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North Atlantic control on precipitation pattern in the eastern Mediterranean/Black Sea region during the last glacial

Published online by Cambridge University Press:  20 January 2017

Olga Kwiecien ,
Helge W. Arz ,
Frank Lamy ,
Birgit Plessen ,
André Bahr  and
Gerald H. Haug
Olga Kwiecien*
Affiliation:
Helmholz Centre Potsdam, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany DFG-Leibniz Center for Surface Process and Climate Studies at Universität Potsdam, Germany
Helge W. Arz
Affiliation:
Helmholz Centre Potsdam, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany
Frank Lamy
Affiliation:
Alfred Wegener Institute for Polar and Marine Research (AWI), 27570 Bremerhaven, Germany
Birgit Plessen
Affiliation:
Helmholz Centre Potsdam, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany
André Bahr
Affiliation:
IFM-GEOMAR, 24148 Kiel, Germany
Gerald H. Haug
Affiliation:
DFG-Leibniz Center for Surface Process and Climate Studies at Universität Potsdam, Germany Swiss Federal Institute of Technology (ETH Zürich), CH-8092 Zürich, Switzerland
*
*Corresponding author. GeoForschungsZentrum Potsdam, 14473 Potsdam, Germany. Fax: +49 331 288 1302. Email Address:kwiecien@gfz-potsdam.de
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Abstract

Based on proxy records from western Black Sea cores, we provide a comprehensive study of climate change during the last glacial maximum and late-glacial period in the Black Sea region. For the first time we present a record of relative changes in precipitation for NW Anatolia based on variations in the terrigenous supply expressed as detrital carbonate concentration. The good correspondence between reconstructed rainfall intensity in NW Anatolia and past western Mediterranean sea surface temperatures (SSTs) implies that during the glacial period the precipitation variability was controlled, like today, by Mediterranean cyclonic disturbances. Periods of reduced precipitation correlate well with low SSTs in the Mediterranean related to Heinrich events H1 and H2. Stable oxygen isotopes and lithological and mineralogical data point to a significant modification in the dominant freshwater/sediment source concomitant to the meltwater inflow after 16.4 cal ka BP. This change implies intensification of the northern sediment source and with other records from the Mediterranean region, consistently suggests a reorganization of the atmospheric circulation pattern affecting the hydrology of the European continent. The early deglacial northward retreat of both atmospheric and oceanic polar fronts was responsible for the warming in the Mediterranean region, leading simultaneously to more humid conditions in central and northern Europe.

Keywords

Black SeaMediterraneanPaleoclimatePrecipitationTerrigenous inputHeinrich events
Type
Articles
Information
Quaternary Research , Volume 71 , Issue 3 , May 2009 , pp. 375 - 384
Copyright
University of Washington

