Out-of-phase relationship of Holocene moisture variations between the northeastern and southeastern Tibetan plateau and its societal impacts.

Moreover, in the vast region influenced by the ISM, records from speleothems [74] and marine and lacustrine sediments [ 75 , 76 ] demonstrate that the ISM and the resulting effective moisture show a decreasing trend during the Holocene.

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The integrated moisture record revealed an overall trend of increasing moisture on the NETP during the Holocene, which favored the development of agropastoral societies in this region during the period of ∼5200‒2200 BP.

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