Articles | Volume 11, issue 12
https://doi.org/10.5194/cp-11-1785-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-11-1785-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
21 Dec 2015
Research article |
| 21 Dec 2015
Reconstruction of MIS 5 climate in the central Levant using a stalagmite from Kanaan Cave, Lebanon
Department of Earth and History of Life, Royal Institute of Natural Sciences (RBINS), Brussels, Belgium
Analytical, Environmental & Geo-Chemistry, Department of Chemistry, Faculty of Sciences, Vrije Universiteit Brussel, Brussels, Belgium
S. Verheyden
Department of Earth and History of Life, Royal Institute of Natural Sciences (RBINS), Brussels, Belgium
Analytical, Environmental & Geo-Chemistry, Department of Chemistry, Faculty of Sciences, Vrije Universiteit Brussel, Brussels, Belgium
S. R. Noble
NERC Isotope Geosciences Laboratory, Keyworth, Nottingham, NG12 5GG, UK
A. R. Farrant
British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK
D. Sahy
British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK
J. Hellstrom
Geochemistry Laboratory, Earth Science Department, University of Melbourne, Melbourne, Australia
J. J. Delannoy
Laboratoire EDYTEM UMR5204 CNRS, Université de Savoie, Bourget-du-Lac, France
P. Claeys
Analytical, Environmental & Geo-Chemistry, Department of Chemistry, Faculty of Sciences, Vrije Universiteit Brussel, Brussels, Belgium
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Speleothems are a popular, multi-proxy climate archive that provide regional to global insights into past hydroclimate trends with precise chronologies. We present an update to the SISAL (Speleothem Isotopes
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Sietske J. Batenburg, David De Vleeschouwer, Mario Sprovieri, Frederik J. Hilgen, Andrew S. Gale, Brad S. Singer, Christian Koeberl, Rodolfo Coccioni, Philippe Claeys, and Alessandro Montanari
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Related subject area
Subject: Continental Surface Processes | Archive: Terrestrial Archives | Timescale: Decadal-Seasonal
50-year seasonal variability in East African droughts and floods recorded in central Afar lake sediments (Ethiopia) and their connections with the El Niño–Southern Oscillation
Reconstructing hydroclimate changes over the past 2500 years using speleothems from Pyrenean caves (NE Spain)
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Miguel Bartolomé, Ana Moreno, Carlos Sancho, Isabel Cacho, Heather Stoll, Negar Haghipour, Ánchel Belmonte, Christoph Spötl, John Hellstrom, R. Lawrence Edwards, and Hai Cheng
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Cited articles
Andersen, M. B., Stirling, C. H., Potter, E. K., Halliday, A. N., Blake, S. G., McCulloch, M. T., Ayling, B. F. and O'Leary, M.: High-precision U-series measurements of more than 500 000 year old fossil corals, Earth Planet. Sc. Lett., 265, 229–245, 2008.
Arz, H. W., Lamy, F., Patzold, J., Muller, P. J., and Prins, M.: Mediterranean moisture source for an early-Holocene humid period in the northern Red Sea, Science, 300, 118–121, 2003.
Ayalon, A., Bar-Matthews, M., and Kaufman, A.: Climatic conditions during marine isotopic stage 6 in the Eastern Mediterranean region as evident from the isotopic composition of speleothems: Soreq Cave, Israel, Geology, 30, 303–306, 2002.
Ayalon, A., Bar-Matthews, M., Frumkin, A., and Matthews, A.,: Last Glacial warm events on Mount Hermon: the southern extension of the Alpine karst range in the east Mediterranean, Quaternary Sci. Rev., 59, 43–56, 2013.
Baker, A. and Smart, P. L.: Recent flowstone growth rates: field measurements in comparison to theoretical predictions, Chem. Geol., 122, 121–128, 1995.
Bar-Matthews, M.: History of Water in the Middle East and North Africa, in: Treatise on Geochemistry, edited by: Holland H. D. and Turekian K. K., Second Edition, Oxford, Elsevier, 109–128, 2014.
