Terrestrial stable isotope records of Late Quaternary paleoclimates in the eastern Mediterranean region |
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| Institution: | 1. Department of Earth and Space Sciences, University of Washington, Johnson Hall Rm-070, Box 351310, 4000 15th Avenue NE, Seattle, WA 98195-1310, United States;2. Department of Geosciences, Pacific Lutheran University, Rieke Rm-158, Tacoma, WA 98447-0003, United States;1. Department of Earth Sciences, ETH Zürich, Sonneggstrasse 5, 8092 Zürich, Switzerland;2. Department of Geological Sciences, Stanford University, 450 Serra Mall, Bldg. 320, Rm. 118, Stanford, CA 94305, USA;1. Department of Stratigraphy, Faculty of Geological Sciences, Complutense University of Madrid, 28040 Madrid, Spain;2. Institute of Geosciences (CSIC-UCM), c/ José Antonio Nováis 12, 28040 Madrid, Spain;3. CENIEH, Paseo Sierra de Atapuerca s/n, 09002 Burgos, Spain;4. Ciemat, Departamento de Medioambiente, Avda. Complutense 22, 28040 Madrid, Spain |
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| Abstract: | Terrestrial stable isotope records (13C/12C, 18O/16O, and D/H ratios) of late Quaternary paleoclimates in the eastern Mediterranean region are reviewed. Significant paleoclimatic reconstructions come from a variety of isotopic studies. Paleogroundwaters, although they cannot be accurately dated, show oxygen and hydrogen isotopic compositions highly depleted in heavier isotopes compared to modern meteoric waters in arid regions of southern Israel, Sinai and northeastern Africa and attest to a major difference in climatic regime some time in the Pleistocene. Th-U dating of land snails showing a similar 18O depletion indicates ages of 100,000 yr and ≥300,000 yr for this climatic regime in the Negev Desert of southern Israel. Carbon isotope records of organic matter have not been studied extensively in the region, except for the record of Holocene land snails in the Negev. These document a southward shift in pure C3 plant communities in the middle and early Holocene relative to their present distribution and indicate wetter conditions at those times. An oxygen isotope curve for the Holocene, reflecting changes in the isotopic composition of precipitation, has been established from analysis of carbonate materials—land snail shells and speleothems. The curve indicates a depletion of ca. 2‰ in 18O centered around 7000 cal yr bp, with modern levels being reached by 5000 cal yr bp. Carbon isotope analysis of soil carbonates in paleosols developed in loess in the Negev show the existence of dramatic north–south climatic gradients at the times of formation of the soils (ca. 13,000, 28,000, and ≥37,000 14C yr bp), as occur also today due to the waning influence of Mediterranean to the south. Some isotopic methods, widely used in other regions, have received little or no attention in the eastern Mediterranean region. These include oxygen and hydrogen isotopes in wood, phosphate oxygen and organic carbon in bones and teeth, and carbon in soil organic matter. |
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