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Sand dunes as a major proximal dust source for late Pleistocene loess in the Negev Desert, Israel

Published online by Cambridge University Press:  20 January 2017

Onn Crouvi ,
Rivka Amit ,
Yehouda Enzel ,
Naomi Porat  and
Amir Sandler
Onn Crouvi*
Affiliation:
Geological Survey of Israel, 30 Malkhe Israel Street, Jerusalem 95501, Israel Institute of Earth Sciences, The Hebrew University of Jerusalem, Jerusalem 91904, Israel
Rivka Amit
Affiliation:
Geological Survey of Israel, 30 Malkhe Israel Street, Jerusalem 95501, Israel
Yehouda Enzel
Affiliation:
Institute of Earth Sciences, The Hebrew University of Jerusalem, Jerusalem 91904, Israel
Naomi Porat
Affiliation:
Geological Survey of Israel, 30 Malkhe Israel Street, Jerusalem 95501, Israel
Amir Sandler
Affiliation:
Geological Survey of Israel, 30 Malkhe Israel Street, Jerusalem 95501, Israel
*
*Corresponding author. Fax: +972 2 5380688. E-mail address:[email protected] (O. Crouvi).
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Abstract

Grain size analyses of three hilltop, primary eolian loess sequences in the Negev desert, southern Israel, show a bimodal grain-size distribution at 50–60 μm and 3–8 μm. Using analyses of mineralogy and OSL ages we demonstrate that the coarse mode is composed mostly of quartz grains and its relative magnitude increases regionally with time, suggesting an enhancement of a time-transgressive proximal dust source compared to a distal, Saharan fine-grain dust. The only proximal dust source for large amount of coarse silt quartz grains is the sands that advanced into Sinai and the Negev concurrently with the loess accretion during the late Pleistocene as a result of the exposure of the Mediterranean shelf. We therefore propose that the coarse silt quartz grains were formed through eolian abrasion within the margins of an advancing sand sea. This relationship between desert sand seas as a source for proximal coarse dust and desert margin loess deposits can be applicable to other worldwide deserts such as Northern Africa, China and Australia.

Keywords

LoessSandProximal dust sourceDesertsPleistoceneNegev
Type
Short Paper
Information
Quaternary Research , Volume 70 , Issue 2 , September 2008 , pp. 275 - 282
Copyright
University of Washington

