Skip to main content Accessibility help
×
Hostname: page-component-76fb5796d-2lccl Total loading time: 0 Render date: 2024-04-27T14:06:24.455Z Has data issue: false hasContentIssue false

19 - Late Quaternary Palaeoenvironments in Northern Levant (Lebanon and Syria)

from Part II: - Palaeoclimates

Published online by Cambridge University Press:  04 May 2017

Yehouda Enzel
Affiliation:
Hebrew University of Jerusalem
Ofer Bar-Yosef
Affiliation:
Harvard University, Massachusetts
Get access

Summary

The northern Levant (Lebanon and Syria) is transitional between the Mediterranean and subtropical deserts and underwent large past climatic shifts with impacts on water resources, vegetation and human populations. This chapter reviews terrestrial sedimentary, geochemical and palaeobotanical evidence of palaeoenvironmental changes in the area over the last four glacial-interglacial cycles, emphasizing the last glacial, the deglacial transition and the early Holocene. The lake Yammoûneh hydroclimatic record reveals interglacials high water availability and generally drier Glacials, in agreement with southeastern Europe. The northern and southern Levant climates evolved in opposite directions at the Glacial-Interglacial time-scale, suggesting heterogeneity of eastern Mediterranean responses to global climates. Harsh Last Glacial Maximum conditions at Yammoûneh may reflect water storage in Mt. Lebanon glaciers. Late Glacial and early Holocene records from the Yammoûneh basin, the Bekaa valley and the Jeita Cave in Lebanon, and from the Ghab in Syria reveal post-glacial warming associated with a rapid re-establishment of humid conditions, and early Holocene moist conditions.
Type
Chapter
Information
Quaternary of the Levant
Environments, Climate Change, and Humans
, pp. 173 - 178
Publisher: Cambridge University Press
Print publication year: 2017

