Abstract
A 700-year record (1.0–1.5 a resolution) of the East Asian winter monsoon (EAWM), based on grain-size analysis and AMS14C dating of Core EC2005 from the inner-shelf mud wedge of the East China Sea (ECS), was compared with the Dongge stalagmite δ18O record during the mid-Holocene. The upper muddy section of Core EC2005 has been formed mainly by suspended sediments derived from the Changjiang (Yangtze) River mouth since 7.3 ka BP. High precipitation and a strengthened EAWM might have played key roles in the high sedimentation rate (1 324–1 986 cm/ka) between 5.9–5.2 ka BP. The EAWM strengthened when the Asian summer monsoon weakened, especially around 5 500 a BP, which corresponded to a worldwide cold event. The EAWM during the mid-Holocene shows statistically significant solar periodicities at 62 and 11 a. The 5 500 a BP cold event might be resulted from orbital forcing and changes in solar activity.
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Supported by the National Natural Science Foundation of China (Nos. 40576032 and 40776030), and Doctor Foundation of China University of Petroleum.
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Xu, F., Li, A., Xu, K. et al. Cold event at 5 500 a BP recorded in mud sediments on the inner shelf of the East China Sea. Chin. J. Ocean. Limnol. 27, 975–984 (2009). https://doi.org/10.1007/s00343-009-9273-1
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DOI: https://doi.org/10.1007/s00343-009-9273-1