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Stable isotopes of a subfossil Tamarix tree from the Dead Sea region, Israel, and their implications for the Intermediate Bronze Age environmental crisis

Published online by Cambridge University Press:  20 January 2017

Amos Frumkin
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Abstract

Trees growing on the Mt. Sedom salt diapir, at the southern Dead Sea shore, were swept by runoff into salt caves and subsequently deposited therein, sheltered from surface weathering. A subfossil Tamarix tree trunk, found in a remote section of Sedom Cave is radiocarbon dated to between ∼ 2265 and 1930 BCE. It was sampled in 109 points across the tree rings for carbon and nitrogen isotopes. The Sedom Tamarix demonstrates a few hundred years of 13C and 15N isotopic enrichment, culminating in extremely high δ13C and δ15N values. Calibration using modern Tamarix stable isotopes in various climatic settings in Israel shows direct relationship between isotopic enrichment and climate deterioration, particularly rainfall decrease. The subfossil Tamarix probably reflects an environmental crisis during the Intermediate Bronze Age, which subsequently killed the tree ∼ 1930 BCE. This period coincides with the largest historic fall of the Dead Sea level, as well as the demise of the large regional urban center of the 3rd millennium BCE. The environmental crisis may thus explain the archaeological evidence of a shift from urban to pastoral culture during the Intermediate Bronze Age. This was apparently the most severe long-term historical drought that affected the region in the mid-late Holocene.

Keywords

Levant paleoclimateClimate deteriorationTree ring isotopesCarbon isotopesNitrogen isotopesDead Sea levelCave depositRadiocarbonSalt karstSedom
Type
Articles
Information
Quaternary Research , Volume 71 , Issue 3 , May 2009 , pp. 319 - 328
Copyright
University of Washington

