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The most abrupt portion of the shift in δO of up to 1‰ also occurred throughout the Last Interglacial Asian Monsoon, with periods at multi-decadal to centennial timescales. L., Cheng, H., Yuan, D., Cai, Y., Zhang, M., Lin, Y., An, Z., Revenaugh, J., 2005. Abrupt decadal to millennial-scale climate events therefore appear to be a general feature of both glacial and interglacial climate. Precise 230Th dating has replicated the chronology of the samples within error.
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