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Warmer shallow Atlantic during deglaciation and early Holocene due to weaker overturning circulation

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Lu, W., Oppo, D.W., Liu, Z. et al. Warmer shallow Atlantic during deglaciation and early Holocene due to weaker overturning circulation. Nat. Geosci. (2025). https://doi.org/10.1038/s41561-025-01751-y

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