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References

Albright, W.F. The Biblical Period from Abraham to Ezra. (1963). Harper & Row, New York. 118 Google Scholar
Amiran, R. The fall of the Early Bronze age II city of Arad. Israel Exploration Journal 36, (1986). 74–76.Google Scholar
Amiran, D.H.K. The climate of the ancient Near East. The early third millennium in the northern Negev of Israel. Erdkunde 45, 3 (1991). 153–162.CrossRefGoogle Scholar
Bell, A. The Dark Ages in Ancient History. I. The first Dark Age in Egypt. American Journal of Archaeology 75, (1971). 1–26.CrossRefGoogle Scholar
Ben-Avraham, Z. and Lazar, M., (2006). The structure and development the Dead Sea Basin: Recent studies. In: Enzel, Y., Agnon, A. and Stein, M. (Editors), New frontiers in Dead Sea paleoenvironmental research, . GSA Special Paper 401, Boulder, pp. 1–13.Google Scholar
Bookman (Ken-Tor), R., Enzel, Y., Agnon, A., and Stein, M. Late Holocene lake levels of the Dead Sea. GSA Bulletin 116, 5/6 (2004). 555–571.CrossRefGoogle Scholar
Bookman, R., Bartov, Y., Enzel, Y. and Stein, M., (2006). Quaternary lake levels in the Dead Sea Basin: Two centuries of research. In: Enzel, Y., Agnon, A. and Stein, M. (Editors), New frontiers in Dead Sea paleoenvironmental research, . GSA Special Paper 401, Boulder, pp. 155–170.Google Scholar
Bronk-Ramsey, C. Development of the radiocarbon program OxCal. Radiocarbon 43, 2A (2001). 355–363.CrossRefGoogle Scholar
Chen, T. et al. Study on the climatic significance of fir tree ring δ13C from Zhaosu County, Xinjiang, China. Journal of Glaciology and Geocryology 22, 4 (2000). 347–351.Google Scholar
Crown, A.D. Toward a reconstruction of the climate of Palestine 8000 BC — 0 BC. Journal of Near Eastern Studies 31, (1972). 312–330.CrossRefGoogle Scholar
Cullen, H.M., deMenocal, P.B., Hemming, S., Hemming, G., Brown, F.H., Guilderson, T., and Sirocko, F. Climate change and the collapse of the Akkadian empire: evidence from the deep sea. Geology 28, 4 (2000). 379–382.2.0.CO;2>CrossRefGoogle Scholar
deMenocal, P.B. Cultural responses to climate change during the late Holocene. Science 292, 5517 (2001). 667 CrossRefGoogle ScholarPubMed
Dever, W.G. The collapse of the urban Early Bronze age in Palestine: toward a systematic analysis. de Miroschedji, P. L'urbanisation de la Palestine à l'âge du Bronze Ancien. (1989). BAR International Series, Oxford. 225–246.Google Scholar
Enzel, Y., Kadan, G., and Eyal, Y. Holocene earthquakes inferred from a fan-delta sequence in the Dead Sea graben. Quaternary Research 53, (2000). 34–48.CrossRefGoogle Scholar
Enzel, Y., Bookman (Ken-Tor), R., Sharon, D., Gvirtzman, H., Dayan, U., Ziv, B., and Stein, M. Late Holocene climates of the Near East deduced from Dead Sea level variations and modern regional winter rainfall. Quaternary Research 60, (2003). 263–273.CrossRefGoogle Scholar
Epstein, S., and Krishnamurthy, R.V. Environmental information in trees. Philosophical Transactions of the Royal Society of London A 330, (1990). 427–439.Google Scholar
Evenari, M., Shanan, L., and Tadmor, N.H. The Negev — The Challenge of a Desert. (1971). Harvard University Press, Cambridge, Mass.Google Scholar
Ferrio, J.P., and Voltas, J. Carbon and oxygen isotope ratios in wood constituents of Pinus halepensis as indicators of precipitation, temperature and vapour pressure deficit. Tellus Series B – Chemical and Physical Meteorology 57B, (2005). 164–173.CrossRefGoogle Scholar
Finkelstein, I. Further observations on the socio-demographic structure of the Intermediate Bronze Age. Levant 21, (1989). 129–140.CrossRefGoogle Scholar
Francey, R.J., Allison, C.E., Etheridge, D.M., Trudinger, C.M., Enting, I.G., Leuenberger, M., Langenfelds, R.L., Michel, E., Steele, L.P., (1999). A 1000-year high precision record of δ13C in atmospheric CO2 . Tellus 51B, 170–193.Google Scholar
Frumkin, A. Hydrology and denudation rates of halite karst. Journal of Hydrology 162, (1994). 171–189.CrossRefGoogle Scholar
Frumkin, A. Salt cave cross sections and their paleoenvironmental implications. Geomorphology 23, (1998). 183–191.CrossRefGoogle Scholar
Frumkin, A., Carmi, I., Zak, I. and Magaritz, M., (1991). The Holocene climatic record of the salt caves of Mount Sedom. Israel: The Holocene, 1,3, 191–200.Google Scholar