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References

Algan, O., Gazioglu, C., Cagatay, M.N., Yücel, Z.Y., and Gonencgil, B. Sediment and water influxes into the Black Sea by Anatolian rivers. Z. Geomorph. N. F. 43, (1999). 61–67.Google Scholar
Allen, J.R.M., Brandt, U., Brauer, A., Hubberten, H.-W., Huntley, B., Keller, J., Kraml, M., Mackensen, A., Mingram, J., Negendank, J.F.W., Nowaczyk, N.R., Oberhansli, H., Watts, W.A., Wulf, S., and Zolitschka, B. Rapid environmental changes in southern Europe during the last glacial period. Nature 400, (1999). 740–743.Google Scholar
Atanassova, J. Palaeoecological setting of the western Black Sea area during the last 15000 years. The Holocene 15, 4 (2005). 576–584.Google Scholar
Bahr, A., Lamy, F., Arz, H., Kuhlmann, H., and Wefer, G. Late glacial to Holocene climate and sedimentation history in the NW Black Sea. Mar. Geol. 214, (2005). 309–322.Google Scholar
Bahr, A., Arz, H.W., Lamy, F., and Wefer, G. Late glacial to Holocene paleoenvironmental evolution of the Black Sea, reconstructed with stable oxygen isotope records obtained on ostracod shells. Earth Planet. Sci. Lett. 241, (2006). 863–875.CrossRefGoogle Scholar
Bahr, A., Arz, H.W., Lamy, F., Major, C., Kwiecien, O., and Wefer, G. Abrupt changes of temperature and water chemistry in the late Pleistocene and early Holocene Black Sea. G-cubed 9, (2008). http://dx.doi.org/10.1029/2007GC001683 Google 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. Quat. Res. 47, (1997). 155–168.Google Scholar
Bard, E., Rostek, F., Turon, J.-L., and Gendreau, S. Hydrological impact of Heinrich events in the subtropical Northeast Atlantic. Science 289, (2000). 1321–1324.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
Bond, G., Broecker, W.S., Johnsen, S.J., McManus, J., Labeyrie, L., Jouzel, J., and Bonani, G. Correlations between climate records from North Atlantic sediments and Greenland ice. Nature 365, (1993). 143–147.Google Scholar
Cacho, I., Grimalt, J.O., Pelejero, C., Canals, M., Sierro, F.J., Flores, J.A., and Shackleton, N. Daansgard-Oeschger and Heinrich event imprints in Alboran Sea paleotemperatures. Paleoceanography 14, (1999). 689–705.Google Scholar
Cacho, I., Grimalt, J.O., Sierro, F.J., Shackleton, N., and Canals, M. Evidence for enhanced Mediterranean thermohaline circulation during rapid climatic coolings. Earth Planet. Sci. Lett. 183, (2000). 417–429.Google Scholar
Cacho, I., Grimalt, J.O., Canals, M., Sbaffi, L., Shackleton, N.J., Schönfeld, J., and Zahn, R. Variability of the western Mediterranean Sea surface temperature during the last 25 000 and its connection the Northern Hemisphere climatic changes. Paleoceanography 16, (2001). 40–52.Google Scholar
Cacho, I., Shackleton, N., Elderfield, H., Sierro, F.J., and Grimalt, J.O. Glacial rapid variability in deep-water temperature and d18O from the Western Mediterranean Sea. Quat. Sci. Rev. 25, (2006). 3294–3311.CrossRefGoogle Scholar
Chapman, M.R., and Maslin, M.A. Low-latitude forcing of meridional temperature and salinity gradients in the subpolar North Atlantic and the growth of glacial ice sheets. Geology 27, (1999). 875–878.Google Scholar
Ciner, A. Turkish glaciers and glacial deposits. Ehlers, J., and Gibbard, P.L. Quaternary Glaciations; Extentand Chronology, Part I: Europe. (2004). Elsevier Publishers, Amsterdam. 419–429.Google Scholar
Combourieu Nebout, N., Turon, J.L., Zahn, R., Capotondi, L., Londeix, L., and Pahnke, K. Enhanced aridity and atmospheric high-pressure stability over the western Mediterranean during the North Atlantic cold events of the past 50 ky. Geology 30, (2002). 863–866.Google Scholar
Demidov, I.N., Houmark-Nielsen, M., Kjaer, K.H., and Larsen, E. The last Scandinavian ice sheet in northwestern Russia: ice flow patterns and decay dynamics. Boreas 35, (2006). 425–443.Google Scholar
Ehrmann, W., Schmiedl, G., Hamann, Y., Kuhnt, T., Hemleben, C., and Siebel, W. Clay minerals in late glacial and Holocene sediments of the northern and southern Aegean Sea. Palaeogeogr., Palaeoclimatol., Palaeoecol. 249, (2007). 36–57.Google Scholar
EIE, State General Directory of Electrical Research Works Sediment data and sediment transport amount for surface waters in Turkey. (1993). EIE, Ankara, Turkey.Google Scholar
Florineth, D., and Schluchter, C. Alpine evidence for atmospheric circulation patterns in Europe during the last glacial maximum. Quat. Res. 54, (2000). 295–308.Google Scholar
