期刊
QUATERNARY SCIENCE REVIEWS
卷 26, 期 3-4, 页码 279-286出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quascirev.2006.12.003
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A stable isotope record from a stalagmite collected from Antro del Corchia cave (Apuan Alps, Central Italy), supported by 17 uranium-series ages, indicates enhanced regional rainfall between ca 8.9 and 7.3 kyr cal. BP at the time of sapropel S I deposition. Within this phase, the highest rainfall occurred between 7.9 and 7.4kyr cal. BP. Comparison with different marine and lake records, and in particular with the Soreq Cave record (Israel), suggests substantial in-phase occurrence of enhanced rainfall between the Western and Eastern Mediterranean basins. There is no convincing evidence for major climatic change at the time of the 8.2 kyr event. (c) 2006 Elsevier Ltd. All rights reserved.
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