Frumkin, A., Kadan, G., Enzel, Y., and Eyal, Y. Radiocarbon chronology of the Holocene Dead Sea: attempting a regional correlation. Radiocarbon 43, 2C, (2001). 1179–1190.CrossRefGoogle Scholar
Gagen, M., McCarroll, D., and Edouard, J.L., (2004). Latewood width, maximum density, and stable carbon isotope ratios of pine as climate indicators in a dry subalpine environment, French Alps. Arctic, Antarctic and Alpine Research, 36, 2, 166–171.Google Scholar
Garten, C.T., and Taylor, G.E. Foliar δ13C within a temperate deciduous forest: spatial, temporal and species sources of variation. Oecologia 90, (1992). 1–7.CrossRefGoogle ScholarPubMed
Gerson, R., (1972). Geomorphic processes of Mount Sdom. PhD thesis (in Hebrew, English abstract), The Hebrew University, Jerusalem.Google Scholar
Glueck, N. Rivers in the Desert. (1959). New York, Google Scholar
Greenbaum, N., Ben-Zvi, A., Haviv, I. and Enzel, Y., (2006). The hydrology and paleohydrology of the Dead Sea tributaries. In: Enzel, Y., Agnon, A. and Stein, M. (Editors), New frontiers in Dead Sea paleoenvironmental research, . GSA Special Paper 401, Boulder, pp. 63–93.Google Scholar
Grintz, Y.M. The Book of Genesis, its Uniqueness and Antiquity (Hebrew). (1983). Magnes, Jerusalem.Google Scholar
Heaton, T.H.E. 15N/14N ratios of plants in South Africa and Namibia: relationship to climate and coastal/saline environment. Oecologia 74, (1987). 236–246.CrossRefGoogle Scholar
Indermühle, T.E., Stocker, T.F., Joos, F., Fischer, H., Smith, H.J., Wahlen, M., Deck, B., Mastroiann, D., Tchhumi, J., Blunier, T., Meyer, R., and Stauffer, B. Holocene carbon-cycle dynamics based on CO2 trapped in ice at Taylor Dome, Antarctica. Nature 398, (1999). 121–126.CrossRefGoogle Scholar
Issar, A.S., and Zohar, M. Climate Change – Environment and Civilization in the Middle East. (2004). Springer – Heidelberg, Berlin – New York.CrossRefGoogle Scholar
Kadan, G., (1997). Evidence of Dead-Sea level fluctuations and neotectonic events in the Holocene fan-delta of Nahal Darga. M.Sc. Thesis (in Hebrew, English abstract), Ben Gurion University of the Negev, Be'er Sheba., 54 pp.Google Scholar
Kahana, R., Ziv, B., Enzel, Y., and Dayan, U. Synoptic climatology of major floods in the Negev Desert, Israel. International Journal of Climatology 22, (2002). 867–882.CrossRefGoogle Scholar
Kenyon, K.M., Bottero, J. and Posener, G., (1974). Syria and Palestine c. 2160–1780 B.C.. Cambridge Ancient History, 3rd revised ed., vol. I, (2). Cambridge University, Cambridge., pp. 532–594.Google Scholar
Leavitt, S.W., (2007). Regional expression of the 1988 U.S. Midwest drought in seasonal delta C-13 of tree rings Journal-of-Geophysical-Research. D:-Atmospheres, 112, (D6), Art. No. D06107 Google Scholar
Leavitt, S.W., Wright, W.E., and Long, A. Spatial expression of ENSO, drought, and summer monsoon in seasonal δ13C of ponderosa pine tree rings in southern Arizona and New Mexico. Journal-of-Geophysical-Research, D:-Atmospheres 107, 18 (2002). 3-1-3-10 CrossRefGoogle Scholar
Lipp, J., Trimborn, P., Edwards, T., Waisel, Y., and Yakir, D. Climatic effects on the δ18O and δ13C of cellulose in the desert tree Tamarix jordanis . Geochim. Cosmochim. Acta 60, 17 (1996). 3305–3309.CrossRefGoogle Scholar
Liu, Y., Ma, L., Leavitt, S.-W., Cai, Q., and Liu, W. A preliminary seasonal precipitation reconstruction from tree-ring stable carbon isotopes at Mt. Helan, China, since AD 1804. Global and Planetary Change 41, 3–4 (2004). 229–239.CrossRefGoogle Scholar
Mayr, C., Frenzel, B., Friedrich, M., Spurk, M., Stichler, W., and Trimborn, P. Stable carbon- and hydrogen-isotope ratios of subfossil oaks in southern Germany: methodology and application to a composite record for the Holocene. The Holocene 13, 3 (2003). 393–402.CrossRefGoogle Scholar
McCarroll, D., and Loader, N.J. Stable isotopes in tree rings. Quaternary Science Reviews 23, (2004). 771–801.CrossRefGoogle Scholar
Meitlis, Y., (2006). Digging the Bible (in Hebrew). Rubin Mass, Jerusalem., 287 pp.Google Scholar
Migowski, C., Stein, M., Prasad, S., Negendank, J.F.W., and Agnon, A. Holocene climate variability and cultural evolution in the Near East from the Dead Sea sedimentary record. Quaternary Research 66, (2006). 421–431.CrossRefGoogle Scholar