Fontugne, M., Kuzucuoglu, C., Karabiyikoglu, M., Hatte, C., and Pastre, J.-F. From Pleniglacial to Holocene: a 14C chronostratigraphy of environmental changes in the Konya Plain, Turkey. Quat. Sci. Rev. 18, (1999). 573–591.Google Scholar
Geological Research Department of the General Directorate of Mineral Research and Exploration, (2002). Geological Map of Turkey.Google Scholar
Grootes, P., Stuvier, M., White, J.W.C., Johnsen, S.J., and Jouzel, J. Comparison of oxygen isotope records from the GISP2 and GRIP Greeenland ice cores. Nature 366, (1993). 552–554.CrossRefGoogle Scholar
Harrison, S.P., Yu, G., and Tarasov, P.E. Late Quaternary lake-level record from Northern Eurasia. Quat. Res. 45, (1996). 138–159.CrossRefGoogle Scholar
Jansen, J.H.F., Van der Gaast, S.J., Koster, B., and Vaars, A.J. CORTEX, a shipboard XRF-scanner for element analyses in split sediment cores. Mar. Geol. 151, (1998). 143–153.CrossRefGoogle Scholar
Jones, M.D., Roberts, C.N., and Leng, M.J. Quantifying climatic change through the last glacial-interglacial transition based on lake isotope palaeohydrology from central Turkey. Quat. Res. 67, (2007). 463–473.CrossRefGoogle Scholar
Kalicki, T., and Sanko, A.F. Palaeohydrological changes in the Upper Dneper Valley, Belarus, during the last 20,000 years. Benito, G. et al. Palaeohydrology and Environmental Change. (1998). Wiley, Chichester, England. 125–135.Google Scholar
Konikov, E., Likhodedova, O., and Pedan, G. Paleogeographic reconstruction of sea-level change and coastline migration on the northwestern Black Sea shelf over the past 18 kyr. Quat. Int. 167–168, (2007). 49–60.CrossRefGoogle Scholar
Kostopoulou, E., and Jones, P.D. Comprehensive analysis of the climate variability in the eastern Mediterranean. Part II: relationships between atmospheric circulation patterns and surface climatic elements. Int. J. Climatol. 27, (2007). 1351–1371.Google Scholar
Kroonenberg, S.B., Rusakov, G.V., and Svitoch, A.A. The wandering of the Volga delta: a response to rapid Caspian sea-level change. Sediment. Geol. 107, (1997). 189–209.Google Scholar
Kwiecien, O., Arz, H.W., Lamy, F., Wulf, S., Bahr, A., Röhl, U., and Haug, G.H. Estimated reservoir ages of the Black Sea since the last glacial. Radiocarbon 50, (2008). 99–118.CrossRefGoogle Scholar
Lamy, F., Arz, H.W., Bond, G., Bahr, A., and Patzold, J. Multicentennial-scale hydrological changes in the Black Sea and northern Red Sea during the Holocene and the Arctic/North Atlantic Oscillation. Paleoceanography 21, (2006). http://dx.doi.org/10.1029/2005PA001184 CrossRefGoogle Scholar
Major, C., Ryan, W., Lericolais, G., and Hajdas, I. Constraints on Black Sea outflow to the Sea of Marmara during the last glacial-interglacial transition. Mar. Geol. 190, (2002). 19–34.Google Scholar
Major, C.O., Goldstein, S.L., Ryan, W.B.F., Lericolais, G., Piotrowski, A.M., and Hajdas, I. The co-evolution of Black Sea level and composition through the last deglaciation and its paleoclimatic significance. Quat. Sci. Rev. 25, (2006). 2031–2047.Google Scholar
Mangerud, J., Jakobsson, M., Alexanderson, H., Astakhov, V., Clarke, G.K.C., Henriksen, M., Hjort, C., Krinner, G., Lunkka, J.-P., and Moller, P. Ice-dammed lakes and rerouting of the drainage of northern Eurasia during the last glaciation. Quat. Sci. Rev. 23, (2004). 1313–1332.Google Scholar
Menot, G., Bard, E., Rostek, F., Weijers, J.W.H., Hopmans, E.C., Schouten, S., and Damste, J.S.S. Early reactivation of European rivers during the last deglaciation. Science 313, (2006). 1623–1625.Google Scholar
Mudie, P.J., Rochon, A., Aksu, A.E., and Gillespie, H. Dinoflagellate cysts, freshwater algae and fungal spores as salinity indicators in Late Quaternary cores from Marmara and Black seas. Mar. Geol. 190, (2002). 203–231.Google Scholar
Mudie, P.J., Marret, F., Aksu, A.E., Hiscott, R.N., and Gillespie, H. Palynological evidence for climatic change, anthropogenic activity and outflow of Black Sea water during the late Pleistocene and Holocene: centennial- to decadal-scale records from the Black and Marmara Seas. Quat. Int. 167–168, (2007). 73–90.CrossRefGoogle Scholar
Müller, G., and Stoffers, P. Mineralogy and petrology of the Black Sea basin sediments. Degens, E.T., and Ross, D.A. The Black Sea: Geology, Chemistry, and Biology. (1974). AAPG, Tulsa, OK. 200–248.Google Scholar
Prasad, S., Vos, H., Negendank, J.F.W., Waldmann, N., Goldstein, S.L., and Stein, M. Evidence from Lake Lisan of solar influence on decadal- to centennial-scale climate variability during marine oxygen isotope stage 2. Geology 32, (2004). 581–584.Google Scholar
