Climate dynamics during the penultimate glacial period recorded in a speleothem from Kanaan Cave, Lebanon (central Levant)

Abstract Little is known about terrestrial climate dynamics in the Levant during the penultimate interglacial-glacial period. To decipher the palaeoclimatic history of the Marine Oxygen Isotope Stage (MIS) 6 glacial period, a well-dated stalagmite (~194 to ~154 ka) from Kanaan Cave on the Mediterran...

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Bibliographic Details
Published in:Quaternary Research
Main Authors: Nehme, Carole, Verheyden, Sophie, Breitenbach, Sebastian F.M., Gillikin, David P., Verheyden, Anouk, Cheng, Hai, Edwards, R. Lawrence, Hellstrom, John, Noble, Stephen R., Farrant, Andrew R., Sahy, Diana, Goovaerts, Thomas, Salem, Ghada, Claeys, Philippe
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2018
Subjects:
General Earth and Planetary Sciences
Earth-Surface Processes
Arts and Humanities (miscellaneous)
Greenland
Dansgaard-Oeschger events
Online Access:http://dx.doi.org/10.1017/qua.2018.18
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589418000182
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Summary:Abstract Little is known about terrestrial climate dynamics in the Levant during the penultimate interglacial-glacial period. To decipher the palaeoclimatic history of the Marine Oxygen Isotope Stage (MIS) 6 glacial period, a well-dated stalagmite (~194 to ~154 ka) from Kanaan Cave on the Mediterranean coast in Lebanon was analyzed for its petrography, growth history, and stable isotope geochemistry. A resolved climate record has been recovered from this precisely U–Th dated speleothem, spanning the late MIS 7 and early MIS 6 at low resolution and the mid–MIS 6 at higher resolution. The stalagmite grew discontinuously from ~194 to ~163 ka. More consistent growth and higher growth rates between ~163 and ~154 ka are most probably linked to increased water recharge and thus more humid conditions. More distinct layering in the upper part of the speleothem suggests strong seasonality from ~163 ka to ~154 ka. Short-term oxygen and carbon isotope excursions were found between ~155 and ~163 ka. The inferred Kanaan Cave humid intervals during the mid–MIS 6 follow variations of pollen records in the Mediterranean basins and correlate well with the synthetic Greenland record and East Asian summer monsoon interstadial periods, indicating short warm/wet periods similar to the Dansgaard-Oeschger events during MIS 4–3 in the eastern Mediterranean region.

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