Deep ocean temperatures through time
<p>Benthic oxygen isotope records are commonly used as a proxy for global mean surface temperatures during the Late Cretaceous and Cenozoic, and the resulting estimates have been extensively used in characterizing major trends and transitions in the climate system and for analysing past climat...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2021-07-01
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| Series: | Climate of the Past |
| Online Access: | https://cp.copernicus.org/articles/17/1483/2021/cp-17-1483-2021.pdf |