Abrupt weakening of deep Atlantic circulation at the last glacial inception.

During the LGI, the particle flux increased at CDH19, was in an increasing trend but did not reach its maximum at V30-99, and did not increase at U1313 (Supplementary Fig. 6 ).

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During the span of MIS 5e, all three Pa/Th records show a decreasing trend starting from an already low Pa/Th, likely indicating a continued AMOC strengthening after the recovery from Heinrich event 11.

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