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8 - Chronologies of Late Quaternary Coral Reefs and Lake Sediments from the Red Sea and Dead Sea Rift Valley

from Part II: - Palaeoclimates

Published online by Cambridge University Press:  04 May 2017

By
Mordechai Stein ,
Boaz Lazar ,
Adi Torfstein  and
Steven L. Goldstein
Edited by
Yehouda Enzel  and
Ofer Bar-Yosef
Yehouda Enzel
Affiliation:
Hebrew University of Jerusalem
Ofer Bar-Yosef
Affiliation:
Harvard University, Massachusetts
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Summary

Lacustrine sediments from the hypersaline and freshwater lakes filling the tectonic depressions along the Dead Sea rift valley archive the environmental history (hydrology, climate, seismicity) of the southern Levant. Deciphering the structure and rates of processes underlying this history comparison and integration with regional and global environmental archives require precise and high–resolution chronologies. We describe the application of U-Th disequilibrium method to the dating of late Pleistocene coral reefs and lake sediments. This method was combined with oxygen isotope stratigraphy to establish the Amora, Samra and Lisan Formations chronologies in the Dead Sea basin. During glacials lake levels rose while during interglacial they receded. These general pattern were interrupted by abrupt aridity at times of the glacial Heinrich events (HE) in the northern Atlantic (e.g. HE4 ~39 ka) and intrusions of wetness from southern sources at times of enhanced monsoon activity in the Nile River sources and sapropels at the Mediterranean Sea during the interglacial peaks (e.g. sapropel S5 at ~129-121 ka).

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Quaternary of the Levant
Environments, Climate Change, and Humans
 , pp. 75 - 82
Publisher: Cambridge University Press
Print publication year: 2017

