Abstract
The mid-Pleistocene climate transition(MPT)has been widely reported in worldwide geological events.As a key issue of the Quaternary geology,it has attracted much attention from the paleoclimate community.MPT refers to a period lasting for several hundreds of thousand years,during which the dominant climate periodicity gradually extended from 41 kyr to 100 kyr(Ruddiman et al.,1989),and glacial-interglacial climate difference became more更多还原
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