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Quantifying climatic change through the last glacial–interglacial transition based on lake isotope palaeohydrology from central Turkey

Published online by Cambridge University Press:  20 January 2017

Matthew D. Jones ,
C. Neil Roberts  and
Melanie J. Leng
Matthew D. Jones*
Affiliation:
School of Geography, University of Nottingham, University Park, Nottingham, NG7 2RD, UK School of Geography, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK
C. Neil Roberts
Affiliation:
School of Geography, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK
Melanie J. Leng
Affiliation:
School of Geography, University of Nottingham, University Park, Nottingham, NG7 2RD, UK NERC Isotope Geosciences Laboratory, British Geological Survey, Nottingham, NG12 5GG, UK
*
*Corresponding author. School of Geography, University of Nottingham, University Park, Nottingham, NG7 2RD, UK. Fax: +44 115 9514249. E-mail address:matthew.jones@nottingham.ac.uk (M.D. Jones).
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Abstract

Questions remain as to the nature of climatic change through the last glacial–interglacial transition in the eastern Mediterranean region, particularly the relative contribution of evaporation and precipitation to regional water balance. Here changes in oxygen isotope values through this time period from Eski Acıgöl, a crater lake in central Turkey, are investigated using hydrological and isotope mass balance models. These allow changes in evaporation and precipitation to be quantified and their relative importance evaluated. We show that it is the volumetric flux rate of water passing through the lake system and not the precipitation-to-evaporation ratio per se which controlled the stable isotope record in Eski Acıgöl. Early Holocene precipitation is shown to be much greater than that during both the latter part of the last glaciation and the present day. We test these calculated values against other records in the same region, firstly with other lake records in Anatolia, the Konya basin and Lake Van, and secondly with isotope-inferred palaeo-precipitation data from Soreq cave in Israel. This reveals a contrast between pre- and post-LGM precipitation values in Turkey (wetter and drier, respectively) and also suggests that during the last glacial–interglacial transition there was a more marked precipitation gradient than at present between northern/interior and southern/coastal parts of the eastern Mediterranean region.

Keywords

Oxygen isotopeLast glacial maximumPrecipitationTurkeyLakes
Type
Research Article
Information
Quaternary Research , Volume 67 , Issue 3 , May 2007 , pp. 463 - 473
Copyright
University of Washington