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References

Almogi-Labin, A., Bar Matthews, M., Shriki, D. et al. 2009. Climatic variability during the last ∼90 ka of the southern and northern Levantine Basin as evident from marine records and speleothems. Quaternary Science Reviews 28: 2882–96.CrossRefGoogle Scholar
Bar-Matthews, M., Ayalon, A., Kaufman, A. & Wasserburg, G.J. 1999. The Eastern Mediterranean paleoclimate as a reflection of regional events: Soreq cave, Israel. Earth Planetary Science Letters 166: 85–95.CrossRefGoogle Scholar
Bar-Matthews, M., Ayalon, A., Gilmour, M., Matthews, A. & Hawksworth, C.J. 2003. Sea–land oxygen isotopic relationships from planktonic foraminifera and speleothems in the eastern Mediterranean region and their implication for paleorainfall during interglacial intervals. Geochimica et Cosmochimica Acta 67: 3181–99.CrossRefGoogle Scholar
Bartov, Y., Goldstein, S.L., Stein, M. & Enzel, Y. 2003. Catastrophic arid perturbations of the East-Mediterranean climate linked to the North Atlantic Heinrich Events. Geology 31: 439–42.2.0.CO;2>CrossRefGoogle Scholar
Belmaker, R., Stein, M., Yechieli, Y. & Lazar, B. 2007. Controls on the radiocarbon reservoir ages in the modern Dead Sea drainage system and in the last Glacial Lake Lisan. Radiocarbon 49: 969–82.CrossRefGoogle Scholar
Belmaker, R., Stein, M., Beer, J. et al. 2014. Beryllium isotopes as tracers of Dead Sea hydrology and the Laschamp geomagnetic excursion. Earth and Planetary Science Letters 400: 233–42.CrossRefGoogle Scholar
Bookman, R., Enzel, Y., Agnon, A. & Stein, M. 2004. Late Holocene levels of the Dead Sea. Geological Society of America Bulletin 116: 555–71.Google Scholar
Bookman, R., Bartov, Y., Stein, M. & Enzel, Y. 2006. Lake level reconstruction in the late Quaternary Dead Sea basin. In New Frontiers in Dead Sea Paleoenvironmental Research, ed. Enzel, Y, Agnon, A & Stein, M, GSA Special Paper 401. Geological Society of America, pp. 155–70.Google Scholar
Edwards, R.L., Chen, J.H. & Wasserburg, G.J. 1987. 238U–234U–230Th–232Th systematics and the precise measurement of time over the past 500,000 years. Earth and Planetary Science Letters 81: 175–92.Google Scholar
Enmar, L. 1999. The travertines in the northern and central Arava: Stratigraphy, petrology and geochemistry. Geological Survey of Israel Report GSI/1/99.Google Scholar
Frumkin, A., Ford, D.C. & Schwarcz, H.P. 1999. Continental oxygen isotopic record of the last 170,000 years in Jerusalem. Quaternary Research 51: 317–27.CrossRefGoogle Scholar
Haase-Schramm, A., Goldstein, S.L. & Stein, M. 2004. U–Th dating of Lake Lisan (late Pleistocene Dead Sea) aragonite and implications for glacial east Mediterranean climate change. Geochimica et Cosmochimica Acta 68: 985–1005.CrossRefGoogle Scholar
Kagan, E., Stein, M., Agnon, A. & Bronks-Ramsey, C. 2010. Paleo-earthquakes as anchor points in Bayesian radiocarbon deposition models: A case study from the Dead Sea. Radiocarbon 52: 1018–26.CrossRefGoogle Scholar
Kagan, E., Stein, M., Agnon, A. & Nuemann, F. 2011. Intrabasin paleoearthquakes and quiescence correlation of the late Holocene Dead Sea. Journal of Geophysical Research 116: B04311.Google Scholar
Kaufman, A. 1971. U-Series dating of Dead Sea Basin carbonates. Geochimica et Cosmochimica Acta 35: 1269–81.CrossRefGoogle Scholar
Kaufman, A. 1993. An evaluation of several methods for determining ages in impure carbonates. Geochimica et Cosmochimica Acta 57: 2303–17.CrossRefGoogle Scholar
Kaufman, A. & Broecker, W.S. 1965. Comparison of 230Th and 14C ages for carbonate material from lakes Lahanton and Bonneville. Journal of Geophysical Research 70: 4039–54.CrossRefGoogle Scholar
Kaufman, A., Broecker, W.S., Ku, T.L. & Thurber, D.L. 1971. The status of U-series methods of mollusk dating. Geochimica et Cosmochimica Acta 35: 1155–83.CrossRefGoogle Scholar
Kaufman, A., Yechieli, Y. & Gardosh, M. 1992. Reevaluation of the lake-sediment chronology in the Dead Sea basin, Israel, based on new 230Th/U dates. Quaternary Research 38: 292–304.CrossRefGoogle Scholar
Ken-Tor, R., Stein, M., Enzel, Y. et al. 2001 Precision of calibrated radiocarbon ages of earthquakes in the Dead Sea basin. Radiocarbon 43: 1371–82.CrossRefGoogle Scholar
