Rigalleau, Vincent, Lamy, Frank, Ruggieri, Nicoletta, Sadatzki, Henrik, Arz, Helge W, Barker, Stephen ![]() ![]() |
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Abstract
Millennial-scale variations in the strength and position of the Antarctic Circumpolar Current exert considerable influence on the global meridional overturning circulation and the ocean carbon cycle. The mechanistic understanding of these variations is still incomplete, partly due to the scarcity of sediment records covering multiple glacial-interglacial cycles with millennial-scale resolution. Here, we present high-resolution current strength and sea surface temperature records covering the past 790,000 years from the Cape Horn Current as part of the subantarctic Antarctic Circumpolar Current system, flowing along the Chilean margin. Both temperature and current velocity data document persistent millennial-scale climate variability throughout the last eight glacial periods with stronger current flow and warmer sea surface temperatures coinciding with Antarctic warm intervals. These Southern Hemisphere changes are linked to North Atlantic millennial-scale climate fluctuations, plausibly involving changes in the Atlantic thermohaline circulation. The variations in the Antarctic Circumpolar Current system are associated with atmospheric CO2 changes, suggesting a mechanistic link through the Southern Ocean carbon cycle.
Item Type: | Article |
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Date Type: | Published Online |
Status: | Published |
Schools: | Schools > Earth and Environmental Sciences |
Additional Information: | License information from Publisher: LICENSE 1: Title: cc by, Type: cc by |
Publisher: | Nature Research |
ISSN: | 2041-1723 |
Date of First Compliant Deposit: | 10 April 2025 |
Date of Acceptance: | 19 March 2025 |
Last Modified: | 10 Apr 2025 11:15 |
URI: | https://orca.cardiff.ac.uk/id/eprint/177572 |
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