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Sea level and deep-sea temperature reconstructions suggest quasi-stable states and critical transitions over the past 40 million years
Sea level and deep-sea temperature variations are key indicators of global climate changes. For continuous records over millions of years, deep-sea carbonate microfossil–based δ(18)O (δ(c)) records are indispensable because they reflect changes in both deep-sea temperature and seawater δ(18)O (δ(w))...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2021
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8232915/ https://www.ncbi.nlm.nih.gov/pubmed/34172440 http://dx.doi.org/10.1126/sciadv.abf5326 |