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Holocene Lakes from Ramlat as-Sab'atayn (Yemen) Illustrate the Impact of Monsoon Activity in Southern Arabia

Published online by Cambridge University Press:  20 January 2017

Anne-Marie Lézine
Affiliation:
ESA 7073-CNRS, Paléontologie et Stratigraphie, UPMC-JUSSIEU, Boı̂te 106, 75252, Paris-cedex 05, France
Jean-François Saliège
Affiliation:
LODYC, UPMC-JUSSIEU, Boı̂te 100, 75252, Paris-cedex 05, France
Christian Robert
Affiliation:
Centre d'Océanographie de Marseille, Luminy Case 901, 13288, Marseille-09, France
Frédéric Wertz
Affiliation:
Centre d'Océanographie de Marseille, Luminy Case 901, 13288, Marseille-09, France
Marie-Louise Inizan
Affiliation:
ERA 28-CNRS (UPR 7549), MAE (Maison R. Ginouvès), 21, rue de l'Université, 92023, Nanterre cedex, France

Abstract

Paleoecology and paleohydrology of the Ramlat as-Sab'atayn (Southern Arabia) are reconstructed from a comparative study including sedimentology, mineralogy, stable isotope ratios of carbonates, and palynology of lacustrine sediments recovered from the al-Hawa depression. The section dates from 8700 to 7200 yr B.P. and records an early phase of flooding followed by distinct lacustrine development from 7800 to 7200 yr B.P., coeval with maximum activity of the Indian monsoon. Comparison of the pollen record with modern pollen deposition suggests that regional vegetation was then already of desert type and was related to strong seasonal trade winds.

