes traced by the Sr–Nd isotopic composition of the subtropical Atlantic sediments: Last Glacial Maximum vs. today. Quaternary Science Reviews 17: 395409.Google Scholar
Grousset, F.E., Pujol, C., Labeyrie, L., Auffret, G. & Boelaert, A. 2000. Were the North Atlantic Heinrich events triggered by the behavior of the European ice sheets? Geology 28: 123–6.2.0.CO;2>CrossRefGoogle Scholar
Haase-Schramm, A., Goldstein, S.L. & Stein, M. 2004. U–Th dating of Lake Lisan (late Pleistocene Dead Sea) aragonite and implications for glacial east Mediterranean climate change. Geochimica et Cosmochimica Acta 68: 9851005.CrossRefGoogle Scholar
Haliva-Cohen, A., Stein, M., Goldstein, S.L., Sandler, A. & Starinsky, A. 2012. Sources and transport routes of fine detritus material to the Late Quaternary Dead Sea Basin. Quaternary Science Reviews 50: 5570.CrossRefGoogle Scholar
Hemming, S. 2004. Heinrich events: Massive late Pleistocene detritus layers of the North Atlantic and their global imprint. Review of Geophysics 42: 143.Google Scholar
Israelevich, P.L., Levin, Z., Joseph, J.H. & Ganor, E. 2002. Desert aerosol transport in the Mediterranean region as inferred from the TOMS aerosol index. Journal of Geophysical Research – Atmospheres 107: 108–20.Google Scholar
Jin-Liang, F., Li-Ping, Z., Xiao-Lin, Z. & Zhao Guo, H. 2009. Grain size effect on Sr and Nd isotopic compositions in eolian dust: Implications for tracing dust provenance and Nd model age. Geochemical Journal 43: 123–31.Google Scholar
Kalderon, B. 2005. Mineralogical and Chemical Characterization of Aerosols Transported to Israel. Unpublished M.Sc. thesis, Hebrew University of Jerusalem.Google Scholar
Kalderon-Asael, B., Erel, Y., Sandler, A. & Dayan, U. 2009. Mineralogical and chemical characterization of suspended atmospheric par-ticles over the east Mediterranean based on synoptic-scale circulation patterns. Atmospheric Environment 43: 3963–70.Google Scholar
Krom, M.D., Cliff, R.A., Eijsink, L.M., Herut, B. & Chester, R. 1999. The characterisation of Saharan dusts and Nile particulate matter in surface sediments from the Levantine basin using Sr isotopes. Marine Geology 155: 319–30.Google Scholar
Meyer, I., Davies, G.R. & Stuut, J.B.W. 2011. Grain size control on Sr–Nd isotope provenance studies and impact on paleoclimate reconstructions: An example from deep-sea sediments offshore NW Africa. Geochemistry, Geophysics, Geosystems 12: 14.Google Scholar
Muhs, D.R., Prospero, J.M., Baddock, M.C. & Gill, T.E. 2014. Identifying sources of aeolian mineral dust: Present and past. In Mineral Dust: A Key Player in the Earth System, ed. Knippertz, P. & Stuut, J.-B.W.. Springer Science Business Media, pp. 5174.Google Scholar
Murozumi, M., Chow, T.J. & Patterson, C. 1969. Chemical concentrations of pollutant lead aerosols, terrestrial dusts and sea salts in Greenland and Antarctic snow strata. Geochimica et Cosmochimica Acta 33: 1247–294.Google Scholar
Palchan, D., Stein, M., Almogi-Labin, A., Erel, Y. & Goldstein, S.L. 2013. Dust transport and synoptic conditions over the Sahara–Arabia deserts during the MIS 6/5 and 2/1 transitions from grain-size, chemical and isotopic properties of Red Sea cores. Earth and Planetary Science Letters 382: 125–39.Google Scholar
Potrel, A., Peucat, J.J., Mark Fanning, C. et al. 1996. 3.5 Ga old terranes in the west African craton, Mauritania. Journal of Geological Society 152: 507–10.Google Scholar
Prospero, J. M., Ginoux, P., Torres, N., Sharon, E. & Thomas, E. 2002. Environmental characterization of global sources of atmospheric soil dust identified with the Nimbus 7 Total Ozone Mapping Spectrometer (TOMS) absorbing aerosol product. Review of Geophysics 40: 1002.Google Scholar
Rabi, R. 2004. Geochemical Characterization of Suspended Desert Dust in Israel. Unpublished M.Sc. thesis, Hebrew University of Jerusalem.Google Scholar
Rasmussen, S.O., Seierstad, I.K., Andersen, K.K. et al. 2008. Synchronization of the NGRIP, GRIP, and GISP2 ice cores across MIS 2 and palaeoclimatic implications. Quaternary Science Reviews 27: 1828.Google Scholar
Revel, M., Ducassou, E., Grousset, F.E. et al. 2010. 100,000 years of African monsoon variability recorded in sediments of the Nile margin. Quaternary Science Reviews 29: 1342–62.Google Scholar
Rognon, P., Coudé-Gaussen, G., Revel, M., Grousset, F.E. & Pédemay, P. 1996. Holocene Saharan dust deposition on the Cape Verde Islands: sedimentological and Nd–Sr isotopic arguments. Sedimentology 43: 359–66.Google Scholar
Scheuvens, D., Schütz, L., Kandler, K., Ebert, M. & Weinbruch, S. 2013. Bulk composition of northern African dust and its source sediments – a compilation. Earth Science Reviews 116: 170–94.Google Scholar
Singer, A., Dultz, S. & Argaman, E. 2004. Properties of the non-soluble fractions of suspended dust over the Dead Sea. Atmospheric Environment 38: 1745–53.Google Scholar
Starinsky, A., Bielski, M., Lazar, B., Wakshal, E. & Steinitz, G. 1980. Marine 87Sr/86Sr ratios from the Jurassic to Pleistocene: Evidence from ground water in Israel. Earth and Planetary Science Letters 47: 7580.Google 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: 3975–92.Google Scholar
Stein, M., Almogi-Labin, A., Goldstein, S.L., Hemleben, C. & Starinsky, A. 2007. Late Quaternary changes in desert dust inputs to the Red Sea and Gulf of Aden from 87Sr/86Sr ratios in deep-sea cores. Earth and Planetary Science Letters 261: 104–19.CrossRefGoogle Scholar
Svensson, A., Biscaye, P.E. & Grousset, F.E. 2000. Characterization of late glacial continental dust in the Greenland Ice Core project ice core. Journal of Geophysical Research 105: 4637–656.Google Scholar
Torfstein, A., Goldstein, S.L., Kagan, E.J. & Stein, M. 2013. Integrated multi-site U–Th chronology of the last glacial Lake Lisan. Geochimica et Cosmochimica Acta 104: 210–31.Google Scholar
Torfstein, A., Goldstein, S.L., Kushnir, Y. et al. 2015. Dead Sea drawdown and monsoonal impacts in the Levant during the last interglacial. Earth and Planetary Science Letters 412: 235–44.Google Scholar
Yaalon, D.H. 1987. Saharan dust and desert loess: Effect on surrounding soils. Journal of African Earth Science 6: 569–71.Google Scholar
Yaalon, D. & Dan, J. 1974. Accumulation and distribution of loess-derived deposits in the semi-desert and desert fringe areas of Israel. Zeitschrift für Geomorphologie 20: 91105.Google Scholar
Yaalon, D.H. & Ganor, E. 1973. The influence of dust on the soils during the Quaternary. Soil Science 116: 146–55.CrossRefGoogle Scholar

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