Bar-Matthews, M., Ayalon, A., Kaufman, A., and Wasserburg, G. J.: The Eastern Mediterranean paleoclimate as a reflection of regional events: Soreq Cave, Israel, Earth Planet. Sc. Lett., 166, 85–95, 1999.
Bar-Matthews, M., Ayalon, A., and Kaufman, A.: Timing and hydrological conditions of Sapropel events in the Eastern Mediterranean, as evident from speleothems, Soreq Cave, Israel, Chem. Geol., 169, 145–156, 2000.
Bar-Matthews, M., Ayalon, A., Gilmour, M., Matthews, M., and Hawkesworth, C.: Sea-land isotopic relationships from planktonic foraminifera and speleothems in the Eastern Mediterranean region and their implications for paleorainfall during interglacial interval, Geochim. Cosmochim. Ac., 67, 3181–3199, 2003.
Bronk Ramsey, C.: Deposition models for chronological records, Quaternary Sci. Rev., 27, 42–60, 2008.
Berger, A. and Loutre, M. F.: Insolation values for the climate of the last 10 million years, Quaternary Sci. Rev., 10, 297–317, 1991.
Cheddadi, R. and Rossignol-Strick, M.: Eastern Mediterranean Quaternary paleoclimates from pollen and isotope records of marine cores in the Nile cone area, Paleoceanography, 10, 291–300, 1995.
Cheng, H., Edwards, R. L., Broecker, W. S., Denton, G. H., Kong, X., Wang, Y., Zhang, R., and Wang, X.: Ice age terminations, Science, 326, 248–252, 2009.
Cheng, H., Sinha, A., Verheyden, S., Nader, F. H., Li, X. L., Zhang, P. Z., Yin, J. J., Yi, L., Peng, Y. B., Rao, Z. G., Ning Y. F., and Edwards R. L.: The climate variability in northern Levant over the past 20 000 years, Geophys. Res. Lett., 42, 8641–8650, 2015.
Cuffey, K. M. and Marshall, S. J.: Substantial contribution to sea-level rise during the last interglacial from the Greenland ice sheet, Nature, 404, 591–594, 2000.
Dansgaard, W.: Stable isotopes in precipitation, Tellus, 16, 436–468, https://doi.org/10.1111/j.2153-3490.1964.tb00181, 1964.
Develle, A. L., Gasse, F., Vidal, L., Williamson, D., Demory, F., Van Campo, E., Ghaleb, B., and Thouveny, N.: A 250 ka sedimentary record from a small karstic lake in the Northern Levant (Yammo\^uneh, Lebanon): Paleoclimatic implications, Palaeogeogr. Palaeoecol., 305, 10–27, 2011.
Dreybrodt, W.: Processes in karst systems, Springer-Verlag, New York, 288 pp., 1988.
Drysdale, R., Zanchetta, G., Hellstrom, J., Fallick, A., and Zhao, J.-X.: Stalagmite evidence for the onset of the Last Interglacial in southern Europe at 129 ± 1 ka, Geophys. Res. Lett., 32, L24708, 2005.
Drysdale, R., Hellstrom, J., Zanchetta, G., Fallick A. E., Sánchez Goñi, M. F., Couchoud I., McDonald J., Maas, R., Lohmann, G., and Isola I.: Evidence for obliquity forcing of glacial Termination II, Science, 325, 1527–1531, 2009.
Drysdale, R. N., Zanchetta, G., Hellstrom, J. C., Fallick, A. E., McDonald, J., and Cartwright, I.: Stalagmite evidence for the precise timing of North Atlantic cold events during the early last glacial, Geology, 35–1, 77–80, https://doi.org/https://doi.org/10.1130/G23161A.1, 2007.
Dutton, A. and Lambeck, K.: Ice volume and sea level during the last interglacial, Science, 337, 216–219, 2012.
Edwards, R. L., Chen, J. H., Ku, T. L., and Wasserburg, G. J.: Precise timing of the last interglacial period from mass-spectrometric determination of 230Th in corals, Science, 236, 1547–1553, 1987.
Emeis K. C., Schulz H., Struck U., Rossignol-Strick M., Erlenkeuser H., Howell M. W., Kroon D., Mackensen A., Ishizuka S., Oba T., Sakamoto T., and Koizumi I.: Eastern Mediterranean surface water temperatures and $\delta ^18$O during deposition of sapropels in the late Quaternary, Paleoceanography, 18, 1005–1029, 2003.
