Miocene ocean circulation shifted expansive oxygen deficient zones to the Atlantic
Abstract Contemporary observations indicate that dissolved oxygen concentrations are generally declining as global temperatures rise, which has broad implications for carbon cycling and the habitable ranges of marine animals. Here, we use the foraminiferal iodine redox tracer to evaluate the distrib...
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| Autori principali: | , , , , |
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Portfolio
2026-05-01
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| Serie: | Nature Communications |
| Accesso online: | https://doi.org/10.1038/s41467-026-73732-7 |
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