Antarctic last interglacial isotope peak in response to sea ice retreat not ice-sheet collapse
The peak in Antarctic ice core isotope values, 128,000 years before present, was concurrent with a significantly warmer-than-present Antarctic climate. Here, the authors show that this isotope maximum was associated with a major retreat of sea ice and not a collapse of the West Antarctic Ice Sheet.
| Main Authors: | , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Nature Publishing Group
2016-08-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/ncomms12293 |