Emiliani, C.: Pleistocene temperatures, J. Geol., 63, 538–578, 1955.
Enzel, Y., Amit, R., Dayan, U., Crouvi, O., Kahana R., Ziv, B., and Sharon D.: The climatic and physiographic controls of the eastern Mediterranean over the late Pleistocene climates in the southern Levant and its neighboring deserts, Global Planet. Change, 60, 165–192, 2008.
Fairchild, I. J., Smith, C. L., Baker, A., Fuller, L., Spötl, C., Mattey, D., and McDermott, F.: Modification and preservation of environmental signals in speleothems, Earth Sci. Rev., 75, 105–153, 2006.
Frumkin, A., Ford, D. C., and Schwarcz, H.P .: Continental oxygen isotopic record of the last 170 000 years in Jerusalem, Quatern. Res., 51, 317–327, 1999.
Frumkin, A., Ford, D. C., and Schwarcz, H.: Paleoclimate and vegetation of the Last Glacial cycles in Jerusalem from a speleothem record, Global Biogeochem. Cy., 14, 863–870, 2000.
Gascoyne, M.: Palaeoclimate determination from cave calcite deposits, Quaternary Sci. Rev., 11, 609–632, 1992.
Gasse, F., Vidal, L., Develle, A.-L., and Van Campo, E.: Hydrological variability in the Northern Levant: a 250 ka multi-proxy record from the Yammo\^uneh (Lebanon) sedimentary sequence, Clim. Past, 7, 1261–1284, https://doi.org/10.5194/cp-7-1261-2011, 2011.
Gasse, F., Vidal L., Van Campo, E., Demory, F., Develle, A.-L., Tachikawa, K., Elias, A., Bard, E., Garcia, M., Sonzogni., C., and Thouveny, N.: Hydroclimatic changes in northern Levant over the past 400 000 years, Quaternary Sci. Rev., 111, 1–8, 2015.
Genty, D., Baker, A., and Vokal, B.: Intra- and inter-annual growth rate of modern stalagmites, Chem. Geol., 176, 191–212, 2001.
Genty, D., Blamart, D., Ouahdi, R., Gilmour, M., Baker, A., Jouzel, J., and Van-Exter, S.: Precise dating of Dansgaard-Oeschger climate oscillations in western Europe from stalagmite data, Nature, 421, 833–837, 2003.
Genty, D., Blamart, D., Ghaleb, B., Plagnes, V., Causse, C.h., Bakalowicz, M., Zouari, K., Chkir, N., Hellstrom, J., Wainer, K., and Bourges, F.: Timing and dynamics of the last deglaciation from European and North African d 13C stalagmite profiles–comparison with Chinese and South Hemisphere stalagmites, Quaternary Sci. Rev., 25, 2118–2142, 2006.
Grant, K. M., Rohling, E. J., Bar-Matthews, M., Ayalon, A., Medina-Elizalde, M., Bronk Ramsey, C., Satow, C., and Roberts, A. P.: Rapid coupling between ice volume and polar temperature over the past 150 kyr, Nature 491, 744–747, 2012.
Hellstrom, J.: U–Th dating of speleothems with high initial 230Th using stratigraphical constraint, Quat. Geochron., 1, 289–295, 2006.
Hellstrom, J., McCulloch, M., and Stone, J.: A detailed 31 000-year record of climate and vegetation change, from the isotope geochemistry of two New Zealand speleothems, Quaternary Res., 50, 167–178, 1998.
Heiss, J., Condon, D. J., McLean, N., and Noble, S. R.: 238U/235U systematics in terrestrial uranium-bearing minerals, Science, 335, 1610–1614, 2012.
Hendy, C. H.: The isotopic geochemistry of speleothems – I., The calculation of the effects of different modes of formation on the isotopic composition of speleothems and their applicability as palaeoclimatic indicators, Geochim. Cosmochim. Ac., 35, 801–824, 1971.