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References

Anderson, T.F., and Arthur, M.A. Stable isotopes of oxygen and carbon and their application to sedimentological and palaeoenvironmental problems. Arthur, M.A., Anderson, T.F., Kaplan, J.R., Veizer, J., Land, L.S. Stable Isotopes in Sedimentary Geochemistry: Society of Economic Palaeontologists and Mineralogists Short Course vol. 10, (1983). Google Scholar
Ariztegui, D., Asioli, A., Lowe, J.J., Trincardi, F., Vigliotti, L., Tamburini, F., Chondrogianni, C., Accorsi, C.A., Mazzanti, M.B., Mercuri, A.M., van der Kaars, S., McKenzie, J.A., and Oldfield, F. Palaeoclimate and the formation of sapropel S1: inferences from Late Quaternary lacustrine and marine sequences in the central Mediterranean region. Palaeogeography, Palaeoclimatology, Palaeoecology 158, (2000). 215–240.CrossRefGoogle Scholar
Bar-Matthews, M., Ayalon, A., and Kaufman, A. Late quaternary paleoclimate in the eastern Mediterranean region from stable isotope analysis of speleothems at Soreq Cave, Israel. Quaternary Research 47, (1997). 155–168.CrossRefGoogle Scholar
Bar-Matthews, M., Ayalon, A., Gilmore, M., Matthews, A., and Hawkesworth, C.J. Sea-land oxygen isotope relationships from planktonic foraminifera and speleothems in the Eastern Mediterranean region and their implications for paleorainfall during interglacial intervals. Geochimica et Cosmochimica Acta 67, (2003). 3181–3199.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.Google Scholar
Bartov, Y., Goldstein, S.L., Stein, M., and Enzel, Y. Catastrophic arid episodes in the Eastern Mediterranean linked with the North Atlantic Heinrich events. Geology 31, (2003). 439–442.2.0.CO;2>CrossRefGoogle Scholar
Benson, L., and Paillet, F. HIBAL: a hydrologic–isotopic-balance model for application to paleolake systems. Quaternary Science Reviews 21, (2002). 1521–1539.CrossRefGoogle Scholar
Benson, L.V., and White, J.W.C. Stable isotopes of oxygen and hydrogen in the Truckee River-Pyramid Lake surface-water system. 3. Source of water vapor overlying Pyramid Lake. Limnology and Oceanography 39, (1994). 1954–1958.Google Scholar
Druitt, T.H., Brenchley, P.J., Gökten, Y.E., and Francaviglia, V. Late Quaternary rhyolitic eruptions from the Acıgöl complex, central Anatolia. Journal of the Geological Society (London) 152, (1995). 655–667.Google Scholar
El-Moslimany, A. Comment on Roberts, N. “Age, palaeoenvironments and climatic significance of Late Pleistocene Konya lake, Turkey”. Quaternary Research 21, (1984). 115–116.Google 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.Google Scholar
Fontugne, M., Kuzucuoğlu, C., Karabıyıkoğlu, M., Hatte, C., and Pastre, J.-F. From Pleniglacial to Holocene: a C-14 chronostratigraphy of environmental changes in the Konya Plain, Turkey. Quaternary Science Reviews 18, (1999). 573–591.Google Scholar
Gibson, J.J., Edwards, T.W.D., and Prowse, T.D. Pan-derived isotopic composition of atmospheric water vapor and its variability in northern Canada. Journal of Hydrology 217, (1999). 55–74.Google Scholar
Harrison, S.P., and Digerfeldt, G. European lakes as palaeohydrological and palaeoclimatic indicators. Quaternary Science Reviews 12, (1993). 233–248.Google Scholar
Hayes, A., Kucera, M., Kallel, N., Sbaffi, L., and Rohling, E.J. Glacial Mediterranean sea surface temperatures based on planktonic foraminiferal assemblages. Quaternary Science Reviews 24, (2005). 999–1016.CrossRefGoogle Scholar
Hazan, N., Stein, M., Agnon, A., Nadel, D., Negendank, J.F.W., Schwag, M.J., and Neev, D. The late Quaternary limnological history of Lake Kinneret (Sea of Galilee), Israel. Quaternary Research 63, (2005). 60–77.Google Scholar
IAEA/WMO, (2001). Global network of isotopes in precipitation. The GNIP Database. Accessible at: http://www.isohis.iaea.org.Google Scholar
Jones, M.D., Leng, M.J., Roberts, C.N., Türkeş, M., and Moyeed, R. A coupled calibration and modelling approach to the understanding of dry-land lake oxygen isotope records. Journal of Paleolimnology 34, (2005). 391–411.Google Scholar
Jones, M.D., Roberts, C.N., Leng, M.J., and Türkeş, M. A high-resolution late Holocene lake isotope record from Turkey and links to North Atlantic and monsoon climate. Geology 34, (2006). 361–364.CrossRefGoogle Scholar
Kim, S.-T., and O'Neil, J.R. Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates. Geochimica et Cosmochimica Acta 61, (1997). 3461–3475.CrossRefGoogle Scholar
Kuzucuoğlu, C., Parish, R., and Karabiyikoğlu, M. The dune systems of the Konya Plain (Turkey): their relation to environmental changes in Central Anatolia during the Late Pleistocene and Holocene. Geomorphology 23, (1998). 257–271.CrossRefGoogle Scholar
Land, L.S. The isotopic and trace element geochemistry of dolomite: the state of the art. Zenger, D.H. Concepts and Models of Dolomitisation. SEPM Special Publication vol. 28, (1980). 87–110.Google Scholar
