Sea surface temperature reconstruction for the Pliocene-Pleistocene climate transition
When comparing new sea surface temperature (SST) records between the western and eastern equatorial Pacific spanning the last 3.2 Ma, we found that the zonal temperature gradient over the entire tropical Pacific irreversibly increased by 3 to 4 °C from 2.2 to 2.0 Ma. Here, we suggest a pronounced in...
| Main Authors: | , , , |
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| Format: | Other/Unknown Material |
| Language: | English |
| Published: |
PANGAEA
2010
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| Subjects: | |
| Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.786701 https://doi.org/10.1594/PANGAEA.786701 |