Kallel, N., Duplessy, J.-C., Labeyrie, L., Fontugne, M., Paterne, M., and Montacer, M.: Mediterranean pluvial periods and sapropel formation during the last 200 000 years, Palaeogeogr. Palaeoecol., 157, 45–58, 2000.
Kallel, N., Paterne, M., Duplessy, J.-C., Vergnaud-Grazzini, C., Pujol, C., Labeyrie, L., Arnold, M., Fontugne, M., and Pierre, C.: Enhanced rainfall in the Mediterranean region during the last sapropel event, Oceanol. Ac., 20, 697–712, 1997.
Kaufman, A., Wasserburg, G. J., Porcelli, D., Bar-Matthews, M., Ayalon, A., and Halicz, L.: U-Th isotope systematics from the Soreq Cave Israel and climatic correlations, Earth Planet. Sci. Lett., 156, 141–155, 1998.
Kim, S. T. and O'Neil, J. R.: Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates, Geochim. Cosmochim. Ac., 61–16, 3461–3475, 1997.
Kopp, R. E., Simons, F. J., Mitrovica, J. X., Maloof, A. C., and Oppenheimer, M.: Probabilistic assessment of sea level during the last interglacial stage, Nature, 462, 863–867, 2009.
Kolodny, Y., Stein, M., and Machlus, M.: Sea-rain-lake relation in the Last Glacial East Mediterranean revealed by d18O-d13C in Lake Lisan aragonites, Geochim. Cosmochim. Ac., 69, 4055–4060, 2005.
Lachniet, M. S.: Climatic and environmental controls on speleothem oxygenisotope values, Quaternary Sci. Rev., 28, 412–432, 2009.
Lisker, S., Vaks, A., and Bar-Matthews, M.: Late Pleistocene palaeoclimatic and palaeoenvironmental reconstruction of the Dead Sea area (Israel), based on speleothems and cave stromatolites, Quaternary Sci. Rev., 29, 1201–1211, 2010.
Litt, T., Pickarski, N., Heumann, G., Stockhecke, M., and Tzedakis, P. C.: A 600 000 year long continental pollen record from Lake Van, eastern Anatoloia (Turkey), Quaternary Sci. Rev., 104, 30–41, 2014.
Lourens, L. J., Antonarakou, A., Hilgren, F. J., Van Hoof, A. A. M., Vergnaud-Grazzini, C., and Zachariasse W. J.: Evaluation of the Plio-Pleistocene astronomical timescale, Paleoceanography, 11, 391–413, 1996.
McDermott, F.: Paleo-climate reconstruction from stable isotope variations in speleothems: a review, Quaternary Sci. Rev., 23, 901–918, 2004.
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 thedD values of speleothem fluid inclusions, Quaternary Sci. Rev., 23, 919–934, 2004.
Moller, T., Schultz, H., Hamann, Y., Dellwig, O., and Kucera, M.: Sedimentology and geochemistry of an exceptionally preserved last interglacial sapropel S5 in the Levantine Basin (Mediterranean Sea), Mar. Geol., 291–294, 34–48, 2012.
NEEM community members: Eemian interglacial reconstructed from a Greenland folded ice core, Nature 493, 489–494, 2013.
Nehme, C., Verheyden, S., Noble, S., Farrant, A., and Delannoy, J. J.: Contribution of an accurate growth rate reconstruction of a stalagmite from the Kanaan Cave-Lebanon to the understanding of humidity variations in the Levant during the MIS 5, Geol. Belg., 18, 2–4, 102–108, 2015.
Neugebauer, I., Schwab, M. J., Waldmann, N. D., Tjallingii, R., Frank, U., Hadzhiivanova, E., Naumann, R., Taha, N., Agnon, A., Enzel, Y., and Brauer, A.: Hydroclimatic variability in the Levant during the early last glacial ( 117–75 ka) derived from micro-facies analyses of deep Dead Sea sediments, Clim. Past Discuss., 11, 3625–3663, https://doi.org/10.5194/cpd-11-3625-2015, 2015.
North Greenland Ice Core Project members: High-resolution climate record of Northern Hemisphere climate extending into the Last Interglacial period, Nature, 431, 147–151, 2004.