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References

Arbogast, A.F., Muhs, D.R., (2000). Geochimical and mineralogical evidence from eolian sediments for northwesterly mid-Holocene paleowinds, central Kansas, USA.. Quaternary International 67, 107–118.Google Scholar
Assallay, A.M., Rogers, C.D.F., Smalley, I.J., Jefferson, I.F., (1998). Silt: 2-62 micron, 9-4 pi.. Earth-Science Reviews 45, 61–88.Google Scholar
Bagnold, R.A., (1941). The physics of blown sand and desert dunes.. Methuen, London.Google Scholar
Bartov, J., (1990). Geological photomap of Israel and adjacent areas.. The Geological Survey of Israel.Google Scholar
Ben David, R., (2003). Changes in Desert Margin Environments during the climate changes of the late Quaternary: Interaction between drainage systems and the accumulation of dust (loess) and the invasion of dunes at the North-West Negev Desert.. Unpublished Ph.D thesis, The Hebrew University of Jerusalem, .Google Scholar
Birkeland, P.W., (1999). Soils and Geomorphology.. Oxford University Press, New York.Google Scholar
Bitan, A., Rubin, S., (1991). Climatic Atlas of Israel for Physical and Environmental Planning and Design.. Tel-Aviv University Press, Tel-Aviv.Google 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, The Hebrew University, .Google Scholar
Bullard, J.E., McTainsh, G., Pudmenzky, C., (2004). Aeolian abrasion and modes of fine particle production from natural red dune sands: an experimental study.. Sedimentology 51, 1103–1125.CrossRefGoogle Scholar
Bullard, J.E., McTainsh, G., Pudmenzky, C., (2007). Factors affecting the nature and rate of dust production from natural dune sands.. Sedimentology 54, 169–182.Google Scholar
Coude-Gaussen, G., Rognon, P., (1988). The upper Pleistocene loess of Southern Tunisia: a statement.. Earth Surface Processes and Landforms 13, 137–151.Google Scholar
Dan, J., Raz, Z., Koyumdjiski, H., (1964). Soil Survey Manual.. Bet Dagan, .Google Scholar
Dan, J., Raz, Z., (1970). The soil association map of Israel. Volcani institute, Bet Dagan, Israel.Google Scholar
Dayan, U., Ziv, B., Shoob, T., Enzel, Y., (2008). Suspended dust over South-Eastern Mediterranean and its relation to atmospheric circulations.. International Journal of Climatology 28, 915–924.Google Scholar
Derimian, Y., Karnieli, A., Kaufman Yoram, J., Andreae, M.O., Andreae, T.W., Dubovik, O., Maenhaut, W., Koren, I., Holben, B.N., (2006). Dust and pollution aerosols over the Negev desert, Israel: properties, transport, and radiative effect.. Journal of Geophysical Research 111, D05205.CrossRefGoogle Scholar
Dutta, P.K., Zhou, Z., dos Santos, P.R., (1993). A theoretical study of mineralogical maturation of eolian sand.. Geological Society of America Special Paper 284, 203–209.Google Scholar
Enzel, Y., Amit, R., Dayan, U., Crouvi, O., Kahana, R., Ziv, B., Sharon, D., (2008). The climatic and physiographic controls of the eastern Mediterranean over the late Pleistocene climates in the southern Levant and its neighboring deserts.. Global and Planetary Change 60, 165–192.CrossRefGoogle Scholar
Friedman, G.M., Sanders John, E., Kopaska-Merkel, D.C., (1992). Principles of Sedimentary Deposits; Stratigraphy and Sedimentology.. Macmillan, .Google Scholar
Galbraith, R.F., Roberts, R.G., Laslett, G.M., Yoshida, H., Olley, J.M., (1999). Optical dating of single and multiple grains of quartz from Jinmium rock shelter, northern Australia: Part I. Experimental design and statistical models.. Archaeometry 41, 339–364.CrossRefGoogle Scholar
Ganor, E. (1975).). Atmospheric dust in Israel - sedimentological and meteorological analysis of dust deposition.. Unpublished Ph.D. thesis, The Hebrew University, .Google Scholar
Gerson, R., Amit, R., (1987). Rates and Modes of Dust Accretion and Deposition in an Arid Region — the Negev, Israel.. Geological Society Special Publication, London.CrossRefGoogle Scholar
Gile, L.H., Peterson, F.F., Grossman, R.B., (1965). The K horizon: a master soil horizon of carbonate accumulations.. Soil Science 99, 74–82.Google Scholar
Ginzburg, D., Yaalon, D.H., (1963). Petrography and origin of the loess in the Be'er Sheva Basin.. Israel Journal of Earth-Sciences 12, 68–70.Google Scholar
Goldberg, P., (1986). Late Quaternary environmental history of the southern Levant.. Geoarcheology 1, (3) 225–244.Google Scholar
Goodfriend, G.A., Magaritz, M., (1988). Paleosols and late Pleistocene rainfall fluctuations in the Negev Desert.. Nature 322, 144–146.CrossRefGoogle Scholar