Landmann, G., Reimer, A., and Kempe, S. Climatically induced lake level changes at Lake Van, Turkey, during the Pleistocene/Holocene transition. Global Biogeochemical Cycles 10, (1996). 797–808.CrossRefGoogle Scholar
Lemke, G., and Sturm, M. δ 18O and trace element measurements as proxy for the reconstruction of climate changes at Lake Van (Turkey): preliminary results. Dalfes, N.D. Third Millennium BC Climate Change and Old World Collapse. NATO ASI Series (1997). 149 Google Scholar
Leng, M.J., and Marshall, J.D. Palaeoclimate interpretation of stable isotope data from lake sediment archives. Quaternary Science Reviews 23, (2004). 811–831.Google Scholar
Linacre, E. Climate Data and Resources: A Reference and Guide. (1992). Routledge, London. 366 pp.Google Scholar
Majoube, F. Fractionnement en oxygène-18 et un deutérium entre l'eau et sa vapeur. Journal of Chemical Physics 187, (1971). 1423–1436.Google Scholar
McGarry, S., Bar-Matthews, M., Matthews, A., Vaks, A., Schilman, B., and Ayalon, A. Constraints on hydrological and paleotemperature variations in the Eastern Mediterranean region in the last 140 ka given by the δD values of speleothem fluid inclusions. Quaternary Science Reviews 23, (2004). 919–934.CrossRefGoogle Scholar
Meteoroloji Bulteni, , (1974). Devlet Meteoroloji Iþleri Genel Müdürlüðü (State Meteorological Services.), Ankara.Google Scholar
Prentice, I.C., Guiot, J., and Harrison, S.P. Mediterranean vegetation, lake levels and palaeoclimate at the Last Glacial Maximum. Nature 360, (1992). 658–660.Google Scholar
Ricketts, R.D., and Johnson, T.C. Climate change in the Turkana basin as deduced from a 4000 year long δ 18O record. Earth and Planetary Science Letters 142, (1996). 7–17.CrossRefGoogle Scholar
Roberts, N. Age, palaeoenvironments and climatic significance of Late Pleistocene Konya Lake, Turkey. Quaternary Research 19, (1983). 154–171.Google Scholar
Roberts, N., Wright, H.E. Jr. Vegetational, lake-level and climatic history of the Near East and Southwest Asia. Wright, H.E. Jr., Kutzbach, J.E., Webb, T. III, Ruddiman, W.F., Street-Perrott, F.A., and Bartlein, P.J. Global Climates Since the Last Glacial Maximum. (1993). Univ. of Minnesota Press, Minneapolis. 194–220.Google Scholar
Roberts, N., Reed, J., Leng, M.J., Kuzucuoğlu, C., Fontugne, M., Bertaux, J., Woldring, H., Bottema, S., Black, S., Hunt, E., and Karabıyıkoğlu, M. The tempo of Holocene climatic change in the eastern Mediterranean region: new high-resolution crater-lake sediment data from central Turkey. Holocene 11, (2001). 721–736.Google Scholar
Robinson, S.A., Black, S., Sellwood, B.W., and Valdes, P.J. A review of palaeoclimates and palaeoenvironments in the Levant and Eastern Mediterranean from 25,000 to 5000 years BP: setting the environmental background for the evolution of human civilisation. Quaternary Science Reviews 25, (2006). 1517–1541.CrossRefGoogle Scholar
Saarnisto, M. Annually laminated sediments. Berglund, B.E. Handbook of Holocene Palaeoecology and Palaeohydrology. (1986). Wiley, Chichester, UK.Google Scholar
Stein, M. The sedimentary and geochemical record of Neogene-Quaternary water bodies in the Dead Sea Basin—Inferences for the regional paleoclimatic history. Journal of Paleolimnology 26, (2001). 271–282.CrossRefGoogle Scholar
Tarutani, T., Clayton, R.N., and Mayeda, T.K. The effect of polymorphism and magnesium substitution on oxygen isotope fractionation between calcium carbonate and water. Geochimica et Cosmochimica Acta 33, (1965). 987–996.CrossRefGoogle Scholar
van Zeist, W., and Bottema, S., (1991). Late Quaternary vegetation of the Near East. Beihefte zum Tübinger Atlas des Vorderen Orients, Reihe A18. Dr L. Reichert Verlag, Wiesbaden., 156 pp.Google Scholar
Wasylikowa, K. Palaeoecology of Lake Zeribar, Iran in the Pleniglacial, Late Glacial and Holocene reconstructed from plant macrofossils. Holocene 15, (2005). 720–735.Google Scholar
Wick, L., Lemcke, G., and Sturm, M. Evidence of Late glacial and Holocene climatic change and human impact in eastern Anatolia: high-resolution pollen, charcoal, isotopic and geochemical records from the laminated sediments of Lake Van, Turkey. Holocene 13, (2003). 665–675.Google Scholar
Woldring, H., and Bottema, S. The vegetation history of East-Central Anatolia in relation to archaeology: the Eski Acıgöl pollen evidence compared with the Near Eastern environment. Palaeohistoria 43/44, (2003). 1–34.Google Scholar
Wyputta, U., and Grieger, B. Comparison of eastern Atlantic atmospheric trajectories for present day and last glacial maximum. Palaeogeography, Palaeoclimatology, Palaeoecology 146, (1999). 53–66.Google Scholar
Zhou, G.-T., and Zheng, Y.-F. An experimental study of oxygen isotope fractionation between inorganically precipitated aragonite and water at low temperatures. Geochimica et Cosmochimica Acta 67, (2003). 387–399.CrossRefGoogle Scholar