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

Authors

Matthias Sinnesael, L'Observatoire de Paris
Boris Theofanis Karatsolis, Uppsala Universitet
Paul N. Pearson, University College London
Anne Briais, Institut Universitaire Européen de la Mer (IUEM)
Sidney R. Hemming, Columbia University
Leah J. LeVay, Texas A&M University
Tom Dunkley Jones, University of Birmingham
Ying Cui, Montclair State UniversityFollow
Anita Di Chiara, Istituto Nazionale Di Geofisica E Vulcanologia, Rome
Justin P. Dodd, Northern Illinois University
Deepa Dwyer, Oregon State University
Deborah E. Eason, School of Ocean and Earth Science and Technology
Sarah A. Friedman, Georgia Southern University
Emma Hanson, University of Birmingham
Katharina Hochmuth, Institute for Marine and Antarctic Studies
Halima E. Ibrahim, Binghamton University State University of New York
Claire E. Jasper, Columbia University
Saran Lee-Takeda, The University of Tokyo
Danielle E. LeBlanc, Boston College
Melody R. Lindsay, Bigelow Laboratory for Ocean Sciences
David D. McNamara, University of Liverpool
Sevasti E. Modestou, University of Northumbria
Margaret A. Morris, Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics
Bramley J. Murton, National Oceanography Centre Southampton
Suzanne OConnell, Wesleyan University Middletown
Gabriel Pasquet, Université de Pau et des Pays de l'Adour
Sheng Ping Qian, Southern Marine Science and Engineering Guangdong Laboratory
Yair Rosenthal, Department of Marine and Coastal Sciences
Sara Satolli, University of G. d'Annunzio Chieti and Pescara
Takuma Suzuki, Japan Agency for Marine-Earth Science and Technology
Thena Thulasi, National Centre for Polar and Ocean Research
Bridget S. Wade, University College London

Document Type

Article

Publication Date

12-1-2025

Journal / Book Title

Nature Communications

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 major NADW components that flow southward over volcanic ridges to the east and west of Iceland are associated with distinct contourite drift systems that are forming off the coast of Greenland and on the eastern flank of the Reykjanes (mid-Atlantic) Ridge. Here we provide direct records of the early history of this drift sedimentation based on cores collected during International Ocean Discovery Programme (IODP) Expeditions 395C and 395. We find rapid acceleration of drift deposition linked to the eastern component of NADW, known as Iceland–Scotland Overflow Water at 3.6 million years ago (Ma). In contrast, the Denmark Strait Overflow Water feeding the western Eirik Drift has been persistent since the Late Miocene. These observations constrain the long-term evolution of the two NADW components, revealing their contrasting independent histories and allowing their links with climatic events such as Northern Hemisphere cooling at 3.6 Ma, to be assessed.

Comments

This Open Access article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made.

DOI

10.1038/s41467-025-59265-5

Journal ISSN / Book ISBN

105004672185 (Scopus)

Published Citation

Sinnesael, M., Karatsolis, B. T., Pearson, P. N., Briais, A., Hemming, S. R., LeVay, L. J., ... & Parnell-Turner, R. E. (2025). Onset of strong Iceland-Scotland overflow water 3.6 million years ago. Nature communications, 16(1), 4323.

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