Goring-Morris, N., Goldberg, P., (1990). Late Quaternary dune incursions in the southern Levant: archeology, chronology and paleoenvironments.. Quaternary International 5, 115–137.Google Scholar
Hall, J.K., (1980). Bathymetric chart of the Southeastern Mediterranean Sea.. The Geological Survey of Israel.Google Scholar
Kaufman, Y.J., Gitelson, A., Karnieli, A., Ganor, E., Fraser, R.S., Nakajima, T., Mattoo, S., Holben, B.N., (1994). Size distribution and scattering phase function of aerosol particles retrieved from sky brightness measurements.. Journal of Geophysical Research 99, 10341–10356.Google Scholar
Kemp, R.A., (2001). Pedogenic modification of loess: significance for palaeoclimatic reconstructions.. Earth-Science Reviews 54, 145–156.Google Scholar
Kukla, G., An, Z., (1989). Loess stratigraphy in central china.. Palaeogeography, Palaeoclimatology, Palaeoecology 72, 203–225.Google Scholar
Levin, Z., Joseph, J.H., Mekler, Y., (1980). Properties of Sharav (Khamsin) dust — comparison of optical and direct sampling data.. Journal of the Atmospheric Sciences 37, 882–891.Google Scholar
Lim, J., Matsumoto, E., (2006). Bimodal grain-size distribution of aeolian quartz in a maar of Cheju Island, Korea, during the last 6500 years: its flux variation and controlling factor.. Geophysical Research Letters 33, L21816.Google Scholar
Magaritz, M., (1986). Environmental changes recorded in the upper Pleistocene along the desert boundary, southern Israel.. Paleogeography, Paleoclimatology, Paleoecology 53, 213–403.Google Scholar
McTainsh, G., Nickling, W.G., Lynch, A.W., (1997). Dust deposition and particle size in Mali, West Africa.. Catena 29, 307–322.Google Scholar
Muhs, D.R., Ager, T.A., Bettis, A.E.I., McGeehin, J.P., Been, J., Beget, J.E., Pavich Milan, J., Stafford, T.W.J., Stevens, D.A.S.P., (2003). Stratigraphy and palaeoclimatic significance of Late Quaternary loess-palaesol sequences of the Last Interglacial-Glacial cycle in central Alaska.. Quaternary Science Reviews 22, 1947–1986.Google Scholar
Muhs, D.R., Budahn, J.R., Reheis, M.C., Beann, J., Skipp, G., Fisher, E., (2007). Airborne dust transport to the eastern Pacific Ocean off southern California: evidence from San Clemente Island.. Journal of Geophysical Research 112, D13203.CrossRefGoogle Scholar
Murray, A.S., Wintle, A.G., (2000). Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol.. Radiation Measurements 32, 57–73.Google Scholar
Offer, Z.Y., Goossens, D., (2001). Airborne particle accumulation and composition at different locations in the northern Negev desert.. Zeitschrift fur Geomorphologie 45, 101–120.CrossRefGoogle Scholar
Offer, Z.Y., Goossens, D., (2004). Thirteen years of aeolian dust dynamics in a desert region (Negev desert, Israel): analysis of horizontal and vertical dust flux, vertical dust distribution and dust grain size.. Journal of Arid Environments 57, 117–140.CrossRefGoogle Scholar
Pieri, L., Bitteli, M., Rossi Pisa, P., (2006). Laser diffraction, transmission electron microscopy and image analysis to evaluate a bimodal Gaussian model for particle size distribution in soils.. Geoderma 135, 118–132.Google Scholar
Porat, N., (2007). Analytical procedures in the luminescence dating laboratory (In Hebrew).. The Geological Survey of Israel, Jerusalem. 33.Google Scholar
Price Williams, D., (1975). The environmental background to prehistoric sites in the Fara region.. University of London Bullatin Institute of Archeology 12, 125–143.Google Scholar
Pye, K., (1995). The nature, origin and accumulation of loess.. Quaternary Science Reviews 14, 653–667.Google Scholar
Pye, K., Tsoar, H., (1987). The mechanics and geological implications of dust transport and deposition in deserts with particular reference to loess formation and dune sand diagenesis in the Northern Negev, Israel.. Frostick, L., Reid, I. Geological Society Special Publication Desert sediments: Ancient and modern 139–156.CrossRefGoogle Scholar
Ravikovitch, S., (1952). The Aeolian Soils of the Northern Negev.. Volcani Agricultural, Rehovot. 36 pp.Google Scholar
Ravikovitch, S., (1969). Manual and map (1:250,000) of soils of Israel.. Magnes press, The Hebrew University, Jerusalem.Google Scholar
Rousseau, D.D., Antoine, P., Kunesch, S., Hatte, C., Rossignol, J., Packman, S., Lang, A., Gauthier, C., (2007). Evidence of cyclic dust deposition in the US Great plains during the last deglaciation from the high-resolution analysis of Peoria Loess in the Eustis sequence (Nebraska, USA).. Earth and Planetary Science Letters 262, 159–174.Google Scholar