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Abi-Saleh, B. & Safi, S. 1988. Carte de la végétation du Liban. Ecologia Mediterranea 14: 123–41.CrossRefGoogle Scholar
Almogi-Labin, A., Bar-Matthews, M., Shriki, D. et al. 2009. Climatic variability during the last 90 ka on the southern and northern Levantine basin as evident from marine records and speleothems. Quaternary Science Reviews 28: 2882–96.Google Scholar
Bar-Matthews, M., Ayalon, A., Gilmour, M., Matthews, A. & Hawkesworth, C.J. 2003. Sea–land oxygen isotopic relationship 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
Baruch, U. & Bottema, S. 1991. Palynological evidence for climatic changes in the Levant ca. 17,000–19,000 B.P. In The Natufian Culture in the Levant, ed. Bar-Yosef, O. & Valla, F.R.. Ann Arbor: International Monographs in Prehistory, pp. 1120.Google Scholar
Bottema, S. 1995. The Younger Dryas in the eastern Mediterranean. Quaternary Science Reviews 14: 865–86.CrossRefGoogle Scholar
Cheddadi, R. & Rossignol-Strick, M. 1995. Eastern Mediterranean Quaternary paleoclimates from pollen and isotope records of marine cores in the Nile cone area. Paleoceanography 10: 883–91.Google Scholar
Develle, A.L., Herreros, J., Vidal, L., Sursock, A. & Gasse, F. 2010. Controlling factors on a paleo-lake oxygen isotope record (Yammoûneh, Lebanon) since the Last Glacial Maximum. Quaternary Science Reviews 29: 865–86.CrossRefGoogle Scholar
Develle, A.L., Gasse, F., Vidal, L. et al. 2011. A 250 ka sedimentary record from a small karstic lake in the northern Levant (Yammoûneh, Lebanon): Paleoclimatic implications. Palaeogeography, Palaeoclimatology, Palaeoecology 305: 1027.Google Scholar
Djamali, M., de Beaulieu, J.L., Shah-Hosseini, M. et al. 2008. A late Pleistocene long pollen record from Lake Urmia, NW Iran. Quaternary Research 69: 413–20.CrossRefGoogle Scholar
Enzel, Y., Amit, R., Dayan, U. et al. 2008. The climatic and physiographic controls of the eastern Mediterranean over the late Pleistocene climates in the southern Levant and its neighboring deserts. Global and Planetary Change 60: 165–92.CrossRefGoogle 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.Google Scholar
Frumkin, A., Bar-Yosef, O. & Schwarcz, H.P. 2011. Possible paleohydrologic and paleoclimatic effects on hominin migration and occupation of the Levantine Middle Paleolithic. Journal of Human Evolution 60: 437–51.Google Scholar
Gasse, F., Vidal, L., Develle, A.L. & Van Campo, E. 2011. Hydrological variability in the northern Levant: A 250 ka multiproxy record from the Yammoûneh (Lebanon) sedimentary sequence. Climate of the Past 7: 1261–84.CrossRefGoogle Scholar
Gasse, F., Vidal, L., Van Campo, E. et al. 2015. Hydroclimatic changes in northern Levant over the past 400,000 years. Quaternary Science Reviews 111: 18.CrossRefGoogle Scholar
Hajar, L., Khater, C. & Cheddadi, R. 2008. Vegetation changes during the late Pleistocene and Holocene in Lebanon: A pollen record from the Bekaa Valley. The Holocene 18: 1089–99.CrossRefGoogle Scholar
Hajar, L., Haïdar-Boustani, M., Khater, C. & Cheddadi, R. 2010. Enviromental changes in Lebanon during the Holocene: Man vs. climate impacts. Journal of Arid Environments 74: 746–55.Google Scholar
IPCC. 2013. Climate Change 2013: The Physical Science Basis. Cambridge: Cambridge University Press.Google Scholar
Kaniewski, D., Guiot, J., Van Campo, E. 2015. Drought and societal collapse 3200 years ago in the eastern Mediterranean: A review. WIRES Climate Change. doi:10.1002/wcc.345.Google Scholar
Kolodny, Y., Stein, M. & Machlus, M. 2005. Sea–rain–lake relation in the Last Glacial East Mediterranean revealed by ∂18O–∂13C in Lake Lisan aragonites. Geochimica et Cosmochimica Acta 69: 4045–60.Google Scholar
Langgut, D., Almogi-Labin, A., Bar-Matthews, M. & Weinstein-Evron, M. 2011. Vegetation and climate changes in the south eastern Mediterranean during the Last Glacial–Interglacial cycle (86 ka): New marine pollen record. Quaternary Science Reviews 30: 3960–72.Google Scholar
Langgut, D., Finkelstein, I., Litt, T., Neumann, F.H. & Stein, M. 2015. Vegetation and climate changes during the Bronze and and Iron ages (3600–600 BCE) in the southern Levant based on palynological records. Radiocarbon 57: 217–35.CrossRefGoogle Scholar
Litt, T., Pickarski, N., Heumann, G., Stockhecke, M. & Tzedakis, P.C. 2014. A 600,000 year long continental pollen record from Lake Van, eastern Anatolia (Turkey). Quaternary Science Reviews 104: 3041.CrossRefGoogle Scholar
Loulergue, E., Schilt, A., Spahni, R. et al. 2008. Orbital and millenial-scale features of atmospheric CH4 over the past 800,000 years. Nature 453: 383–6.Google Scholar
Meadows, J. 2005. The Younger Dryas episode and the radiocarbon chronologies of the Lake Huleh and Ghab Valley pollen diagrams, Israel and Syria. The Holocene 15: 631–36.CrossRefGoogle Scholar
Moulin, A. Benedetti, L., Van der Woerd, J. et al. 2011. LGM glaciers on Mount Lebanon? New insights from 36Cl exposure dating of moraine boulders. Geophysical Research Abstracts 13: EGU2011-11465.Google Scholar
Niklewski, J. & Van Zeist, W. 1970. A Late Quaternary pollen diagram from north-western Syria. Acta Botanica Neerlandica 19: 737–54.CrossRefGoogle Scholar
Rossignol-Strick, M. 1995. Sea–land correlation of pollen records in the eastern Mediterranean for the glacial–interglacial transition: biostratigraphy versus radiometric time-scale. Quaternary Science Reviews 14: 893915.Google Scholar
Sharon, D. & Kutiel, H. 1986. The distribution of rainfall intensity in Israel, its regional and seasonal variations and its climatological evaluation. Journal of Climatology 6: 277–91.CrossRefGoogle Scholar
Stockhecke, M., Kwiecien, O., Vigliotti, L. et al. 2014a. Chronostratigraphy of the 600,000 year old continental record of Lake Van (Turkey). Quaternary Science Reviews 104: 817.Google Scholar
Stockhecke, M., Sturm, M., Brunner, I. et al. 2014b. Sedimentary evolution and environmental history of Lake Van (Turkey) over the past 600 000 years. Sedimentology 61: 1830–61.Google Scholar
Torfstein, A. Goldstein, S. L., Stein, M., and Enzel, Y. 2013. Impacts of abrupt climate changes in the Levant from last glacial Dead Sea levels. Quaternary Science Reviews 69: 17.CrossRefGoogle Scholar
Tzedakis, P.C., Hooghiemstra, H. & Pälike, H. 2006. The last 1.35 million years at Tenaghi Philippon, revised chronostratigraphy and long-term vegetation trends. Quaternary Science Reviews 25: 3416–30.CrossRefGoogle Scholar
Vaks, A., Bar-Matthews, M., Ayalon, A. et al. 2003. Paleoclimate reconstruction based on the timing of speleothem growth and oxygen and carbon isotope composition in a cave located in the rain shadow in Israel. Quaternary Research 59: 182–93.Google Scholar
Vaks, A., Bar-Matthews, M., Ayalon, A. et al. 2007. Desert speleothems reveal climatic window for African exodus of early humans. Geology 35: 831–34.Google Scholar
Vaks, A., Bar-Matthews, M., Matthews, A., Ayalon, A. & Frumkin, A. 2010. Middle–Late Quaternary paleoclimate of northern margins of the Saharan–Arabian Desert: Reconstruction from speleothems of Negev Desert, Israel. Quaternary Science Reviews 29: 2647–62.CrossRefGoogle Scholar
Van Zeist, W. & Bottema, S. 1991. Late Quaternary Vegetation of the Near East. Wiesbaden: Dr Ludwig Reichert Verlag.Google Scholar
Van Zeist, W. & Woldring, H. 1980. Holocene vegetation and climate of northwestern Syria. Paleohistoria 22: 111–25.Google Scholar
Verheyden, S., Nader, F.H., Cheng, H.J., Edwards, L.R. & Swennen, R. 2008. Paleoclimate reconstruction in the Levant region from the geochemistry of a Holocene stalagmite from the Jeita Cave, Lebanon. Quaternary Research 70: 368–81.Google Scholar
Waldmann, N., Torfstein, A. & Stein, M. 2010. Northward intrusions of low- and mid-latitude storms accross the Saharo-Arabian belt during the past interglacials. Geology 38: 567–70.CrossRefGoogle Scholar
Yasuda, Y., Kitagawa, H. & Nakagawa, T. 2000. The earliest record of major anthropogenic deforestation in the Ghab Valley, northwest Syria: A palynological study. Quaternary International 73/74: 127–36.Google Scholar

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×