ArticleNature communications2025
790,000 years of millennial-scale Cape Horn Current variability and interhemispheric linkages.
Article in Nature communications, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 3 papers.
What it found
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
The trial behind it
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Who cites it
3 citing papers in PubMed.
- Patagonian Ice Sheet discharge enhanced by AMOC slowdown through thermal bipolar seesaw.Proceedings of the National Academy of Sciences of the United States of America · 2026Article
- Zonally asymmetric changes in the Antarctic Circumpolar Current strength over the past million years.Nature geoscience · 2026Article
- South Pacific sea surface temperature and global ocean circulation changes since the late Miocene.Nature communications · 2025Article
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Authors and funding
13 authors.
Funding
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 CO
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