Singer, A., Ganor, E., Dultz, S., Fischer, W., (2003). Dust deposition over the Dead Sea.. Journal of Arid Environments 53, 41–59.Google Scholar
Smalley, I.J., Vita-Finzi, C., (1968). The formation of fine particles in sandy deserts and the nature of ‘desert’ loess.. Journal of Sedimentary Petrology 38, 766–774.Google Scholar
Smalley, I.J., Krinsley, D.H., (1978). Loess deposits associated with deserts.. Catena 5, 53–66.Google Scholar
Smalley, I.J., Kumar, R., Dhand, K.O.H., Jefferson, I.F., Evans, R.D., (2005). The formation of silt material for terrestrial sediments: particularly loess and dust.. Sedimentary Geology 179, 321–358.Google Scholar
Smith, B.J., Wright, J.S., Whalley, W.B., (2002). Sources of non-glacial, loess-size quartz silt and the origins of “desert loess”.. Earth-Science Reviews 59, 1–26.Google Scholar
Soil Survey Staff (1999). Soil Taxonomy: A Basic System of Soil Classification for Making and Interpreting Soil Surveys.. U.S. Government Printing Office, Washington DC.Google Scholar
Stuut, J.-B.W., Prins, M.A., Schneider, R.R., Weltje, G.J., Jansen, J.H.F., Postma, G., (2002). A 300-kyr record of aridity and wind strength in southwesten Africa: inferences from grain-size distributions of sediments on Walvis Ridge, SE Atlantic.. Marine Geology 180, 221–233.Google Scholar
Sun, D., Bloemendal, J., Rea, D.K., Zhisheng, A., Vandenberghe, J., Huayu, L., Ruixia, S., Tungsheng, L., (2004). Bimodal grain-size distribution of Chinese loess, and its palaeoclimatic implications.. Catena 55, 325–340.Google Scholar
Tsoar, H., Moller, J.T., (1986). The role of vegetation in the formation of linear sand dunes.. Nickling, W.G. Aeolian Geomorphology Allen and Unwin, Boston., pp. 75–95.Google Scholar
Tsoar, H., Pye, K., (1987). Dust transport and the question of desert loess formation.. Sedimentology 34, 139–153.Google Scholar
Vandenberghe, J., An, Z., Nugteren, G., Lu, H., van, H.K., (1997). New absolute time scale for the Quaternary climate in the Chinese loess region by grain-size analysis.. Geology 25, 35–38.Google Scholar
Vriend, M., Prins, M.A., (2005). Calibration of modeled mixing patterns in loess grain-size distributions: an example from the north-eastern margin of the Tibetan plateau, China.. Sedimentology 52, 1361–1374.CrossRefGoogle Scholar
Waelbroeck, C., Labeyrie, L., Michel, E., Duplessy, J.C., McManus, J.F., Lambeck, K., Balbon, E., Labracherie, M., (2002). Sea-level and deep water temperature changes derived from bentic foraminifera isotopic records.. Quaternary Science Reviews 21, 295–305.Google Scholar
Whalley, W.B., Marshall, J.R., Smith, B.J., (1982). Origin of desert loess from some experimental observations.. Nature 300, 433–435.Google Scholar
Wright, J.S., (2001). Making loess-sized quartz silt: data from laboratory simulations and implications for sediment transport pathways and the formation of ‘desert’ loess deposits associated with the Sahara.. Quaternary International 76/77, 7–19.Google Scholar
Xiao, J., Porter, S.C., An, Z., Kumai, H., Yoshikawa, S., (1995). Grain size of quartz as an indicator of winter monsoon strength on the loess plateau of central China during the last 130,000 yr.. Quaternary Research 43, 22–29.Google Scholar
Yaalon, D.H., (1969). Origin of desert loess.. Etudes sur le Quaternaire dans le Monde vol. 2, Bulletin de l'Association Francaise pour l'Etude du Quaternaire. Association Francaise pour l'Etude du Quaternaire (AFEQ), Paris, France., pp. 755.Google Scholar
Yaalon, D.H., Ganor, E., (1973). The influence of dust on soils during the Quaternary.. Soil Science 116, 146–155.Google Scholar
Yaalon, D.H., Dan, J., (1974). Accumulation and distribution of loess-derived deposits in the semi-desert and desert fringe areas of Israel.. Zeitschrift fur Geomorphologie Supplementband 20, 91–105.Google Scholar
Yaalon, D.H., Ganor, E., (1979). East Mediterranean trajectories of dust-carrying storms from the Sahara and Sinai.. Morales, C. Saharan Dust John Wiley and Sons, 187–193.Google Scholar
Zilberman, E., (1992). The Late Pleistocene sequence of the northwestern Negev flood plains — a key to reconstructing the paleoclimate of southern Israel in the last glacial.. Israel Journal of Earth Science 41, 155–167.Google Scholar
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