High-latitude biomes and rock weathering mediate climate–carbon cycle feedbacks on eccentricity timescales
Climate and carbon cycle interactions during major Earth system changes through the Cenozoic remain unclear. Here, the authors present a combined δ13C-δ18O megasplice for the last 35 Ma which allows them to identify three marked intervals of distinct climate–carbon cycle interactions.
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| Autores principales: | , , , , , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2020
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/e28e567d3fb849f083b8021ac6294731 |
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