Type
Original Articles
Copyright
University of Washington

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References

Al-Hubaishi, A., and Müller-Hohenstein, K. (1984). An Introduction to the Vegetation of Yemen. GTZ, Eschborn.Google Scholar
Bunker, D.G. (1953). The South-West borderlands of the Rub' Al Khali. The Geographical Journal 119, 420430.CrossRefGoogle Scholar
Chamley, H. (1989). Clay Sedimentology. Springer-Verlag, Berlin.CrossRefGoogle Scholar
Clark, I.D., and Fontes, J.-C. (1990). Paleoclimatic reconstruction in Northern Oman based on carbonates from hyperakaline groundwaters. Quaternary Research 33, 320336.Google Scholar
Craig, H. (1965). The measurement of oxygen isotope paleotemperatures. Stable Isotopes in Oceanographic Studies and Paleotemperatures p. 161–182Google Scholar
El Ghazali, G.A. (1991). Pollen Flora of Qatar. Scientific and Applied Research Center, University of Qatar, Google Scholar
El-Moslimany, A (1983). History of Climate and Vegetation in the Eastern Mediterranean and the Middle East from the Pleniglacial to the Mid-Holocene. Unpublished Ph.D. Dissertation, University of Washington, .Google Scholar
El-Moslimany, A. (1990). Ecological significance of common non-arboreal pollen: Examples from drylands of the Middle East. Review of Palaeobotany and Palynology. 64, 343350.Google Scholar
Emrich, K., Enhalt, D.H., and Vogel, J.C. (1970). Carbon isotope fractionation during the precipitation of calcium carbonate. Earth and Planetary Science Lettres 8, 363371.CrossRefGoogle Scholar
Faegri, K., and Iversen, J. (1975). Textbook of Pollen Analysis. Blackwell, Oxford.Google Scholar
Gasse, F., and Fontes, J.-Ch. (1989). Palaeoenvironments and palaeohydrology of a tropical closed lake (Lake Asal, Djibouti) since 10,000 yr B.P. Palaeogeography, Palaeoclimatology, Palaeoecology 69, 67102.Google Scholar
Fritz, P., and Poplawski, S. (1974). 18 13 . Earth and Planetary Science Lettres 24, 9198.CrossRefGoogle Scholar
Gebel, H.G., Hannss, C., Liebau, A., and Raehle, W. (1989). The late Quaternary environment of Ain al-Faidha/Al-Ain, Abu Dhabi Emirate. Archaeology in the United Arab Emirates, IV Google Scholar
Inizan, M.L., and Ortlieb, L. (1987). Préhistoire dans la région de Shabwa au Yémen du sud (R.D.P. Yémen). Paléorient 13, 521.CrossRefGoogle Scholar
Leroux, M. (1996). La dynamique du temps et du climat. Masson, Enseignement des Sciences de la Terre, Paris.Google Scholar
Lézine, A.-M., Casanova, J., and Hillaire-Marcel, C. (1990). Across an early Holocene humid phase in western Sahara: Pollen and isotope stratigraphy. Geology 18, 264267.Google Scholar
Petit-Maire, N., Sanlaville, P., and Yan, Z. (1995). Oscillations de la limite nord du domaine des moussons africaine, indienne, et asiatique au cours du dernier cycle climatique. Bulletin de la Société Géologique de France 166, 213230.Google Scholar
Reille, M. (1992). Pollen et spores d'Europe et d'Afrique du Nord. Laboratoire de Botanique Historique et Palynologie, Marseille.Google Scholar
Ritchie, J.C., and Haynes, C.V. (1987). Holocene vegetation zonation in the eastern Sahara. Nature 330, 645647.CrossRefGoogle Scholar
Roberts, N., and Wright, H.E. (1993). Vegetational, lake-level, and climatic history of the Near East and Southwest Asia.. In Global Climates since the Last Glacial Maximum Wright, H.E. pp. 194220. University of Minnesota Press, Minneapolis.Google Scholar
Rubinson, M., and Clayton, R.N. (1969). Carbon 13 fractionation between argonite and calcite. Geochimica Cosmochimica Acta 33, 9971002.CrossRefGoogle Scholar
Sanlaville, P. (1992). Changements climatiques dans la Péninsule Arabique durant le Pléistocène supéieur et l'Holocène. Paléorient 18, 525.CrossRefGoogle Scholar
Schultz, E., and Whitney, J.W. (1986). Upper Pleistocene and Holocene lakes in the An Nafud, Saudi Arabia. Hydrobiologia 143, 175190.Google Scholar
Sirocko, F., and Lange, H. (1991). Clay-mineral accumulation rates in the Arabian Sea during the late Quaternary. Marine Geology 97, 105119.CrossRefGoogle Scholar
Sirocko, F., Sarnthein, M., Lange, H., and Erlenkeuser, H. (1991). Atmospheric summer circulation and coastal upwelling in the Arabian Sea during the Holocene and the Last Glaciation. Quaternary Research 36, 7293.CrossRefGoogle Scholar
Sirocko, F., Sarnthein, M., Erlenkeuser, H., Lange, H., Arnold, M., and Duplessy, J.C. (1993). Century-scale events in monsoonal climate over the past 24,000 years. Nature 364, 322324.CrossRefGoogle Scholar
Stabel, H.H. (1986). Calcite precipitation in Lake Constance: Chemical equilibrium, sedimentation, and nucleation by algae. Limnology Oceanography 3, 10811093.Google Scholar
Stuiver, M., and Polach, H.A. (1977). Discussion reporting14 . Radiocarbon 19, 355363.Google Scholar
Talbot, M.R., and Allen, P.A. (1996). Lakes.Reading, M.G. Sedimentary Environments Blackwell, London.83124.Google Scholar
Tarutani, T., Clayton, R.N., and Mayada, T. (1969). The effect of polymorphism and magnesium substitution on oxygen isotope fractionation between calcium carbonate and water. Geochimica Cosmochimica Acta 33, 987996.CrossRefGoogle Scholar
Walter, H., Harnickell, E., and Mueller-Dombois, D. (1975). Climate-Diagram Maps of the Individual Continents and the Ecological Climatic Regions of the Earth. Gustav Fischer, Springer Verlag, Berlin.Google Scholar
Whitney, J. W., Faulkender, D. J., Meyer, R, (1983). The environmental History and Present condition of Saudi Arabia's northern sand seas.. USGS Open File Report 83-749.Google Scholar
Wood, J.R.I. (1997). A Handbook of Yemen Flora.. Royal Botanic Gardens, Kew.Google Scholar
Zarins, J., Ibrahim, M., Potts, D., and Edens, C. (1979). Preliminary report on the survey of the central province. 1978. Atlal 3, 1419.Google Scholar