Beyond the ice: shifts in productivity and carbonate oversaturation at the Eocene–Oligocene transition
Abstract During the Eocene–Oligocene Transition (EOT; 34 Ma), Earth’s climate shifted from a warm, unglaciated state to a colder, glaciated state, marked by the formation of large dynamic ice sheets on Antarctica. For decades, it was believed that calcareous nannoplankton showed little response to t...
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| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2025-05-01
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| Series: | Scientific Reports |
| Online Access: | https://doi.org/10.1038/s41598-025-99630-4 |
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