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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))...
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| Udgivet i: | Sci Adv |
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| Main Authors: | , , , , , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
American Association for the Advancement of Science
2021
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC8232915/ https://ncbi.nlm.nih.gov/pubmed/34172440 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.abf5326 |
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