A millennial scale planktonic foraminifer record of the mid-Pleistocene climate transition from the northern South China Sea [An article from: Palaeogeography, Palaeoclimatology, Palaeoecology]

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Description:
A high resolution record (~1100 yr) of planktonic foraminifers from ODP Site 1144 in the northern South China Sea reveals rapid and strongly variable climatic changes during the mid-Pleistocene transition period. The abundance of warm water species decreased from an average of 60% in marine isotope stage (MIS) 29 to