Kiro, Y., Goldstein, S.L., Lazar, B., Stein, M. 2016. Environmental implications of salt facies in the Dead Sea. Geological Society of America Bulletin. 128: 824–841.10.1130/B31357.1CrossRefGoogle Scholar
Kitagawa, H., Stein, M., Goldstein, S.L., Nakamura, T. & Lazar, B., DSDDP Scientific Party. 2016. Radiocarbon chronology of the DSDDP CORE at the deepest floor of the Dead Sea. Radiocarbon (2016): 1–12. DOI:10.1017/RDC.2016.120.Google Scholar
Kolodny, Y., Stein, M. & Machlus, M. 2005. Sea-rain–lake relation in the last Glacial East Mediterranean revealed by δ18O–δ13C in Lake Lisan aragonites. Geochimica et Cosmochimica Acta 69: 4045–60.10.1016/j.gca.2004.11.022CrossRefGoogle Scholar
Ku, T.-L. & Liang, Z.C. 1984. The dating of impure carbonates with decay-series isotopes. Nuclear Instruments and Methods in Physics Research 223: 563–71.CrossRefGoogle Scholar
Lazar, B. & Stein, M. 2011. Freshwater on the route of hominids out of Africa revealed by U–Th in Red Sea corals. Geology 39: 1067–70.CrossRefGoogle Scholar
Lazar, B., Enmar, R., Schossberger, M. et al. 2004. Diagenesis in live corals from the Gulf of Aqaba: The effect on the U –Th system. Geochimica et Cosmochimica Acta 68: 4583–93.CrossRefGoogle Scholar
Lazar, B., Sivan, O., Yechieli, Y. et al. 2014. Long-term freshening of the Dead Sea brine revealed by porewater Cl- and δ18O in ICDP Dead Sea deep-drill. Earth and Planetary Science Letters 400: 94–101.CrossRefGoogle Scholar
Lev, L., Almogi-Labin, A., Mischke, S. et al. 2014. Paleohydrology of Lake Kinneret during the Heinrich event H2. Palaeogeography, Palaeo-climatology, Palaeoecology, 396: 183–93.10.1016/j.palaeo.2014.01.005CrossRefGoogle Scholar
Lin, J.C., Broecker, W.S., Anderson, R.F. et al. 1996. New 230Th/U and 14C ages from Lake Lahontan carbonates, Nevada, USA, and a discussion of the origin of initial thorium. Geochimica et Cosmochimica Acta 60: 2817–32.CrossRefGoogle Scholar
Livnat, A. & Kronfeld, J. 1985, Paleoclimatic implications of U-series dates for lake sediments and travertines in the Arava Rift Valley, Israel. Quaternary Research 24: 164–72.CrossRefGoogle Scholar
Luo, S. & Ku, T.-L. 1991. U-series isochron dating: A generalized method employing total-sample dissolution. Geochimica et Cosmochimica Acta 55: 555–64.CrossRefGoogle Scholar
Machlus, M., Enzel, Y., Goldstein, S.L., Marco, S. & Stein, M. 2000. Reconstruction of low-levels of Lake Lisan between 55 and 35 kyr. Quaternary International 73/74: 137–44.Google Scholar
Marco, S., Stein, M., Agnon, A. & Ron, H. 1996. Long-term earthquake clustering: 50,000- year paleoseismic record in the Dead Sea graben. Journal of Geophysical Research 101 B3: 6179–91.10.1029/95JB01587CrossRefGoogle Scholar
Migowski, C., Agnon, A., Bookman, R., Negendank, J. & Stein, M. 2004. Recurrence pattern of Holocene earthquakes along the Dead Sea rift revealed by varve counting and radiocarbon dating of lacustrine sedi-ments. Earth Planetary Science Letters 222: 301–14.CrossRefGoogle Scholar
Migowski, C., Stein, M., Prasad, S., Negendank, J.F.W. & Agnon, A. 2006. Dead Sea levels, climate variability and human culture evolution in the Holocene Near East. Quaternary Research 66: 421–31.CrossRefGoogle Scholar
Neev, D. & Emery, K.O. 1995. The Destruction of Sodom, Gomorrah, and Jericho. Geological, Climatological, and Archaeological Background. New York: Oxford University Press.Google Scholar
Neugebauer, I., Brauer, A., Waldmann, N. et al. & DSDDP Scientific Party. 2014. Lithologies and depositional environments of the last two climatic cycles in the deep hypersaline Dead Sea: New observations from the ICDP Dead Sea Deep Drilling Project (DSDDP). Quaternary Science Reviews 102: 149–65.Google Scholar
Prasad, S., Vos, H., Negendank, J.F.W. et al. 2004. Evidence from Lake Lisan of solar influence on decadal to centennial climate variability during the late glacial. Geology 32: 581–4.10.1130/G20553.1CrossRefGoogle Scholar
Schramm, A., Stein, M. & Goldstein, S.L. 2000. Calibration of the 14C time scale to >40 ka by 234U–230Th dating of Lake Lisan sediments (last glacial Dead Sea). Earth and Planetary Science Letters 175: 27–40.CrossRefGoogle Scholar
Scholz, D., Mangini, A. & Felis, T. 2004. U-series dating of diagenetically altered fossil reef corals. Earth and Planetary Science Letters 218: 163–78.CrossRefGoogle Scholar