Neev, D., and Emery, K.O. The Dead Sea, depositional processes and environments of evaporites. Geological Survey of Israel Bulletin 41, (1967). 1–147.Google Scholar
Nissenbaum, A. Sodom, Gomorrah and the other lost cities of the plain — a climatic perspective. Climatic Change 26, 4 (1994). 435–446.CrossRefGoogle Scholar
Pe'eri, S., Zebker, H.A., Ben-Avraham, Z., Frumkin, A., and Hall, J.K. Spatially-resolved uplift rate of the Mount Sedom (Dead Sea) salt diapir from InSAR observations. Israel Journal of Earth Sciences 2, 2 (2004). 99–106.CrossRefGoogle Scholar
Prag, K. The Intermediate Early Bronze-Middle Bronze Age: an interpretation of the evidence from Transjordan, Syria and Lebanon. Levant 6, (1974). 69–116.CrossRefGoogle Scholar
Rast, W.E. Bab edh-Dhr'a and the origin of the Sodom saga. Perdue, L.G., Toombs, L.E., and Johnson, G.L. Archaeology and Biblical Interpretation. (1987). John Knox Press, Atlanta. 185–201.Google Scholar
Reimer, P.J., Baillie, M.G.L., Bard, E., Bayliss, A., Beck, J.W., Bertrand, C., Blackwell, P.G., Buck, C.E., Burr, G., Cutler, K.B., Damon, P.E., Edwards, R.L., Fairbanks, R.G., Friedrich, M., Guilderson, T.P., Hughen, K.A., Kromer, B., McCormac, F.G., Manning, S., Bronk Ramsey, C., Reimer, R.W., Remmele, S., Southon, J.R., Stuiver, M., Talamo, S., Taylor, F.W., J., v.d.P., and Weyhenmeyer, C.E. IntCal04: calibration issue. Radiocarbon 46, 3 (2004). 1029–1058.Google Scholar
Richard, S. Toward a consensus of opinion on the end of the Early Bronze age in Palestine-Transjordan. Bulletin of the American Schools of Oriental Research 237, (1980). 5–34.CrossRefGoogle Scholar
Rosen, A.M. Environmental change at the end of Early Bronze age Palestine. de Miroschedji, P. L'urbanisation de la Palestine à l'âge du Bronze Ancien. (1989). BAR International Series, Oxford. 247–255.Google Scholar
Speiser, E.A. The Anchor Bible — Genesis. (1964). Doubleday, New York. 377 Google Scholar
Stager, L.E. The periodization of Palestine from Neolithic through Early Bronze times. Ehrlich, R.W. Chronologies in Old World Archaeology (third edition). (1992). Chicago: The University of Chicago Press, Chicago. 22–41.Google Scholar
Stewart, G.R., Turnbull, M.H., and Schmidt, S. 13C Natural abundance in plant communities along a rainfall gradient: a biological intergrator of water availability. Australian Journal of Plant Physiology 22, (1995). 51–55.Google Scholar
Swap, R.J., Aranibar, J.N., Dowty, P.R., Gilhooly, W.P. III, and Macko, S.A. Natural abundance of 13C and 15N in C3 and C4 vegetation of southern Africa: patterns and implications. Global Change Biology 10, (2004). 350–358.CrossRefGoogle Scholar
Treydte, K., Schleser, G.H., Schweingruber, F.H., and Winiger, M. The climatic significance of δ13C in subalpine spruces (Lotschental, Swiss Alps). Tellus-Series-B:-Chemical-and-Physical-Meteorology 53, 5 (2001). 593–611.Google Scholar
Warren, C.R., McGrath, J.F., and Adams, M.A. Water availability and carbon isotope discrimination in conifers. Oecologia 127, (2001). 476–486.CrossRefGoogle ScholarPubMed
Weinberger, R., Begin, Z.B., Waldmann, N., Gardosh, M., Baer, G., Frumkin, A. and Wdowinski, S., (2006). Quaternary rise of the Sedom Diapir, Dead Sea basin. In: Enzel, Y., Agnon, A. and Stein, M. (Editors), New frontiers in Dead Sea paleoenvironmental research, GSA Special Paper 401. GSA, Boulder., pp. 33–51.Google Scholar
Weinstein, J.M. Radiocarbon dating in the Southern Levant. Radiocarbon 26, 3 (1984). 297–366.CrossRefGoogle Scholar
Weiss, H., and Bradley, R.S. What drives social collapse?. Science 291, (2001). 609–610.CrossRefGoogle ScholarPubMed
Yair, A., and Garti, A. The water supply at ancient Arad. Amiran, R., and Ilan, O. Early Arad. (1996). The Israel Museum and the Israel Exploration Society, Jerusalem. 127–138.Google Scholar
Yakir, D., Gat, J., Issar, A., Adar, E., Trimbom, P., and Lipp, J. 13C and 18O of wood from the Roman siege rampart in Masada (AD 70–73): evidence for a less arid climate for the region. Geochim. Cosmochim. Acta 58, 16 (1994). 3535–3539.CrossRefGoogle Scholar
Zak, I., (1967). The geology of Mount Sedom. PhD thesis (in Hebrew, English abstract), The Hebrew University, Jerusalem., 208 pp.Google Scholar