North Atlantic ocean circulation and abrupt climate change during the last glaciation
The most recent ice age was characterized by rapid and hemispherically asynchronous climate oscillations, whose origin remains unresolved. Variations in oceanic meridional heat transport may contribute to these repeated climate changes, which were most pronounced during marine isotope stage 3, the g...
| Published in: | Science |
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| Main Authors: | , , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
AAAS
2016
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| Subjects: | |
| Online Access: | http://eprints.esc.cam.ac.uk/3739/ http://eprints.esc.cam.ac.uk/3739/4/F1.large.jpg http://eprints.esc.cam.ac.uk/3739/1/Henry%20accepted%20Ms%20Science%202016.pdf http://eprints.esc.cam.ac.uk/3739/2/Henry%20et%20al.,%20Science%202016%20Supplement-1.pdf http://eprints.esc.cam.ac.uk/3739/3/Henry%20et%20al.,%202016%20Science%20published%20PDF.pdf http://science.sciencemag.org/content/353/6298/470.full https://doi.org/10.1126/science.aaf5529 |
| Summary: | The most recent ice age was characterized by rapid and hemispherically asynchronous climate oscillations, whose origin remains unresolved. Variations in oceanic meridional heat transport may contribute to these repeated climate changes, which were most pronounced during marine isotope stage 3, the glacial interval 25 thousand to 60 thousand years ago. We examined climate and ocean circulation proxies throughout this interval at high resolution in a deep North Atlantic sediment core, combining the kinematic tracer protactinium/thorium (Pa/Th) with the deep water-mass tracer, epibenthic δ13C. These indicators suggest reduced Atlantic overturning circulation during every cool northern stadial, with the greatest reductions during episodic Hudson Strait iceberg discharges, while sharp northern warming followed reinvigorated overturning. These results provide direct evidence for the ocean’s persistent, central role in abrupt glacial climate change. |
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