Past intrusion of Circumpolar Deep Water in the Ross Sea: Impacts on the ancient Ross Ice Shelf.

Sci Adv · 2025 · PMC12204156 · PMID 40577460

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a decreasing trendno p-value reported

In the distal sub–ice shelf unit (unit A, 40.5 to 20.4 ka B.P.), paleo-SOT shows a decreasing trend from 40 ka B.P. to the LGM, indicating a general cooling consistent with the final stages of MIS 3 ( Fig. 3J ).

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