Prentice, I.C., Guiot, J., and Harrison, S.P. Mediterranean vegetation, lake levels and paleoclimate at the last glacial maximum. Nature 360, (1992). 658–660.Google Scholar
Renssen, H., and Bogaart, P. Atmospheric variability over the ∼ 14.7 kyr BP stadial-interstadial transition in the North Atlantic region as simulated by an AGCM. Clim. Dyn. 20, (2003). 301–313.CrossRefGoogle Scholar
Reimer, P.J., Baillie, M.G.L., Bard, E., Bayliss, A., Beck, J.W., Bertrand, C.J.H., Blackwell, P.G., Buck, C.E., Burr, G.S., Cutler, K.B., Damon, P.E., Edwards, R.L., Fairbanks, R.G., Friedrich, M., Guilderson, T.P., Hogg, A.G., Hughen, K.A., Kromer, B., McCormac, G., Manning, S., Ramsey, C.B., Reimer, R.W., Remmele, S., Southon, J.R., Stuiver, M., Talamo, S., Taylor, F.W., van der Plicht, J., and Weyhenmeyer, C.E. IntCal04 terrestrial radiocarbon age calibration, 0–26 cal kyr BP. Radiocarbon 43, (2004). 1029–1085.Google Scholar
Rinterknecht, V.R., Clark, P.U., Raisbeck, G.M., Yiou, F., Bitinas, A., Brook, E.J., Marks, L., Zelcs, V., Lunkka, J.-P., Pavlovskaya, I.E., Piotrowski, J.A., and Raukas, A. The last deglaciation of the Southeastern sector of the Scandinavian ice sheet. Science 311, (2006). 1449–1452.CrossRefGoogle ScholarPubMed
Rohling, E.J., Hayes, A., Kroon, D., De Rijk, S., Zachariasse, W.J., and Eisma, D. Abrupt cold spells in the NW Mediterranean. Paleoceanography 13, (1998). 316–322.CrossRefGoogle Scholar
Ryan, W., Major, C., Lericolais, G., and Goldstein, S.L. Catastrophic flooding of the Black Sea. Ann. Rev. Earth Planet. Sci. 31, (2003). 525–554.Google Scholar
Sánchez Goñi, M.F., Turon, J.-L., Eynaud, F., and Gendreau, S. European climatic response to millennial-scale changes in the atmosphere–ocean system during the last glacial period. Quat. Res. 54, (2000). 394–403.Google Scholar
Sánchez Goñi, M.F., Cacho, I., Turon, J.L., Guiot, J., Sierro, F.J., Peypouquet, J.P., Grimalt, J.O., and Shackleton, N.J. Synchroneity between marine and terrestrial responses to millennial scale climatic variability during the last glacial period in the Mediterranean region. Clim. Dyn. 19, (2002). 95–105.Google Scholar
Schrader, H.J. Quaternary paleoclimatology of the Black Sea basin. Sediment. Geol. 23, (1979). 165–180.Google Scholar
Sierro, F.J., Hodell, D.A., Curtis, H.J., Flores, J.A., Reguera, I., Colmenero-Hidalgo, E., Barcena, M.A., Grimalt, J.O., Cacho, I., Frigola, J., and Canals, M. Impact of iceberg melting on Mediterranean thermohaline circulation during Heinrich events. Paleoceanography 20, (2005). http://dx.doi.org/10.1029/2004PA001051 Google Scholar
Stuiver, M., Reimer, P.J., and Reimer, R.W., (2005). Calib 5.0. (www pragram and documentation). URL: http://calib.qub.ac.uk/calib/.Google Scholar
Svendsen, J.I., Alexanderson, H., Astakhov, V.I., Demidov, I., Dowdeswell, J.A., Funder, S., Gataullin, V., Henriksen, M., Hjort, C., and Houmark-Nielsen, M. Late Quaternary ice sheet history of northern Eurasia. Quat. Sci. Rev. 23, (2004). 1229–1271.Google Scholar
Tjallingii, R., Röhl, U., Kölling, M., and Bickert, T. Influence of the water content on X-ray fluorescence corescanning measurements in soft marine sediments. Geochem. Geophys. Geosystems 8, (2007). http://dx.doi.org/10.1029/2006GC001393 CrossRefGoogle Scholar
Touchan, R., Akkemik, U., Hughes, M.K., and Erkan, N. May–June precipitation reconstruction of southwestern Anatolia, Turkey during the last 900 years from tree rings. Quat. Res. 68, (2007). 196–202.Google Scholar
Türkes, M., and Erlat, E. Climatological responses of winter precipitation in Turkey to variability of the North Atlantic Oscillation during the period 1930–2001. Theor. Appl. Climatol. 81, (2005). 45–69.Google Scholar
Vescovi, E., Ravazzi, C., Arpenti, E., Finsinger, W., Pini, R., Valsecchi, V., Wick, L., Ammann, B., and Tinner, W. Interactions between climate and vegetation during the Lateglacial period as recorded by lake and mire sediment archives in Northern Italy and Southern Switzerland. Quat. Sci. Rev. 26, (2007). 1650–1669.Google Scholar
von Grafenstein, U., Erlernkeuser, H., and Trimborn, P. Oxygen and carbon isotopes in modern fresh-water ostracod valves: assessing vital offsets and autecological effects of interest for palaeoclimate studies. Palaeogeogr., Palaeoclimatol., Palaeoecol. 148, (1999). 133–152.Google Scholar
Wigley, T.M.L., and Farmer, G. Climate of the Eastern Mediterranean and the Near East. Bintliff, J.L. et al. Paleoclimates, Paleoenvironments and Human Communities in the Eastern Mediterranean Region in Later Prehistory. (1982). 3–37.Google Scholar