Journal article
Climatic conditions during marine oxygen isotope stage 6 in the eastern Mediterranean region from the isotopic composition of speleothems of Soreq Cave, Israel
Geology, Vol.30(4), pp.303-306
Apr/2002
Abstract
At several times during marine oxygen isotope stage 6, the eastern Mediterranean region was influenced by two extreme climatic systems: the large ice sheet over northern Europe and the wet tropics associated with African monsoons. During this interval, two major climatic events occurred in the region; the sapropel S6 layer formed ca. 176 ka in the eastern Mediterranean basin owing to the increase in the African monsoon, and another event, although not large enough to form sapropel, occurred ca. 151 ka. The isotopic composition of Soreq Cave speleothems seems to record these events as very low delta(18)O-delta(13)C values dated as ca. 178 and 152 ka. The very low delta(18)O-delta(13)C values of -6parts per thousand, and -11parts per thousand, to -12parts per thousand, respectively, are typical of interglacial intervals, but here they were recorded during a glacial interval. Such low peaks indicate that in this part of the eastern Mediterranean region, i.e., Israel, the rainfall amount increased dramatically. Moreover, the isotopic record of the speleothems also shows that during the entire stage 6, although the climate was as cold as much of the last glacial, the conditions were never as dry.
Details
- Title
- Climatic conditions during marine oxygen isotope stage 6 in the eastern Mediterranean region from the isotopic composition of speleothems of Soreq Cave, Israel
- Creators
- A Ayalon (null)M Bar-Matthews (null)Ami Kaufman (null) - The Weizmann Institute of Science
- Resource Type
- Journal article
- Publication Details
- Geology, Vol.30(4), pp.303-306; Apr/2002
- Number of pages
- 4
- Language
- English
- DOI
- https://doi.org/10.1130/0091-7613(2002)030<0303:CCDMOI>2.0.CO;2
- Scientific Unit
- The Weizmann Institute of Science
- Record Identifier
- 993263126603596
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