Onset of strong Iceland-Scotland overflow water 3.6 million years ago

Onset of strong Iceland-Scotland overflow water 3.6 million years ago

Abstract North Atlantic Deep Water (NADW), the return flow component of the Atlantic Meridional Overturning Circulation (AMOC), is a major inter-hemispheric ocean water mass with strong climate effects but the evolution of its source components on million-year timescales is poorly known. Today, two...

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Main Authors: Matthias Sinnesael, Boris-Theofanis Karatsolis, Paul N. Pearson, Anne Briais, Sidney R. Hemming, Leah J. LeVay, Tom Dunkley Jones, Ying Cui, Anita Di Chiara, Justin P. Dodd, Deepa Dwyer, Deborah E. Eason, Sarah A. Friedman, Emma Hanson, Katharina Hochmuth, Halima E. Ibrahim, Claire E. Jasper, Saran Lee-Takeda, Danielle E. LeBlanc, Melody R. Lindsay, David D. McNamara, Sevasti E. Modestou, Margaret A. Morris, Bramley J. Murton, Suzanne OConnell, Gabriel Pasquet, Sheng-Ping Qian, Yair Rosenthal, Sara Satolli, Takuma Suzuki, Thena Thulasi, Bridget S. Wade, Nicholas J. White, Tao Wu, Alexandra Y. Yang, Ross E. Parnell-Turner
Format: Article
Language:English
Published: Nature Portfolio 2025-05-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-025-59265-5
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https://doi.org/10.1038/s41467-025-59265-5

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