Otto-Bliesner, B. L., Rosenbloom, N., Stone, E. J., McKay, N. P., Lunt, D. J., Brady, E. C., and Overpeck, J. T.: How warm was the Last Interglacial? New model-data comparisons, Philos. T. R. Soc. A, 371, 1–20, 2013.
Parton, A., White, T. S., Parker, A. G., Breeze, P. S., Jennings, R., Groucutt, H. S., and Petraglia, M. D.: Orbital-scale climate variability in Arabia as a potential motor for human dispersals, Quaternary Int., 382, 82–97, 2015.
Petit-Maire, N., Carbonel, P., Reyss, J.L., Sanlaville, P., Abed, A., Bourrouilh, R., Fontugne, M., and Yasin, S.: A vast Eemian palaeolake in Southern Jordan (29° N), Global Planet. Change, 2, 72, 368–373, 2010.
Republic of Lebanon: Policy Note on Irrigation Sector Sustainability, Report No. 28766–LE, the World Bank, Middle-East and North Africa Region, 2003.
Rohling, E. J., Cane, T. R., Cooke, S., Sprovieri, M., Bouloubassi, I., Emeis, K. C., Schiebel, R., Kroon, D., Jorissen, F. J., Lorre, A., and Kemp, A. E. S.: African monsoon variability during the previous interglacial maximum, Earth Planet Sci. Lett., 202, 61–75, 2002.
Rohling, E. J., Sprovieri, M., Cane, T. R., Casford, J. S. L., Cooke, S., Bouloubassi, I., Emeis, K. C., Schiebel, R., Hayes, A., Jorissen, F. J., and Kroon, D.: Reconstructing past planktic foraminiferal habitats using stable isotope data: a case history for Mediterranean sapropel S5, Mar. Micropaleontol., 50, 89–123, 2004.
Rohling, E. J., Sprovieri, M., Cane, T., Casford, J. S. L., Cooke, S., Bouloubassi I., Emeis K. C., Schiebel R., Rogerson M., Hayes A., Jorissen F. J., and Kroon D.: Reconstructing past planktic foraminiferal habitats using stable isotope data: a case history for Mediterranean sapropel S5, Mar. Micropaleontol., 50, 89–123, 2015a.
Rohling, E. J., Marino, G., and Grant, K. M.: Mediterranean climate and oceanography, and the periodic development of anoxic events (sapropels), Earth Sci. Rev., 143, 62–97, 2015b.
Rossignol-Strick, M. and Paterne, M.: The Holocene climatic optimum and pollen records of sapropel 1 in the Eastern Mediterranean, 9000–6000 BP, Quaternary Sci. Rev., 18, 515–530, 1999.
Rozanski, K., Araguas, L., and Gonfiantini, R.: Isotopic patterns in modern global precipitation, in: Climate Change in Continental Isotopic Record, Geophysical Monograph Series, Washington DC, AGU, 78, 1–37, 1993.
Saaroni, H., Ziv, B., Bitan, A., and Alpert, P.: Easterly wind storms over Israel, Theor. Appl. Climatol., 59, 61–77, 1998.
Schmiedl, G., Mitschele, A., Beck, S., Emeis, K. C., Hemleben, C., Schultz, H., Sperling, M., and Weldeab, S.: Benthic foraminiferal record of ecosystem variability in the eastern Mediterranean Sea during times of sapropel S5 and S6 deposition, Palaeogeogr. Palaeoecol., 190, 139–164, 2003.
Scrivner, A. E., Vance, D., and Rohling, E. J.: New neodymium isotope data quantify Nile involvement in Mediterranean anoxic episodes, Geology, 32, 565–568, 2004.
Shackleton, N. J., Chapman, M., Sanchez Goni, M. F., Pailler, D., and Lancelot, Y.: The classic marine isotope substage 5e, Quaternary Res., 58, 14–16, 2002.
Shtokhete, M., Sturm, M., Brunner, I., Schmincke, H.-U., Sumita, M., Kipfer, R., Cukur, D., Kwiecien, O., and Anselmetti, F.: Sedimentary evolution and environmental history of Lake Van (Turkey) over the past 600 000 years, Sedimentology, 61, 1830–1861, 2014.
