reconstruction of mis 5 climate in the central levant using a stalagmite from kanaan cave, lebanon
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ID: 206982
2015
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Abstract
Lying at the transition between the temperate Mediterranean domain and
subtropical deserts, the Levant is a key area to study the palaeoclimatic
response over glacial–interglacial cycles. This paper presents a precisely
dated last interglacial (MIS 5) stalagmite (129–84 ka) from the Kanaan
Cave, Lebanon. Variations in growth rate and isotopic records indicate a
warm humid phase at the onset of the last interglacial at ~ 129 ka that lasted until ~ 125 ka. A gradual shift in speleothem
isotopic composition (125–122 ka) is driven mainly by the δ18O
source effect of the eastern Mediterranean surface waters during sapropel 5 (S5). The onset of glacial inception began after ~ 122 ka,
interrupted by a short wet pulse during the sapropel 4 (S4) event. Low growth rates and
enriched oxygen and carbon values until ~ 84 ka indicate a
transition to drier conditions during Northern Hemisphere glaciation.
| Reference Key |
nehme2015climatereconstruction
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|---|---|
| Authors | ;C. Nehme;S. Verheyden;S. R. Noble;A. R. Farrant;D. Sahy;J. Hellstrom;J. J. Delannoy;P. Claeys |
| Journal | proceedings - 16th ieee/acis international conference on computer and information science, icis 2017 |
| Year | 2015 |
| DOI |
10.5194/cp-11-1785-2015
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| URL | |
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