Schwarcz, H.P. 1982. Applications of U-series to archaeometry. In Uranium Series disequilibrium: Applications to Environmental Problems, ed. Ivanovich, M. & Harmon, R.S.. Oxford: Clarendon Press.Google Scholar
Shaked, Y., Lazar, B., Marco, S., Stein, M. & Agnon, A. 2009. Late Holocene events that shaped the shoreline at the northern Gulf of Aqaba recorded by a buried fossil reef. Israel Journal of Earth Sciences 58: 355–68.10.1560/IJES.58.3-4.355CrossRefGoogle Scholar
Stein, M. 2014. The evolution of Neogene–Quaternary water-bodies in the Dead Sea Rift Valley. In Dead Sea Transform Fault System: Reviews, ed. Garfunkel, Z., Ben-Avraham, Z. & Kagan, E.. Dordrecht: Elsevier Science, pp. 279–316.CrossRefGoogle Scholar
Stein, M., Wasserburg, G.J., Aharon, P. et al. 1993. TIMS U-series dating and stable isotopes of the last interglacial event in Papua New Guinea. Geochimica et Cosmochimica Acta 57: 2541–54.10.1016/0016-7037(93)90416-TCrossRefGoogle Scholar
Stein, M., Starinsky, A., Katz, A. et al. 1997. Strontium isotopic, chemical, and sedimentological evidence for the evolution of Lake Lisan and the Dead Sea. Geochimica et Cosmochimica Acta 61: 3975–92.10.1016/S0016-7037(97)00191-9CrossRefGoogle Scholar
Stein, M., Migowski, C., Bookman, R. & Lazar, B. 2004. Temporal changes in the radiocarbon reservoir age in the Dead Sea. Radiocarbon 46: 649–55.CrossRefGoogle Scholar
Stein, M., Lazar, B. & Goldstein, S.L. 2013. Radiocarbon reservoir ages as freshwater-brine monitors in Lake Lisan–Dead Sea system. In Proceedings of the 21st International Radiocarbon Conference, ed. Jull, A.J.T. & Hatté, C.. Radiocarbon 55: 1050–7.Google Scholar
Torfstein, A., Haase-Schramm, A., Waldmann, N., Kolodny, Y. & Stein, M. 2009. U-series and oxygen isotope chronology of the mid-Pleistocene Lake Amora (Dead Sea basin). Geochimica et Cosmochimica Acta 73: 2603–30.CrossRefGoogle Scholar
Torfstein, A., Goldstein, S.L., Kagan, E. & Stein, M. 2013a. Multi-site integrated U–Th chronology of the last glacial Lake Lisan. Geochimica et Cosmochimica Acta 104: 210–34.10.1016/j.gca.2012.11.003CrossRefGoogle Scholar
Torfstein, A., Goldstein, S.L., Enzel, Y. & Stein, M. 2013b. Impacts of abrupt climate changes in the Levant from last glacial Dead Sea levels. Quaternary Science Reviews 69: 1–7.10.1016/j.quascirev.2013.02.015CrossRefGoogle Scholar
Torfstein, A., Goldstein, S.L., Kushnir, Y. et al. 2015. Dead Sea drawdown and monsoonal impacts in the Levant during the last interglacial. Earth and Planetary Science Letters 412: 235–44.CrossRefGoogle Scholar
van der Borg, K., Stein, M., de Jong, A.F.M., Waldmann, N. & Goldstein, S.L. 2004. Close to zero Δ14C-values at 32 kyr cal BP observed in the high-resolution 14C record from U–Th dated sediment of Lake Lisan. Radiocarbon 46: 785–96.CrossRefGoogle Scholar
Waldmann, N., Starinsky, A. & Stein, M. 2007. Ca-chloride brines as paleo-hydrological monitors of the Dead Sea basin. Quaternary Science Reviews 26: 2219–28.10.1016/j.quascirev.2007.04.019CrossRefGoogle Scholar
Waldmann, N., Stein, M., Artiztegui, D. & Starinsky, A. 2009. Stratigraphy, depositional environments and level reconstruction of the last interglacial Lake Samra in the Dead Sea basin. Quaternary Research 72: 1–15.10.1016/j.yqres.2009.03.005CrossRefGoogle Scholar
Weil, N. 2010. Holocene Coral Reefs Evolution in the Gulf of Elat: Terraces, Sea-Levels and Growth Patterns. Unpublished M.Sc. thesis, Hebrew University of Jerusalem.Google Scholar
Winograd, I.J., Szabo, B.J., Coplen, T.B. & Riggs, A.C. 1988. A 250,000 year climatic record from Great Basin vein calcite: Implications for Milankovitch theory. Science 242: 1275–80.10.1126/science.242.4883.1275CrossRefGoogle ScholarPubMed
Winograd, I.J., Coplen, T.B., Landwehr, J.M. et al. 1992. Continuous 500,000 year climate record from vein calcite in Devils Hole, Nevada. Science 258: 255–60.CrossRefGoogle Scholar
Yehudai, M., Lazar Bar, N., Agnon, A., Shaked, Y. & Stein, M. 2017. U–Th dating of calcitic corals from the Gulf of Aqaba. Geochimica et Cosmochimica Acta 198: 285–98.CrossRefGoogle Scholar
Zak, I. 1967. The Geology of Mount Sedom. Unpublished Ph.D. thesis, Hebrew University of Jerusalem.Google Scholar

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