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

M Matthias Sinnesael B Boris-Theofanis Karatsolis P Paul N. Pearson (Department of Earth Sciences, University College London) A Anne Briais S Sidney R. Hemming L Leah J. LeVay T Tom Dunkley Jones Y Ying Cui (Department of Oncology, The Sidney Kimmel Comprehensive Cancer Center at Johns Hopkins, The Johns Hopkins University School of Medicine) A Anita Di Chiara J Justin P. Dodd D Deepa Dwyer D Deborah E. Eason S Sarah A. Friedman E Emma Hanson K Katharina Hochmuth (Australian Centre of Excellence in Antarctic Science) H Halima E. Ibrahim C Claire E. Jasper S Saran Lee-Takeda D Danielle E. LeBlanc M Melody R. Lindsay D David D. McNamara S Sevasti E. Modestou M Margaret A. Morris B Bramley J. Murton S Suzanne OConnell G Gabriel Pasquet S Sheng-Ping Qian Y Yair Rosenthal (Department of Marine Sciences, Rutgers University) S Sara Satolli T Takuma Suzuki T Thena Thulasi B Bridget S. Wade (Department of Earth Sciences, University College London) N Nicholas J. White (Mahidol Oxford Tropical Medicine Research Unit, Bangkok, Thailand) T Tao Wu A Alexandra Y. Yang R Ross E. Parnell-Turner

Abstract

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.

Article Details

Volume / Issue Vol. 16, Issue 1
Published May 09, 2025
ISSN 2041-1723
Publisher Nature Portfolio

Journal Info

Nature Communications

Nature Portfolio

ISSN: 2041-1723 Open Access Life Sciences

Authors (36)

M

Matthias Sinnesael

B

Boris-Theofanis Karatsolis

P

Paul N. Pearson

Department of Earth Sciences, University College London

A

Anne Briais

S

Sidney R. Hemming

L

Leah J. LeVay

T

Tom Dunkley Jones

Y

Ying Cui

Department of Oncology, The Sidney Kimmel Comprehensive Cancer Center at Johns Hopkins, The Johns Hopkins University School of Medicine

A

Anita Di Chiara

J

Justin P. Dodd

D

Deepa Dwyer

D

Deborah E. Eason

S

Sarah A. Friedman

E

Emma Hanson

K

Katharina Hochmuth

Australian Centre of Excellence in Antarctic Science

H

Halima E. Ibrahim

C

Claire E. Jasper

S

Saran Lee-Takeda

D

Danielle E. LeBlanc

M

Melody R. Lindsay

D

David D. McNamara

S

Sevasti E. Modestou

M

Margaret A. Morris

B

Bramley J. Murton

S

Suzanne OConnell

G

Gabriel Pasquet

S

Sheng-Ping Qian

Y

Yair Rosenthal

Department of Marine Sciences, Rutgers University

S

Sara Satolli

T

Takuma Suzuki

T

Thena Thulasi

B

Bridget S. Wade

Department of Earth Sciences, University College London

N

Nicholas J. White

Mahidol Oxford Tropical Medicine Research Unit, Bangkok, Thailand

T

Tao Wu

A

Alexandra Y. Yang

R

Ross E. Parnell-Turner