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Northern Borneo stalagmite records reveal West Pacific hydroclimate across MIS 5 and 6
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文摘

N. Borneo rainfall response to glacial conditions differs from regional SST response.

Mulu View the MathML source has a significant 23 ky signal in phase with boreal fall insolation.

Terminations 1–5 are marked by extreme View the MathML source enrichments in Mulu stalagmite records.

N. Borneo convection responds to combined NH and SH forcing across deglaciations.

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