Synchronous deglacial thermocline and deep-water ventilation in the eastern equatorial Pacific
Potential age model problems with marine Δ14C records have obscured our understanding of the role of the deep-ocean in deglacial atmospheric CO2rise. Here, the authors show that deglacial ventilation of EEP thermocline and deep waters occurred synchronously and was coeval with changes in Atlantic re...
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| Autores principales: | , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2017
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/e467fc4c3a1d444884952e4cc420a8e8 |
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| Sumario: | Potential age model problems with marine Δ14C records have obscured our understanding of the role of the deep-ocean in deglacial atmospheric CO2rise. Here, the authors show that deglacial ventilation of EEP thermocline and deep waters occurred synchronously and was coeval with changes in Atlantic records. |
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