Torfstein A., Goldstein, S. L., Kushnir, Y., Enzel, Y., Haug, G., and Stein, M.: Dead Sea drawdown and monsoonal impacts in the Levant during the last interglacial, Earth Planet. Sci. Lett., 412, 235–244, 2015.
Vaks, A., Bar-Matthews, M., Ayalon, A., Schilman, B., Gilmour, M., Hawkesworth C. J., Frumkin A., Kaufman A., and Matthews A.: Paleoclimate reconstruction based on the timing of speleothem growth, oxygen and carbon isotope composition from a cave located in the "rain shadow", Israel, Quaternary Res., 59, 182–193, 2003.
Vaks, A., Bar-Matthews, M., Ayalon, A., Matthews, A., Frumkin, A., Dayan, U., Halicz, L., Almogi-Labin, A., and Schilman, B.: Paleoclimate and location of the border between Mediterranean climate region and the Saharo-Arabian desert as revealed by speleothems from the northern Negev Desert, Israel, Earth Planet. Sci. Lett., 249, 384–399, 2006.
Vaks, A., Bar-Matthews, M., Matthews A., Ayalon, A,. and Frumkin, A.: Middle-Late Quaternary paleoclimate of northern margins of the Saharan-Arabian Desert: reconstruction from speleothems of Negev Desert, Israel, Quaternary Sci. Rev., 29, 2647–2662, 2013.
Van Geldern R. and Barth Johannes A. C.: Optimization of instrument setup and post-run corrections for oxygen and hydrogen stable isotope measurements of water by isotope ratio infrared spectroscopy (IRIS), Limnol. Oceanogr.-Methods, 10, 1024–1036, 2012.
Verheyden, S., Nader, F. H., Cheng, H. J., Edwards, L. R., and Swennen, R.: Paleoclimate reconstruction in the Levant region from the geochemistry of a Holocene stalagmite from the Jeita cave, Lebanon, Quaternary Res., 70, 368–381, 2008.
Verheyden S., Nehme C., Nader F. H., Farrant A. R., Cheng H., Noble S. R., Sahy D., Edwards R. L., Swennen R., Claeys P., and Delannoy, J. J.: X. The Lebanese speleothems and the Levant palaeoclimate, in: Quaternary Environments, edited by: Bar, J. Y. and Enzel, Y., Climate Change, and Humans in the Levant, Cambridge University Press, UK, accepted, 2015.
Waldmann, N., Stein, M., Ariztegui, D., and Starinsky, A.: Stratigraphy, depositional environments and level reconstruction of the last interglacial Lake Samra in the Dead Sea basin, Quaternary Res., 72, 1–15, 2009.
Wang, Y. J., Cheng, H., Edwards, R. L., An, Z. S., Wu, J. Y., Shen, C. C., and Dorale, J. A.: A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu cave, China, Science, 294, 2345–2348, 2001.
Zanchetta, G., Drysdale R. N., Hellstrom J. C., Fallick, A. E., Isola, I., Gaganf, M. K., and Pareschi, M. T.: Enhanced rainfall in the Western Mediterranean during deposition of sapropel S1: Stalagmite evidence from Corchia cave (Central Italy), Quaternary Sci. Rev., 26, 279–286, 2007.
Ziegler, M., Tuenter, E., Lourens, L. J.: The precession phase of the boreal summer monsoon as viewed from the eastern Mediterranean (ODP Site 968), Quaternary Sci. Rev. 29, 1481–1490, 2010.
Short summary
The Levant is a key area to study palaeoclimatic responses over G-IG cycles. A precisely dated MIS 5 stalagmite (129–84ka) from Kanaan Cave, Lebanon, with growth rate and isotopic records variations indicate a warm humid phase at the last interglacial (~129-125ka). A shift in δ18O values (125-122ka) is driven by the source effect of the eastern Med. during sapropel 5 (S5). Low growth rates and high δ18O-δ13C values (~122-84ka) mark the onset of glacial inception and transition to drier phase.
The Levant is a key area to study palaeoclimatic responses over G-IG cycles. A precisely dated...
